ajarttell UniocrBtti} SIthratg Jtljara. SJjib Sotk CHARLES WILLIAM WASON COLLECTION CHINA AND THE CHINESE THE GIFT OF CHARLES WrLLlAM WASON CLASS OF 1876 1918 Cornell University Library F 595.G78 '^/ Cornell University Library The original of this book is in the Cornell University Library. There are no known copyright restrictions in the United States on the use of the text. http://www.archive.org/details/cu31924023250636 32 ^ 5= EMINENT AMERICAN EXPLORERS AND ARTISTS. -Gen. Custer. 2.-Ge„. Fre,„„„t .3._Lieut. Wheeler. 4.-Prof. F. V. Hayden. 5.-Albert Bierstadt 6.— Maj. J. W. Powell. 7.— Thomas Moran. The G-eeat West: Mis Mtmciions anb M^aomcts. CONTAINING A POPULAE DESCEIPTION OF THE MARVELLOUS SCENERY, PHYSICAL GEOGRAPHY, FOSSILS, AND GLACIERS OF THIS WONDERFUL REGION; RECENT EXPLORATIONS IN THE YELLOWSTONE PARK, "THE WONDERLAND OF AMERICA," BY Peof. F. V. HAYDEN, LL.D., FORMERLY UNITED STATES GEOLOGIST. ALSO, VAIITABP INFORMATION TO TEATELLEKS AND SETTLERS CONCERNDfO CLIMATE, HEALTH, MINING, HUSBANDKY, EDUCATION, THE INDIANS, MORMONISM, THE CHINESE; WITH THE f^omcsteatr, ^te^emption, Eantr,- anb iiEinitts ILatos. BY A CORPS OF ABLE CONTRIBUTORS. HANDSOMELY ILLUSTRATED WITH ENG'RAVINGS AND MAPS. SOLD ONLY BT SUBSCRIPTION. ELOOMINGTON, ILL. : CHARLES R. BRODIX. 1880. ;('fi Copyright, C. R. BRODIX. 1880. Westcott & Thomsou, Shekman & Co. Stereotyjim and Electrolypera, PUlada, FnnUrs, Philada. CONTENTS Relating to China and the Chinese Chinese Quarter in San Francisco attractive to visitors; Chinatown described No Chinese in Leadville^ Colorado Chinese Labor emiloyed Employed as domestic Servants Chinese Question . . . . Occupation . .... Mentioned . .... Yale (Charles G-. ) The Chinese Question . Importance of Question of Chinese Immigration to California Claims of Opponents to Iramigration Characteristics Attitude of California toward the Question Chief Ohjection to the Chinese Meade(Edwin R.) A Labor Question . . . . The Chinese as a Laborer Wages in China Wages in California 92 147 221 234 359 379 382 387 389 Cost of Living Disadvantage to White Lator Decision Ijy the Circuit Cojirt 391 Extract from an Address by Rev. Joseph Cook . . 392 Comparison of the Wage is in the East and West A Plea for the Chinese Williams (S.W.) Our Relations with China 393 The Burlingame Treaty ■ Immigration encouraged by Pacific Railroad Our Demands in China Treatment of Chinese in California Indemnity paid by Chinese Assaults in California on peaceable Chinese Immigration from Kwangtung Province Chinese not given the same advantages as other immigrants The Burlingame Treaty 398 NOTE BY THE PUBLISHERS. The rapidity with which the far Western portion of our country has been explored and mapped, and the extraordinary changes made by bring- ing the vast Plains — ^but lately the roving-grounds of wild Indians and herds of buffaloes — ^into cultivation, furnishing flourishing and happy homes for hundreds of thousands of the restless population of the East or of Europe, are facts that have excited the astonishment of the world. Immigration has been, and is now, advancing with a ceaseless current, impelled by various motives. Some of the individuals composing this great army are actuated by a thirst for gold, excited by the marvellous stories of the wealth hidden in the rocks and ravines of the mountains ; others, moved by reports of the cheapness and fertility of the land and the salubrity of the climate, and undazzled by the stories of gold and silver deposited centuries ago to be excavated by this generation, decide on the wiser course of cultivating the earth. To these two great motives are added many that bring the merchant, the speculator, the schoolmas- ter, and others that follow in the train of immigration. To no one is the country more indebted for opening up this formerly unknown land to the settler than to Professor F. V. Haydbn, who for nearly thirty years has been engaged in the great work of scientific ex- ploration. Professor Asa Gray, Professor of Natural History in Har- vard University, and America's most eminent botanist, says : " It has come in my way to know a good deal about Dr. Hayden's Territorial surveys for several years past, especially as to their scientific results ; and of late my attention has been still more called to them. I wish here not only to express, emphatically, my own opinion of their great value and of the importance of continuing them, but also to testify to the deep im- o NOTE BY THE PUBLISHERS. pression they are making upon the scientific world. In Europe the learned societies, the scientific journals, as also the working naturalists in correspondence, speak with one accord in terms oiF admiration, not un- mixed with envy, of what our government has done and is doing in this regard; and' I observe that Dr. Hayden's survey and the resulting publi- cations are put forward as the type and exemplar." From a letter of Baron von Eichtofen, President of the Berlin Geo- graphical Society, we extract the following : " Your eminent exploring work, the energy with which you have conducted it, and your faculty of managing the working-power of a large staff so as to arrive at its full efficiency and to put every man in his proper place, have earned for you the admiration and praise of the scientific world in general and many eminent men in particular." These two extracts from numerous notices of the kind, and the fact that Dr. Hayden has been made an honorary member of very many of the principal scientific societies of Europe and other foreign countries, prove how eminently qualified he is for the great task of his life. The matters pertaining to the historical, agricultural, mining, and other departments of the various countries described have been also confided to writers of eminent ability, who have, by reason of long residence and careful study, made themselves well qualified for the task. We would here also express our grateful acknowledgments to the New York Independent, New York Tribune, and the governors and other offi- cials of the various States and Territories, for documents containing the latest information and placed in our hands for publication. LIST OF ILLUSTRATIONS. PAGE Fkontispiece, Yosemite Falls and Valley (Steel engraving). Eminent Explorers and Artists. Winter Forest-Scenes in the Sierra Nevadas 75 Map oe Kansas, Colorado, New Mexico, and Indian Territory. . 81 DoNNER Lake, from the Snoav-Sheds 89 Cedar Creek CaSon, Colorado 99 Mountain of the Holy Cross, Colorado 105 Interior of Shaft-Hottse, Lbadville 113 Williams CaSton, Colorado Springs 121 Bestored Tower and Cliff-Houses 129 View in Chestnut Street, Lbadville 145 View in Harrison Avenue, Leadville 153 A Glimpse of Denver, Colorado 161 Lake Tahoe, Nevada 177 Giant's Butte, Green Biver, Wyoming . : . 201 Map of Nebraska, Minnesota, and Dakota 241 Shoshone Falls, Idaho 289 Echo CaSon, Utah 313 Salt Lake City and Wahsatch Mountains, Utah 321 Map of California, Oregon, Idaho, Utah, Nevada, Arizona, and Washington S53 Scenes in the Yosemite Valley — Bridal-Veil* Fall and Mirror Lake 369 The Big Trees of California 377 San Francisco, from Goat Island 385 An Attack on a Village of Cave-Dwellers 449 Vernal Fall, Yosemite 465 Eastport (Stickeen Village), Alaska 473 Greek Church, Sitka, Alaska 477 United States Bonded Warehouse, Fort Wrangell, Alaska . . .481 r CONTENTS, PAET FIRST. PAGB THE GBEAT WEST 17 Comparative Size of the East and the West — Government Expeditions — The Two Mountain Systems — General Divisions — Mountain - Kanges — Geological Structure — ^The Sources of the Yellowstone and Missouri — Immense Fossil Trunks — Petrified Forests — Yellowstone National Park — Boiling Springs — Yel- lowstone Lake — Geysers — Mud-volcanoes — Legislation respecting Yellowstone Park — Principal Elvers of the North-west — Missouri, Yellowstone, Tongue, Powder, Teton, White, and Niobrara Elvers — The Tertiary Lake-Basins of the West — The Fossil Structures — Fossil Remains of the Ehinoceros, Camel, Horse, Mastodon, Elephant, etc. — The Pre-historic Geography — Supposed Condition of the Country in Pre-historic Times — North America in the Tertiary Age — Ancient Life in the Far West — Immense Eeptiles — Searching for Fossils— Saurlans — Snake Elver — High Mountain-Peaks — The Plateau Eegion of the Colorado Elver — Deep Canons — Euins in the South-western Territories — Estufas — Cliff Houses — The Great Basin — Wahsatch Mountains — Great Salt Lake — The North- ern System of Mountains — Cascade Eange— The Sierra Nevada — Glaciers — Glacial Action in the Eocky Mountains — Timber Belts — ^The Yosemite Valley — Waterfalls — Features of the Two Mountain Systems — Mineral Deposits of the West — Fossils in the Lake-Basins — Extinct Plants— Eainfall — Average Eleva^ tion of the Land — Stock-Eaising. PART SECOND. THE TEIP OVEELAND . The Start ii-om Omaha — Platte Valley — The Plains — Cheyenne — Echo and Weber Canons — High Cliff— The Union Pacific — The Central Pacific — To the Sierras — Donner Lake— Oakland — San Francisco — Hotels — Chinatown — Woodward's Garden — Climate — The Geysers — Yosemite Valley — Big Trees— Southern Cali- fornia and Arizona — The Trip to Oregon — Puget Sound — Alaska — Fort Wrangell. COLOEADO General History — Expeditions — Discovery of Grold and Silver — Union Pacific Eailroad — Entered the Union July 4, 1876— Climate and Health— Eainfall, Scenery — Canons — Points of Interest — Platte Cafion— Colorado Springs — Garden of the Gods — Parks and Elvers of Colorado — Eesources — Flora — Wild Animals — Ancient Euins — Agriculture — Cattle, Sheep, Dairying — Towns and Villages — Leadville and Adjacent Camps — Denver — Society and Churches— Educational, 9 10 CONTENTS. PAGE PEOSPECTING 164 Hunting for Mineral — Seeking the "Blossom" — Carbonate Mineral — "Grub Stakes " — Locating a Mine^ — Bonding a Mine — Wages — Definitions of Mining Terms. NEBRASKA AND ITS BESOURCES 172 Introductory — Geography — Geology — Climatic Conditions — Natural Productions — The Native Trees— The History of Nebraska— The Great Pood-Belt of the Con- tinent — Nebraska the Best part of the Belt — The Cattle-Farm — Experience of Flock-Masters — Successful Fruit-Culture — Pisciculture — The Honey-Bee and the Prairie Flowers — Three Districts in Nebraska — North-eastern Nebraska — -South- eastern Nebraska — The Centre of the BaUroads — School System — Growth — State Institutions — Opportunities for Acquiring Land — XJ. P. E. E. Lands — Burlington and Missouri River R. R. Lands. Heaith or Nebraska 189 NEW MEXICO 190 Agriculture — The Rio Grande Valley — The Pecos River Valley — Cattle- and Sheep-Grazing — Minerals. Eesotjbces op New Mexico 193 Sheep-Raising — Cattle-Raising— Fruit-Raising — Vineyards and Wine-Making — Market-Gardens— WooUen-Mills — Tanneries — Brickmakers — Banking — Mining — The Professions. WYOMING 200 Scenery — Population — Stock-business — Mining. EbPOBT op the StrBVEYOB-GENERAL 202 General Description — Climate — Topography — Coal — Gold — Soda — Forests — Agri- culture — Cities, Towns, and Villages — Game — Manufacturing Eesources. MONTANA 210 General Description— Climate — A Healthy Region — Natural Scenery — Yellow- stone Park — Big Potatoes — Stock-Eaising — Vast Pastures — Details of the Busi- ness — Dairying — Poultry— Prices of Products — Getting Homes — Mining — Busi- ness, Wages, Expenses — About the Towns — Eailroads — Montana Points — What the Governor says. Mineral Eesources 221 Rich Placers — Gold Quartz-Mines — Silver Camps — Dishonest Management — " Ore in Posse." Stock-Eaising in Montana 224 The Best Grazing Country in the World— Marvellous Eeports of Profits— Grass Abundant— Not Necessary to Feed Cattle in Winter — Cattle Branded and Turned Out— Non-resident Speculators interested in Herds— Dividing the Prof- its-Sheep— Examples of Good Investments— Number of Cattle and Sheep in the Territory — Diseases. Bints to Men Without Capital 231 Cost of Travel— Establishing a Eanche— Wages of SkUled Mechanics— Skilled Miners — Domestic Help — The Professions. CONTENTS. 11 PAGE DiSTAiTCBS, Time, Fabe, Baagage Allowed, etc 236 Fares from Omaha, Extra Baggage and Household Goods — Distances and Fares in the Territory — Population^ Distances, etc. — Average Wages. DAKOTA 240 General Description — Immigration — Dalrymple's Great Farm — Northern Dakota —Eastern Dakota— The Black Hills— Gulch-Mining— The Gold Yield— Oppor- tunities for Intending Settlers — Chances for the Professions — Eailroad Facilities — Correct Table of Distances, MINNESOTA 251 General Description — Climate — Soil and Productions — Wheat, Corn, Oats, and other Grains — Stock-Raising — Manufacturing — Great Water-Power— Minnesota Flour — Trade to Foreign Ports — Population. THE KANSAS EMIGRANTS 257 KANSAS 258 General Description — History. The Geology of Kansas 260 Elevation — Drainage — Soil — Uplifting of the Ground — Building Material. Wheat — Horticulture — Stock-Eaising — Sheep-Husbandry — Live-Stock — Loca- tion of the Best Farming Lands — Grasses — Prices of Improved and Unimproved Farms — Wild Lands — Abandoned Farms — Population. TEXAS ■ 275 Area— History — Physical Features — Climate — Minerals — Agricultural Products — Animals — Miscellaneous. IDAHO 279 Mountains and Table-Land — Climate — Agriculture — Mining — Gold HUl — Eocky Bar — Scarcity of Mills to Work the Ore — The Placer-Grounds at Idaho City — Population^Transportation — Stock-Growing — Resources — Irrigation — Idaho in 1879 — Boundaries — Area suitable for Culture. ARIZONA 296 Only lately Opened to Travel — Elevation of the Ground — Dryness— Climate — Mineral Wealth — Mineral Park and Bradshaw District — Peculiar Method of Mining — Silver "Farms" — -Territorial Prison — Qualifications of Voters — Area of Lands suitable for Cultivation — Population. NEVADA , 302 History — Physical Features — Agricultural Lands — Minerals — Agriculture — Ani- mals — Climate — Education. 12 CONTENTS. PAGE THE SUTRO TUNNEL 305 "A Tough Job "—Blasting through Solid Eock— A Chapter on Mules— Obstacles to Progress— Bad Air— Accidents- Eiddled with Rocks— Cares— Fast in the Mud — Hospital— Miners' Union — Starting a Grave7ard — Advantages of the Sutro Tunnel. UTAH 312 Acquisition by Treaty — Area — Drainage — Topography and General Features — Great Salt Lake Basin— Cache, San Pete, and Sevier Valleys— Great Salt Lake Valley — The Mountains — Agriculture — Stock-Raiping — Minerals — Railroads — Climate — Health— Salt Lake City. MORMONISM 322 Origin and Early History — Exodus from Nauvoo — Profanity of Brigham Young — • Temples — Present Condition and Attitude of Mormonism — Condition of Educa- tion — Polygamy. Disloyal Mormootsm 330 The American Bluebeard — Anti-Polygamy Laws — Plural Wives — Weakness of the Laws — Mormons Refuse to Answer Questions — Confessions of Apostate Mormons — The Endowment-House — Penalties and Signs — Blood Atonement — President Hayes' Plan — The Remedy. OREGON 340 Extreme North-western State — Ex:tent — Historical — Geographical— Western Ore- gon — Exempt from Violent Atmospheric Disturbances — Soil, Resources, and Productions — Fisheries — Towns — Routes and Scenery — Approaches. WASHINGTON TERRITORY 347 Western Washington — Fir Timber— Resources — Puget Sound — Climate — Eastern Washington — Grapes and Peaches — Wheat — Area — Towns — Snake River — Co- lumbia Basin — Lands — Northern Pacific Railroad — Short Winters — The " Chi- nook," or Warm Wind — Health. CALIFORNIA I 354 History — Vague Impressions of the State — Sir Francis Drake — The Spaniards — The Franciscan Friars — The Digger Indians — The Mexican Dominion — The Discovery of Gold — Influx of Population — Irrigation — The Seasons — Drainage — Area of Rivers — Irrigating-Cauals — Artesian Wells— Tule-Lands — Salt Marsh- Lands — Reclamation Schemes — Embankments — Chinese Labor — Large Crops — River Navigation. Cereal Crops of CALrpoENiA 374 Improvement of the Seed — Preparation of the Soil — Gang Ploughs — Harvest — Head- ing-Machines — Burning Straw — Barley and Oats — Horticultural Products — Fresh Fruit every Month in the Year — Truck-Gardens — Fruits of both Temperate and Semi-Tropical Regions — Oranges — Dried Fruits — Nuts — Coffee-Culture. G0LD-M1NIN& 382 First Attempts — Picks, Pans, and Shovels — Washing the Dirt — The Rocker — Quicksilver — Long Toms — Mining - Sluices — River-bed Mining — Blue -gravel Leads— Hydraulic Mining— Vein Mining— Quartz-Mills— Quicksilver-Mines. CONTENTS. 13 PAGE The Chinese Question . ^ 387 Pro and Con. — Habits of the Chinese — How they Work-:-Eestricting Immigration. A Labor Question 389 The Chinaman a Mere Machine — Wages in China and California — Coolies — Labor Disturbances. Decision by the Circuit Court 391 Extract from an Address by Eev. Jos. Cook 392 Our Eelations with China 393 How the Chinese were Induced to Come to the United States — Transported by British Ships — Discriminating Laws — Eesponsibilty of the Government — Op- pression of the Chinese — Where the Fault Lies. BuRi/iNGAME Treaty 398 PART THIRD. EDUCATION WEST OP THE MISSISSIPPI 401 Exhibits of American Education — Foreign Critics — Magnitude of the School Sys- tem — General View of Educational Condition — Early Action — Examination by States — Texas, Louisiana, and Kansas : A Chance Picture — Schools of New Or- leans I Arkansas : Elementary Schools — Collegiate Institutions — Benefits of the Peabody Fund; Missouri: Education in the Counties—City Systems — Schools of St. Louis — State University ; Kansas, Iowa, and Minnesota : Instruction of Teachers — Increase of Schools — Statistical Summary — Illustrative Examples — Provisions for Higher Education — Normal Departments — ^The State Universities — Private Schools — Religious Educational Institutions ; Nebraska : Present Con- dition — State University ; Colorado : Salaries of Teachers ; Nevada : Present Condition — Teachers' Institutes — State University; Dakota, Montana, Idaho, Wyoming, and Washington Territories ; New Mexico and Arizona ; Utah : Op- position of the Hierarchy ; Indian Territory : Schools — Teachers — Income and Expenditure — Schools of the Five Nations ; Oregon : Practical Education — Park School, Portland — The Universities ; California : Number of Schools — Expendi- tures — ^New School Law — Supervision — Normal School — The University — Pri- vate Schools — Schools of San Francisco. — Institutions for the Deaf and Dumb and for the Blind. NOETH AMEEICAN INDIANS 431 Eeligion of the Indians — Origin of the Indian Eace — The Beginning of the Great Conflict between the Eaces — The Number of Indians Now and Then — Intro- duction of European Laws — Love of Native Land — Establishing a Permanent Home for the Indians — Cost of Indian Wars— Eemoval of Indians — Uncivilized Indians — Is the Indian Eace Dying Out? — The Indian has the Essential Ele- ments of Manhood. THE CLIFF-DWELLEES 445 Discoveries in Southern Colorado — Eomantie Night-Camp — Hayden Survey— Euined Villages — Immense Stone Buildings — Battle Eock — Hovenweep Castle — Pueblo Indians — Fire- Worshippers — Pitiorial Word- Writing and Hiero- glyphics — Inscriptions on the Walls — Wonderful Caves— Picturesque Euins — Caso del Eco — Pueblo Penasco Blanca — Estufas — Eemains of a Once-Powerful Nation. 14 CONTENTS. PAGB THE YOSEMITE 457 The Big Tree Groves — Their Location — Approaches to the Valley — Inspiration Point — Merced Eiver — Bridal- Veil Fall — Yosemite PaU — In the Valley — Digger Indians — Hotels — Drives and Eides — A Sweeping View. ALASKA AND ITS INHABITANTS 472 The Sail from Victoria— Mount Baker — Great Island Eegion — Glaciers — Fish — Eaking in Canoe-loads of Fish — Furs — Climate — St. Paul — Fort Wrangell — Mission-Work — Native Eaces — Alaska Canoes — Ornaments — Marriage — Polyg- amy — Slaves — Burials — Food — Widow-Biu^ing — Murder of the Old and Feeble — Women denied Burial — Shamans — Cannibals. ALASKA 486 The Greatest of the Territories — Early History — General Description — Settle- ments — Fort Wrangell ^ — Sitka — Cook's Inlet — Vegetables raised on Frozen Earth — One Hundred-pound Salmon — St. Paul — Afognak — The Ice Company — Sea-Otter Grounds — Aleutian Islands — The Pribylof {or Fur-Seal) Mauds — The Alaska Commercial Company — Habits of the Fur-Seal. LAWS IN EELATION TO EXEMPTION, MAEEIED WOMEN, AND IN- TEEEST 501 California, 501 ; Washington Territory, 503 ; Montana, 505 ; Kansas, 506 ; Wyom- ing, 508; Idaho, 509; New Mexico, 511; Oregon, 513; Nevada, 515; Nebraska, 517 ; Colorado, 518 ; Dakota, 520. Government Lands, and How to Get Them 523 Soldiers' and Sailors' Homesteads — Homesteads to Citizens — Pre-emption — The Timber-Culture Act. MISCELLANEOUS INFOEMATION FOE TEAVELLERS ....:... 524 Hints for the Trip Overland— Eoutes—Eates of Fare to California— Union Pacific Eailroad — Information for Emigrants— Special Eates for Excursions — Trans- Continental Time-Tables — Differences in Time. THE FAR WEST. BY HENEY WADSWOETH LONGFELLOW. Fae in the West there lies a desert land, where the mountains Lift, through perpetual snows, their lofty and luminous summits. Down from their jagged, deep ravines, where the gorge, like a gateway, Opens a passage rude to the wheels of the emigrant's wagon. Westward the Oregon flows, and the Walleway and Oyhee Eastward, with devious course, among the Wind River Mountains ; Through the Sweetwater Valley precipitate leaps the Nebraska ; And to the south, from the Fontaine-qui-bout and the Spanish sierras. Fretted with sands and rocks, and swept by the wind of the desert, Numberless torrents, with ceaseless sound, descend to the ocean, Like the great chords of a harp in loud and solemn vibrations. Spreading between these streams are wondrous, beautiful prairies. Billowy bays of grass ever rolling in shadow and sunshine, Bright with luxuriant clusters of roses and purple amorphas. Over them wander the buffalo herds and the elk and the roebuck ; Over them wander the wolves and herds of riderless horses ; Fires that blast and blight, and winds that are weary with travel ; Over them wander the scattered tribes of Ishmael's children. Staining the desert with blood ; and above their terrible war-trail Circles and sails aloft, on pinions majestic, the vulture. Like the implacable soul of a chieftain slaughtered in battle, By invisible stairs ascending and scaling the heavens. Here and there rise smokes from the camps of these savage marauders ; Here and there rise groves from the margins of swift-running rivers. And the grim, taciturn bear, the anchorite monk of the desert. Climbs down their dark ravines to dig for roots by the brookside ; While over all is the sky, the clear and crystalline heaven. Like the protecting hand of God inverted above them. IS THE GREAT WEST. THE GREAT WEST. BY PEOF. F. V. HAYDEN, U. S. GEOLOGICAL SURVEY. "VTEYER in the history of our country has the term " the Great West " -1- ' possessed so much significance as at the present time. Forty years ago, Ohio, Indiana, and Illinois were called the far Western States, while but little was known of the vast regions beyond ; now farms, villages, and cities, with the sites of future cities, are dotted over the plains and mountain-slopes as they stretch westward toward the setting sun. At the very threshold of our undertaking it is proper that we should make some inquiry into the extent and capacities of this great country, and into the physical causes that have produced its present configuration. If we examine any good geographical map of our country, we shall see at a glance that at least two-thirds of the United States of America, an area of more than two millions of square miles, lie west of the Missis- sippi River. In the portion lying east of that river, and containing less than half that area, now dwell between thirty and forty millions of peo- ple. The Atlantic coast, with its crowded population, its refined civiliza- tion, its great cities, its seats of learning and industrial operations, forms only a fringe on the eastern border of this vast continent. It was not until within the present century that the country possessed any very definite knowledge of the geography of the mountain-regions of the Far West. Upon the old maps the mountain-ranges were shown by a single line of hatchings, with a few minor ranges branching ofF, the whole trending nearly north and south, or rather west of north and east of south. , The first important government expedition that was sent out to explore the great unknown mountain-regions of the extreme West was that of Lewis and Clarke, which in 1804-6 passed up the Missouri Eiver to its 2 IT 18 THE great' WEST. source, crossed the main Divide of the Rocky Mountains, and followed the Columbia River to its entrance into the Pacific Ocean. Although this expedition was a great and successful achievement in a geographical point of view, taking into consideration the time and the means at its command, yet much of the information it obtained was very vague, and limited to a narrow belt across the northern portion of the country. Lewis and Clarke, however, fixed pretty well the positions of the Missouri and Columbia Rivers. The two volumes which contain the result of these explorations, although possessing the intrinsic evidence of having been written with the utmost candor and truthfulness, read like a romance. The party was small and comparatively unprotected, the country utterly unknown, and occupied only with tribes of Indians, many of whom were inclined to be hostile. Every item of information which they secured was new and strange, and of the highest interest. The next explorer was Major Z. M. Pike, who in 1805-7 crossed the country farther south, and discovered the head-waters of the Arkansas River and the lofty peak which now bears his name. He crossed the Divide into the Great Basin. In 1819-20, Stephen H. Long was sent out by the government with a well-equipped party, comprising not only topographers, but also geologists and naturalists, among whom was the celebrated Thomas Say. After Long came Bonneville, Ross Cox, School- craft, Nicollet, Fremont, and others, all of whom added more or less to the store of knowledge of this great area. From 1844 to 1860 more than twenty expeditions were sent out by the government with the object of determining the best route for a railroad to the Pacific. In 1853, Congress passed a bill making appropriations for the determination of the most practicable route for a railroad from the Valley of the Missis- sippi to the Pacific coast. No expense was spared in equipping expedi- tions, which traversed the country from east to west at various points from latitude 49° to the southern boundary of the United States. The information thus obtained was embraced in a large series of maps and reports, which were published by the general government. Although so very much had been done toward the development of the resources of the great West, yet prior to 1868 no imj)ortant portion had been exam- ined with such care and detail as to render the maps anything more than approximately correct. The information thus obtained could only be placed on a map projected on a small scale, where an error of five or ten miles would be overlooked. "Within the past ten or twelve years several exi>editions have been organized, under King, Wheeler, Powell, liayden, and others, with the object of working out certain areas with considerable THE GREAT WEST. 19 detail, including topography, geology, and natural history; and more definite knowledge of the remote West has been obtained within that period than in all the previous years. Indeed, the period from 1868 to 1878, inclusive, will ever be regarded in the history of our country as the true era of scientific exploration in the West. THE TWO MOUNTAIN-SYSTEMS. According to Professor J, D. Whitney, two great ranges of mountains form the skeleton of the North American continent — viz. the Appala- chian and the Cordilleras. The Cordilleras ranges border on the Pacific coast, extending southward to Patagonia, being so depressed at the Isth- mus of Darien as to seem almost interrupted or broken for a time. The term " Cordilleras " has been adopted by Professor Whitney for the series of mountain-ranges bordering the Pacific, extending from Mexico north- ward into British America. The term " Rocky Mountains " is limited so as to embrace only those numerous ranges that lie east of the Great Basin, and really form the watershed of the continent. The name " Rocky Mountains " has been applied indefinitely to an extended series of mountain-ranges west of the Mississippi, of a great variety of form and structure. The term " Stony Mountains " was originally used, ap- parently with no intention of applying it to any one range or group of ranges. This term probably suggested itself to the earliest travellers on account of the vast masses of debris or loose, broken masses of rock which cover all the ranges from base to summit. This is made more conspicuous by the general absence of timber. From the eastern slope westward we pass over range after range to the Pacific coast for a thousand miles or more, interspersed here and there with a valley or park. The greatest width of the mountain-system lies between parallels 38° and 42°. Here the mass of the mountains is a thousand miles or more in breadth, though the entire country west of the Mississippi, embracing an area of over two millions of square miles, has been in- fluenced by the mountain-ranges, and may therefore be called the " moun- tain-region." The great group of the Cordilleras extends southward through Mexico and Central America to the Isthmus of Darien, and northward into British America and Alaska to the Arctic Ocean. The great chain of the Andes of South America is an extension southward of the same group, and in a general view they all belong to one great system. The principal ranges on the Pacific coast are the Sierra Nevada and the Coast Ranges, while to the eastward, in the interior basin, are numerous smaller ranges. The Wahsatch range forms the eastern wall 20 T3E GREAT WEST. of what may be called the main Cordilleras group or Pacific Coast Mountains. The great group of mountains which forms the backbone or watershed of the continent may be denominated the Kocky Mountain group as a sub-generic term. We shall note hereafter the influence which these mountain-ranges have exerted upon the destiny and resources of this great country. GENEEAL DrVTSIONS. Having given in the preceding pages a brief outline of the surface character of the great country west of the Mississippi, we shall find it an interesting subject of study to inquire into the plan of the growth and development of this vast region. The great area west of the Mississippi seems to have been at one time an enormous plateau, out of which were evolved the different ranges of mountains, as if they had been thrust up by some volcanic force. Let the traveller pass southward from Cheyenne to Denver, along the imme- diate base of the eastern range ; he will find that the mountains of which the snow-covered summits of Pike's and Long's Peaks form a part rise rather abruptly out of what appears to the eye an almost level prairie- region, and will see the inclined ridges of the various sedimentary forma- tions elevated to view, as if the huge granite nucleus had been thrust up, leaving upon its sides the sandstones and limestones of the more modern beds. These magnificent scenes at once fill the thoughtful mind with wonder and delight, and the first inquiry is as to the manner in which these stupendous changes have been brought about. In general terms, we may divide the country west of the Mississippi into mountain and prairie, or " plains." This latter term may be regard- ed as the more comprehensive one, including in the mind of the "Western people the numerous parks and basins among the mountains. The prai- rie country refers more especially to the vast grassy, treeless plains of the eastern slope. To understand more clearly the original plateau character of this region, we have only to examine the numerous barometrical profiles which have already been constructed across the continent for railroad and other purposes. The explorations made in past years under the direction of the War Department, and those more recently for the different lines of rail-routes, afford ample means for its study to the trav- eller. If we proceed westward from any point along the Missouri or Mississippi River, we will find that the ascent is gradual, at first not more than one foot per mile, but steadily increasing until we reach the base of the mountains, when the ascent is fifty to one hundred feet per THE GREAT WEST. 21 mile. The profile of the Pacific Eailroad shows that Omaha, on the Missouri River, is 1060 feet above sea-level, while at Columbus, 91 miles by rail westward, the elevation is 1470 feet, showing an ascent of about four and a half feet per mile. At Cheyenne, 516 miles west of Omaha, the elevation is 6076 feet, showing an ascending grade from Omaha of nearly ten feet per mile. This entire distance is over an apparently level plaiu, most of the way by the valley of the Platte River. From Chey- enne to the highest point along the line of the railroad, at Sherman, 8271 feet, the distance is 33 miles, when suddenly the grade increases to over sixty-six feet per mile. From thence across the continent are numerous ranges of mountains, with valleys of greater or less area intervening, with a general elevation varying from 4000 to 6000 feet ; whence the descent to the Pacific is somewhat rapid and abrupt. The profile of the Kansas Pacific Railroad from Kansas City, on the Missouri River, to Denver, Colorado, shows similar results. At Kansas City the elevation is 764 feet, at Denver, 639 miles westward, 5197, making an average ascent of nearly seven feet per mile across an apparently level, treeless plain. A few miles west of Denver the great Colorado or Front Range seems to rise abruptly out of the plains, its summits reaching the line of perpetual snow. Similar results will be found by examining the profile of the Northern Pacific Railroad route anywhere between the meridians of 45° and 48° to the Pacific coast. Indeed, there appears to have been a grad- ual expansion of the earth's crust until it yielded, revealing the vast mass of mountain-ranges which extend across the continent. The details of the causes of these phenomena, and the varied conditions under which they have occurred, are too extended for such an article as this. The great mass of the mountain-ranges lie west of the 105th' merid- ian ; the united groups trend about 20° west of north. Along the east- ern slope the smaller or minor ridges have a trend more to the north- west, so that they constantly die out in the plains, giving to the eastern side an echelon appearance. As the small ridges run out, they terminate frequently in a perfect example of an anticlinal, as may be seen near Cache-la-Poudre River. From the notches in the outline of the ranges the Platte, Arkansas, and many other rivers open into the plains. About the sources of the Missouri River the main chain is nine degrees of lon- gitude farther west than in Colorado. In this broad space, and to the eastward, are numerous outliers, as the Black Hills, Big Horn, Bear's Paw, Judith group, etc., all more or less distinctly connected with the main chain. The Black Hills are connected with the Laramie range near the Red Buttes by an anticlinal valley, while the Big Horn is related in 22 THE GREAT WEST. the same way, showing that all these apparently isolated ranges are due to one uniform cause and were elevated at about the same time. MOXJNTAIN-EANGES ON THE EASTERN SLOPE. It may not be' out of place here to describe briefly some of the moun- tain-ranges on the eastern slope, which have already attracted much at- tention, and will receive far more from the public at no distant day. The Black Hills of Dakota, which of late years have received such a large share of public attention on account of the discoveries of valuable gold-mines within their limits, are located mostly in Dakota Territory, between the 43d and 45th degrees of latitude and 103d and 105th degrees of longitude, and occupy an area about one hundred miles in length and sixty in breadth. According to General Warren, the shape of the mass is elliptical, and the major axis trends about ninety degrees west of north. The base of these hills is from 2500 to 3000, and the highest point is about 7000 or 8000 feet, above sea-level. The whole range is embraced, as it were, within the forlfs of the Cheyenne Eiver, called the North and South Branches, which, united, constitute the most important stream flowing into the Missouri River from the south side. The North Branch passes along the north- ern side of the range, receiving very many of its tributaries and most of its waters from it, but takes its rise far to the west of the range, near the source of Powder River, in the " divide " between the waters of the YelloAvstone and those of the Missouri. The South Branch also rises in t]je same divide, flowing along the southern base of the range, and also receives numerous tributaries which have their sources in it. These two main branches unite about thirty miles east of the Black Hills, form- ing the Big Cheyenne, which flows into the Missouri about sixty miles above old Fort Pierre. The Moreau, Grand, Cannon Ball, and other rivers flowing into the Missouri north of the Cheyenne and south of the Yellowstone rise in a high Tertiary divide north of the Black Hills, and are for the greater part of the season quite shallow, and sometimes nearly dry ; but the Little Missouri derives a portion of its waters from the Black Hills through a number of small branches which flow from the north-western slope. We thus see that the Black Hills do not give rise directly to any im- portant stream, if we except the Little Missouri, a few brasches of which flow from springs near the base of the hills, affording but a comparatively small supply of water from that source. Besides the mineral resources of the Black Hills, which of late years have turned out to be so valuable, the timber as well as the agricultural THE GREAT WEST. 23 and pastoral capacities are important All around the base are fertile lands, and among the Hills are large open areas which afford most excel- lent feeding-grounds for stock. As we have previously remarked, these Hills occupy an area about one hondred miles in length and sixtv in breadth, or 6000 square miles. Xearly one-third of this area, or about 2000 square miles, is covered to a greater or less extent with pine timber. Since the settlement of this country demands these resources, the facilities for transportation of this timber over the treeless portions of the plains will be provided, and the importance of these forests cannot be over-esti- mated. The dark appearance which the dense forests of pine timber give to the Black Hills at a distance has given origin to their name. The geolc^cal structure of the Black Hills may be briefly mentioned in this connection. The nucleus or the central portion is composed of red feldspathic granite, with a series of metamorphic slates and schists superimposed, and thence, upon each side of its axi^ of elevation, the va- rious fossiliferous formations of this r^on foUow in their order to the summits of the Cretaceous, the whole inclining against the granitoid rocks at a greater or less angle. There seems to be no marked unconformability in the fcKsiUferous rocks, fiom the Potsdam inclusive to the top of the Cretaceous. From these facts we draw the inference that prior to the elevation of the Black Hills — ^which must have occurred after the deposi- tion of the Cretaceous rocks — all these groups of strata presented an un- broken continuity over the area occupied by these mountains. If this conclusion is a correct one, it will have an important bearing on the physical history of many of the minor ranges of mountains on the eastern slope. It will also enable the geologist to form an approximate estimate of the amount of erosion that has taken place since these minor mountain-groups b^an to rise above the general level of the plains. Proceeding in a south-west direction from the Black Hills, we find there are ample proofs of the connection of these hilL? with the Laramie Mountains through a low anticlinal, which can be followed for many miles. It is sometimes concealed by the recent Tertiary beds, bat it reappears at different points. By the Laramie ^Mountains we designate that group of ranges which extends &om the Red Buttes southward to the ArkauFsas River. This group, when examined in detail, is found to be composed of a large number of smaller ranges — all, as far as I have oteerved, of the true granitic tvpe. The trend of the whole group is very nearly north and south — ^northward as &r as Fort Laramie, where it makes an abrupt flexure around to the west and north-west, and gradually ceases or dies out at the Red Butf^s. From this point westward and northward there 24 THE GREAT WEST. is a space from twenty to forty miles in width destitute of mountain- elevations, though the strata exhibit evidences of dislocations or crust movements. The Laramie range is also composed geologically of a granitoid nucleus, with the fossiliferous formations— Silurian, Carboniferous, Jura-Trias, Cre- taceous, and in many places the Lignitic Tertiary— inclining from each side of a central axis at various angles. It is from these mountains that the numerous branches of the Platte Eiver have their sources, extending a distance of nearly four hundred miles. From the observations which I have made in this range, it seems to me the conclusion is plain that all the above-named rocks, in a nearly or quite .horizontal position, were some time during the Tertiary period continuous over the whole area occupied by them at the present time. The most important outlier of the Eocky Mountains on the eastern slope is the Big Horn range, which, though somewhat irregular in the shape of its mass, has a general trend nearly north-west and south-east. It occupies an area about one hundred miles in length and fifty in breadth. Near latitude 43J° and longitude 102° the line of fracture seems to have partially died out toward the south and south-east, and to have made a gradual flexure around to the west, the whole range soon losing its granitoid character in the volcanic groups near the Wind River group. At the southern end of the Big Horn range we can trace a single low anticlinal across the prairie, connecting these mountains with the Laramie range at the Red Buttes on the North Platte River. They also form a connection with the Wind River Mountains. The central portion of these mountains is also composed of granitic rocks, with the same series of sedimentary beds turned from either flank, inclining at various angles from the axis of elevation, as is seen around the Black Hills and the Laramie. Some of the more lofty peaks are from eight to twelve thou- sand feet high, and are covered with perpetual snow. We may say again, in this connection, that the evidence seems conclusive that up to the time of the accumulation of a large portion of the Lignite beds at least, all these formations, from the Silurian to the true Lignite strata, inclusive, were in a horizontal position, extending continuously over the whole area occupied by the mountains, but as they were slowly elevated the central portions were removed by the erosive action of water. Like the Black Hills, the Big Horn range does not give rise to any important sub-hydrographical basins. The largest stream in this region, and one which gives name to the mountains, rises in the Wind River THE GREAT WEST. 25 range, passes through the Big Horn Mountains, and unites with the Yellowstone about seventy miles to the northward. Before reaching the mountains it takes the name of "Wind Eiver, and assumes the name of Big Horn after emerging from them. This range constitutes quite an important feeder of the Yellowstone. Powder Eiver, which rises in this range by numerous branches, drains a large area, mostly lignitic Tertiary, and pours a considerable volume of water into the Yellowstone near longitude 105J° and latitude 46|°. Tongue River is the next most im- portant stream, which, though not draining so great an area, empties into the Yellowstone a much larger volume of water. Near the junction of the Popo Agie with "Wind River we come in full view of the "Wind River Mountains, which form the dividing crest of the continent, the streams on the one side flowing into the Atlantic and those on the other into the Pacific. This range is also composed to a large extent of red and gray feldspathic granite, with the fossiliferous rocks in- clining from the eastern side. The great Teton range is formed mostly of granitic rocks, though intersected with iykes of trachyte. Basalts are found on the plains to a greater or less extent, in Pierre's Hole, Jack- son's Hole — broad oval parks or basins among the mountains. On Snake River the ancient volcanic rocks seem to have been poured out over the country, and to have cooled in layers, thus giving to great thicknesses the appearance of stratification. THE SOUECES OF THE YELLOWSTONE AND MISSOURI. The mountains about the sources of the Missouri and Yellowstone Rivers are largely of eruptive origin. Enormous gorges have been worn through two to three thousand feet in thickness of volcanic breccia, ex- posing nearly vertical walls on either side. Probably nowhere on the continent can be found more striking proofs of volcanic action, and it appears to have occurred at a modern date, in a geological sense. Here and there, however, are mica and clay-slates, also feldspathic granites, rising from beneath the eruptive layers and inclining at various angles. One of the most -extraordinary features in the region about the sources of the Yellowstone are a series of what appear to be stratified rocks, composed of volcanic products, which were thrown out of the earth's interior during the remarkable period of volcanic activity, the remains of which are now seen in the numerous geysers and hot springs that have given such celebrity to the country. These volcanic products seem to have been thrown out into water, and afterward redistributed in the form of strata of breccias, conglomerates, tuffs, and sandstones. Alon^; the 26 THE GREAT WEST. East Fork of the Yellowstone Eiver, and in the Gallatin range, about the sources of Canon and Boulder Creeks, these beds reach a thickness of from three to five thousand feet. Among the breccias are found remark- able specimens of silicified wood. Trunks of trees several feet in diameter, and in one instance twelve feet in length and ten feet across, occur in an upright position. Prostrate trunks of trees fifty to sixty feet in length and five to six feet in diameter are not uncommon. Mr. W. H. Holmes, who was a member of the United States Geological Survey of the Terri- tories in charge of Dr. Hayden, made an examination of these curious trees in the Yellowstone Park. From an article in the Bulletin of the survey, February, 1879, I make the following extracts, which must be read with deep interest : " The standing trunks are generally rather short, the degradation of the compact enclosing strata being so slow that the brittle trunks break down almost as fast as they are exposed. In many cases the roots are exposed, and may be seen penetrating the now solid rock with all the original ramifications. One upright frunk, of gigantic proportions, rises from the enclosing strata to the height of twelve feet. By careful measure- ment it w.as found to be ten feet in diameter, and as there is nothing to indicate to what part of the tree the exposed section belongs, the roots may be far below the surface, and we are free to imagine that there is buried here a worthy predecessor of the giant Sequoias of California. Although the trunk is hollow and partly broken down on one side, the woody structure is perfectly preserved, the grain is straight, and the circles of growth distinctly marked. The bark, which still remains on the firmer parts, is four inches thick, and retains perfectly the original deeply-lined outer surface. Specimens of the wood and bark were col- lected, but no microscopic examinations have been made. It is clear, how- ever, that the tree was not a conifer. The strata which enclose this trunk are chiefly fine-grained greenish sandstones, indurated clays, and moder- ately coarse conglomerates. They have been built around it as it stood in comparatively shallow but doubtless quiet waters. As would naturally be expected, these strata contain many vegetable remains : branches, root- lets, fruits, and leaves are extensively enclosed. One stratum of sand- stone that occupies a horizon nearly on a level with the present top of the giant tree contains a great variety of the most perfectly preserved leaves. Such specimens as we were able to bring away with us have been submitted to Professor Leo Lesquereux for identification. They are found by him to belong to the Lower Pliocene or Upper Miocene THE GREAT WEST. 27 and correspond in a number of their species with the Chalk Bluffs specimens of Professor Whitney " As far above the leaf-bearing horizon as I was able to ascend the silicified trunks were very numerous and well preserved, and by the aid of a field-glass others could be detected in all parts of the cliff to the highest stratum. "At another point, nearly a mile. farther east, I climbed the rugged walls of the mountain for the purpose of examining a number of large trees that were visible from below. Trunks and fragments of trunks were found in great numbers and in all conceivable positions. In most cases the woody structure is well preserved ; the trunks have a tendency to break in sections, and on the exposed ends the lines of growth, from centre to circumference, can be counted with ease. In many cases the wood is quite completely opalized or agatized, and such cavities as ex- isted in the decayed trunks are filled with beautiful crystals of quartz and calcite. Our party was so fortunate as to procure some very hand- some specimens of amethyst and ferruginous quartz. It is a matter worthy of observation that nearly all of the beautiful crystals that occur so plentifully in this region have been formed in the hollows of silicified trees. The same fact has been noticed in regard to similar crystals ia many parts of the West, and notably in the case of the smoky quartz of the Pike's Peak region in Colorado. " The silicifying agents have been so unusually active in the strata of the volcanic Tertiary that not only are all organic remains thoroughly silicified, but all cavities in the loosely-bedded rocks and all fracture- lines in the strata are filled with chalcedony or other forms of quartz. " On reaching the heavily-bedded conglomeratas of the upper third of the cliff, I found the trees still more perfectly preserved. Many of the trunks are twenty and thirty feet in height. Their roots are in most cases imbedded in the layei's of finer-grained materials in which they grew, while the battered and branchless trunks are encased in the coarse conglomerates and breccias. These latter rocks are composed chiefly of basaltic fragments, many of which are of great size ; there is, however, always enough tufaceous and other fine-grained material to fill in the interstices and act as a cement. These beds are massive and irregular, and seem to have accumulated too fast to be thoroughly redistributed by the waters. Only the stronger trees of the forest seem to have with- stood the fierce storms of rocks that must have prevailed at the period of their entombment, as the smaller trunks and branches are prostrate or totally destroyed. In most cases where upright trunks penetrate the 28 THE GREAT WEST. entire thickness of an enclosing bed, the tops may be seen to terminate with the upper surface of that bed, as if causes had acted at the begin- ning of the deposition of the succeeding stratum to plane down the irregularities of the old surface. In due course of time this succeeding stratum produced its growth of forest, which followed its many prede- cessors into the subterranean depths, and in its turn was buried by the rapidly-accumulating conglomerates. This remarkable alternation of events seems, in a general way, to have been kept up from the beginning to the end of the period. " The very precipitous character of the cliffs prevented me from reach- ing the upper part of the wall at this point, but I succeeded in making my way to the summit of the mountain at two other points, and found that everywhere the section was practically the same. " On the opposite side of the valley the same conditions were observed : the fossil trees occur at the highest point reached — three thousand feet above the river. The ranges that form the rim of this valley on the north and east reach an elevation of eleven thousand five hundred feet, and as the conglomerates may be seen reaching and forming the loftiest summits without perceptible break or change of character, it is probable that they will be found to enclose the remains of forests throughout. " On some of the higher summits to the east of Yellowstone Lake similar stratified conglomerates contain silicified wood in a very frag- mentary state. These conglomerates are composed mainly of basaltic and trachytic materials, but contain large quantities of fragments of sand- stones and quartzites, which leads to the conclusion that portions of the earlier Tertiary strata have been broken up and ejected with the igneous products. It is quite probable that these strata were among the later products of the volcanic Tertiary age proper. They are generally found abutting against masses of unstratified igneous materials that probably mark the sites of islands which were doubtless volcanic centres. I find that as we recede from these centres of eruption the strata diminish very perceptibly in thickness and coarseness of materials, and have at the same time a very perceptible dip toward the surrounding valleys. One is at times led to suspect that portions at least of these beds are of sub- aerial formation, as is the case with extensive strata about the cones of modern volcanoes, but there are a multitude of facts that go to prove that the greater part of the formations of this age were rearranged or sedi- mented in water." The plains along the lower Yellowstone are in many localities so thickly covered with silicified trees that they have received the name of THE GREAT WEST. 29 " petrified forests." The strong resemblance of these stony trees to the dry fallen trunks of modern timber is most remarkable. The woody fibre and the layers of growth are as perfect and natural as in our living trees. Yet they all belong to a past age, the Tertiary, and the species or varieties are extinct, yet undoubtedly are the true ancestors of our living vegetation. (We may refer to this subject again in connection with remarks on the ancient vegetation of the West.) YELLOWSTONE NATIONAL PAEK. In this connection we may describe briefly some of the wonders of the Yellowstone National Park and its surroundings. Within the last decade the remarkable scenery of the Rocky Mountain region has become more and more familiar to the travelling public, and as the facilities for reaching every portion of our great West are increasing every year, those portions which have hitherto been considered accessible only to the adventurous explorer or pioneer will soon be easily reached by the general public. Already a railroad from Cheyenne, Wyoming Territory, to the Yellow- stone Park has been commenced, and 125 miles of it are to be completed during the year 1880. The far-famed Yosemite Valley, the Snowy Sierras, the deep gorges of the Colorado of the West, the great area of lofty mountain-peaks in Central Colorado — not surpassed by the world- renowned scenery of the Alpine districts of Europe — are now reached with comparatively little diificulty by the travelling public. Indeed, it may now be said that the era of exploration is past for the United States and Territories, for there are now no tracts of any size that have not been examined with more or less care, and the novelty taken from them. Located in the north-western corner of Wyoming Territory, about the head-waters of the Missouri and Yellowstone Rivers, is a tract of coun- try more remarkable for the wonderful phenomena of Nature than any other region of the globe. It may very properly be called the " North- ern Wonderland," in contradistinction to a similar region in New Zea- land which is now known as the " Southern Wonderland." It is a sin- gular fact that this marvellous region has been known to the world with any certainty only for a period of about ten years. Vague rumors of burning plains, boiling springs, volcanoes ejecting water and mud, great lakes, and other wonders, had indeed reached the civilized world from time to time, but as the most astounding stories of petrified forests, of animals turned to stone, and of streams flowing so rapidly that their waters became heated were intermingled with these rumoi's, the latter 30 THE GREAT WEST. were disregarded altogether, and were looked upon as the wild vagaries of wandering mountaineers.- Captains Lewis and Clarke, in their exploration of the head-waters of the Missoviri in 1805, seem to have heard nothing of the marvels at the sources of the Madison and Yellowstone Rivers. The Yellowstone Lake was placed by them on the map as a large body of water, but they had no personal knowledge yet, their information having been, in all prob- ability, derived from the Indians. The first trustworthy accounts that made any impression on the public were given by a small party under General Washburne, the surveyor-general of Montana, and escorted by a small body of United States soldiers under Lieutenant G. C. Doane, in 1870. This party spent about a month in these interesting localities. Hon. N. P. Longford the same year gave a popular account of these phenomena in Soribner's Monthly, which excited great interest. Many other expeditions, official and unofficial, too numerous to mention in this connection, have since visited this region. During the seasons of 1871 and 1872 the writer conducted a thoroughly-organized corps in this dis- trict, and made a systematic survey of it. The official report of the expe- dition of 1871, published by the government, created so great an interest among the people that, through the effi)rts of the writer, in February, 1872, Congress was induced to pass an act withdrawing from settlement, occupancy, or sale under the laws of the United States an area about the sources of the Yellowstone Eiver embracing about thirty-five hundred square miles, dedicating and setting it apart as a public park or pleasure- ground for the benefit and enjoyment of the people. Up to the time of these explorations the great Divide or watershed of the continent was probably the least-known region in America, although it exceeds all other regions in geographical as well as geological interest. So much information of a strictly scientific character was obtained at that time, so many new streams and lakes were surveyed and properly located, that our knowledge of this wonderful land may be said to have been placed upon a reliable basis. From a purely geographical point of view, the Yellowstone National Park may be said to embrace some of the most remarkable and instruc- tive features in North America. It forms the very apex or divide of the continent. Within a radius of twenty-five miles may be found the sources of three of the largest rivers in America. The general elevation is from six to eight thousand feet above sea-level, while the mountains, the eternal snows of which form the sources of the great rivers just men- tioned, rise to the height of from ten to twelve thousand feet. Flowing THE GREAT WEST. 31 northward are the numerous branches of the Missouri, Yellowstone, and Wind Rivers, all of which eventually unite in one great stream, the Mis- souri ; to the south are the branches of Green Eiver, which latter unites with the Colorado and finally empties into the Gulf of California ; while south and west flow the branches of Snake River, which, joining the Columbia, pour their vast volume of water into the Pacific. The Yellowstone Lake, which is one of the most beautiful bodies of water on the continent, is always of a deep emerald-green color, and is set like a gem amid the surrounding volcanic mountain-peaks. On the south side of the lake, not more than half a mile distant from it, and not over three hundred feet above the level of its surface, is the Divide between the drainage of the Atlantic and Pacific slopes. It would require but little labor to turn the waters of the lake into Snake River. Here is located the celebrated Two-Ocean Pass, where at certain seasons of the year the waters of the same channel separate, a portion flowing in either direction. From the summits of the snow-capped peaks surrounding the lake the view is grand beyond description. From the top of Red Moun- tain, on the south side, the scope of vision embraces a circle having a radius of one hundred and fifty miles, within which four hundred and seventy mountain-peaks worthy of a name can be distinctly seen. The area swept by the eye from this point cannot be much less than from thirty to fifty thousand square miles, embracing portions of Wyoming, Montana, Idaho, and Utah, and exhibiting every variety of the grandest and most beautiful scenery. Ten large lakes and several smaller ones are taken in by this view, and the entire Yellowstone Park is spread out under the eye. The purity of the atmosjjhere in these high latitudes is well known, so tliat these statements will not seem exaggerated. On the east side of the Yellowstone River, between the first and second canons, we find one of the most symmetrical and remarkable ranges of mountains to be seen in the West. This range was called the Yellowstone, and has been pro- nounced by Alpine travellers to be equal in beauty and artistic form to any in Central Eiu-ope. Sharp, jagged peaks and pyramidal masses stand out boldly against the sky, their snow-crowned heads glittering in the sunlight. The central portion of this range is composed of granite rocks, through the fissures of which the igneous matter has risen to the surface, covering the sides and summits and giving to the entire mass a peculiarly sombre hue. At > the west base of this range is one of the remarkable lake-basins for which the West has now become famous. This basin has a length of thirty miles and an average width of five miles. It is sup- posed that during the Pliocene Tertiary period there was a series of these 32 THE GREAT WEST. peculiar lake-;basins all along the upper portions of the great rivers of the West, in the sediments of which were entombed the remains of many extinct animals, such as the mastodon, elephant, rhinoceros, camel, horse, etc., which thousands of years ago roamed over this broad region unmo- lested by man. To the geologist the Yellowstone Park offers an endless field for obser- vation and speculation. As we have previously remarked, this entire area was, in comparatively modern geological times, the scene of the most won- derful volcanic activity known in any portion of our country. From innumerable craters or vast fissures in the earth's crust were ejected in Pliocene or Post-Pliocene times vast quantities of fragments of rocks, ashes, tuffs, etc. into the surrounding waters, where they were rearranged in horizontal beds from three to five thousand feet in thickness. It was from these beds that the strange, marvellous forms which meet the eye at every point have been carved out by the erosive action of water. The Grand Canon of the Yellowstone River, the towers of Tower Falls, and the deep gorges of the branches of the East Fork are marked illustrations of this strange scenery. These walls are surmounted by a great variety of architectural forms, among which it does not require a vivid imagi- nation to trace huge castles and fortress-walls. The prevailing hue is a sombre black, although in many localities almost every shade of color is represented. Perhaps the most prominent feature of the park, in which it differs from the Yosemite Valley and other remarkable localities, is the variety of its scenery. The traveller passes from one Tinique scene to an- other, so that his vision never wearies and is never satisfied. THE HOT SPRINGS OF YELLOWSTONE NATIOSTAL PAEK. Among the remarkable natural phenomena of the Yellowstone National Park, none have attracted more attention from travellers and scientists than the thermal springs, which occur in great numbers. Almost every known variety of hot springs is found here, which are the result of vol- canic action. The Geysers of Iceland, which have excited the wonder of scientific men for several centuries, the still more remarkable and nume- rous hot springs of New Zealand, the mud springs and mud geysers of Java, the sulphur and steam vents which occur in almost all volcanic regions, exist here in vast numbers. Indeed, they surpass in number and magnitude all the world besides. These hot springs, which are slowly dying out, represent the last of a series of remarkable phys- ical events. The hot springs of the park may be separated into tsvo classes, based THE GREAT WEST. 33 on the character of their deposits — namely, those in the deposits of which lime predominates, and those in which silica is most abundant. The remarkable group on Gardiner's River illustrates the first class, while the Upper and Lower .Geyser Basins of the Firehole River are the most striking examples of the second class. The character of the deposit de- pends upon the nature of the underlying rocks through which the heated waters reach the surface. Beneath the calcareous deposit of the hot springs of Gardiner's River there are from fifteen hundred to two thou- sand feet of limestone strata. The heated waters on their way upward dissolve the lime, and the latter reaches the surface in solution, and is left by evaporation in the beautiful and imique forms which so much ex- cite the admiration of the observer. The siliceous springs come to the surface through volcanic and other rocks in which silica is the principal constituent, and the silica is deposited about the orifice in the same way as the lime, but at a far less rapid rate. Here it is again the process of evaporation which forms the beautiful decorations about the springs. It is, however, to the wonderful variety, exquisitely delicate colors, and the almost unnatural transparency of the waters that these springs owe much of their attractiveness. The orifices through which the hot waters issue are beautifully enamelled with a porcelain-like lining, and around the edges a layer of sulphur is precipitated. Along the sides and bottoms of the numerous little channels of the streams that flow from these springs there is a striking display of the most vivid colors, consisting of various shades of red, from scarlet to a bright rose-tint, and yellow, from bright sulphur through all conceivable shades to light cream-color. There are also various shades of green, arising from fhe peculiar vegetable forms with which many of the springs are filled. Great quantities of a fibrous, silky substance, which occurs in the little streams that flow from the boil- ing springs, and vibrates with the smallest movement of the water, add still more to the beauty of the scene. The remarkable transparency and deep, vivid blue color of the waters, as seen in many of the springs, are marvels which attract the eye of the traveller. The sky, with the smallest cloud that flits across its face, is reflected in the clear depth of these waters, and the ultramarine colors displayed by them, more vivid even than the deep blue of the sea, are greatly heightened by the constant gentle vibration. One can look down into the clear depths and see with perfect distinctness the minutest orna- ment on the inner sides of the basin. These springs represent every stage of development, from the most ac- tive geysers of the first class in power and size to the entire extinction of 3 .34 THE GREAT WEST. all activity. In the Upper and Lower Geyser Basins of the Firehole River there are about iifty springs that might be regarded as geysers of the first class, throwing upward a column of water from a few feet to over\wo hundred feet in height. Then there is' every grade downward to simple boiling, or even quiet, hot springs. All about are seen great numbers of dead springs which may once have been geysers of the first class. Among the hundreds of groups of springs that are distributed over the park the proofs of former intensity are everywhere to be found, showing that the springs still left are only remnants as compared with the number and power of those that must have existed at the cessation of the true volcanic forces. Next to the geysers are the mud volcanoes, mud springs, fumaroles, or salses, as they are usually termed. They also vary in grade from a sim- ple bowl of turbid water to a vast crater of seething mud fifty to one hundred feet in diameter. Many of these mud springs are of great beauty, the siliceous fine clay presenting every shade of yellow and pink, derived from the ferric oxides, and a fineness of composition that would equal the purest meerschaum. There are also deep boiling caldrons from which are emitted clouds of sulphurous vapors and steam that settle down upon the surrounding veg- etation, encrusting it with fine mud. Dr. Hochstetter, speaking of the same phenomena in the great Southern Wonderland of New Zealand, de- scribes them as follows : " The entrance to the ravine is overgrown with a thicket, and is rather difficult of access; it also requires considerable caution, as suspicious places have to be passed where the visitor is in danger of being swal- lowed up in the heated mud. Inside, the ravine has the appearance of a volcanic crater. The bare walls, utterly destitute of vegetation, are ter- ribly fissured and torn, and odd-looking serratures, threatening every mo- ment to break loose, loom up like dismal spectres of red, white, and blue fumarole clay, evidently the last remains of decomposed rocks. The bot- tom of the ravine is simmering. There lies a deep basin of boiling wa- ter ; next to this is a terrible hole emitting hissing jets of steam ; and farther on are mud-cones, from two to five feet high, vomiting hot mud from their craters with dull rumblings, and imitating on a small scale the play of large fire volcanoes." * I will not dwell on the probable origin of these thermal springs, as they have been studied by some of the ablest men of science in Europe, as Bunsen, Bischofi", Tyndall, and others, and their conclusions have been * Hochstetter's New Zealand, p. 414. THE GREAT WEST. 35 accepted. It is supposed that they are all remnants of volcanic action, and, like volcanoes, derive their heat from some deep-seated portion of the earth's crust. Geysers may be regarded as volcanoes, except that the former throw out heated waters, while the latter eject melted materials, etc. LEGISLATION RESPECTING YELLOWSTONE NATIONAL PARK. . As has been previously stated, during the session of 1871-72 both Houses of Congress passed a bill to set apart an area about the sources of the Yellowstone River embracing these wonderful curiosities as a public park for the benefit and instruction of the people. At the request of the committee to whom the bill wasVeferred, the writer prepared the fol- lowing report, and on the strength of the information contained therein the bill became a law: " The Committee on the Public Lands, having under consideration bill H. R. 764, would report as follows : "The bill now before Congress has for its object the withdrawal from settlement, occupancy, or sale under the laws of the United States a tract of land fifty-five miles wide by sixty-five long about the sources of the Yellowstone and Missouri Rivers, and dedicates and sets it apart as a great national park or pleasure-ground for the benefit and enjoyment of the people. The entire area comprised within the limits of the reserva- tion contemplated in this bill is not susceptible of cultivation with any degree of certainty, and the winters would be too severe for stock-raising. Whenever the altitude of the mountain-districts exceeds six thousand feet above tide-water, their settlement becomes problematical, unless there are valuable mines to attract the people. The entire area within the limits of the proposed reservation is over six thousand feet in altitude, and the Yellowstone Lake, which occupies an area fifteen by twenty-two miles, or three hundred and thirty square miles, is 7788 feet. The ranges of mountains that hem the valleys in on every side rise to the height of ten to twelve thousand feet, and are covered with snow all the year. These mountains are all of volcanic origin, and it is not probable that toy mines or minerals of value will ever be found there. During the months of June, July, and August the climate is pure and most invigor- ating, with scarcely any rain or storms of any kind, but the thermometer frequently sinks as low as 26°. There is frost every month in the year. This whole region was in comparatively modern geological times the scene of the most wonderful volcanic activity of any portion of our country. The hot springs and geysers represent the last stages — the vents or escape-pipes — of these remarkable volcanic manifestations of 36 THE GREAT WEST. the internal forces. All these springs are adorned with decorations more beautiful than human art ever conceived, and which have required thou- sands of years for the cunning hand of Nature to form. Persons are now waiting for the spring to open to enter in and take possession of these remarkable curiosities, to make merchandise of these beautiful specimens, to fence in these rare wonders so as to charge visitors a fee, as is now done at Niagara Falls, for the sight of that which ought to be as free as the air or water. " In a few years this region will be a place of resort for all classes of people from all portions of the world. The Geysers of Iceland, which have been objects of interest for the scientific men and travellers of the entire world, sink into insignificance in comparison with the hot springs of the Yellowstone and Firehole Basins. As a place of resort for in- valids it will not be excelled by any portion of the world. If this bill fails to become a law this session, the vandals who are now waiting to enter into this wonderland will in a single season despoil beyond recovery these remarkable curiosities, which have required all the cunning skill of Nature thousands of years to prepare. " We have already shown that no portion of this tract can ever be made available for agricultural or mining purposes. Even if the altitude and the climate would permit the country to be made available, not over fifty square miles of the entire area could ever be settled. The valleys are all narrow, hemmed in by high volcanic mountains like gigantic walls. " The withdrawal of this tract, therefore, from sale or settlement takes nothing from the value of the public domain, and is no pecuniary loss to the government, but -will be regarded by the entire civilized world as a step of progress and an honor to Congress and the nation. "Department of the Inteeioe, 1 Washington, D. C, January 29, 1872. j " SiE : I have the honor to acknowledge the receipt of your commu- nication of the 27th inst., relative to the bill now pending in the House of Representatives dedicating that tract of country known as the Yellow- stone Valley as a national park. " I hand you herewith the report of Dr. F. V. Hayden, United States Greologist, relative to said proposed reservation, and have only to add that I fully concur in his recommendations, and trust that the bill referred to may speedily become a law. Very respectfully, your obedient servant, " C. Delano, Seardary. " Hon. M. H. DuNNELL, House of Eepresentatives. THE GREAT WEST. 37 " The committee therefore recommend the passage of the bill without amendment." The text of the bill is as follows : "An act to set apart a certain tract of land lying near the head-waters of the Yellowstone River as a Public Park. Be it enacted by the Senate and House of Representatives of the United States of America, in Con- gress assembled, That the tract of land in the Territories of Montana and Wyoming lying near the head-waters of the Yellowstone River, and described as follows — to wit : commencing at the junction of Gardiner's River with the Yellowstone River, and running east to the meridian passing ten miles to the eastward of the most eastern point of Yellow- stone Lake ; thence south along said meridian to the parallel of latitude passing two miles south of the most southern point of Yellowstone Lake ; thence west along said parallel to the meridian passing fifteen miles west of the most western point of Madison Lake ; thence north along said meridian to the latitude of the junction of the Yellowstone and Gardi- ner's Rivers ; thence east to the place of beginning, — is hereby reserved and withdrawn from settlement, occupancy, or sale under the laws of the United States, and dedicated and set apart as a public park or pleasuring- ground for the benefit and enjoyment of the people ; and all persons who shall locate or settle upon or occupy the same or any part thereof, except as hereinafter provided, shall be considered trespassers and removed therefrom. " Sec. 2. That said public park shall be under the exclusive control of the Secijf tary of the Interior, whose duty it shall be, as soon as prac- ticable, to make and publish such rules and regulations as he may deem necessary or proper for the care and management of the same. Such regulations shall provide for the preservation from injury or spoliation of all timber, mineral deposits, natural curiosities, or wonders within said park, and their retention in their natural condition. The Secretary may, in his discretion, grant leases for building purposes, for terms not exceeding ten years, of small parcels of ground, at such places in said park as shall require the erection of buildings for the accommodation of visitors ; all of the proceeds of said leases and all other revenues that may be derived from any source connected with said park to be expended under his direction in the management of the same and the construction of roads and bridle-paths therein. He shall provide against the wanton destruction of the fish and game found within said park, and against their capture or destruction for the purpose of merchandise or profit. He shall also cause all persons trespassing upon the same after the pas- 38 THE GREAT WEST. sage of this act to be removed therefrom, and generally shall be author- ized to take all such measures as shall be necessary or proper to fully car- ry out the objects and purposes of this act." Approved March 1, 1872. PEINCIPAL EIVEKS OP THE NOETH-WEST. In this connection it is thought best to present a brief account of the principal rivers that drain the vast area of the North-west. The Missouri River and its tributaries form one of the largest as well as most important hydrographical basins in America. They drain an area of nearly or quite one million square miles. Rising in the loftiest portion of the Rocky Mountains, the Missouri flows northward in three principal branches — Madison, Gallatin, and Jefferson Forks — to their junction, and then proceeds onward until it emerges from the Gate of the Mountains, nearly two hundred miles ; it then bends to the eastward, flow- ing in this direction to the entrance of White Earth River, a distance of nearly five hundred miles ; it then gradually bends southward to its junc- tion with the Mississippi, a distance of fifteen hundred to two thousand miles. The branches which form the sources of the Missouri rise in and near the Yellowstone National Park, flowing for the most part through metamorphic and volcanic rocks, until the main river emerges from the mountains into the plains, where it passes over Jura-Trias beds. The Falls of the Missouri, which extend for a distance of twenty or thirty miles, cut their way through a great thickness of these Jura-Trias rocks. Below the falls the channel passes through the soft yielding clays and sands of the Cretaceous beds for two hundred and fifiy miles, with the exception of the Judith Tertiary Basin, which is about forty miles in length. The Cretaceous beds then reappear, extending nearly to the mouth of Milk River, where the Lignitic beds commence. These are also composed of sands, marls, and clays, with intercalated beds of brown coal of greater or less economic value. The river flows through these Lignitic beds to the mouth of Heart River, below Fort Union, a distance of nearly two hundred and fifty miles, where the Cretaceous rocks rise to the surface again. These latter formations extend to within a short distance of Council Bluffs, more than five hundred miles. (I have esti- mated the distance in a straight line as nearly as possible.) Just above Council Bluffs the Coal-measure limestones commence, and the valley of the Missouri gradually becomes more restricted, though it is still of mod- erate width below the mouth of the Kansas. The Yellowstone River is by far the largest branch of the Missouri, and for four hundred miles, from its mouth up, it seems to be as large as THE GREAT WEST. 39 the Missouri itself from Fort Eeno to Fort Union. It is navigable for steamers during the spring and early summer for three or four hundred miles above its junction with the Missouri. This river takes its rise in the main Divide of the Rocky Mountains, properly in the beautiful and now well-known Yellowstone Lake. Its channel is worn through rocks very similar to those of the Missouri and its branches, the lower four hun- dred miles of its course being through the Lignitic beds for the most part. The character of its valley is very similar to that of the Missouri. It is now settled up by farmers almost continuously from the lower caflon to its junction with the Missouri. Tongue and Powder Rivers, which are quite long branches, have their origin in the Big Horn Mountains, their channels cutting through the rocks that surround the Big Horn range. Tongue River is nearly one hundred and fifty miles in length, and flows for the most part through soft, yielding rocks of the Lignitic group. Powder River is from two hundred and fifty to three hundred miles in length, and also flows nearly all its course through the same Lignitic beds. Below the mouth of the Yellowstone River we observe on the right side of the Missouri River several large branches, as Little Missouri, Big Knife, Heart, Cannon Ball, Grand, Moreau, and Big Cheyenne. These streams are confined mostly to the plains, and often cease to be running streams in the dry season, except about their sources. The Teton River takes its origin in the north-western rim of the White River Tertiary Lake-Basin, and runs nearly east, for the most part through formations of Upper Cretaceous age. It drains an area about one hun- dred miles in length and thirty to fifty in breadth. The next most prominent stream is "White River, which flows directly through the Bad Lands, and gives the name to one of the most remark- able Tertiary deposits in the world. (This interesting lake-basin will be referred to again farther on.) The river takes its rise in the plains near latitude 42J° and longitude 104°, flows for a time in a north-east direc- tion, then bends so as to enter the Missouri a little south of east near latitude 43° 41' and longitude 99|°. Nearly its entire course lies through the White River Tertiary beds, and for the greater part of the year its waters are so full of sediment as to be unfit for use. When the water stands for a time a thick scum accumulates on the surface, which has much the color and consistency of cream. The water itself looks very much like turbid lime-water, and is very astringent to the taste. The valley is gen- erally open, tolerably well wooded, abounding in fine grass, and has always been a favorite resort for the Indians. The road between Fort Reno on 40 THE GREAT WEST. the Missouri River and Fort Laramie passes up the valley for a consider- able distance through some of the most picturesque scenery in the West. The river has numerous branches, but the only one of importance is called the South Fork, and is nearly as large and as long as the main stream. It drains an area about two hundred and fifty miles in length and forty to sixty in breadth. The Niobrara is the next most important stream, and is about four hun- dred and fifty miles in length. This also flows for the most part through the sands and clays of the Great Lake-Basin, of which the well-known " Bad Lands " form a conspicuous part. It is a beautiful stream of rather swift running water, generally ten to fifteen feet in width, but widening as it descends. There is much fertile land in this valley, possessing many attractions for the settler. It has always been a favorite camping-place for the various bands of Indians that roam over this region. The great sub-hydrographical basin, and perhaps in many respects the most important one in the Missouri Valley, is that of the Platte, which empties into the Missouri River near latitude 41° 3' 24". Its valley forms a natural grade for a railroad to the foot of the mountains, and already one has been constructed from Omaha City across the continent. The Platte River takes its rise in the Laramie range, and flows for the greater part of its course through the more recent beds of the Tertiary de- posits. The area drained by this river must be at least six hundred miles from west to east, and eighty to one hundred and fifty from north to south. Although this stream is one thousand yards or more in width, the water is so shallow and the channel so .shifting that it can never be rendered navigable, even for small boats. In early days the fur-traders were never able to rely on it for the transportation of their peltries, furs, and skins. On the left or north side of the Missouri River there are comparatively few branches ; the principal of them are Milk, White Earith, James, Ver- milion, and Big Sioux. The three last named rise in the far north and flow through a much more rocky region and over a stonier bed, and their waters, as they pour into the Missouri, contain less sediment than any of the others. Indeed, most of the rivers previously described flow through a generally barren country, with a thirsty atmosphere and a still more thirsty soil, and on their way to the Missouri Valley they lose nearly or quite all their waters. Many of these long rivers, as Grand, Cannon Ball, and Cheyenne, in the autumn frequently have so little water as to cease to be running streams, while perhaps one hundred miles above their mouths, if in the vicinity of some mountain, there is a full supply of water. The Musselshell River is a fine example : toward its source it is THE GitEAT WEST. 41 a fine running stream ; in the dry season it is lost almost entirely before reaching the Missouri. Much more might be said in this connection, but .enough has been given to enable the reader to comprehend to some extent the geographical area drained by the Missouri Eiver and its tributaries. THE TERTIAEY LAKE-BASINS OF THE WEST. We have frequently spoken in reference to the wonderful Tertiary lake- basins of the West. These were first made known on the eastern slope of the Rocky Mountains, and among the most wonderful is that of the Mauvaises Terres, or " Bad Lands," of Dakota. These lake-basins are found all over the West, from the Missouri River to the Pacific coast, and belong in age to various divisions of the Tertiary epoch. There is no water in them at this time, and their existence is only known to the student of geology. During the Tertiary period the Bad Lands Basin occupied an area of at least one hundred thousand, and very possibly one hundred and fifty thousand, square miles. It will thus be seen that our greatest northern lakes, of which we so proudly boast, are but ponds in comparison with some that once existed in this mountain-region. The close observer will notice at once that he is passing into a district, the rock-formations of which are quite different from any that he has seen before. He finds also that he is passing beyond the region of great fertility, luxuriant vegetation, fine farms, and fields of grain to a comparatively arid, sterile region; still, the broad bottoms of the Platte are covered with a fair growth of grass, but the chances for the successful cultivation of crops of any of the cereals are very small. The soil becomes too thin, sandy, and arid for the growth of anything more than a scanty vegetation. We might linger here for a moment and inquire into some of the causes that have produced this scantiness of vegetation and almost entire absence of trees over so large an area. There is quite a remarkable belt or zone of country along the eastern base of the Rocky Mountains, ex- tending from the Arctic Sea far south to Mexico, upon which but a small amount of moisture ever falls. This has often been denominated the Great American Desert. In years past this belt was supposed to com- prise the greater portion of the area i lying between the Missouri River and the foot of the mountains, but every year, as we know more and more of the country, this belt becomes narrower and narrower, and as a continuous area it has already ceased to exist, even in imagination. There are, however, large portions of the country that are comparatively worth- 42 THE GREAT WEST. less and arid, which may be called barren or sterile. It is now pretty well understood that the cause of the absence of timber in this great region is want of moisture. A very clear explanation of this subject, and one which seems in accordance with the facts, is given by Professor Dana in Silliman's Journal (vol. xl., page 393). If we were to examine a rain-chart, we should find that where the forests are most luxuriant, as along the Atlantic coast in the southern portion of the Mississippi Valley, the greatest amount of rain falls annually — say fifty to sixty-five inches ; and as soon as we approach any of the interior basins of the Western continent, or any portion of this dry belt, we observe that the amount of moisture diminishes to thirty, twenty, fifteen, ten, and in some cases to as low as five inches, annually. Again, along the Missouri River, where the vegetation is quite extensive and the forest trees abundant, we have twenty to thirty inches of rain, but as soon as we pass to the westward three hundred miles we have but ten or fifteen inches. On the Pacific coast of Oregon and Washington, whose gigantic forests are celebrated all over the world, we find that from fifty-five to sixty-five inches of rain fall annually. We might multiply these illustrations, but the evidence seems to be conclusive. There is another point that may be worthy of note here, and that is the prevailing impression among all the inhabitants of the West of a gradual change of climate by settlement and the cultivation of the soil. It is a fact that over a width of one hundred miles or more along the Missouri River the little groves of timber are extending their area, that springs of water are continually issuing from the ground where none were ever known before, and that the distribution of rain throughout the year is more equable. Such being the case, time may work import- ant changes, and settlements may at some period cause a large portion of that belt which has hitherto been regarded as given up to sterility to become of value for the abode of man. The valleys of the Loup Fork and the Niobrara Rivers, although largely uninhabitable, are full of interest to the geologist. Located along these rivers is one of those grand cemeteries of extinct animals which have excited the wonder of intelligent men all over the world. Farther to the north-west, on White Earth River, is another of these far-famed bone-deposits. These two interesting localities bear such a relation to each other in the order of time and the relationship of the animals preserved in them that they should be described in the same connection. I will therefore take the reader at once to the valley of White Earth River, near the south-western base of the Black Hills, and THE GREAT WEST. 43 there we shall behold one of the wildest regions on this continent. It has always gone by the name of " Bad Lands ;" by the Canadian French known as Mauvaises Terres; in the Dakota tongue, Ma-ko6-si-tcha. These words signify a very difficult country to travel through, not only from the ruggedness of the surface, but also from the absence of any good water and the small supply of wood and game. In the summer the sun pours its rays on the bare white walls, which are reflected on the weary traveller with double intensity, not only oppressing him with the heat, but so dazzling his eyes that he is not unfrequently affected with temporary blindness. I have spent many days exploring this region when the thermometer was 112° in the shade and there was no water suitable for drinking purposes within fifteen miles. But it is only to the geologist that this place can have any permanent attractions. He can wind his way through the wonderful caflons among some of the grandest ruins in the world. Indeed, it resembles a gigantic city fallen to decay. Domes, towers, minarets, and spires may be seen on every side, which assume a great variety of shapes when viewed in the distance. Not unfrequently, the rising or the setting sun will light up these grand old ruins with a wild, strange beauty, reminding one of a city illumi- nated in the night when seen from some high point. The harder layers project from the sides of the valley or cation with such regularity that they appear like seats, one above the other, of some vast amphitheatre. THE FOSSIL TEBASUEES OF THE LAKE-BASINS. It is at the foot of these apparent architectural ruins that the curious, fossil treasures are found. In the oldest beds we find the teeth and jaws of a hyopotamus, a river-horse much like the hippopotamus, who must have sported in his pride in the marshes that bordered this lake. So, too, the titanotherium, a gigantic pachyderm, was associated with a species of hornless rhinoceros. These huge rhinoceroid animals appear at first to have monopolized this entire region, and the plastic, sticky clay of the lowest bed of this basin, in which the remains were found, seems to have formed a suitable bottom to the; lake in which these thick- skinned monsters could wallow at pleasure. As we pass higher up in the sediments, we find the remains of a great variety of land animals mingled with those that were aquatic in their nature. In a bed of flesh- colored marl which is visible for a great distance, like a broad band in the sides of these washed hills, thousands of turtles- were imbedded, and are preserved to the present time with surprising perfection, the hard portions of them being as complete as when they were swimming about 44 THE GREAT WEST. ill these Tertiary waters hundreds of thousands of years ago. They vary in size from an inch or two across the back to three or four feet. But one species has ever been discovered in this basin, and so far as we know these reptiles made up in numbers what they lacked in variety. Associated with the remains of the turtles are those of a number of ruminants, all belonging to extinct genera, and possessing peculiar cha- racters which ally them to the deer and. the hog. Indeed, Dr. Leidy calls them ruminating hogs. Like the domestic species, they were pro- vided with cutting teeth and canines, but the grinding teeth are con- structed after the same pattern as those of all living ruminants. The feet of these animals were also provided with four toes as in the hog, and none of them possessed horns or antlers. They appear to have existed in immense numbers, and to have lived in great herds like the bisons of the West. Remains of more than seven hundred individuals of one species have been already studied and described by Dr. Leidy. Their enemies were numerous — ^wolves, hyaenodons, and sabre-tooth tigers. If we pass for a moment southward into the valleys of the Niobrara and Loup Fork, we shall find a fauna closely allied, yet entirely distinct from the one on White River, and plainly intermediate between that of the latter and of the present period ; one appears to have lived during the Middle or Miocene Tertiary period, and the other at a later time, in what is called the Pliocene. In the later fauna were the remains of a number of species of extinct camels, one of which was of the size of the Arabian camel, a second about two-thirds as large ; also a smaller one. The only animals akin to the camels at the present time in the Western hemisphere are the llama and its allies in South America. Not less in- teresting are the remains of a great variety of forms of the horse family, one of which was about as large as the ordinary domestic animal, and the smallest not more than two or two and a half feet in height, with every intermediate grade in size. There was still another animal allied to the horse, about the size of a Newfoundland dog, which was provided with three hoofs to each foot, though the lateral hoofs were rudimental. Although no horses were known to exist on this continent prior to its discovery by Europeans, yet Dr. Leidy has shown that before the age of man this was emphatically the country of horses. Dr. Leidy has re- ported twenty-seven species of the horse family which are known to have lived on this continent prior to the advent of man — about three times as many as are now found living throughout the world. Among the carnivores were several foxes and wolves, one of which was larger than any now living ; three species of hyanodon — animals whose THE GREAT WEST. 45 teeth indicate that they were of remarkably rapacious habits ; also five animals of the cat tribe were found, one about the size of a small panther and another as large as the largest wolf. Several of the skulls of the tiger-like animals exhibited the marks of terrible conflicts with the con- temporary hysenodons. Among the rodents were a porcupine, small beaver, rabbit, mouse, etc. The pachyderms, or thick-skinned animals, were quite numerous and of great interest, from the fact that none of them are living on this continent at the present time, and yet here we find the remains of sev- eral animals allied to the domestic hog — one about the size of this animal, another as large as the African hippopotamus, and a third not much larger than the domestic cat. Five species of the rhinoceros roamed through these marshes, ranging from a small, hornless species, about the size of our black bear, to the largest, which was about the size of the existing unicorn of India. No animals of the kind now inhabit the "Western hemisphere. Among the thick-skinned animals were the remains of a mastodon and a large elephant, distinct from any others heretofore discovered in any part of the world. Dr. Leidy says that "it is remarkable that among the remains of mammals and turtles there are none of crocodiles. Where were these creatures when the shores of the ancient Dakotan and Nebraskan waters teemed with such an abundant provision of sa- vory ruminating hogs?" During the Tertiary period Nebraska and Dakota were the homes of a race of animals more closely allied to those inhabiting Asia and Africa now, and from their character we may sup- pose that during that period the climate was considerably warmer than it is at present. The inference is also drawn that our world, which is usually called the New, is in reality the Old World, older than the East- ern hemisphere. THE PEE-HISTOEIC GEOGEAPHY OF THE LAKE-BASINS. Ever since the commencement of creation constant changes of form have been going on in our earth. Oceans and mountains have disap- peared, and others have taken their place. Entire groups of animal and vegetable life have passed away, and new forms have come into exist- ence through a series of years which no finite mind can number. To enable the mind to realize the physical condition of our planet during all these past ages is the highest end to be attained by the study of geological facts. It has been well said by an eloquent historian that he who calls the past back again into being enjoys a bliss like that of creating. 46 THE GREAT WEST. We may attempt to form some idea of the physical geography of this region at the time when these animals wandered over the country, and to speculate as to the manner in which their remains have been so beau- tifully preserved for our examination. We may suppose that here was a large fresh-water lake during the Middle Tertiary period ; that it began near the south-eastern side of the Black Hills, not large at first, nor deep, but as a marsh or mud-wallow for the gigantic pachyderms that lived at the time — that as time passed on it became deeper and expanded its limits until it covered the vast area which its sediments indicate. We cannot attempt to point out in detail all the changes through which we may suppose, from the facts given us, this lake has passed during the thousands of years that elapsed from its beginning to its extinction — time long enough for two distinct faunse to have commenced their existence and passed away in succession, not a single species passing from one into the other. Even that small fraction of geological time seems in- finite to a finite mind. We believe that the great range of mountains that now lies to the west of this basin was not as lofty as now — ^that doubtless the treeless plains were covered with forests or grassy meadows upon which the vast herds of gregarious ruminants cropped their food. Into this great lake on every side poured many little streams from broad valleys, fine ranging-ground for the numerous varieties of creatures that existed at that time. Large numbers of fierce carnivorous beasts mingled with the multitudes of gregarious ruminants, constantly devour- ing them as food. As many of the bones, either through death by vio- lence or natural causes, were left in the valleys, they would be swept down by the first high waters into the lake and enveloped in the sedi- ments at the bottom. As the gregarious ruminants came down to the little streams or by the shores of the lake to quench their thirst, they would be pounced upon by the flesh-loving hysenodon, drepanodon, or dinictis. It was probably near this place also that these animals would meet in fierce conflicts, the evidences of which remain to the present time in the cavities which the skulls reveal ; one of these, of a huge cat, shows on either side the holes through the bony covering which had partially healed before the animal perished, and the cavities seem to correspond in form and position with the teeth of the largest hy- asnodon. The remains of those animals which, from their very nature, could not have existed in great numbers, are not abundant in the fossil state, while those of the ruminants occur in the greatest abundance and are widely diffused in the sediments, not only geographically, but vertically. THE GREAT WEST. 47 The chances for the preservation of the remains of a species seem to depend upon the number of individuals that existed. The remains of ruminants already obtained comprise at least nine-tenths of the entire collection, while of one species portions of at least seven hundred indi- viduals have been discovered. We might take examples from the ani- mals that exist in this region at the present time that would illustrate the point. The wolves watch the deer, antelope, and other feebler ani- mals as they go down to the little streams for water, and all over the wide bottoms their skeletons are distributed in a more or less perfect condition. Whenever a bison becomes too feeble by disease or age to offer a successful resistance, the wolves soon despatch him and his bones are left bleaching on the ground. In most cases these animals when pursued betake themselves to the water, where they are not unfrequent- ly drowned or despatched on a sand-bar or island; Annually, thousands of buffaloes, in attempting to cross the Missouri River and some of its large tributaries on the ice as it is breaking up in the spring, are drowned. For many days their bodies are seen floating down the river by Fort Union or Fort Clark, and, lodging on some of the islands or sand-bars, fill the air with the stench of their decay. In the spring of 1857 thousands of their bodies floated down the Kansas River past Fort Riley, and were carried into the Missouri River. These animals are often mired in the marshes or the muddy shores of lakes or streams in great numbers. We know what vast numbers of the naastodon have been preserved in the Big Bone Licks of Kentucky, and of the Irish elk in the bogs of Ireland. We might instance hundreds of examples to show how easily these animals, roaming and feeding along the numerous streams flowing into some great lake, could be transported in part or entire into the lake, and sinking to the bottom would be enveloped in the muddy sediments. There is another interesting feature in regard to these remarkable fossils, and that is the beauty and perfection of their preservation ; the bones are so clean and white and the teeth so perfect that, when ex- posed upon the surface, they present the appearance of having bleached only for a season. They could not havp been transported from a great distance, neither could the waters have been swift and turbulent, for the bones seldom show any signs of having been water-worn, and the nice sharp points and angles are as perfect as in life. I have dwelt thus long on the details of this great lake-basin not only on account of the universal interest that invests it, and the wonderful treasures of the past which it has revealed to the world, but because its history is applicable 48 THE GREAT WEST. in the main to the numbers of the other fresh-water lake-basins of the geological past which are distributed throughout the Eocky Mountain region. Before leaving thig subject there is another interesting topic of in- quiry — why such a beautiful series of vertebrate remains should be so perfectly preserved in this lake-deposit, and yet the remains of other forms of animal and vegetable life be almost entirely absent. The sedi- ments seem to be peculiarly adapted to the preservation of a full series of documents bearing upon the history of those times. And yet in the older beds, where the mammalian remains are most abundant, only one small species of snail, a land-shell, is found preserved. Where is the evidence of the swarms of fishes that must have filled the streams and lakes of that time ? Of the vegetable life, if any existed, only now and then a fragment of silicified wood is found, and that, too, in the latest deposits. I am prepared to believe that the broad plains were, even at the time of the existence of these animals, as treeless as at present, yet I am quite unprepared to explain the almost entire absence of vegetable remains. We know that fresh-water shells, much like those existing in the little clear streams of the present time, as well as some remains of fishes, are found in some limestones on the summits of hills near Pinos Spring on the northern rim of the lake. Another interesting question occurs to me in this connection : How was it that a complete fauna, comprising more than forty species of animals, was introduced upon the earth, lived through its legitimate period, entirely perished or was swept out of existence, and an entirely new fauna, com- prising about the same number and variety, was again introduced in the same region ? It too lived out its period of existence, which must have been hundreds of thousands of years, and yet every one of this group of animals disappeared from the globe, leaving nothing behind to tell the tale but fragments of their bony skeletons accidentally enveloped in the sediment at the bottom of an estuary or lake. It will be seen at a glance that this is a fruitful topic for speculation, and I leave it with the reader. Some of the species of animals found in the latest deposits seem to have lived very nearly up to our present period. The horns of a deer and the bones of a sand-hill crane have such a modern aspect that the thought arises. Where was man when these animals were roaming over this region ? Eecent investigations show quite conclusively that man was an inhabitant of Europe contemporaneously with many of the extinct animals of the Quaternary period, but it is doubtful whether we have ever found any evidence that he lived at a very remote period THE GREAT WEST. 49 on this continent. Indeed, so far as we know at present, the West is singularly silent as to the existence of man in what are now understood as pre-historic times. NORTH AMERICA IN THE TERTIARY AGE. . The following picture of North America during the Tertiary age is drawn by Professor Newberry in Hayden's Annual Report for 1870 : " Then a warm and genial climate prevailed from the Gulf to the Arctic Sea ; the Canadian highlands were higher, but the Eocky Mountains lower and less broad. Most of the continent exhibited an undulating surface — rounded hills and broad valleys covered with forests grander than any of the present day, or wide expanses of rich savannah, over which roamed countless herds of animals, many of gigantic size, of which our present meagre fauna retains but a few dwarfed representatives. Noble rivers flowed through plains and valleys, and sea-like lakes, broader and more numerous than those the continent now bears, diversified the scenery. Through unnumbered ages the seasons ran their ceaseless course, the sun rose and set, moons waxed and waned over this fair land, but no human eye was there to mark its beauty nor human intellect to control and use its exuberant fertility. Flowers opened their many-colored petals on meadow and hillside, and filled the air with their perfumes, but only for the delectation of the wandering bee. Fruits ripened in the sun, but there was no hand there to pluck nor any speaking tongue to taste. Birds sang in the trees, but for no ears but their own. The surface of lake or river was whitened by no sail, nor furrowed by any prow but the breast of the water-fowl ; and the far-reaching shores echoed no sound but the dash of the waves and the lowing of the herds that slaked their thirst in the crystal waters. " Life and beauty were everywhere, and man, the great destroyer, had not yet come ; but not all was peace and harmony in this Arcadia. The forces of Nature are always at war, and redundant life compels abundant death. The innumerable species of animals and plants had each its he- reditary enemy, and the struggle of life was so sharp and bitter that in the lapse of ages many genera and species were blotted out for ever. " The herds of herbivores — which included all the genera now liviag on the earth's surface, with many strange forms long since extinct — ^formed the prey of carnivores commensurate to these in power and numbers. The coo of the dove and the whistle of the quail were answered by the scream of the eagle, and the lowing of herds and the bleating of flocks come to the ear of the imagination mingled with the roar of the lion, the howl of 50 THE GREAT WEST. the wolf, and the despairing cry of the victim. Yielding to the slow- acting but irresistible forces of Nature, each in succession of these various animal forms has disappeared, till all have passed away or been changed to their modem representatives, while the country they inhabited, by the upheaval of its mountains, the deepening of its valleys, the filling and draining of its great lakes, has become what it is." ANCIENT LIFE IN THE PAK WEST DURING THE CEBTACEOUS EPOCH. In the following sketch the ancient life in the far West during the Cretaceous period has been most eloquently described by the eminent palaeontologist, Prof. E. D. Cope, in the Anmial Report of the Geological Survey of the Territories for 1871 : " That vast level tract of our territory lying between Missouri and the Rocky Mountains represents a condition of the earth's surface which has preceded, in most instances, the mountainous or hilly type so prevalent elsewhere, and may be called, in so far, incompletely developed. It does not present the variety of conditions, either of surface for the support of a very varied life or of opportunities for access to its interior treasures, so beneficial to a high civilization. It is, in fact, the old bed of seas and lakes, which has been so gradually elevated as to have sufiered little dis- turbance. Consistently with its level surface, its soils have not been carried away by rain and flood, but rather cover it with a deep and widespread mantle. This is the great source of its wealth in Nature's creations of vegetable and animal life, and from it will be drawn the wealth of its future inhabitants. On this account its products have a character of uniformity ; but viewed from the standpoint of the political philosopher, so long as peace and steam bind the natural sections of our country together, so long will the plains be one important element in a varied economy of continental extent. But they are not entirely unin- terrupted. The natural drainage has worn channels, and the streams flow below the general level. • The ancient sea- and lake-deposits have neither been pressed into very hard rock beneath piles of later sediment, nor have they been roasted and crystallized by internal heat. Although limestone rock, tJiey easily yield to the action of water, and so the side-drainage into the creeks and rivers has removed their high banks from many rods to many miles from their original positions. In many cases these banks or bluffs have retained their original steepness, and have increased in eleva- tion as the breaking down of the rock encroached on higher land. In other cases the rain-channels have cut in without removing the interven- ing rocks at once, and formed deep gorges or canons, which sometimes THE GREAT WEST. 51 extend to great distances. They frequently communicate in every direc- tion, forming curious labyrinths, and when the intervening masses are cut away at various levels or left standing like monuments, we have the characteristic peculiarities of ' bad lands,' or mauvaises terres. " In portions of Kansas tracts of this kind are scattered over the coun- try along the margins of the river and creek valleys and ravines. The upper stratum of the rock is a yellow chalk, the lower bluish, and the brilliancy of the color increases the picturesque effect. From elevated points the plains appear to be dotted with ruined villages and towns, whose avenues are lined with painted walls of fortifications, churches, and towers, while side-alleys pass beneath natural bridges or expand into small pockets and caverns, smoothed by the action of the wind carrying hard mineral particles. But this is the least interesting of the peculiar- ities presented by these rocks. On the level surfaces, denuded of soil, lie huge oyster-like shells, some opened and others with both valves together, like remnants of a half-finished meal of some titanic race which had been frightened from the board never to return. These shells are not thick- ened like most of those of past periods, but contained an animal which would have served as a meal for a large party of men. One of them measured twenty-six inches across. " If the explorer searches the bottoms of the rain-washes and ravines, he will doubtless come upon the fragment of a tooth or jaw, and will generally find a line of such pieces leading to an elevated position on the bank or bluff, where lies the skeleton of some monster of the ancient sea. He may find the vertebral column running far into the limestone that locks him in his last prison ; or a paddle extended on the slope, as though entreating aid ; or a pair of jaws lined with horrid teeth, which grin despair on enemies they are helpless to resist; or he may find a conic mound on whose apex glisten in the sun the bleached bones of one whose last office has been to preserve from destruction the friendly soil on which he reposed. Sometimes a pile of huge remains will be discov- ered, which the dissolution of the rock has deposited on the lower level, the force of rain and wash having been insufiicient to carry themi away. " But the reader inquires, What is the nature of these creatures thus left stranded a thousand miles from either ocean ? How came they in the limestones of Kansas, and were they denizens of land or sea ? It may be replied that our knowledge of this chapter of ancient* history is only about five years old, and has been brought to light by geological explora- tions set on foot by Dr. Turner, Professor Mudge, Professor Marsh, 52 THE GREAT WEST. W. E. Webb, and the writer. Careful examinations of the remains dis- covered show that they are nearly all to be referred to the reptiles and fishes. We find that they lived in the period called Cretaceous, at the time when the chalk of England and the green-sand marl of New Jer- sey were being deposited, and when many other huge reptiles and fishes peopled both sea and land in those quarters of the globe. The twenty- four species of reptiles found in Kansas up to the present time varied from ten to eighty feet in length, and represented six orders, the same that occur in the other regions mentioned. Two only of the number were terrestrial in their habits, and two were flyers ; the remainder were inhabitants of the salt ocean. When they swam over what are now the plains, the coast-line extended from Arkansas to near Fort Eiley on the Kansas Kiver, and, passing a little eastward, traversed Minnesota to the British possessions, near the head of Lake Superior. The extent of sea to the westward was vast, and geology has not yet laid down its bound- ary ; it was probably a shore now submerged beneath the waters of the North Pacific Ocean. " Far out on this expanse might have been seen in those ancient days a huge, snake-like form which rose above the surface and stood erect, with tapering throat and arrow-shaped head, or swayed about, describing a circle of twenty feet radius above the water. Then it would dive into the depths, and naught would be visible but the foam caused by the dis- appearing mass of life. Should several have appeared together, we can easily imagine tall, twining forms rising to the height of the masts of a fishing-fleet, or like snakes twisting and knotting themselves together. This extraordinary neck — for such it was — rose from a body of elephan- tine proportions, and a tail of the serpent-pattern balanced it behind. The limbs were probably two pairs of paddles like those of Plesiosawims, from which this diver chiefly differed in the arrangement of the bones of the breast. In the best-known species twenty-two feet represent the neck in a total length of fifty feet. " This is the Elasmosaurm platyurus (Cope), a carnivorous sea-reptile, no doubt adapted for deeper waters than many of the others. Like the snake-bird of Florida, it probably often swam many feet below the sur- face, raising the head to the distant air for a breath, then withdrawing it and exploring the depths forty feet below, without altering the position of its body. From the localities in which the bones have been found in Kansas, it must have wandered far from land, and that many kinds of fishes formed its food is shown by the teeth and scales found in the posi- tion of its stomach. THE GREAT WEST. 53 "A second species of somewhat similar character and habits differed 'very much in some points of structure. The neck was drawn out to a wonderful degree of attenuation, while the tail was relatively very stout — more so, indeed, than in the Elasmosaurus — as though to balance the anterior regions while occupied in various actions ; e. g., while capturing its food. This was a powerful swimmer, its paddles measuring four feet in length, with an expanse therefore of about eleven feet. It is known as Polycotylus latipinnis (Cope). " The two species just described formed a small representation in our great interior sea of an order which swarmed, at the same time or near it, over the gulfs and bays of old Europe. There they abounded twenty to one. Perhaps one reason for this was the almost entire absence of the real rulers of the waters of ancient America — viz. the Pythonomorphs. These sea-serpents — for such they were — embrace more than half the species found in the limestone rocks in Kansas, and abound in those of New Jersey and Alabama. Only four have been seen as yet in Europe. " Researches into their structure have shown that they were of won- derful elongation of form, especially of tail ; that their heads were large, flat, and conic, with ' eyes directed partly upward ; that they were fur- nished with two pairs of paddles like the flippers of a whale, but with short or no portion representing the arm. With these flippers and the ell-like strokes of their flattened tail they swam, some with less, others with greater speed. They were furnished, like snakes, with four rows of formidable teeth on the roof of the mouth. Though these were not designed for mastication, and, without paws for grasping, could have been little used for cutting, as weapons for seizing their prey they were very formidable. And here we have to consider a peculiarity of these creatures in which they are unique among animals. Swallowing their prey entire like snakes, they were without that wonderful expansibility of throat due in the latter to an arrangement of levers supporting the lower jaw. Instead of this, each half of that jaw was articulated or jointed at a point nearly midway between the ear and the chin. This was of the ball-and-socket type, and enabled the jaw to make an angle outward, and so widen by much the space enclosed between it and its fellow. The arrangement may be easily imitated by directing the arms forward, with the elbows turned outward and the hands placed near together. The ends of these bones were in' the Pythonomorpha as inde- pendent as in the serpents, being only bound by flexible ligaments. By turning the elbows outward and bending them, the space between the arms becomes diamond-shaped, and represents exactly the expansion 54 THE GREAT WEST. seen in these reptiles to permit the passage of a large fish or other body. The arms, too, will represent the size of jaws attained by some of the smaller species. The outward movement of the basal half of the jaw necessarily twists in the same "direction the column-like bone to which it is suspended. The peculiar shape of the joint by which the last bone is attached to the skull depends on the degree of twist to be permitted, and therefore to the degree of expansion of which the jaws were capable. As this differs much in the different species, they are readily distinguish- ed by the column or 'quadrate' bone when found. There are some curious consequences of this structure, and they are here explained as an instance of the mode of reconstruction of extinct animals from slight materials. The habit of swallowing large bodies between the branches of the under jaw necessitates the prolongation forward of the mouth of the gullet ; hence the throat in the Pythmiomorpha must have been loose and almost as baggy as a pelican's. Next, the same habit must have compelled the forward position of the glottis or opening of the wind- pipe, which is always in front of the gullet. Hence these creatures must have uttered no other sound than a hiss, as do animals of the present day which have a similar structure ; as, for instance, the snakes. Third- ly, the tongue must have been long and forked, and for this reason : its position was still anterior to the glottis, so that there was no 'space for it except it were enclosed in a sheath beneath the windpipe when at rest, or thrown out beyond the jaws when in motion. Such is the arrange- ment in the nearest living forms, and it is always in these cases cylindric and forked. " The giants of the Pytlionomorpha of Kansas have been called Liodon proriger (Cope) and Liodon dyspelor (Cope). The first must have been abundant, and its length could not have been far from fifty feet ; certainly not less. Its physiognomy was rendered peculiar by a long projecting muzzle, reminding one of that of the blunt-nosed sturgeon of our coast ; but the resemblance was destroyed by the correspondingly massive end of the branches of the lower jaw. Though clumsy in appearance, such an arrangement must have been effective as a ram, and dangerous to its enemies in case of collision. The writer once found the wreck of an individual of this species strewn around a sunny knoll beside a bluff, and his conic snout pointing to the heavens formed a fitting monument, as at once his favorite weapon and the mark distinguishing all his race. " Very different was the Liodon dyspelor, a still larger animal than the last, with a formidable armature. It was, indeed, the longest of known reptiles, and probably equal to the great finner-whales of modern oceans. THE GREAT WEST. 55 The circumstances attending the discovery of one of these will always be a pleasant recollection to the writer. A part of the face, with teeth, was observed projecting from the side of a bluff by a companion in ex- ploration, Lieutenant James H. Whitten, United States army, and we at once proceeded to follow up the indication with knives and picks. Soon the lower jaws were uncovered, with their glistening teeth, and then the vertebrae and ribs. Our delight was at its height when the bones of the pelvis and part of the hind limb were laid bare, for they had never been seen before in the species and scarcely in the order. While lying on the bottom of the Cretaceous sea the carcass had been dragged hither and thither by the sharks and other rapacious animals, and the parts of the skeleton were displaced and gathered into a small area. The massive tail stretched away into the bluff, and after much laborious excavation we left a portion of it to more persevering explorers. "The species of Clidastes did not reach such a size as some of the Idodons, and were of elegant and flexible build. To prevent their habits of coiling from dislocating the vertebral column, these had an additional pair of articulations at each end, while their muscular strength is attested by the elegant striae and other sculptures which appear on all their bones. Five species of this genus occur in the Kansas strata, the largest {Cli- dastes cineriarwm, Cope) reaching forty feet in length. The discovery of a related species {Hohodus coryphaeus, Cope) was made by the writer under circumstances of difficulty peculiar to the plains. After examining the bluffs for half a day without result, a few bone fragments were found in a wash above their base. Others led the way to a ledge forty or fifty feet from both summit and foot, where, stretched along in the yellow chalk, lay the projecting portions of the whole monster. A considerable number of vertebrae were found preserved by the protective embrace of the roots of a small bush, and when they were secured the-pick and knife were brought into requisition to remove the remainder. About this time one of the gales so common in that region sprang up, and, striking the bluff fairly, reflected itself upward. So soon as the pick pulverized the rock, the limestone dust was carried into eyes, nose, and every available opening in the clothing. I was speedily blinded, and my aid disappeared in the cafion, and was seen no more while the work lasted. Only the enthusiasm of the student could have endured the discomfort, but to him it appeared a most unnecessary 'conversion of force' that a geologist should be driven from the field by his own dust. A handkerchief tied over the face, and pierced by minute holes opposite the eyes, kept me from total blindness, though dirt in abundance penetrated the mask. But a 56 THE GREAT WEST. fine relic of creative genius was extricated from its ancient bed, and one that leads its genus in size and explains its structure. " On another occasion, riding along a spur of yellow-chalk bluff, some vertebrae lying at its foot met my eye. An examination showed that the series entered the rock, and, on passing round to the opposite side, the jaws and muzzle were seen projecting from it, as though laid bare for the convenience of the geologist. The spur was small and of soft material, and we speedily removed it in blocks to the level of the rep- tile, and took out the remains as they lay across the base from side to side. " A genus related to the last is Edestosaurus. A species of thirty feet in length, and of elegant proportions, has been called U. tortor (Cope). Its slenderness of body was remarkable, and the large head was long and lance-shaped. Its flippers tapered elegantly, and the whole ani- mal was more of serpent than any other of its tribe. Its lithe move- ments brought m,any a fish to its knife-shaped teeth, which are more efficient and numerous than in any of its relatives. It was found coiled up beneath a ledge of rock, with its skull lying undisturbed in the centre. A species distinguished for its small size and elegance is Clidastes pumilus (Marsh). This little fellow was only twelve feet in length, and was prob- ably unable to avoid occasionally furnishing a meal for some of the rapa- cious fishes which abounded in the same ocean. " The flying saurians are pretty well known from the descriptions of European authors. Our Mesozoic periods had been thought to have lacked these singular forms until Professor Marsh and the writer discovered re- mains of species in the Kansas chalk. Though these are not numerous, their size was formidable. One of them, Ornithoohirus harpyia (Cope) spread eighteen feet between the tips of its wings, while the 0. umbrosus (Cope) covered nearly twenty-five feet with his expanse. These strange creatures flapped their leathery wings over the waves, and, often plunging, seized many an unsuspecting fish, or, soaring at a safe distance, viewed the sports and combats of the more powerful saurians of the sea. At nightfall we may imagine them trooping to the shore and suspending themselves to the cliffs by the claw-bearing fingers of their wing-limbs. " Tortoises were the boatmen of the Cretaceous waters of the Eastern coast, but none had been known from the deposits of Kansas until very recently. But two species are on record ; one, large and strange enough to excite the attention of naturalists, is the Protostega gigas (Cope). It is well known that the house or boat of the tortoise or turtle is formed by the expansion of the usual bones of the skeleton till they meet and unite, THE GREAT WEST. 57 and thus become continuous. Thus the lower shell is formed of united ribs of the breast and of the breast-bone, with bone deposited in the skin. In the same way the roof is formed by the union of the ribs with bone deposited in the skin. In the very young tortoise the ribs are separate, as in other animals ; as they grow older they begin to expand at the upper side of the upper end, and with increased age the expansion extends throughout the length. The ribs first come in contact where the process commences, and in the land-tortoise they are united to the end. In the sea-turtle the union ceases a little above the ends. The fragments of the Protostega were seen by one of my party projecting from the ledge of a low bluff. Their thinness and the distance to whicji they were traced excited my curiosity, and I straightway attacked the bank with the pick. After several square feet of rock had been removed, we cleared up one floor, and found ourselves well repaid. Many long, slender pieces of two inches in width lay lipon the ledge. They were evidently ribs with the usual heads, but behind each head was a plate like the flattened bowl of a huge spoon, placed crosswise. Beneath these stretched two broad plates, two feet in width and no thicker than binder's board. The edges were fingered, and the surface hard and smooth. All this was quite new among full-grown animals, and we at once determined that more ground must be explored for further light. After picking away the bank and carving the soft rock, new masses of strange bones were disclosed. Some bones of a large paddle were recognized, and a leg-bone. The shoulder-blade of a huge tortoise came next, and further examination showed that we had stumbled on the burial-place of the largest species of sea-turtle yet known. The single bones of the paddle were eight inches long, giving the spread of the ex- panded flippers as considerably over fifteen feet. But the ribs were those of an ordinary turtle just born, and the great plates represented the bony deposit in the skin, which, commencing independently in modern turtles, unite with each other below at an early day. But it was incredible that the largest of known turtles should be but just hatched, and for this and other reasons it has been concluded that this 'ancieat mariner' is one of those forms not uncommon in old days, whose incompleteness in some respects points to the truth of the belief that animals have assumed their modern perfections by a process of growth from more simple beginnings. " The Cretaceous ocean of the West was no less remarkable for its fishes than for its reptiles. Sharks do not seem to have been so common as in the old Atlantic, but it swarmed with large predaceous forms related to the salmon and saury. " Vertebrae and other fragments of these species project from the worn 58 THE GREAT WEST. limestone in many places, I will call attention to perhaps the most for- midable as well as the most abundant of these. It is the one whose bones most frequently crowned knobs of shale which had been left standing amid surrounding destruction. The density and hardness of the bones shed the rain off on either side, so that the radiating gutters and ravines finally isolated the rock-mass from that surrounding. The head was as long as, or longer than, that of a fully-grown grizzly bear, and the jaws were deeper in proportion to their length. The muzzle was shorter and deeper than that of a bull-dog. The teeth were all sharp cylindric fangs, smooth and glistening, and of irregular size. At certain distances in each jaw they projected three inches above the gum, and were sunk one inch into the jaw-margin, being thus as long as the fangs of a tiger, but more slender. Two such fangs crossed each other on each side of the middle of the front. This fish is known as Porthetcs molossus (Cope). Besides the smaller fishes, the reptiles no doubt supplied the demands of his appetite. " The ocean in which flourished this abundant and vigorous life was at last completely enclosed on" the west by elevations of sea-bottom, so that it only communicated with the Atlantic and Pacific at the Gulf of Mex- ico and the Arctic Sea. The continued elevation of both eastern and western shores contracted its area, and when ridges of the sea-bottom reached the surface, forming long, low bars, parts of the water-area were enclosed and connection with salt water prevented. Thus were the living beings imprisoned and subjected to many new risks tc life. The stronger could more readily capture the weaker, while the fishes would gradually perish through the constant freshening of the water. With the death of any considerable class the balance of food-supply would be lost, and many larger species would disappear from the scene. The most omnivorous and enduring would longest resist the approach of starvation, but would finally yield to inexorable fate ; the last one caught by the shifting bottom among shallow pools, from which his exhausted energies could not extricate him." SNAKE EIVEE. The Snake or Lewis Fork of the Columbia heads in the Yellowstone National Park, opposite the heads of the Madison and Yellowstone Rivers. Its sources are in beautiful lakes embosomed in heavily-wooded hills. Flowing southward, it soon enters a mountainous country, from which it receives several large tributaries — Barlow's Fork, Buffalo Fork, Gros Ventre Creek, and Hoback Eiver. It washes the east base of the Teton Range, which rears its rugged Gothic spires seven thousand feet above its valley. Turning to the west, the river cuts across the mountains which THE GREAT WEST. 59 seek to check its course in a terrific gorge wellnigh impassable. On the west side of these mountains it enters upon a great field of basalt, a great volcanic plain covered with drifting sand and seamed with crevasses like those of a glacier. This is known as the Snake River Plain. It crosses this plain by a southerly course, then gradually sweeping around to the westward, it hugs the southern border of this basalt field as far as longi- tude 117°, when it turns northward, then for a short distance westward again to its junction with Clark's Fork, making the mighty Columbia. In its course across and around the basalt plain it is rapid and tumult- uous, boiling and seething along, its bed broken by boulders and ledges. In several places there are noteworthy falls. The upper of these is the American Fall, at a point a few miles below the mouth of the Portneuf, where the " Mad " River — as it was called in early days — ^leaps over a wall of basalt. Farther down is the Shoshone Fall, by far the greatest and finest on the river. This fall was visited in October, 1868, by Mr. Clarence King, and I quote his fine description of it : " The wall of the gorge opposite us, like the cliff at our feet, sank in perpendicular bluffs nearly to the level of the river. A horizon as level as the sea ; a circling wall, whose sharp edges were here and there battle- mented in huge fortress-like masses ; a broad river, smooth and unruffled, flowing quietly into the middle of the scene, and then plunging into a labyrinth of rocks, tumbling over a precipice two hundred feet high, and flowing westward in a still deep current to disappear behind a black promontory Dead barrenness is the whole sentiment of the scene "In plan the fall recurves up-stream in a deep horseshoe, resembling the outline of Niagara. The total breadth is about seven hundred feet, and the greatest height of a single fall about one hundred and ninety. .... The whole mass of the fall is one ever-varying sheet of spray. In the early spring, when swollen by the rapidly-melted snows, the river pours over with something of the volume of Niagara There are no rocks at the base of the fall. The sheet of foam plunges almost ver- tically into a dark, beryl-green lake-like expanse of the river. Immense volilmes of foam roll up from the cataract-base, and, whirling about in the eddying winds, rise often one thousand feet into the air The incessant roar, reinforced by a thousand echoes, fills the cafion." HIGH MOTJNTAICf-PEAKS. Southward from the Wind River chain the mountainous character of the Divide or continental watershed is interrupted for a short distance by 60 THE GREAT WEST. comparatively level plateaus, while to the east are the Laramie Plains, bounded by a comparatively low range, of which Laramie Peak is about ten thousand feet high, and, on account of its isolation and the insignificance of the mountains in the vicinity, is one of the great landmarks of the West. Still farther south, are the remarkable mountain-regions and the parks of Colorado. The Colorado or Front Range rises up before the traveller on the plains like a gigantic wall, with Long's Peak at the north and Pike's Peak at the south as high bastions. West of this range are three great depressions, North, Middle, and South Parks. In the Front Range are several peaks over fourteen thousand two hundred feet high (according to the latest surveys) — Long's, 14,271 feet; Evans's, 14,330 feet ; and Gray's and Torrey's, -twin-peaks, with an interval of less than a mile, 14,341 and 14,336 feet. In this range are the oldest known silver- and gold-mines in Colorado. On the west side of the parks is the Park range, in which are several peaks of over thirteen thousand feet, and a few, as Mount Lincoln, of over fourteen thousand feet. From Mount Lincoln one can look down into the valley of the upper Arkansas River and across to the Sawatch range, one of the most remarkable in the West. At its north end is the Holy Cross group, in latitude 39° 30' and longitude 106° 33', composed of gneiss and coarse massive granite. For eighty miles to the southward this range literally bristles with peaks, many of which rise over fourteen thousand feet. Harvard, Yale, and Princeton are respectively 14,384, 14,150, 14,199 feet, and many others are over thirteen thousand feet. The rocky mass is mostly granite, inter- sected with igneous dikes. The general trend of this range is about 20° west of north, and it forms one of the most gigantic anticlinals in the entire Rocky Mountain region. Vast ranges of massive granitic rock, capped with limestone and sandstone, incline from either side, with broad valleys intervening. The proofs of ancient glacial action on both sides of the range are wonderful. In the valley of Roches Moutonnfies Creek, which flows into Eagle River from its north-east base, are very remark- able rounded masses of granite. Such have long been called in Swiss geology sheep-backs, or roches moutonnies. Here they are shown on a grand scale. In the valley of the Arkansas or the Gunnison are marvellous examples of lateral and terminal moraines, and there are numerous lakes whose basins have been scooped out by some extended glacial action. The Twin Lakes are beautiful sheets of water on the east side of the Sawatch range, from two to three miles in diameter and about eighty feet deep. These are two glacial lakes. The proofs of glacial action are common throughout the Rocky Mountain region, but THE GREAT WEST. 61 they are nowhere shown to a more marked extent east of the Sierra Ne- vadas than in the Sawatch range. From the west side of this range flow the Gunnison River and the southern branches of the Grand, which, after cutting deep caflons or gorges, unite near the western boundary of Colo- rado ; and, cutting a still deeper cafion, the stream flows into the great Colorado of the "West. West of the Sawatch or great " Mother " (Madre) range is another remarkable group in the drainage that leads to the great Colorado, called the Elk range. It is about fifty miles in length, with a trend about north-west and south-east, and differs from any of the others mentioned both in form and structure. In this range are seven peaks of the first order, rising to an elevation of nearly fourteen thousand feet, and many others ranging from twelve to thirteen thousand feet. The geological structure is very peculiar. It appears that the vast thickness of sedimentary strata once rested upon a floor of igneous granite in a pasty or semi-pasty condition, and that these high peaks were thrust up through the overlying beds, in many instances completely overturning them for miles in extent. There are faults two thousand feet in extent, and dikes without number where the igneous material seems to have been squeezed through flssures into thousands of feet of overlying strata, vertically as well as horizontally. Deep gorges and amphitheatres meet the eye on every side. Snow-mass Peak, 13,961 feet high, is so called from the immense mass of perpetual snow on its side. At its immediate base, on all sides, are beautiful lakes, the surface is remarkably rugged, and as far as the eye can reach on every side are high peaks, with deep gorges in one continuous succession, while the sedimentary rocks are thrown into chaos. On the north-west end of the range is a remarkable peak which forms an excellent landmark, known among miners and pros- pectors for years as Sopris Peak, 12,972 feet high. From this point the land slopes off into the remarkable plateau country bordering on the Colorado River, literally gashed, as it were, by the little streams which have cut innumerable canons through it. There is probably no country in the world that presents more obstructions to the traveller. At first glance, the Park range appears to be connected with the Sangre de Cristo range, which bounds the east side of the San Luis Valley ; but the former is separated from the latter by the Arkansas Valley, and really lies parallel with it. It begins in latitude 38° 26' and longitude 106°, trends south 30° east, and shows on its summit a continuous series of sharp peaks. Parallel to it on the east, and. bordering the plains, is the Wet Mountain range. The interval is known as the Wet Mountain Valley and Huerfano Park, one of the most beautiful and fertile districts 62 THE GREAT WEST. « in Colorado. These mountains extend far down into New Mexico. South- ward, the Sierra Blanca and the Spanish Peaks are lofty landmarks. Fort Garland, an old military post in the San Luis Valley, though nearly sur- rounded with high ranges is not a park, but a valley thirty to fifty miles wide, through which the Rio Grande flows after emerging from the San Juan Mountains, cutting a gorge through its basaltic floor one thousand to fifteen hundred feet in depth for sixty to eighty miles. I Immediately west of the upper portion of the San Luis Valley, in South-western Colorado, is a most interesting as well as lofty group of mountains, forming what is now called the San Juan district. These mountains give origin to a great number of streams. On the north are many branches of the Gunnison, on the east the Rio Grande, and on the south and west the various branches of the San Juan, which flow south- west and west, and unite with the Colorado. Within an area of about four thousand square miles is the most important and rugged group of peaks in Colorado, and probably in this portion of the mountain-region of the West. More than one hundred points are above thirteen thousand feet high, and about ten peaks are over fourteen thousand feet. Large areas here are composed entirely of quartzites, and others wholly of igneous rocks. Toward the south, in Southern Colorado and in New Mexico and Arizona, the volcanic action seems to have been very great, and the area covered with igneous rocks increases; sometimes they occupy several thousand square miles to the exclusion of all others. What are called the broad table-lands or mesas of New Mexico are simply floors of basalt. Colorado may be regarded as the culminating area of lofty points in the eastern division of the Rocky Mountain region, as California is in the Sierra Nevada ranges. Within the limits of Colorado are fifty or more points exceeding fourteen thousand feet in height, and more than two hun- dred and fifty of over thirteen thousand feet, while the number reaching thirteen thousand feet is unknown. The average elevation of Colorado State is greater than that of any other State or Territory in the Union, being six thousand six hundred feet, while California, with its magnificent group of peaks in the Sierra Nevada, averages only two thousand eight hundred feet. THE PLATEAU REGION OF THE COLORADO RIVER. — GENERAL VIEW. ' The country drained by the Colorado River is a peculiar region. It is a country of plateaus and cafions, the plateaus mainly arid and sterile, where the new streams flow in deep gorges far below the surface. THE GREAT WEST. 63 The longest and most northern branch of the Colorado is Green Eiver, ■which heads in the Wind River Mountains, against the sources of the Big Horn and the Snake Rivers. This stream, in its long course toward the south, receives the waters of the Uintah from the west and the Yam- pah and White Rivers from the east. Near latitude 38° 15' and longitude 110° it is joined by the Grand River, a stream of nearly equal size, which heaxis in Middle Park, Colorado, drawing its first supplies of water from the snow-fields of Long's Peak. The stream below the junction of these two forks is known as the Colorado. Below their junction the principal branches of the Colorado from the east are the San Juan, the Colorado Chiquito or Flax River, William's Fork, and the Gila; on the west, the Dirty Devil, Paria, and Virgen. This region is limited on the east, north, and north-west by high mountain-ranges. Its surface is nearly flat, but by no means unbroken. There is little rolling or undulating country. Changes of level take place by very gentle uniform slopes or by abrupt precipitous steps. A large part of the surface consists of bare rocks, with no soil or vegeta- tion. A part is covered with a thin sandy soil, which supports a growth of sage and cacti, or even a few pifion pines and cedars. The only veg- etation is that eminently characteristic of an arid country. This aridity has modified orographic forms to an astonishing degree. Where, under different climatic conditions, there would be produced a region similar in most respects to the prairies of the Mississippi Valley, we find a country flat indeed or inclined at low angles, but one whose watercourses are far beneath the general level, deep down in cailons, hundreds, thousands of feet beneath the surface. Great cliffs, thousands of feet in height and extending like huge walls for hundreds of miles, change the level of the country at a single step. Isolated buttes and mesas of great height are scattered over the plateaus, indicating the former height of the plain of which they formed parts. " The landscape everywhere away from the river is of rock — cliffs of rock, tables of rock, plateaus of rock, terraxjes of rock, crags of rock — ten thousand strangely-carved forms. Rocks everywhere, and no vegeta- tion ; no soil ; no land When speaking of these rocks, we must not conceive of piles of boulders or heaps of fragments, but a whole land of naked rock, with giant forms carved on it — cathedral-shaped buttes, towering hundreds or thousands of feet ; cliffs that cannot be scaled ; and caflon-walls that shrink the river into insignificance, with vast hollow domes and tall pinnacles, and shafts set on the verge over- 64 THE GREAT WEST. head, and all highly colored — buff, gray, red, brown, and chocolate; never lichened, never moss-covered, but bare, and often polished." The above description by Major J. W. Powell, who has explored the canons of the Colorado, gives a graphic pen-picture of the lower and more arid plateaus of this region. Nearly every watercourse, whether perennial or not, is a cafloii — a nar- row valley with precipitous walls, often of enormous height. In many cases these caflons are so numerous that they cut the plateau into shreds — a mere skeleton of a country. Of such a section Lieutenant Ives, who explored the course of the Lower Colorado, writes : " The extent and magnitude of the system of canons in that direction is astounding. The plateau is cut into shreds by these gigantic chasms, and resembles a vast ruin. Belts of country miles in width have been swept away, leaving only isolated mountains standing in the gap ; fissures so profound that the eye cannot penetrate their depths are separated by walls whose thick- ness one can almost span, and slender spires that seem tottering on their base shoot up a thousand feet from vaults below." But few of these caflons contain water throughout the year. Most of them are dry at all times excepting for a few days in the early spring or for a few minutes or hours at most after a heavy shower. It is a charac- teristic of Western North America, as of all arid countries, that the streams, away from their sources in the mountains, lose water, rather than gain it, in traversing the lower country. The dry atmosphere and the thirsty soil absorb it, and in very many cases large streams entirely disappear in this way. This is the case to a great extent in the plateau country, and still more so in the Great Basin, where these are the only outlets to the drainage. A few words will suffice to sketch the manner in which the climate has acted in producing these strange and unique orographic effects. The great degree of aridity of the atmosphere and the slight rainfall, coupled with its sudden explosive character, render plant-life very limited in amount. The soil, having little or no protection against the sudden floods, is washed away as fast, or nearly as fast, as it is formed ; or, in other words, transportation nearly or quite keeps pace with disintegration. The rains, coming as they always do in floods, run immediately off the bare rock or over and through the thin sandy soil, sweeping it with them, and, collecting in the little runs with incredible rapidity, rush down them in great body and with great velocity, sweeping everything before them. The waters are turbid and thick with sediment, coarse and sharp-edged from the rapid cutting of the rocks. It is this detritus which Dame THE GREAT WEST. 65 Nature uses as her chisel in carving cafions, cliffs, buttes, and the other quaint and curious forms which one meets in this strange land. A clear stream, whatever may be its velocity, has little erosive power ; but put these tools in its possession, give it the quantity of coarse sand and gravel which the Colorado and its tributaries always hold in suspension, and its cutting power is enormous. The difference in climatic conditions between the district under discussion and the plains is one of degree only, but it is sufficient to produce very marked differences in orographic forms. Wher- ever the climatic conditions are such that soil can be formed and be cov- ered with vegetation, there cafions cannot be produced, other than as gaps for the passage of streams through mountain-ranges ; and, in proportion as the climate becomes more arid, so will the country approach in its physical features a caflon-land. While every stream in this region flows in a cafion — and there are thousands of cafions which contain no water whatever — the most remark- able succession of these clefts is that on the main stream of the -region, the Colorado, and its main branch, the Green. The lower cafions of the river were explored in 1857 by Lieutenant Ives as far as the head of the Black Cafion. In 1869, Majqr J. W. Powell explored the main portion of the river in boats. He started from Green Eiver City, in South- western Wyoming, and safely threaded the devious path of the cafions as far as the mouth of the Grand Wash, a distance of one thousand miles. Throughout this distance there are but few miles where the river is not deep in the bowels of the earth. The*following vivid description of the Grand Cafion cannot fail to be read with interest : " The walls now are more than a mile in height, a vertical distance difficult to appreciate A thousand feet of this is up through granite crags, then steep slopes and perpendicular cliffs rise, one above another, to the summit. The gorge is black and narrow below, red and gray and flaring above, with crags and angular projections on the walls, which, cut in many places by side-cafions, seem to be a vast wilderness of rocks. Down in these grand, gloomy depths we glide, ever listening, for the mad waters keep up their roar; ever watching, ever peering ahead, for the narrow cafion is winding and the river is closed in, so that we can see but a few hundred yards, and what there may be below we know not ; but we listen for falls and watch for rocks, or stop now and then in the bay of a recess to admire the gigantic scenery. And ever as we go there is some new pinnacle or tower, some crag or peak, some dis- tant view of the upper plateau, some strange-shaped rock, or some deep, 5 66 THE GREAT WEST. narrow side-cafion. Then we come to another broken fall, which appears more difficult than the one we ran this morning. " Clouds are playing in the cafion to-day. Sometimes they roll down in great masses, filling the gorge with gloom ; sometimes they hang above from wall to wall, and cover the canon with a roof of impending storm ; and we can peer long distances up and down this cafion-corridor, with its cloud-roof overhead, its walls of black granite, and its river bright with the sheen of broken waters. Then a gust of wind sweeps down a side- gulch, and, making a rift in the clouds, reveals the blue heavens, and a stream of sunlight pours in. Then the clouds drift away into distance, and hang around crags and peaks and pinnacles and towers and walls, and cover them with a mantle that lifts from time to time and sets them all in sharp relief. Then baby-clouds creep out of side-caflons, glide around points, and creep back again into more distant gorges. Then clouds set in strata across the cafion, with intervening vista-views to cliffs and rocks beyond. The clouds are children of the heavens, and when they play among the rocks they lift them to the region above " The varying depths of this cafion, due to the varying altitudes of the plateaus through which it runs, can only be seen from above. As we wind about in the gloomy depths below, the difference between four thousand and six thousand feet is not discerned, but the characteristics of the cafion — the scenic features — change abruptly with the change in the altitude of the walls as the falls are passed. In running the channel which divides the twin plateaus we pass round the first great southern bend. In the very depths of the cafion we have black granite,*with a narrow cleft through which a great river plunges. This granite portion of the walls is carved with deep gulches and embossed with pinnacles and towers. Above are broken, ragged, nonconformable rocks, in many places sloping back at a low angle. Clambering over these, we reach rocks lying in horizontal beds. Some are soft, many very hard; the softer strata are washed on, the harder remain as shelves. Everywhere there are side-gulches and caflons, so that these gulches are set about ten thousand dark, gloomy alcoves. One might imagine that this was intended for the library of the gods ; and it was. The shelves are not for books, but form the stony leaves of one great book. He who would read the language of the universe may dig out letters here and there, and with them spell the words, and read, in a slow and imperfect way, but still so as to understand a little, the story of creation." * * Exploration of the Colorado River of the West: Washington, 1875; pp. 83, 85, 193, 194. THE GREAT WEST. 67 EtriNS IN THE SOUTH-WESTEEN TEEEITOEIES. In the Territories bordering upon the Coloraxlo drainage-system are found ruins and other remains of a people evidently more or less distinct from the Mound-builders, and probably much more closely related to the Aztecs of Mexico. All oyer Arizona, the western half of New Mexico, the south-western portion of Colorado, the southern part of Utah and Ne- vada, with the south-eastern portion of California, are found the ruins of structures raised by this people. -They resemble in many important par- ticulars the towns and houses of the Moquis and Pueblo Indians of the present day, which are described elsewhere in this volume, and who are probably the last remnants of a once great race which covered this region at one time with a dense population. These ruins, in their locations and characters, serve to sketch in rough outline the history of this people — ^their peaceful, quiet, pastoral, and agri- cultural lives, then the rude onslaught upon them by the barbarous tribes from the North, who drove them from their indefensible agricultural towns, first, to take shelter upon the summits of high mesas, and then, as they became weaker and less able to cope with their formidable enemies, to the clefts and crannies of the rocks, to the most inaccessible places which Nature had provided. So we can easily distinguish two entirely different classes of structures — first, the agricultural settlements ; and second, those used as fortresses or retreats in time of war. Those of the first class were built in the fertile river-bottoms, close to water and arable land. The houses were mainly communal, several stories high, similar to the pueblos of the present day. They were made of stone, laid in more or less regular courses in mortar, or of adobe (sun-dried) brick. In their ground-plan these communal houses are rectangular, cir- cular, or elliptical, or, more rarely, of irregular form. They are usually built around or nearly around a rectangular or circular court, into which the houses open, while on the outside the structure presents a blank wall, broken only by small apertures which served as windows. In every town has been found one or more estufas, or sweat-houses, as they are called, for the sake of a name. The building or room is rectan- gular or circular, and much more commonly the latter. In some cases, however, it is an underground aipartment. However built, it is always with very great care, and oftentimes with a view to architectural effect. It is usually the most pretentious building in the settlement. A very common form is that of a tower, usually with a double wall, the annular space between the two walls being subdivided into rooms. One of these 68 THE GflEAT WEST. having a triple wall has been found. It is probable that this building was used as a place of woi'ship or was in some way connected with their religion. It may also have been used as the council-house where the grave affairs of state were discussed. At a locality in South-western Colorado known as Aztec Spring is situated one of the largest of these towns. The ma.ss of ruins — for the town is in a very ruinous state — covers an area of about four hundred and eighty thousand square feet, and is about three to four feet in depth, making one million five hundred thousand cubic feet of masonry. The stone used is from a cliff fully a mile away. At Ojo Caliente, New, Mex- ico, are the ruins of another large town. It is placed upon a high terrace near Caliente Creek. It was built chiefly of adobe, and consisted of rows of rooms built around central courts. On the Rios San Juan, Chaco, and De Chelly are found a number of other towns more or less similar. The second class of structures — those built mainly for purposes of de- fence — are in general in a much better state of preservation, owing in part to their more sheltered position, but mainly, undoubtedly, to the fact that they are of a somewhat more recent date, as indicating a later chapter in the history of this people. Some of them, and perhaps the more elabo- rate structures, are built upon the summits of almost inaccessible mesas, as are the Moquis' towns of the present day. Here are found round tow- ers of considerable height, serving not only as fortresses but as watch- towers. But the cave-dwellings, as they are called, are by far the more numerous and interesting. This country, as was stated in the geographical description, is very arid. There are but few streams, and most of these traverse the country deep down below the surface in canons, with rocky, precipitous walls. Different strata in these canon-walls have been eroded in different degrees, so that one finds horizontal caves in the walls where one of the horizontal beds has weathered back a few feet farther than the harder beds above and below it. In many cases where these caves have occurred part-way up a cliff these people — sore beset by their enemies — have built places of refuge, secure from attack from above by reason of the overhanging cliff, and nearly so from below, as the occupants had to depend upon ladders or steps cut in the nearly perpendicular face of rock. Travelling down the cafion of the Rio Mancos in South-western Colorado, one sees everywhere on the walls which encompass him on either hand these structures, like swallows' nests, in the clefts and crannies of the rocks. In some cases there are quite large groups of houses, well built of stone, even two stories in height. In others a simple wall has been thrown up across the front of a crevice. THE GREAT WEST. 69 Other traces of this ancient people are not wanting. Great areas — hundreds of square miles, indeed — are so thickly strewn with fragments of pottery that one may ride for days and at every step his horse's hoofs will strike them. Few whole vessels have been found in the ruins. They have been thoroughly explored by the Indians, who have taken almost everything of value to them. The pottery resembles very closely, in material and in the designs painted upon it, that of the Moquis and Pueblo people of the present, but in quality it is vastly superior to the latter. Again, in many localities arrow-heads of chalcedony and obsidian have been found in abundance, indicating the scenes of many a bloody conflict. As to the age of these ruins little is known. It is certain that they date back several centuries, undoubtedly before the first Spanish conquest, and a few facts point to a very great antiquity. That ' they may have been a colony of the Aztecs, founded by them in their southward migration to the table-lands of Mexico, is not improbable. But few facts are known on which to base a theory. THE GEEAT BASIN. Between the "Wahsatch range and the Sierra Nevada lies a great area which has no outlet to either ocean — an area containing many great ranges of mountains, with broad valleys at their bases ; but the moun- tains send down to the plains few permanent streams, and nearly all of these are absorbed by the thirsty soil immediately, or flow into salt lakes to feed the increasing thirst of the dry atmosphere. On the east this region is tolerably well defined by the Wahsatch and other ranges — on the west by the Sierra Nevada. On the north and south, however, its limits are not sharply defined, the divides being in most cases mere swells in otherwise flat valleys. The scenery in the vicinity of the Wahsatch Mountains has long been celebrated for its grandeur and beauty. Mount Nebo, one of its promi- nent peaks and a noted landmark, is 11,992 feet high. The trend of this range is nearly north and south, while projecting like a spur toward the east is the Uintah range, with a trend nearly east and west, and with a number of peaks over thirteen thousand feet high. This is one of the most beautiful and symmetrical ranges in the West. The nucleus is com- posed of quartzites, which are so elevated that the central mass seems to have been lifted up horizontally or nearly so. The entire range is a re- markable example of a huge anticlinal, and on either side of the axis are the numerous pyramidal peaks, rising far above the timber-line and 70 THE GREAT WEST. covered with perpetual snow. Three distinct belts may be noted in this range — one above the timber-line, revealing only the bare, bleak rocks ; below, a dense belt of pine timber ; and near the base and sloping oif into the plains, another comparatively barren belt. The Wahsatch range has a gray granite nucleus, with a great thickness of sedimentary beds lying on the sides and often rising to the very summits. In the Great Basin between the Wahsatch Mountains and the Sierra Nevada are many smaller mountain-ranges, lying nearly parallel with each other, some of which seem to rise abruptly out of the surrounding plateau. This great depression was undoubtedly at no remote period, geologically speaking, a lake of several hundred miles in extent, out of whose waters the sum- mits of the mountains projected like islands. In the Shoshone Basin, forming the eastern portion of Oregon and west part of Idaho, are a great number of similar ranges, all lying parallel with each other, ap- pearing like the waves of the sea after a storm. The Salmon River Mountains, Blue Mountains, and many others are composed of a series of remarkably regular ridges, trending mainly north and south. Between the mountain-ranges in the Great Basin are valleys of greater or less breadth, floored with a modern Pliocene formation, which in turn is covered with detritus, so that their bases are concealed. The mountains and plain show proof of immense erosion, so that the mountain-ranges themselves are only remnants of their former magnitude. They are composed largely of sedimentary rocks, mostly metamorphosed; also of granitic and volcanic rocks. The valleys are really arid deserts to a great extent, with very little water the greater portion of the year. A few springs here and there supply the thirsty traveller. Immedi- ately around Great Salt Lake are numerous valleys watered by the streams that flow from the mountains, and in such cases the soil is remarkably productive. In this basin are some quite large rivers, as the Humboldt, Sevier, Jor- dan, Bear, etc. Jordan and Bear Rivers are large streams, but pour their waters into Great Salt Lake, which has no outlet. Humboldt River takes its rise in the Humboldt range, flows south-westward, and is lost in Hum- boldt Lake, or " Sink," as it was called by the early pioneers. Sevier is a very sinuous stream, waters a narrow valley, and disappears in Sevier Lake. The following general description of the features of the Great Basin is found in the Report of the U. S. Geological Survey for 1870, made by Dr. Hayden : " Let us for a moment take a bird's-eye view of the great inland basin THE GREAT WEST. 71 of which Salt Lake Valley forms only a part. "We shall find that what is termed the Great Basin of the West comprises the vast area enclosed by the Wahsatch Mountains on the east and the Sierra Nevada on the west, the crest or water-divide of the Columbia on the north, and that of the Colorado on the south. We shall also observe that this great region has no visible outlet ; that it is composed of a multitude of smaller basins or valleys, each of which has its little lakes, springs, and watercourses, their surplus water either evaporating or sinking beneath the surface. If we examine the elevations in this region, we observe a wonderful uni- formity in the surface of the valleys, and find that none of them are much above the level of the waters of Great Salt Lake I infer that a fresh-water lake once occupied all this immense basin ; that the smaller ranges of mountains were scattered over it as isolated islands, their summits projecting above the surface ; that the waters have grad- ually and slowly passed away by evaporation, and the terraces are left to reveal certain oscillations of level and the steps of progress toward the present order of things ; and that the briny waters have concentrated in those lake-basins which have no outlet." GEEAT SALT LAKE. The principal lake in the Great Basin is Great Salt Lake, which receives its principal waters from the Wahsatch Mountains. It might be called a vast inland sea, as it occupies an area of 2360 square miles. It is quite shallow, frequently not more than from ten to twenty feet, and its greatest depth not far from sixty feet. Having no outlet, the evap- oration is very great. The amount fluctuates, somewhat depending upon the character of the seasons. However, the surface has gradually risen since 1849 about eleven feet, and the area covered by the lake is said to be forty per cent, greater, indicating an important increase in the moisture of the climate in later years. Great Salt Lake is but the ruin of a much grander lake which in ages past covered a large part of the area of the Great Basin. The shore- line of this great lake — ^for which the name of Bonneville has been pro- posed — is yet distinctly marked high up on the slopes of the Wahsatch ' and other ranges in this part of the basin, 970 feet above its present sur- face. At that time it had an outlet, draining northward into the Snake or Lewis Fork of the Columbia. During the process of desiccation of the country, caused by the rise of the Sierra Nevada, the lake receded, but its recession was checked for greater or less intervals, which are 72 THE GREAT WEST. indicated by minor beach-lines which form a succession of steps upon the mountain-side. The waters of this lake are said to be the strongest brine known. The human body floats almost entirely on the surface. At the time of Captain Stansbury's survey in 1850 the water contained 22.4 per cent, of solid matter ; at present the percentage of solid matter is much less. In 1869 it was reduced to 14.8. An analysis of the solid matter by the survey of the 40th parallel (vide Bept. Sur. 4.0th Par., vol. ii. p. 433) gave in 150 parts — Magnesia 6.301 Lime 0.357 Soda 66.978 Potassa 2.901 Sulphuric acid 8.215 Chlorine 83 946 168.698 Less oxygen of soda and magnesia 18 .758 149.940 or, in other words — Chloride of sodium 79.11 Chloride of magnesium 9.95 Sulphate of soda 6.22 Sulphate of potassa 3.58 Sulphate of lime 0.57 Excess of chlorine 0.57 100.00 The elevation of the lake above sea-level is 4218 feet. THE NOETHEEN SYSTEM OF MOUNTAINS. A grand system of mountains stretches from the Arctic Ocean on the north to Mexico on the south, fronting the Pacific Ocean. Portions of this system are known as the Cascade, the Sierra Nevada, Coast Range, etc. These mountains, as they extend into Mexico, have long been known as the Cordilleras of Mexico, and the main ranges of South America bear the name of Cordilleras or Andes. As Professor Whitney insists, prior- ity would demand that the appellation of " Cordilleras " be continued to this great group of mountains in their extension northward on the Pacific coast to British America. I therefore regard it as just that the term " Cordilleras " shall be used as the main generic term, while the more indefinite term, " Rocky Mountains," should fall under it as sub-generic. The term " Rocky Mountains " has been so long applied to the eastern division that this section, including as it does the water-divide of the continent, should not have its weight or importance diminished in our THE GREAT WEST. 73 geographical nomenclature. This becomes the more important if, as I believe, all the great groups of mountains west of longitude 105° will be found, when carefully studied, to be a unity in a general geographical and geological point of view. North of latitude 49° but little is known of these western ranges, but it is known that they extend without any permanent interruption to the Arctic Ocean, with here and there a lofty peak, which from ignorance of its precise character has been assigned a greatly exaggerated elevation. In regard to the height of these peaks there is a great disagreement among observers. Mount Hood was ascended in 1864 by Messrs. Wood and Atkinson, and pronounced 17,430 feet above sea-level. In 1867 Lieut.-Col. Williamson, with excellent and reliable instruments, found its height to be only 11,225. Professor Whitney's trigonometrical mea.s- urement of the same peak showed, by a rough calculation, about 11,700 feet. The latter measurements are undoubtedly very nearly correct. The same discrepancies exist in regard to the elevation of the other mountain- peaks, but careful instrumental measurements have reduced them to a raoderate figure. Mount Baker and Mount Hood, both of which are enormous volcanic cones, may be regarded as respectively about 11,100 and 11,225 feet. The elevation of Mount Ranier, or Lachoma, may be regarded as pretty definitely settled by the observations of Professor Davidson of the U. S. Coast Survey at 14,444 feet — four feet higher than Mount Shasta, and therefore the most elevated point in the Cascade range. The Cascade Range is a continuation northward of the Sierra Nevada or Snowy Range, and is separated only by the chasm of the Klamath River. Through the entire length of Oregon and Washington Territo- ries the Cascade Range runs north and south, parallel to, and about one hundred miles from, the Pacific shore. Near the 49th parallel it is bent north-westerly, conforming with the trend of the coast, and in British Columbia is called the Marine Range. The average elevation is five to six thousand feet. It obtained its name from the Cascades of the Co- lumbia, which are formed by the passage of that river through it. The country along the immediate coast is but a narrow belt, much broken, while the shore is indented with great numbers of bays or inlets, of which the estuary of the Columbia, Shoalwater Bay, and Gray's Harbor are noted. Promontories and rocky islets are visible everywhere as surviv- ing monuments of the terrific erosion which has swept away entire moun- tain-ranges, leaving at this time only the single group of the Cascade range. A few of the peaks are said to be at times active volcanoes. 74 THE GREAT WEST. Mount St. Helen's is reported, upon good authority, as having in Febru- ary, 1842, discharged lava, sending streams of it down its sides. Mount Baker is said to be still smoking, and others show some signs of volcanic activity. South of Cape Mendocino, in latitude 40° 30', to Point Conception, near latitude 34° 30', the Coast Range of California is composed of a succession of parallel ranges, with intervening valleys of great beauty and fertility. Between the Coast Range and the Cascades is a longitu- dinal depression which forms the valley of the Willamette, extending northward to the Gulf of Georgia. Similar valleys occur in California, as the San Joaquin and Sacramento. In this northern region the forests are very dense, and the undergrowth so thick that it is difficult to pene- trate it. Trees occur of majestic size, of which the yellow fir {Abies Douglasii) predominates over all others. The cedar {Thuya giganted) is also very abundant. The lumber interests of this country are immense. Between the Cascades and the eastern group of mountains lies the basin of the Columbia, which is an arid plain covered with artemisia or wild sage and bunch-grass. The surface is cut through by deep canons, through which the large rivers flow between huge walls of basalt. Al- though there are great varieties of climate in this division, it is extremely mild on the immediate coast. At Puget Sound snow seldom falls, and remains but a short time. Rains are very abundant, reaching sixty inches during the year. According to Professor J. D. Whitney, the Coast Range is coincident with the Sierra Nevada, both north and south. Near Lejon Pass, in latitude 35°, the ridges are topographically indistinguishable from each other, and it is only by carefully studying the position of the strata that it can be determined where one system begins and the other ends. The Coast Ranges are composed of newer formations than the Sierra, and have been subjected to greater disturbances up to a recent period ; and they contain no rocks older than the Cretaceous. In point of elevation the parts of this system vary widely. From three to four thousand feet above the sea in main height in North-western Oregon, it rises southward until in the southern part of this State, and in California nearly as far as the Bay of San Francisco, it has a mean height of not less than six thousand feet. The Bay of San Francisco lies just in the trend of this system, a great gap. South of it the ranges have much less height, reaching only two to three thousand feet above the sea. One of the most prominent peaks is Monte Diablo, rising right up from the bay to a height of three thousand eight hundred and sixty feet, and WINTER FOREST SCENE IN THE SIERRA NEVADAS. BY TH0M;i.3 MORAN. THE GREAT WEST. 75 commanding a most beautiful view of one of the finest harbors' in the world lying spread out at the feet ; while to the west, away across the yellow plain of the Sacramento Valley, stands the splendid panorama of the snowy crest of the Sierra Nevada. THE SIEEEA NEVADA. The Sierra Nevada, or Snowy Range, forms the western border of the great continental plateaus, corresponding with the Rocky group on the east. While the base of the eastern mass is everywhere four to five thou- sand feet above the sea-level, and the descent to the sea imperceptible to the eye, the Sierra slopes rapidly, so that the sea-level is reached within one hundred miles. So far as now known, the highest peak of the United States is in the Sierra group — viz. Mount Whitney, 14,887 feet. The peak which is believed to be the next in height is in Southern Colorado — Blanca Peak of Sierra Blanca, 14,464 feet. The scenery of the Sierra group is of surpassing grandeur and beauty. There is not such a vast number of high peaks as in the Colorado group, but it may fairly claim the highest ; and inasmuch as the surrounding country has a much lower altitude, there is a massiveness about this magnificent range that even the Sawatch of Colorado cannot boast. The Sierra chain is about four hundred and fifty miles in length, and averages about eighty miles in width, supposing its northern terminus to be at Lassen's Butte, latitude 40° 30'. The central mass or core is chiefly granite, with meta- morphic slates on either side, capped with basaltic and other kinds of lava and heavy beds of ashes and breccia. All these rocks are visible from the Central Pacific Railroad between Truckee and Sacramento. The evidences of very modern volcanic action are visible everywhere. Even now there are numerous hot springs and geysers, as well as an occasional earthquake shock. The height of some of the dominating peaks is as follows: Mount Shasta, 14,442 feet; Mount Tyndall, 14,386; Mount Kaweah, 14,000 ; Mount Brewer, 13,886 ; Red Slate Peak, 13,400 ; Mount Dana, 13,277. On the mountains snow falls to the depth of forty or fifty feet, and much of it remains all the year. Enormous glaciers exist here even at the present time, and the evidences of ancient glacial action are wonderful. The worn and rounded granites of the Sierra Nevada were well adapted to preserve the records of the old glaciers, and they everywhere testify to the intensity of their former power. These old glaciers have been continued down to the present time, in a modified condition. All the glaciers occur on the .north side of the mountains, and are very numerous — now estimated, according to 76 THE GREAT WEST. Mr. John Muir, at sixty-five. The number known in the Alps is eleven hundred, of which about one hundred may be considered as primary. Some of these great masses of snow and ice, which are not considered true glaciers by good authority, are nearly as large as the Alpine — as the Lyell, North Kettle, and others not named. Although the existence of glacial phenomena on the Pacific slope has been known for many years, the subject has received comparatively little attention, but enough is known to invest them with the highest interest. Moraines and morainal lakes occur in the Sierras in great number. Lake Tenaya, at the head of the Merced River, or a branch of the same name, is a conspicuous ex- ample. Traces , of the existence of an immense flow of ice are shown here in the valley occupied by the lake, according to Whitney, and the ridges on either side of the trail are so worn by glacial action that the rocks are slippery, rendering travel dangerous. In our country the Glacial period proper has passed away, and the masses of snow and ice that now remain behind are only remnants. GLACIAL ACTION IN THE EOCKY MOUNTAINS. All through the Rocky Mountain group, on both sides of the great Divide, are remarkable examples of glacial action — moraines and morainal lakes. In Central Colorado, in the Sawatch and Elk Mountains, are large ai-eas of glaciated granites, which are usually called sheep-backs or roehes moutonnSes. The first true glaciers on the Atlantic slope or in the Rocky Mountain group were observed in the summer of 1878 by the writer in the "Wind River Mountains, in Wyoming Territory. On the south-east side of Fremont's Peak are two fine long glaciers, occupying an area of about two square miles, which are now named the Upper and Lower Fre- mont Glaciers. The neve is distinctly shown, and the crevasses produced by the slow movements are all large and well marked. Indeed, all the characters of a first-class Swiss glacier are found here. Several smaller ones are found in this range. Even these are comparatively only the very insignificant remnants of the immense glaciers of the true Glacial epoch. On the west side of the Wind River range the morainal ridges are of im- mense size, and glacial lakes of all sizes are scattered about in great niun- bers. There must have been here at one time a mass of snow and ice moving down into the plains sixty-five miles long and twelve to fifteen broad. TIMBEE-BBLTS. Four pretty well-marked belts of forest vegetation were observed by Whitney in the Sierra Nevada. The lowest is the foo1>hills, with THE GREAT WEST. 77 oaks, buckeyes, and small Digger pines ; the second belt lies between four and five thousand feet, and consists of pitch-pine (Piniis ponderosa), bastard cedar, and Douglas spruce ; the third zone, between seven and nine thou- sand feet, is that of firs, as Picea grandis and amabilis, tamarack-pine, etc. ; and on the highest belt, above nine thousand feet, where vegetation begins to dwindle, a dwarf pine [Ptnus cristata) is seen up to the level of per- petual snow. There are great numbers of beautiful lakes in the Sierras, fed by the melting of the snows, among which are Lake Tahoe and Donner's Lake. THE YOSEMITE VALLEY. The Yosemite Valley, so remarkable for its rugged scenery, and which has been set apart by legislative action as a pleasure-ground, is in the Sierra. Through this valley flows the Merced Eiver, and at its source is a fine group of mountain-peaks, thirteen thousand feet high, called the Merced group. We cannot do better, in order to give a general idea of this remarkable natural feature, than to quote the description of this valley written by Professor J. D. Whitney in the Guidebook of the Yosemite, p. 84, et seq. : " The Yosemite Valley is nearly in the centre of the State (California) north and south, and just midway between the east and west bases of the Sierra, here a little over seventy miles wide The valley is a nearly level area, about six miles in length and from half a mile to a mile in width, and sunken almost a mile in perpendicular depth below the general level of the adjacent region. It may be roughly likened to a gigantic trough hollowed in the mountains, nearly at right angles to their regular trend This trough .... is quite irregular, having, several re- entering angles and square recesses, let back, as it were, into its sides ; still, a general north-east by easterly direction, is maintained in the de- pression until we arrive near its upper end, where it turns sharply, at right angles almost, and soon divides into three branches, through either of which we may, going up a series of gigantic steps as it were, ascend to the general level of the Sierra. Down each of these branches, or cafions, de- scend streams, forks of the Merced, coming down the steps in a series of stupendous waterfalls. At its lower fend the valley contracts into a narrow gorge or canon, with steeply-inclined walls, and not having the U-shape of the Yosemite, but the usual V-form of Californian valleys. "The principal features of the Yosemite, -and those by which it is dis-. tinguished from all other known valleys, are — first, the near approach to verticality of its walls ; second, their great height, not only absolutely, but 78 THE GREAT WEST. as compared with the width of the valley itself; and, finally, the very small amount of talus or ddbris at the base of these gigantic cliffs. These are the great characteristics of the Yosemite throughout its whole length, but besides these there are many other striking peculiarities, and features both of sublimity and beauty, which can hardly be surpassed, if equalled, by those of any mountain-valley in the world. The domes or the water- falls of the Yosemite, or any single one of them even, would be sufficient in any European country to attract travellers from far and wide in all directions. Waterfalls in the vicinity of the Yosemite, surpassing in beauty many of those best known and most visited in Europe, are actually left entirely unnoticed by travellers because there are so many other ob- jects of interest." The objects of interest in this valley, which render it without a rival in scenic effects in the known world, are^— firgt, the great cliffs and crags which border it, rising three to four thousand feet in vertical height above its level ; second, the wonderful bas-reliefs of columns, spires, and arches upon its granite walls ; and, third, the grand and beautiful waterfalls by which the many tributaries to the Merced enter the valley, leaping over its walls from great heights. These deserve a more particular mention. Chief among them is the Yosemite Fall. This has a total height of twenty-six hundred feet, the upper fifteen hundred of which are in a clear leap from the top of the cliff. Then follows a succession of cascades of six or seven hundred feet, below which the stream makes a second fall to the bottom of the valley. The Bridal Veil Fall, though carrying much less water, is very beautiful. In its leap of six hundred and thirty feet the column of water is swayed hither and thither by the wind, and nearly dissolved into spray, which makes its fanciful name by no means inap- propriate. Other notable falls are the Vernal, four hundred feet, and the Nevada, six hundred feet, in height. PEATTJEES OF THE TWO MOTJNTAIK-SYSTEMS. So far as structure and topography are concerned, the great mountain- systems extending along the western borders of the Western hemisphere from the Arctic Ocean to Patagonia may be regarded as a unit and due to one great cause. So far as we know at the present time, the general geological features are very similar, so that the application of a single comprehensive name to both groups as one grand system may not be deemed inappropriate. It may be said, then, that as North America has its lofty North Cordilleras group opposite the deep North Pacific Ocean, and its small Appalachian group opposite the shallower North Atlantic, THE GREAT WEST. 79 so South America has its still higher Andes or Southern Cordilleras group opposite the deeper South Pacific, and the smaller Brazilian ranges oppo- site the South Atlantic. This generalization, as stated by Dana, is founded on a deep-seated structural cause. The elevation of a portion of the earth's crust requires in close proximity a corresponding depression. The great mountain-system of the Western United States may be primarily divided into two principal portions — the Sierra Nevada and Coast ranges, fronting the Pacific Ocean, and the Rocky chain, which forms the great water-divide of the continent. Each of these chains or groups is made up of a great number of smaller ranges, in the aggregate apparently possessing a considerable degree of regularity, but when studied in detail showing less system. Sometimes, as in the Great Basin, the main ranges seem to lie parallel for the most part, but usually the minor ranges branch oif in some special direction. More commonly, the trend is about north-east and south-west, but in some instances it is due north and south or east and west. The Wahsatch range in Utah trends nearly north and south, while the Uintah range, which seems to branch off from it, trends nearly east and west. The area west of the Missis- sippi may be divided into mountain and prairie or plain country. The belt of plains on the east slope averages about five hundred miles in width, and gradually rises to the base o'f the mountains. The mountain portion has its greatest breadth between the 36th and 41st parallels, where it varies from eight hundred to one thousand miles. In this belt are the greatest number of lofty peaks, including the highest portion of the Sierra Nevada. Among the numerous ranges of the mountain-system of the West are many valleys and plateaus, varying from a few acres to hundreds, or even thousands, of square miles. Sometimes they are formed by erosion or by depression ; many of them are ancient lake-basins. In all the great mountain-districts of the West are thousands of these openings, into which settlements have«already penetrated. In the San Juan Mountains is Baker's Park, with an extensive settlement of miners, and in the sur- rounding mountains are some of the richest silver-mines in America. The North, Middle, and South Parks in Colorado are areas of depression, underlaid with sedimentary strata and walled in on every side by lofty mountain-ranges ; they are really old lake-basins. The North Park has a comparatively level surface and an average elevation of eight thousand feet. South of this, and only separated by a rather low mountain-range, is the Middle Park, which is much larger and far more rugged ; indeed, there is very little of what should be called plain country, but a succes- 80 THE GREAT WEST. sion of high ridges, many of which are of volcanic origin. The average elevation is about seven thousand five hundred feet. Still farther south, but separated by a much wider belt of mountainous district, is the South Park, which is mostly a plain with an average elevation of nine thousand feet. In these parks there is frost every month in the year. San Luis Valley, in Southern Colorado and Northern New Mexico, has an average elevation of seven to eight thousand feet. The Llano Estacado of Texas and New Mexico averages 3200 to 4700 feet above the sea-level ; the Colorado Plain in Arizona, 5500 feet ; Salt Lake Valley, Utah, 4200 to 4600 feet ; Laramie Plains, "Wyoming Territory, 7000 feet ; Snake River Plain, in Idaho, 4000 to 4500 feet; Sevier Lake-Basin, Utah, 4700 feet; Humboldt River Basin (Lassen's Meadows), Nevada, 4700 feet ; Carson River Basin, 3800 feet ; Walker's River Basin, 4100 feet ; and Mojave River Basin, California, 1100 feet. Comparing the mountain-plateaus or basins of the Western mountain- region with some of those in the Andean region of South America, the difference of elevation is very great. The Antisana plateau of South America is 13,451 feet; the basin of Santa Fd de Bogota, 8413 feet; and the basin near Lake Titicaca, 12,853 feet. Perhaps as great an extent of plateau is comprised in the belt between the 38th and 44th parallels of latitude as in any other portion of the Cordilleran area. Through this belt the Pacific Railroad passes. From Omaha to Cheyenne the track lies nearly all the way on the most modern Tertiary formations. From Cheyenne westward the road crosses the Laramie range, the highest point, Sherman, being 8271 feet. After passing over about fifteen miles of granitic rocks it descends into the Laramie Plains. Thence to the Wah- satch Mountains in Utah no more granitic rocks are met with, only Cre- taceous or Tertiary. In crossing the water-divide at Creston, 7030 feet high, the stranger would not suspect that he was passing from the Atlantic to the Pacific slope. The railroad runs through the Wahsatch range at right angles to its trend in the channel of the Weber River, with only four miles of granitic rocks ; so that from Omaha to Ogden, a distance of over one thousand miles, only about eighteen miles of metamorphic rocks are crossed. Hence the Central Pacific crosses the Salt Lake Basin, enters the Humboldt Valley, and really meets with no mountains until it reaches the Sierra Nevada, where a most formidable obstacle presents itself in a massive granite range, which, however, is crossed at an eleva- tion of only 7042 feet. liungltiLde Inl Weal fi-oni DIO Gi 10* i; Ci-etc XM I (1^ jiV 1 A ii~&"--^ uk^- risoj T^-T^iLoui^m. SON r ■ v^ 'M "T^Si^"^'"^^ d„.,„t:k 3Si ^;3:»^~ limlmjojuc __*JS-^ XynKong' ,£y\^ — LjEpa61„ p I 1, -Jii '( O S A OES ^ ^^ Atoklv' ^ Pri'Btu J(i'i1 Ki-rer llMiisiai 'AJ.E OF SlTf.RS \ IIKl SAHSAS, , WE W MEXICO K IKDIAN' TEIMMTf^RT. ^^=t=^ THE GREAT WEST. 81 MINERAL DEPOSITS IN THE WEST. According to Messrs. Blake and King, there are seven longitudinal zones or belts of mineral deposits in the West, following the prevailing direction of the mountain-ranges. Mr. King says : " The Pacific coast ranges upon the west carry quicksilver, tin, and chromic iron. The next belt is that of the Sierra Nevada and Oregon Cascades, which upon their west slope bear two zones, a foot-hill chain of copper-mines, and a middle line of gold-deposits. These gold-veins and the resultant placer-mines extend far into Alaska, characterized by the occurrence of gold in quartz, by a small amount of that metal which is entangled in iron sulphurets, and by occupying splits in the upturned metamorphic strata of the Jurassic age. Lying to the east of the zone, along the east base of the Sierras, and stretching southward into Mexico, is a chain of silver-mines, containing comparatively little base metal, and frequently included in volcanic rocks. Through Middle Mexico, Arizona, Middle Nevada, and Central Idaho is another line of silver-mines, mineralized with compli- cated association of the base metals, and more often occurring in older rocks. Through New Mexico, Utah, and Western Montana lies another zone of argentiferous galena-lodes. To th^ east, again, the New Mexico, Colorado, Wyoming, and Montana gold belt is an extremely well defined and continuous chain of deposits." The yield of gold and silver for the year from July 1, 1877, to July 1, 1878, in the several States and Territories, is given by the Director of the United States Mint as follows : Gold. Silver. Total. California . $15,260,676 $2,373,389 $17,634,068 Nevada 19,546,513 28,130,350 47,676,863 Montana 2,260,511 1,669,635 3,930,146 Idaho 1,150,000 2,200,000 1,350,000 Utah 382,000 5,208,000 5,600,000 Arizona 500,000 8,000,000 3,500,000 New Mexico 175,000 500,000 675,000 Oregon 1,000,000 100,000 1,100,000 Washington 300,000 25,000 325,000 Dakota 3,000,000 none. 3,000,000 Colorado 3.366,404 5,394,940 8,761,344 $46,941,104 $48,601,314 $93,552,421 The development of the gold- and silver-mines in Colorado and the Black Hills of Dakota has been wonderful in extent, the details of which are too extended for this article. It has usually been understood that there is no coal in the true Coal- measures west of the 100th meridian, but of late years a few thin seams of no practical importance have been reported as occurring in the south 82 THE GREAT WEST. and south-west. In Colorado, Wyoming, Utah, Montana, and New Mexico vast areas are underlaid by thick beds of coal belonging to the Cretaceous and Tertiary groups. In Southern Colorado, New Mexico, and in the interior of Utah thick and important beds of coal are found in the Cretaceous group, while along the east slope of the Rocky chain in Colorado, as at Raton Hills, Caflon City, Colorado Springs, Golden City, and northward, are numerous coal-beds belonging to the Post-Cre- taceous group, which are now wrought to a large extent. In the north- west the coal-area covers not far from one hundred thousand square miles. Along the Union Pacific Railroad are coal-fields of the same age, with- out which the railroad would be of no practical value. Not less than twenty thousand tons a month are mined at Evanston, Rock Springs, and Carbon in Wyoming Territory for the use of this road alone. From Coalville, Utah, no remarkable beds of coal are found along the imme- diate vicinity of the Pacific Railroad to San Francisco. The scarcity of tree vegetation over the greater portion of our West- ern country renders this coal of vital importance to the present and future industries of the great West. To show the extent to which this brown coal is already employed in the industries in some of the Western States and Territories, we may cite the following reliable statistics : In the year 1877 there were mined or used in California 600,000 tons; Oregon, 200,000 ; Washington Territory, 150,000; Colorado, 300,000; Wyoming, 100,000 ; Utah, 45,000. I do not know the exact amount for 1879-80, but do not doubt that it has more than doubled that of 1877. From the Mining and Scientific Press for February, 1880, 1 take the following statistics of the coal-trade at Seattle, Washington Territory, alone. The greater portion of this coal is transported to the port of San Francisco. In 1871, 4918 tons; 1872, 14,830; 1872, 13,572; 1874, 9027; 1875, 70,157; 1876, 112,734; 1877, 104,556; 1878, 128,582; 1879, 132,264 tons; total, 590,639 tons. Although the trade in this lignitie or brown coal has sprung up within a few years, brought about largely by the extension of the system of railroads throughout the West, it is becoming extremely important year by year, and the absence of tim- ber over so large a proportion of the Western country renders its exist- ence a vital element of its settlement as well as its prosperity. FOSSILS IN THE LAKE-BASINS. The true brown-coal formations of the West form, as it were, the foundation, as well as a part, of the remarkable old estuaries or lake- basins that are found in every State and Territory west of the Missis- THE GREAT WEST. 83 sippl. The thickest beds occur in a series of strata that seem to form a transition series from purely marine beds to purely fresh-water strata. We have already, in a preceding portion of this article, described the wonderful lake-basins in the vicinity of the Black Hills of Dakota, from the sediment at the bottom of which have been obtained the remains of a great variety of extinct animals, including camels, rhinoceroses, elephants, mammoths, turtles, birds, etc. In the Sweetwater Vallej^, near the Three Forks of the Missouri, in Oregon, California, Texas, New Mexico, and in Colorado, are similar lake-basins, filled with the remains of these ex- tinct animals. On the Laramie Plains, about Fort Bridger and far south on Green River, are lake-basins of older date, referred to the Lower Miocene or Upper Eocene, in the deposits of which have been discovered the abundant remains of hundreds of extinct forms of vertebrate ani- mals entirely distinct from those just mentioned, as of more recent age. The energetic explorations of Professor Cope within the past few years in all these remarkable localities have resulted in making known to the public hundreds of species of the most wonderful animal forms, a his- tory of which he is now preparing for publication by the United States government. Great quantities of fossil insects, fishes, and plants are found in these older lake-beds. In the South Park of Colorado and in the Green River group of Wyoming over a thousand species of fossil insects have been found, representing almost all the families of that class of life. These fossil insects are now in the hands of Mr. S. H. Scudder of Cambridge, Massachusetts, the best American authority on this sub- ject, and the final results of his studies will appear in a large quarto vol- ume — vol. xiii. of the final Reports of the U. S. Geological Survey of the Territories. A couple of paragraphs which appeared in the American Naturalist in February, 1868, from the pen of Mr. Scudder, describing a small collection of these fossil insects from Green River, may be quoted here with interest : " The masses of rock were crowded with remains of insects and leaves of deciduous trees. Between sixty and seventy species of insects were brought home, representing nearly all the different orders ; about two- 1;hirds of the species were flies — some of them the perfect insect, others the maggot-like larva, but in no instance did the imago and larva of the same insect occur. The greater part of the beetles were quite small. There were three or four kinds of Homeoptera (allied to the treehoppers), ants of two different genera, and a poorly-preserved moth. Perhaps a minute Thrips, belonging to a group which has never been found fossil in any part of the world, is of the greatest interest. 84 THE' GREAT WEST. "At the present day these tiny and almost microscopic insects live among the petals of flowers, and one species is supposed by some entomolo- gists to be injurious to the wheat ; others believe that they congregate in tlie wheat as well as in the flowers in the hope of finding food in the still smaller and more helpless insects which are found there. It is as- tonishing that an insect so delicate and insignificant in size can be so per- fectly preserved' in these stones ; in the best specimens the body is crushed and displaced, yet the wings remain uninjured, and every hair of their broad but microscopic fringe can be counted." Over five hundred species of extinct forms of plants have been found, mostly in connection with the coal, indicating that at a comparatively modern period, geologically speaking, this great region, occupied with mountains and barren plains, was covered with forests as luxuriant as those of the Gulf States. These plants belong mostly to the early Ter- tiary period. Not unfrequently strata several feet in thickness occur, composed almost entirely of leaves of the fig, sycamore, willow, poplar, walnut, oak, etc., so well preserved that they seem to have fallen from their branches only yesterday. Even the delicate veins and serrated edges are as perfect as if pressed in an herbarium. Groves of palms waved their broad leaves over the ground, some of which had a spread of twelve feet. At the present time the true fan-palms are found only within the tropics. Many of the native ornamental trees and shrubs are the lineal descendants of the Tertiary species, and so nearly resemble the ancient forms that it is difficult to distinguish them. Professor Lesquereux says that among the genera found to be indigenous to our continent are the Virginia creeper (Ampelopsis) and the mulberry (Morus). Both the fossil species are in intimate affinity with the living ones. " They are seen everywhere and known and liked by everybody. The one is the friend of the farmer by its shade — of his children, delighted by the pleasantness of its fruits ; the other adorns our dwellings when allowed to grow in our gardens, and when left to its own work it covers with green foliage the dead trees and the barren rocks, tempering desolation and ruin by hiding them under elegant fringes and garlands painted by the richest colors. It is worth something to know that the origin of the Yirginia creeper and of the red mulberry is traceable to the Tertiary formations of North America." The gigantic Sequoias of California have their ancestors in several species. The present scarcity of timber or forests in the Western or central portions of the continent at the present time is well known, and the question arises as to the climatic conditions which should have produced THE GREAT WEST. 85 60 marked a change from the luxuriant and sub-tropical vegetation of the modern Tertiary epoch in this region to present scarcity or almost entire absence over large areas. We now know that the principal winds come from the west and north-west, and as they pass over the summits of the different ranges of mountains from the Pacific coast eastward, laden with moisture, discharge a portion of it from summit to summit, until on the eastern slope the air is almost dry. The absence of timber is due to the absence of moisture, and the inference from the fact of the dense forests existing in the present mountainous districts of the West during the early Tertiary period is that these high summits did not then exist. For the purpose of showing the average annual rainfall in inches in the different drainage-areas of the West we will state these briefly here. They are all well marked out. The Missouri River and its great branches, the Yellowstone and Platte, have their sources in the main Rocky range, and, gathering their waters from myriads of branches, flow at first east across the dry plains, and gradually turn south-east and join the Mississippi ; the average rainfall in the Upper Missouri drainage is eighteen inches. The second drainage is that of the Arkansas, farther south, which rises in the Sawatch and Park ranges of Colorado, flows south to latitude 38° 30' and longitude 106°, then bends east and flows across the plains to unite with the Mississippi ; the average rainfall is twenty-eight inches. The third system of drainage is still farther south, that of the Rio Grande, which rises in the San Juan Mountains of Southern Colorado, flows south through New Mexico and between Texas and Mexico, and empties into the Gulf of Mexico ; average rainfall, sixteen inches. West of the last is the drainage of the Colorado of the West, which, rising far north (in its branches, the Green and Grand Rivers), near the Yellowstone National Park, flows south and south-west across Wyoming, Utah, and Arizona, and empties into the Gulf of California ; the average annual rainfall in this vast area is only fifteen inches. North and west of the Colorado drainage is the great interior basin, between the Wahsatch Mountains and the Sierra Nevada, with no known outlet, the great rivers sinking ; here the average annual rainfall is only twelve inches. To the north is the great drainage of the Columbia, the branches of which rise in the main chain of the Rocky Mountains, far to the east in Idaho ; the average annual rainfall is only eighteen inches. There are several smaller areas of drainage on the Pacific coast. The limited rainfall in all these drainage-areas mentioned shows that successful agriculture is only possible with the aid of irrigation. East of the Sierra Nevada the rains are not 86 THE GREAT WEST. frequent, the snows are very light, and the amount not great, so that the supply of water from the melting of the snows is not extensive. The difference between high and low water-mark in the streams is very great. For a short time in May and June the streams are high and large, but they soon dwindle greatly, and even disappear altogether. So little snow falls on the eastern ranges that the streams which flow into the plains from the east slope will not supply water to irrigate all the fertile land that is available for agricultural purposes, and the deficiency must yet be supplied by the use of artesian wells. The timber-line, or highest limit of tree vegetation, does not vary much in the main mountain-masses of the West. In Colorado and Utah it is from 11,000 to 12,000 feet; in Northern Wyoming and Montana, from 8000 to 11,000 feet; on Mount Shasta, California, 8000 feet; while as far south as San Francisco Mountain, Arizona, between latitude 35° and 36°, it is 11,547 feet. According to observations made up to this time, the timber-line is lower to the far North. Between latitude 45° and 46°, in Montana, it varies from 8800 to 9600 feet, while from latitude 40° to 35° it is quite uniformly from 11,000 to 12,000 feet. These state- ments may be regarded as approximately accurate, though more obser- vations ought to be made. The mean elevation along several parallels of latitude has been ascer- tained approximately. For instance, along the 32d parallel, between longitude 95° and 96°, the mean elevation is 500 feet ; the highest mean between 108° and 110° in the Sierra Madre plateau is 5000 feet; 35th parallel, first mean, 650 feet, highest mean, between longitude 107° and 109°, at Zuni Mountains, 7000 feet ; 39th parallel-, first mean, 1000 feet, highest mean, between longitude 105° and 107°, in the Colorado, Sawatch, and Elk ranges, 11,000 feet; 41st parallel, first mean, 1000 feet, highest mean, between longitude 105° and 107°, Laramie range and South Park, 8000 ; 45th parallel, first mean, 1000 feet, highest mean, between longi- tude 108° and 110°, Big Horn Mountains and Yellowstone range, 7000 feet ; 48th parallel, first mean, 1500 feet, highest mean, between longitude 113° and 114°, the main mountain chain, 4000 feet. The mean eleva- tion of Arizona is 4200 feet ; of California, 2800 ; of Colorado, 6600; of Idaho, 3800 ; of Montana, 3950 ; of Nevada, 4900 ; of New Mexico, 5400; of Oregon, 2700; of Washington Territory, 1800; of Wyoming, 6450. STOCK-EAISING. I have not spoken of what may form one off the most important indus- tries in the West, and one which is now assuming most formidable pro- THE GREAT WEST. 87 portions ; and that is stock-raising. The great Plains form one great cattle- range. From Texas to Montana we find them dotted over with the huts of the ranchmen and covered with herds of cattle. They follow closely the retreating steps of the buffalo. So in the great valleys of Montana, the great valleys of California, and those of Oregon — indeed, wherever grass grows and hostile Indians are not too plentiful, there we find herds of cattle. Some of the cattle-men are very wealthy, numbering their cattle by the hundreds of thousands. Next to the gold- and silver-mines, no industry adds more to the wealth of the country than this. The de- mand for the foreign market has been very great, and over two million pounds of meat per month have been transported to Europe. We have touched upon but a few of the topics of interest in regard to our great West, either scientific or practical, but we trust we have said enough to convey at least a glimpse of its almost unlimited future. THE TRIP OVERLAND. BY CHARLES RAYMOND. STAETING out from Omaha, a prosperous city of twenty-one thou- sand inhabitants, situated upon the west bank of the Missouri, we set " sail " for the Far West. Nothing can be more delightful than a journey in a Pullman car on the Pacific Railroad. The rate of speed in the East, of forty miles an hour, renders travel tiresome, btit on the Pacific road the uniform rate of twenty miles an hour, with the smoothness of the track, makes the journey a pleasure. The Platte Valley opens before our view. We follow the old trail, and enter the bottom-lands as rich as Egypt. Here Lewis and Clarke started out on their long journey overland in 1804. Millions of butter- flies, those winged flowers, met their gaze, and they christened the spot Papilion. The name remains, but the men have gone. The Platte River is over three-quarters of a mile wide, with an average depth of six inches, in which the old emigrants, as one told the writer, dared not halt or tarry in the crossing, for fear of sinking so deep in the treacherous sand as not to be extricated. The rapid settlement of this valley by a thrifty and industrious class of people makes the wilderness to blossom as a rose, and the thrifty towns springing up all along the line of the Central Pacific Railroad give token of prosperity. Oftentimes at night can be seen the prairie-fires so dreaded by the emi- grant, yet so grand when seen from the car-window as they sweep over the plains. THE PLAINS, which extend through Nebraska, are familiar to all persons who made the journey or read of the travels of emigrants in early days. We pass the old emigrant road, "a trail drawn across the continent, like the tremulous writing of a death-warrant when Mercy holds the pen," and DONNER LAKE, FROM THE SNOW-SHEDS. THE TRIP OVERLAND. 89 we can but compare the present mode of travelling with former days. The contrast is marked. Nearly all the stations passed on the road have the same characteristics. They are of rapid growth, and have a population varying from several thousand to a score or less. Between them may occasionally be seen the prairie-dog villages and herds of antelope. Bufialoes have disappeared. The traveller rejoices when the first sight of the Rocky Mountains appears. Some people imagine that the mountains are almost perpendicular, and are surprised to find them- selves at an altitude of 6041 feet when they redch Cheyenne, having as- cended imperceptibly to that height, as the altitude above sea-level at Omaha was only 966 feet. Cheyenne is known as the "Magic City of the Plain," from its rapid growth. In July, 1867, there was one house here ; six months later there were three thousand houses. The mountains form a massive background. At present the city is prosperous, with a population of seven thousand. From Cheyenne the tourist can make the dMour of Colorado, and no ' finer scenery can be found, 'while the wonderful development of the minerals and other material resources of the State /offers strong induce- ments to the emigrants. Leaving Cheyenne, we pass through many snow-sheds, and soon reach Sherman, the highest point on the road, at an altitude of 8242 feet, and at a distance of 549 miles from Omaha. The ascent has been so gradual that the height can hardly be realized. From here the scenery is amazingly strange. Odd and fantastic shapes crowd the landscape on both sides of the track. The scenery is now very much changed. We pass Laramie City, a thriving place of three thousand inhabitants, 572 miles from Omaha. From here the traveller will gain new ideas of the sublimity of Nature in the scenery of the Rocky Mountains. The train West-bound leaves here in the evening. The Green River country, through which we pass the following day, is marked by a most peculiar formation. The rocks are so worn by the elements as to re- semble the ruins of some deserted temples or castles. Many beautiful impressions of fish and insects are found preserved in the sandstone. ECHO AND WEBER CAffONS are perhaps the most far-famed of all the scenery on the Union Pacific, and crowded into a distance of sixty miles, hardly three hours' ride, we catch a glimpse of the wonderful in Nature that has not been revealed elsewhere. B. F. TaylOr, in his admirable work, Between the Gates, thus describes it: 90 THE GREAT WEST. " The train seems hopelessly bewildered. It makes for a mountain- wall eight hundred feet high, just doubles it by a hand-breadth, sweeps around a curve, plunges into a gorge that is so narrow you think it must strangle itself if it swallows the train ; red rocks everywhere huge as great thunder-clouds touched by the sun, and big enough for the kernel of such a baby planet as Mars ; monuments graven by the winds ; ter- races along whose mighty steps the sun goes up to bed, the glow of his crimson sandal on the topmost stair ; and it is twilight in the valley and midnight in the gorge. It is a fearful nightmare of stone giants, weird witches in gray groups, whispering together in the hollow winds, of the mountains — ^witches' baths for high revels; Egyptian tombs; fortresses that can never be stormed. Yonder, a thousand years ago, they were launching a ship six hundred feet high in the air, but it holds fast to the 'ways' still. Its stately red bow carries a cedar at the fore for a flag. It is a craft without an admiral. Some day an earthquake out of business will turn shipwright, put a shoulder to the hull, and Leviathan will be seen no more." But you are soon in the valley 9f the Weber River, and the cultivated fields, in contrast with the rugged scenery, appear as fair as the Garden of the Lord. Ogden, which is the junction of the Central Pacific and Union Pacific, is also the point where the transfer is made to visit Salt Lake City, made notorious as the home of the Mormons. A few days spent here can be most interestingly employed. The various attractions of the city, as Temple, Tabernacle, co-operative store, can all be seen in a day or two, and the journey resumed westward. The magnitude of undertaking the building of a railroad through this country is more and more impressed upon the mind, and it may be well to consider briefly the construction of the Union Pacific and Central Pacific Railroads. THE UNION PAcaric was chartered in 1862, yet the grading was not done until 1864, and the first rail was laid in 1865. At that time there was no railroad communi- cation from the East, and a gap of one hundred and forty miles existed between Omaha and Des Moines. For five hundred miles westward from the Missouri River the country was completely destitute of timber, and ties were transported from six diflerent States and Territories, at a cost often of two dollars and a half per tie — thus can be seen the difficulties encountered at the outset — ^yet so vigorously was the work prosecuted that in three years six months and ten days the road was completed. TI^E TRIP OVERLAND. 9] THE CENTEAL PACIFIC. But while the plains of Nebraska were filled with the army of work- men, the Sierra Nevadas were teeming with laborers on the Central Pacific. Though the Central Pacific was begun in 1860, several years sooner than the Union, yet the difficulties encountered were so much greater that the construction was not consummated so quickly as in the case of that road. The rails, cars, locomotives, all had to be transported around th§-Horn, and at one time there were thirty vessels en route from New York with supplies for the Central Pacific. The most serious difficulty was the Sierra Nevadas, but by tunnelling and blasting the way was forced through. More powder was expended in the effijrt than was needed to fight half the battles of the Revolution. In April of 1869 ten miles of the road were built in one day. This is probably the greatest feat of railroad-building on record. What is more remarkable about it is, that eight men handled all the iron on this ten miles. These eight giants walked ten miles that day, and lifted and handled one thousand tons of rail each. On May 10, 1869, the two roads clasped hands at Promontory Point, and a railroad from Omaha to San Francisco, a distance of 2221 miles, was built in less than five years. Columbus, sent out by Ferdinand and Isabella to discover the Indies, was halted by a continent ; that continent is now spanned by a railroad. May not imagination picture the form of Columbus standing upon the summit of the Rocky Mountains, with a scroll in his hand, pointing to the setting sun, saying, "There is India; there is the Past"? TO THE SIEEEAS. The trip through the desert in Central Nevada is very monotonous. Sahara itself could not surpass the landscape in woe-begone infertility. This is the dreariest day of the overland trip, and should it be in sum- mer the traveller will find the dust very disagreeable. But the Sierra Nevadas, when reached, are appreciated more fully, however, for the ride of the past day. When evening comes the outlook is desolate and barren, but when the curtain of night is lifted we are in the very heart of the Sierras, upon which the snow falls to a depth of thirty feet, and often the traveller finds himself in winter when the lowlands are hot in August. At Reno the change of cars is made to visit Virginia City, the famous mining camp of the Pacific coast. Near here is Lake Tahoe, one of the finest sheets of water on the continent, and far-famed as a pleasure resort. 92 THE GREAT WEST. 4 Near Truckee the road passes Donner Lake, where a party of emi- grants in 1846 were overtaken by a severe snowstorm, and were com- pelled to spend the. winter. Many perished, and dark tales are told of cannibalism. No one can think of this tragedy without a shudder. In crossing the Sierras the most famous scenery is at Cape Horn, where you peer down a caflon half a mile below. The scenery through this region is grand beyond description, while a peculiar blue haze adds a charm to the landscape. We soon enter the warm lowlands, and reach the capital of the State, Sacramento. The population is about twenty-five thousand. The State Capitol building, a magnificent structure, is the most attractive object to visitors. To San Francisco, the Athens of the Occident, the distance is but one hundred and thirty-eight miles. The overland train first reaches Oakland, a most beautiful city of forty thousand inhabitants, and bearing the same relation to San Francisco that Brooklyn does to New York. Leaving the cars, you enter a splendid ferry-boat and cross the Bay of San Francisco, one of the finest natural harbors in the world. SAN FEANCISCO, a city with a growth of only twenty-seven years, contains over three hundred thousand inhabitants and covers a territory of forty-two square miles. It is a city of boarding-houses; not less than fifty thousand people eat at restaurants, and thirty thousand more at the ninety hotels and eight hundred lodging-houses. The city is celebrated for its hotels. The Palace ranks first, while the Baldwin, Grand, Lick, Occidental, Russ, are among the most prominent. The commerce of the city is very extensive, while ships from all quarters of the globe can be seen in its harbor. The Chinese quarter contains many attractions for the visitor, and will well repay a visit. A guide can be procured from police head-quarters, and a tour of " Chinatown " made in perfect safety. The most interesting objects to be seen are stores, shops, restaurants, and temples (or joss-houses), and opium-dens. The stores are open late at night, and on Sundays as well, and are found in one quarter crowded together. The temples or joss- houses, where they worship their gods or graven images, are open to the public, but the visitor will find the light that constantly burns within to be dim, though not religious. The various gods or images are placed in alcoves, while before them are offerings of food by their worshippers. Some of these temples are very gaudily and expensively ornamented. The theatres are a curiosity. They have no curtain, and when the play THE TRIP OVERLAND. 93 ends the victims in the play are dragged from the platform, or even if the hero is killed in the play, he may get up and leisurely walk away. The orchestra sits upon the stage and discourses music during the entire performance, but " horrible " is the word that best describes it. The ac- robatic performances are really creditable, though a short stay generally satisfies the visitor. The opium-dens can be visited, and this debasing vice be seen as practised by the " heathen Chinee." Woodward's Garden, a combination of museum, menagerie, theatre, aquarium, and botanic garden, has become a favorite pleasure resort. The traveller should drive to the Cliff House, where the seals may be seen disporting upon the rocks and a splendid view of the Pacific Ocean can be obtained. There are two systems of streets, Market street being the dividing- line. The wholesale business of the city is done along the water-front and north of Market street; retail business of all kinds is found in Kearney, Montgomery, Third, and Fourth streets. One noticeable fea- ture is the number of bay-windows in the houses. So numerous are they that San Francisco has been aptly called the " Bay-Window City." The palatial residences of the railroad magnates and "bonanza" kings on Knob Hill are an ornament to the city. The climate of San Francisco is very peculiar. The coldest month is July, when furs and overcoats are in demand. The seasons are not divided as in the East, but into wet and dry. The winter is usually rainy, beginning about October and lasting until May, and it is dry during summer. The mornings in San Francisco are usually warm and bright, but the sea-breeze from the ocean, which springs up about 3 P. M., makes the afternoons and evenings chilly. However, on the opposite side of the bay, at Oakland, and in many suburban nooks where the sea-breeze does not reach, the climate is uniform and delightful. There are very many interesting excursions from San Francisco which can easily be made. The trip to the Geysers will occupy but a few days. Leaving San Francisco in the morning early, you will reach the Geysers late in the evening of the same day. The distance is about one hundred miles north, and will include a ride by steamboat, cars, and stage. The best time to see the Geysers is in the early morning, before the sun has drunk up the vapors. The ground literally boils and bubbles under foot. The steam issues from many holes in the earth, but they are not spouting springs, so that a person should not go with Icelandic pictures in his or her mind, expecting to see anything like them ; but a cafion 94 THE GREAT WEST. filled with vapor and steam boiling and bubbling, surrounded by the wild scenery of the mountains, makes the scene strange and weird. The trip can be made vid St. Helena and return by Calestoga, near where the Petrified Forest can also be seen. The cost of the trip is about sixteen dollars for fare, and time three days. Another pleasant excursion from San Francisco is the trip to San Jos6 (pronounced San Ho-zay), fifty miles south — one of the loveliest inland cities in California, with a population of twenty thousand. From here the distance is short to Monterey, the old capital of the State. But the trip to Yosemite Valley and Big Trees surpasses any other, and is called " the excursion " in California, and you have not seen the wonder of the Pacific coast till you have made this trip. The distance is about two hundred and forty miles, and the train leaves at 4 P. M. There are four different routes, any one of which is very good. The one to Mederia may be mentioned as an example. The train arriving in the evening, the traveller can enjoy a good night's rest, and then have an early start by stage for the valley. This occupies two days, arriving in the afternoon of the second day. The Big Trees can be seen en route or else on the return trip. They are so large that at first one does not ap- preciate their magnitude, and when their great age is contemplated it gives one a queer feeling to look at a tree that may have been waving its green branches high in the air before Julius Caesar landed on the shores of Great Britain. Yosemite Valley, th^e " Mecca of the Beautiful," will awaken new visions of beauty that cannot be seen elsewhere ; but as the famous resort has been so admirably described elsewhere in this work, a description will not be attempted here. The cost of the trip for fare is sixty dollars, and the time from San Francisco is a week to ten days. SOUTHERN CALIFOENIA AITD ARIZONA have been lately opened to public travel by the building of the Southern Pacific Railroad, which now extends from San Francisco to Central Arizona, and is being rapidly pushed forward, and will soon make a Southern Transcontinental route. The scenery along this highway is varied, as the road passes through a desert; and, what is remarkable, in the Tihachapi Pass, where it crosses a range of mountains, it forms a loop and recrosses itself, one portion of the track being far above the other. This is probably one of the most difficult feats of engineering in the world. Los Angeles, the metropolis of Southern California, contains about THE TRIP OVERLAND. 95 sixteen thousand inhabitants, and is situated four hundred and seventy miles south from San Francisco. Here oranges grow in perfection, and all the semi-tropical fruits flourish in abundance. This city will furnish a pleasant sojourn for the traveller. Arizona, which has so long been barred to the travelling public by the difficulty of access to it, is now being penetrated by several lines of rail- roads, and this unknown part of our country will be more fully explored and settled in the next few years, as the recent valuable mineral develop- ments are attracting great attention. This State can be reached by rail from Los Angeles, and offers many points of interest to the traveller. THE TRIP TO OREGON can be taken by the Oregon Steamship Ojmpany's steamers, which ply regularly between San Francisco and Portland, sailing every five days. The trip occupies two to three days, as the distance is over seven hundred miles, but not two days on the ocean, as the Columbia River furnishes over one hundred miles of the voyage before reaching Portland. This is the route most patronized, and does the bulk of the business, but should the traveller prefer it the trip can be made md Sacramento by railroad to Eedding, and then two hundred and seventy-five miles of stage, which goes through some of the finest of scenery, passing Mount Shasta, the famous mountain of Xorthem CaHfomia, to Roseburg, and thence two hundred miles by rail to Portland, the metropolis of the North- west. This city of twenty thousand inhabitants does more busiaess for its size than any in the United States. The scenery of Oregon and of Washington Territory is among the finest in the world. The river-steamers on the Columbia are fitted up very handsomely, and a sail up the river will be foimd exceedingly en- joyable. The Cascades contain some wild and grand scenery. Here a transfer for a short distance must be made by rail, and then another steamer taken. Should the excursion extend to Wallula (or Walla Walla), the scenery will be found magnificent, and if it should be in harvest, when the immense shipments of wheat are made, the traveller will be amazed at the resovirces of this inland empire. The tide of emigration is tending strongly to Eastern Washington and Oregon, where the vast extent of lands adapted to wheat>raLsing is rapidly being occupied. This imdoubtedly is one -of the finest wheat- producing sections of the entire country, and railroads are being rapidly constructed toward this portion of the land, when in a few years several outlets will be given to the immense supply of surplus products. 96 THE GREAT WEST. From Portland a trip can be made to Puget Sound, one of the finest sheets of water on 'the continent, and which has been well named the " Mediterranean of America." Seattle, which is the largest town on the Sound, does an extensive coal-shipping business. From here the trip can easily be extended to Victoria in British Columbia, which is a beau- tiful place of five thousand people. In this section the scenery is very striking and grand. -The opinion is prevalent that a trip to Alaska is very disagreeable and unpleasant, whereas, on the contraiy, it is one of the most delightful of summer ocean-voyages. The regular steamer " California " starts from Portland the first of each month, and touches at Victoria, B. C, on the way to Sitka. This part of the voyage is in open sea, but the tourist can cross the Sound and meet the steamer at Victoria, when the continuation of the voyage is as delightful as river-sailing. The inland passage, as it is called, lies between the islands and mainland nearly the entire distance, and mountain-peaks rising to great heights on either side often very near to the vessel, while waterfalls and cascades add new beauty to the scene, present a panorama of the beautiful in Nature for nearly a thousand miles, unequalled perhaps in the world save in the open sea of Japan. The town of Fort Wrangell, at the mouth of the Stickeen River, is the trading-post for this region and the supply-station for the Stickeen mines. While ihe ocean-steamer is landing and discharging cargo, if the traveller could arrange with one of the river-steamers to ascend the Stickeen River and see the immense glacier, one of the largest in the world, he will be amazed and delighted with the scenery of the trip. The voyage to Sitka, where many curious specimens of Indian carvings can be obtained, will occupy a few days longer, and the entire round trip from Portland but two to three weeks. ' It is impossible to fully describe the beauty of this voyage. The water is so smooth, the land constantly in sight, the traveller can hardly believe he is on the ocean. Suffice it to say that for a summer trip of a few weeks the voyage to Alaska cannot be surpassed, and all on board the California in August, 1879, will agree with the writer in this assertion. TO THE WEST! TO THE WEST! BY CHAELES MACKAY. To the "West ! to the West ! to the land of the free, Where mighty Missouri rolls down to the sea ; Where a man is a man if he's willing to toil, And the humblest may gather the fruits of the soil ; Where children are blessings, and he who hath most Hath aid for his fortune and riches to boast ; Where the young may exult, and the aged may rest, — Away, far away, to the land of the West ! To the West ! to the West ! where the rivers that flow Run thousands of miles, spreading out as they go ; Where the green waving forests that echo our call Are wide as old England, and free to us all ; Where the praiifies, like seas where the billows have rolled, Are broad as the kingdoms and empires of old ; And the lakes are like oceans in storm or in rest, — Away, far away, to the land of the West ! To the West ! to the West ! There is wealth to be won ; The forest to clear is the work to be done ; We'll try it, we'll do it, and never despair While there is light in the sunshine and breath in the air. The bold independence that labor shall buy Shall strengthen our hands and forbid us to sigh. Away, far away ! Let us hope for the best. And build up new homes in the land of the West ! 7 97 COLORADO. BY W. B. VICKEES. GENEKAL HISTORY. EARLY in 1541 an expedition, well armed and equipped, under com- mand of Vasquez Coronado, a Spanish military chief, was fitted out by the viceroy of New Spain to explore the country lying to the north- ward, comprising what is now known as New Mexico, Arizona, and Col- orado. Previous to this, however, between the years 1530 and '40, two or three partial and unsatisfactory attempts had been made to explore the country by Friar Niza and others, who had returned to Mexico with highly-colored accounts, secured from Indians, of untold wealth existing in a section termed the " Seven Cities of Cibola." Stimulated by these reports, the viceroy of New Spain was induced to organize the expedition under Coronado, and early in January, 1541, the band of explorers, con- sisting of about four hundred men, many of them cavaliers of distinc- tion and of the best blood of Spain, left Compostella, a point on the coast of Mexico nearly due west from the capital, and commenced their journey. For a long time they kept near the shores of the Pacific Ocean, then made their way back into the country. On the Gila River, Coronado found thickly-populated settlements, but no evidence of great wealth. Continuing his march in a north-easterly direction, in fifteen days he reached Cibola, but, instead of the fabulous wealth that had been reported, he found a town of about two hundred inhabitants, having but little knowledge of any gold and silver treasure. These people were probably the ancestors of the present tribe of Zuni Indians. Continuing in a general north-easterly direction, he crossed the Rio Grande del Norte, and entered the San Luis Valley, making his way out over the Sangre de Christo Pass to the plains of Southern Colorado ; thence southward 98 CLEAR CREEK CaSON, COLORADO. COLORADO. 99 to Mexico, returning with a record of disappointment that resulted in an abandonment of all effort in that direction. Up to the year 1600 the territory comprised within the present limits of Colorado was supposed to belong to Spain, but in that year France claimed possession. During the seventeenth century at least three expe- ditions were sent into these vast and unknown regions. In 1769 the province was ceded to Spain by France, but in 1800 the French regained control, keeping it until 1803, when by treaty and purchase the United States became the owner of the province, and took prompt measures to establish its authority and government in due form over the country. In 1806, Major Pike, by authority of the War Department, with a party of twenty-three men traversed the entire extent of Colorado, north and south, without finding a single settlement of civilized beings ; only the wild savages roamed over the land. In 1819, Colonel Uong's expedition entered the country, following up the South Platte River to where it escapes from the canon. A careful examination was made of some of the mountains and of the plains from the South Platte to the Arkansas. In 1832, Captain Bonneville made a very thorough explora- tion of the Rocky Mountains in the interest of the American Fur Com- pany, and is said to have been the first who proved that the head-waters of the great rivers flowing east and west had their origin nearly together in the great Sierra Madres. In 1843, Colonel Fremont commanded the next expedition sent out by the United States government. He camped some time in the St. Yrain Valley, and afterward journeyed north, reaching Fort Laramie. He found the Indians already troublesome to parties who were passing through the country on their way to California. There is no evidence to show that there were any white settlers in Col- orado previous to 1843, save trappers, traders, and employes of the Amer- ican Fur Company. There was no knowledge of the treasures hidden in the soil or in the rocks at that time. The vast country was given over to the savage Pawnees, Cheyennes, Arapahoes, and Utes. From the time of Fremont's last expedition in 1844 up to 1858 the "country was under no regular form of government. The only recognized authorities were the Fur Company and the United States military, and these were confined to the limits of the posts and forts. In 1852 came the discovery of gold by one Parks, a Cherokee cattle- trader, who, en route to the shores of the Golden Coast with a party of followers, discovered the precious metal on the banks of Ralston Creek. Tidings of this discovery after a long time reached Georgia, and in 1858 Russell's expedition was organized, reaching Cherry Creek in June, 1858. 100 THE GREAT WEST. In the fall Russell returned to Georgia, taking with him his precious sam- ples and giving glowing descriptions of the country. The Pike's Peak excitement then began to spread, and palefaces, with immense trains of supplies, commenced traversing the great Plains, and disputed possession of the country with the Indians, who refused to recognize the right of the white men to occupy their vast domains. But the onward march of the Caucasian could not be stayed, and by the time the winter of 1858- 59 set in settlements had been made at Auraria and other points, and at least four hundred persons were in the Territory. In the spring of 1859, Green Russell's journal was printed by Major D. C. Oaks, with descriptions of the best routes to the new Land of Prom- ise. This book, full of glowing descriptions of the Land of Gold, was extensively circulated throughout the Eastern States, and caused thou- sands to leave their homes and turn their faces westward to the land of untold treasures. The discovery of the first gold-bearing lode was made in Gilpin coun- ty, May 6, 1859, by John H. Gregory, and ere long the gulches were full of prospectors and all the mountains in the vicinity covered by eager seekers after the shining ore. By the spring of 1860 at least twenty thousand persons were scattered over the country, and the development of the greatest mining district in the world had begun. Silver ore was discovered as early as 1861, but not until 1864 was it actually demonstrated beyond question that there existed in this new re- gion of mineral wealth the richest belts of silver-mines in the known world; and an impetus was then given to mining enterprises that rivalled that of California in its early days. The necessity of local laws and the taking of steps to connect the district with some legislative body was soon apparent. A county was therefore defined and named Arapahoe, with Auraria as the county-seat; a representative sent to the Legislature of Kansas, as well as a Delegate to Congress to secure recognition and the establishment of a Territorial form of government. An organization imder the name of Jefferson Ter- ritory was perfected and a provisional government formed. This body passed the act consolidating Auraria and Highland under the corporate name of Denver. Ditch and wagon-road companies soon followed, and healthy legislation prepared the way for the inauguration of a Territorial form of government. February 26, 1861, Congress passed an act, and Colorado took her place under the fostering care of the general govern- ment. In May of the same year the Territory had a population of 25,329, of whom 4484 were females. In September a Delegate to Con- COLORADO. 101 gress was elected and took his seat. Nine counties had been organized, and a Legislature chosen by the votes of the people, ^ During the period of the war of the Rebellion the country did not de- velop as rapidly as might have been expected, although speculation was rife and very many mining companies were organized in the East, stocked at enormous figures, and placed on the market. The great majority of these came to grief, and by the year 1866 the mining-camps of Colorado wore a very discouraging appearance. In 1864 and '65 the Plains Indians inaugurated war upon the white settlers, and during these years numberless disasters occurred. But little communication could be had with the States. Stages had to fight their way through. Wagon-trains were attacked and destroyed, and machinery of immense value was abandoned in the endeavor to reach the camps. But the gradual advances of the Union Pacific and Kansas Pacific Rail- ways had their due effect, and the Indian fell back as the whistle of the locomotive was heard over the desolate prairies, and Civilization's finger pointed the savage to the parks and valleys on the western slope, where, by treaty, they were secured, for a time, the hunting-grounds they de- sired. In 1867 the Union Pacific Railroad reached Cheyenne, and Denver was thus brought within 104 miles of direct communication with the East, In 1868 the Denver Pacific, to connect at Cheyenne with the for- mer road, was begun, and finished in 1870 ; in which year also the Kan- sa.s Pacific reached Denver and the Colorado Central was constructed to Golden. From this date the prosperity of the country and the perma- nence of the towns already established were assured. Little attempt had as yet been made to establish any industry save mining ; but the settle- ment of the Union Colony at Greeley in the spring of 1870 was the in- auguration of a development of the agricultural resources of the country and an earnest of its stabiliiy. The success of this colonial experiment having been demonstrated, others followed in its wake — one in Wet Moun- tain Valley, one on the South Platte River, one in the valley of the St. Vrain, and one at the junction of the Monument and Fontaine-qui- Bouille. Towns were founded, farming settlements established, and indus- tries of every kind prospered. In 1871 the Denver and Rio Grande Railway began to feel its way southward, reaching Colorado Springs in the fall of that year, and in a short time afterward it was extended to Pueblo. About this time (1870) probably forty thousand people were in the Territory, but the means of communication being now rapid and assured, 102 THE GREAT WEST. it was believed that a steady growth in population would follow ; which was found to be true. The mines were producing largely of the precious metals, the farmers rejoiced in the possession of bountiful harvests, and the cattle upon the Plains prospered and increased rapidly, to the delight of those who had invested in stock. In 1874-75 a second effort was made to establish a State government, and proved successful. On July 4, 1876, Colorado entered the Union as the Centennial State. In 1876 the Atchison and Topeka Railroad reached Pueblo, giving the State a third outlet to the East. The following year the Carbonate Camp at Leadville began to attract attention from all parts of the State, and the Denver and South Park road, begun in 1874, and built to Morrison in that year, began to reach up Platte Caaon, while the Colorado Central had been extended to Georgetown, and a broad-gauge line built north to Longmont, tapping the great agricultural area of the State. The Denver and Rio Grande pushed its way over the Sangre de Christo range, and rested at Fort Garland, preparatory to reaching the shores of the Rio Grande del Norte at Alamosa. Meanwhile, during these years important geological and geographical surveys were being conducted by the United States government under the superintendence of Professor Hayden, and their reports, when published, became important factors in the develop- ment of the internal resources of the country, attracting the attention of the people of the entire Union. These reports have been of value, and have very materially aided in advancing the general prosperity of the country. The opening of the year 1880 shows Colorado to be making rapid strides toward the front rank as a mineral-producing region, while her • agricultural resources are also being permanently developed. Her climate is the admiration of invalids, her scenery the delight of tourists. She has yielded out of her bountiful bosom ten billion dollars of gold and silver since 1859. Her real estate and personal property foot up over seventy- five million dollars. She has thirty-one counties, having a population of nearly two hundred and fifty thousand. The counties in which farming ■ and stock-raising predominate are "Weld, Larimer, Boulder, Jefferson, Arapahoe, Douglas, El Paso, Fremont, and Las Animas. Those devoted almost wholly to cattle and sheep are Elbert, Bent, Pueblo, and Huerfano. The principal mining counties are Park, Lake, Gilpin, Clear Creek, Summit, Custer, Hinsdale, San Juan, and Ouray. The growth of the cities and large towns has been proportionate with the general advance of the State, and everywhere new towns have been COLORADO. 103 created by the extension of the railway system and the discovery of new mines. CJLIMATB AlTD HEALTH. ' The climate of Colorado, to which so many are looking as a possible home, is an important topic and one to be carefully considered. A few statistics, therefore, gathered from the reports issued by the Signal Service station at Denver, will give information of value in reference to the at- mospheric condition of the country during the period of one year. The entire amount of precipitation (rain and melted snow) was 10.86 inches. This accmnulated from rains and snows, which fell on sixty-one days. But two storms during the year exhibited unusual severity. The first took place May 11th, the second July 22d. There were 190 clear days, 139 fair or partly clear days, and but 35 reported cloudy. The temperature, while it exhibited some sudden changes, was not of unusual range. The highest reading, 98° above zero, occurred on July 13th ; the lowest, 17° below, was on December 24th. During the' year the ther- mometer read 96° or above but seven times. It read below zero on six days in January, one in February, and six in December — thirteen in all. The mean temperature for the year was 50° ; the mean for July, the warmest month, 74°. The last frost of spring appeared April 27th, while the first frost of autumn was observed October 9th. The former was not as late as usual, nor the latter as early as. in other years. Each month furnished south as the prevailing direction of the wind. Colorado is included in the boundaries of the temperate zone. The Plains portion is within the isothermal lines that take in New York, Columbus, and Council Blufis. The foot-hills are included in the lines that embrace Boston, Albany, Detroit, St. Paul's, and Omaha. The main range and the western half of the State show the same lines that include Halifax, Burlington, Montreal, the upper Lake Superior region, and ihe head-waters of the Red River of the North. But the extremes of heat and cold are not so great as at these, points. The absence of any very great quantity of moisture has a wonderful effect upon the air, and Colo- rado is famous for its clear skies and invigorating atmosphere. The cloudy days are so few as to be considered a rarity. The average tem- perature of the Plains is from 50° to 55° ; of the foot-hills, from 45° to 50° ; of the mountains, 40° to 45°. As has been admirably summed up, " The results of the climatological conditions of Colorado are an extremely healthful and invigorating atmosphere, peculiarly beautiful and enjoyable, well adapted to all pursuits and all out-door avocations." It might be 104 THE GREAT WEST. added that as a health resort Colorado is without an equal for the cure of tubercular and pulmonary affections, asthma, and dyspepsia. Consumptives who reach the country before the disease has too greatly developed are almost certain to recover; those in whom the disease has advanced will find it possible to live for many years in compara-' tive comfort and vigor. But it is unwise for those who have suffered for years, and in whom the insidious enemy has become deeply rooted, to seek Colorado expecting a cure. Confirmed cases are as hopeless as in the East ; in fact, the end is likely to come sooner, on account of the very rarity of the air and the necessity of increased respiration. These, in the early stages, are conducive to recovery; in the later, to a speedy ending of the life of the patient. Asthma, however, in its most aggravated form, and no matter how long seated, is relieved in every instance by a residence in Colorado. The right altitude to suit the patient's case having been found, relief is at once felt, and a perfect immunity from this distressing complaint may be relied upon as long as one remains in the country. Hence it follows that those who seek Colorado for relief from asthma must expect to make their home for life in the State. A temporary residence will not suifice, since the disease, apparently, is not eradicated. A return to the old home would carry with it a return to the old troubles in a very short time. The change of residence must be considered permanent, therefore, and those who are afflicted and would be relieved must accept this fact as one not to be questioned, and prepare their plans accordingly. Dyspepsia is one of those distressing complaints connected with the condition of the human system which will lead the sufferer therefrom to adopt any course from which relief may be obtained. The most pleasant sugar-coated remedy we know of is to live in Colorado, thus recovering the lost powers of assimilation, and in its bright days, inducing out-of- door exercise, and its cool nights, wherein refreshing slumber is assured, find a sovereign panacea for one of the most grievous ills that flesh is heir to. Once more may food be relished and enjoyed, and hearty meals be made on substantial bread, blood-invigorating beef, tempting mountain- trout, and juicy wild meats, without the fear of an after-punishment. Many other diseases that afflict humanity are partially eradicated or relieved by a change of residence to the altitudes of the Kocky Moim- tains, but it would be impossible to enumerate them all. There is an exception, however, it would be proper to name — catarrh. It is ex- tremely doubtful if the peculiar dryness of the atmosphere is favorable to the cure of this disease. In fact, it is asserted by high authorities that iiorsTArs OF the holy cross, Colorado. COLORADO. 105 the dryness tends to aggravate many cases by forming concretions on the inflamed mucous surfaces, and so irritating them. The rainfall is so meagre, the fine dust so common, that these are causes naturally tending to further the advance, rather than retard the progress, of catarrh. There is no country yet discovered in this world that has in it the elements of cure for every ill that human flesh is unfortunately subject to. When such a country is discovered on this habitable globe, paradise will lose some of its prospective charms, and the song of " I would not live alway" be paraphrased to suit this desirable location. 8CENEEY — CAffONS OF COLOEADO — POINTS OF INTEREST. On the upper Cache-la^Poudre may be found some very wild and ro- mantic spots. It is a point as yet but little known to tourists, though sportsmen have found that it furnishes excellent trout-fishing, with an occasional bear- or deer-hunt thrown in by way of giving variety to it. The solitude of the mighty pine forests that crowd to the very water's edge at occasional points has a calm delight in it that must be experienced to fully realize its delightful charm. Here and there beautiful parks and lovely meadows break the monotony of the forest, and offer a landscape that would tempt an artist to linger long enough to catch its beauties and pinion them upon his canvas. Secluded glens abound, suitable for cozy camping-grounds, and the murmur of the limpid waters of the Cache-la- Poudre, as they rush with precipitate haste to seek the bosom of the South Platte River, falls most musically upon the ear. A week can be pleasantly spent in this vicinity by those who like the silence of the woofls for their souls and the succulent sweetness of trout for their sus- tenance. Estes Park is now rapidly growing into popular favor as a, summer pleasure resort, and is likely to be still better known in the future. It is easily reached by a few hours' ride from Longmont, on the Colorado branch of the Union Pacific Railway. Lying at the base of Long's Peak, the third highest mountain in the State, Estes Park is a lovely emerald area hemmed in by mountains and full of meadows and groves, with here and there a sparkling trout^brook. To " camp out " in Estes Park is the height of enjoyment for hundreds of the country-people within fifty miles of the park, and indeed city-folks and Eastern pleasure- seekers are beginning to discover that out-of-door enjoyment can here be realized to its fullest extent at a point where " the scene is replete with grassy slopes, crystalline streams that course down from the melting snow-banks, broad zones of pine forests, towering heights of mountains, 106 THE GREAT WEST. and shadv nooks." Such a spot as this is one for the tourist to linger in during the summer months, -when numberle^ wild flowers burden the air with theit perfume. Boulder and its vicinity are prolific in health resorts and ftoints of interest to visitors in search of the elixir of life and of pleasure. At Springdale, near bv, it possesses a spring whcee waters are a sparkling seltzer that is verv efficacious for cases of scrofula and for diseases of the blood, while their location, in the immediate vicinity of a large number of valuable silver-mines, lends them an additional attraction. But Boulder Canon is the admiration of all, for it has been very aptly de- scribed as Colorado's Yosemite, Many of the well-known places in tlie East, such as the Delaware Water-Gap, the point where the Potomac passes through the Blue Eidge, or even Xiagara Falls, wane in grandeur before the scenery to be encountered at every step in this magnificent theatre of Nature's faultless construction. The walls stand up, at points, two thousand feet high, while below leap and sparkle the crystal waters of the stream as they hvury over the big boulders from whence the river takes its name, to leap into the arms of the St, Vrain, awaiting them on the plains below. The infinite variety of the scenery hereabout is a con- stant surprise : the foliage has a beauty whose refireshing charm never tires ; while at tiie falls proper, where the water drops fifty feet from the rocky edge into a deep basin, above which the rocks tower in solemn grandeur, one can only, with hushed bfeath, look, linger, and admire. This caflon has not been " written up '' as much as some others in the State, but it is to be said in its behalf that there are few more striking in the points of grandeur presented. Clear Creek Canon is one of the most sublime of Xature's handiworks, and, in addition to its natural attractions, teaches a lesson by which the ingenuity, the persistence, and the power of man are shown by utUiring even the most rugged paths and almost inaccessible points for his own purposes. The ride by rail up Clear Creek Canon must be made by all who visit the State, or they miss one of its greatest attractions. To the sublime scenery of the hills is added the skill of the engineer, and we behold Xature and art in such happy combination as we follow the serpen- tine track of the narrow-gauge railwav up the steep declivities of the caflon, over beds cut out of sohd granite walls, over numberless bridsji-s across the same sinuous stream, that the ride to Central Citv is one long period of bewildering suspense, for we do not know what we may see next, and of overwhelming wonder as siuprise follows sui-prise last as the shadow hides the sunshine, while we glide in and out under over^ COLORADO. 107 hangmg arches or between the m^ed defiles. At Unuis the waters of the stream touch the ver\' rails oar car i? on ; again they are to be seen dashing over the Jiones manv feet bdow. The nomb^ of Iwidgts i* about twentv-five on this short line erf railway, and the diang^ now on tMs side, now on the other, as we ^ide along over a highway of short tangents and ntunberles; carves, are enough to bewilder those who are onaiccastomed to the moantain-scenray. The climbing is at the rate of one himdred and seventy-five feet to the nule, and the foliage of the pines against the sombre gray and brown of the rocks presents a constant series of ever-fihifting views whose beaur\- is as rare as it is indescribable. We would like to give more space to the wondeifnl canons for whidi Colorado Is so remarkable, but cannot. We can only say that if you want to S€e Xature in all her roj^ed grandeur and rude sublimity, aaso- dated with skill in art, in a combination of the beantifdl and the usei'al, yon can see her in Clear Creek Canon, and need not eros? the seas to htmt for her among the monntains of Switzerland. Pl^te Cafion is another wonda* ; and mention of its name reminds us of the s^ing of some one, that " the Lord didn't make Platte Cafion ; it was a fieak of Xatnre ;'* and we are almost inclined to agree with him, for the mountain-scoiery here opoied up to the tourist world by the en- trance into and parage through Platte Canon by the Denver and .S:>uth Park BaUway is singularly imiqne. Here is presemed mountain-scenery that has been, on account of its ccmpaiative inacc^sibility, hitherto im- known. In these wilds and festne^es are hidden scenic beauties and natural wonders that fer exceed ai^thing yet desmbed by tourists and engineers. Twenty miles firom Denver the visitor reaches the entrance to the canon, and fiom thence to the top of the pas there is a gradual ascent of fiom one hundred and thirty-seven to one hundred and fifiy- d^t feet to the mile. The curves on this road are not quite as sharp, nor the hills quite as high, as in Clear Creek Canon, but the angry torrent is here, dashing offcen over solid beds of rock without sand, gravel, or boulder. Here and there are little stretches in the stream where the water glides along as smoothly and as unruffled as one's thoughts glide in a dream where love and happiness constitute the principal charm in the sltmiberoas blis. As one has described it, " walls of granite, rising per- pendicularly to a height of five himdred feet in s<:'me places, to fifteen hundred in others, capped with columns, pyramids, domes, and grotesque figures resembling nothing, rise up on either side of the river, overhang- ing it and the puny track at their base in many places. Anon the spark- ling waters of a cataract come dashing down the mountain-side fiom a 108 THE GREAT WEST. thousand feet overhead to join the sheeny tide that murmurs its sad re- frain at the bottom of a gorge ; then a lateral cafion is passed, glorious in its wealth of verdure or grim in its poverty of life ; here a grand old hill, exquisitely rounded and covered with a beautiful growth of pine or spruce ; near it a weatherbeaten mound, so thickly strewn with fallen timber as to suggest a mammoth game of jackstraw, with the Devil and his imps for players ; opposite it, mayhap, a perpendicular wall of gran- ite of varied hue — ^greenish-yellow, yellowish-pink, gray and black mot- tle — the ever-changing lichens lending additional beauty to its wrinkled front ; then a mass of gnarled and twisted granite, gnarled into twists and twisted out of all semblance of shape. Thus for ten miles or more the caflon presents a panorama of Nature in her wildest, most weird, and grotesque moods." About Colorado Springs, within a radius of twelve miles, there clusters a greater number of natural scenic beauties than anywhere else in the State. These points have been written up by journalists and tourists .and bookmakers to so great an extent that their names are familiar to all, and Manitou, Cheyenne Canon, Ute Pass, Garden of the Gods, Glen Eyrie, Queen's Caflon, Monument Park, and Pike's Peak are as house- hold words everywhere. Manitou has become the fashionable watering- place of the Western continent. It has an elevation of 6321 feet in six miles from Colorado Springs, and has six famous mineral springs, whose medicinal qualities have been highly recommended. Manitou in summer is a rural paradise ; the waters of the Fontaine-qui-Bouille ripple music- ally through the romantic valley ; along the banks of the stream cotton- woods, pines, cedars, and willows abound, giving abimdant shade, aside from that cast by the hills about it. In this secluded retreat charming cottages abound, and many of the wealthy and well-known citizens of the United States here seek during the summer months that recreation and repose so much needed by brain-workers. Ute Pass is a narrow roadway built almost out of perpendicular walls of rock and full of tiny waterfalls, where the Fontaine-qui-Bouille drops down from its source in the hills beyond ; but its solitude has been for ever destroyed by the track of the long wagon-trains and the uncouth voices of rough mule-drivers en route to the Carbonate Camp. It is still, however, visited in the cool of the evening by the habituds of Manitou. The Garden of the Gods, as it is called, lies about two miles west of Manitou, and is easily reached ; it is a singularly picturesque spot, replete with interest. Two high ridges of white and red sandstone rocks rise perpendicularly in air about three hundred feet high, forming a sort of COLORADO. 109 amphitheatre, the entrance to which is an opening in rocks but a few rods apart. There is a weird grandeur about this spot suggesting natural forces that must, in ages long past, have mingled and combated with fiery en- ergy to leave behind them such monuments of fantastic shapes. Cheyenne Caflon is some seven miles south of the city of Colorado Springs, and a carriage-drive there gives one an opportunity to explore the quiet beauty and enjoy a few hours of unmixed pleasure. The path up the canon is intricate, and can only be made on foot, but it will amply ' repay those who find their way to the foot of the seven falls to watch the ribbons of liquid silver unfurl and droop downward to the basin waiting to gather and hide them in its bosom for a moment, and then send them coursing down over the stones to the outlet beyond. Glen Eyrie, the summer residence of Gen. William J. Palmer, Presi- dent of the Denver and Eio Grande Railway, is a lovely dell, full of points of interest and beauty, especially Queen's Cafion, with its charm- ing waterfalls, Hebe's Bowl, tiny rivulet, and rugged scenery. Monument Park takes its name from the • many remarkable forms carved out of sandstone in days agone by. Scores of columns can be found standing, alone, in groups, and in combined masses, each one sur- mounted with a cap of some harder material, probably sand cemented with oxide of iron, and so more capable of resisting erosion. Air, rain, snow, water, have left behind them a record full of curious interest to the tourist, of study to the geologist, in these monuments, and the visitor can fake unqualified delight in tracing beast, bird, man, woman, cathedrals, groups of statuary, and the multifold forms of art and Nature in these grotesque formations. Caflon City is the warder of a combination of cafions whose natural beauty borders on the sublime. These caflons and gorges are full of pleasure to all who take delight in beholding the wonderful beauties of Nature in all her ruggedness of repose. We can touch but briefly upon a few of these. Grape Creek Caflon is named from the vines that hang so abundantly upon its crags, and the defile is singularly beautiful ; its sides present rocks with all the colors of the rainbow, lifted up to various heights, and of all shapes, some of them extremely grptesque. Temple Cafion, entered from Grape Caflon, has thus been described : " Nature has carved a wondrous structure which is an exact counterpart of what we mortals know as a theatre. Before a broad floor there stands an im- mense stage, with a flat and flies and wings and dressing-room ; while the broad plateau in front makes an excellent orchestra, and one may readily find room for the fancy that the ledges towering hundreds of feet above 110 THE GREAT WEST. may, in some distant age, have been used as galleries for- low-grade gods who wished to see the play." Oak Creek Caflon, fifteen miles distant, is another point replete with interest ; and when the tourist reaches Curios- ity Hill he finds it aptly named, inasmuch as it is covered with all sorts of odd and unique specimens of minerals of more or less value. By the use of the pick or by blasting crystals of remarlcable beauty are found imbedded in agate of various colors. Oil Creek Caflon takes its name from the evidences along its banks of the presence of petroleum. Its rocks are full of strange formations that suggest many familiar forms to the beholder. It has been described as a great natural arfc-gallery, full of fortifications, of pictures, and of sculptured figures. There are other points of interest in this vicinity that we might name had we space, such as Marble Cave, Talbot Hill, and the celebrated coal- mines, where one can ride for miles through the drifts on a small wooden car, deep down in the bowels of the earth and away from the bright, warm sunshine and^he sweet influences of the outer world. The dark- ness suggests that gnomes might well abound in such a locality, and sjjring out at any moment to demand toll of the helpless victim caught in the darkness and the gloom of their underground hiding-place. The Grand Canon of the Arkansas and the Royal Gorge are now open to the railway-travel of the country, and one can stand upon the brink of vast precipices and gaze down two thousand feet — so far that it is almost impossible to see the foamy current of the Arkansas River as it rushes in tumultuous torrents over its " cribbed, cabined, and confined " narrow bed. In this deep defile the sunshine seldom penetrates, and the blue sky is as much a novelty as a pencil of sunshine would be suddenly streaming through a keyhole into a cell to its solitary occupant. The old way of seeing the caflon was from above, but its sublime grandeur is heightened by observations within its defiles. One can look up without dizziness, biit to look down is often dangerous ; one glance is sufficient to many who are not counted timorous. To look down a perpendicular wall two thousand feet is no trifling performance. Looking up, one sees " overhanging crags, black and blasted at their summits, reaching up into profoundly dizzy heights, while monstrous rocks threaten to topple down and carry to destruction any foolhardy climber who would venture upon them." More of awe than admiration is excited by a visit to this caflon and gorge. The tremendous forces of Nature, as displayed in this bit of her handiwork, are calculated to impress solemnity upon the mind of the beholder ; for, added to the sublimity, there is a certain underlying sense of danger in the situation that makes one ever cautious of speech COLORADO. Ill in a defile where sound can dislodge a fragment of rock and send it hurt- ling down to the ground on which stands the awestruck visitor. La Veta Pass is another point of exceeding great interest. One must have seen the mountain-regions in the early days in Colorado, when " bull- teams " and " prairie-schooners " were the only conveyances within the reach of the traveller, to fully appreciate the ease, convenience, and swift- ness of travel in these railway eras. One of the finest rides in the world — rivalling, and perhaps excelling, the famous scenery in the gorge of the Wahsatch range lying south of Salt Lake — is found in the enchanting trip from La Veta, a cozy little village lying at the feet of the Spanish Pealcs, over the celebrated Sangre de Christo range to the summit, from whence the road runs down to the valley of the Rio Grande del Norte. It is one of bewildering beauty, and has called forth the encomiums of talented writers and of people of all grades and professions. One is lost in wonder at the skill displayed as seemingly inaccessible heights are scaled and the gallant little engine puffs and pulls its train around Mule- shoe Bend, where it takes a run of two miles to gain a distance of one quarter and four hundred feet in elevation. From La Veta to Garland the ride may be denominated one magnificent panorama of natural beauiy, changing as the conformations of the kaleidoscope change. Here are to be met towering and storm-splintered crags, whose vast masses of prim- itive porphyry tell a silent but suggestive story of the days when the fiery element forced them upward into the atmosphere. In the distance, like a dream of glory. Sierra Blanca lifts its eternal snow-covered sum- mit to the empyrean, 14,464 feet above the level of the sea, the superb culmination of that mighty accumulation of mountain-ranges known as the Sangre de Christo. The pass at its summit is 9339 feet, and the Denver and Rio Grande Railway was the first in the United States to attain such an elevation. In a distance of a little over fourteen miles an elevation of 2250 feet is reached. In order to make the comparison clearer, we will mention that the elevation at the summit is one mile higher than at Pueblo, while Blanca Peak towers still a mile higher. Buena Vista is the latest candidate for the favor of the tourist, and during the coming season of travel will claim, and readily obtain, its share of attention. It is located on both sides of Cottonwood Creek, near where it empties into the Arkansas, and at the entrance to a pleasant valley opening out on a plateau some five miles wide. A park containing a large lake has been set apart for public use, and sailboats are kept for the accommodation of visitors. Good hunting and fishing are in the im- mediate vicinity, while five miles from the town are the celebrated Cotton- 112 TEE GREAT WEST. wood Hot Springs, becoming favorably known for their efficacy in curing rheumatism and neuralgia in their most aggravating forms. In the im- mediate vicinity are some of the noblest mountain-peaks of the mighty range, lifting their summits up to the clouds. There is but little doubt that Buena Yista, with its splendid site, beautiful scenery, close prox- imity to first-class hunting- and fishing-grounds, located at the junction of two railroads, which here intersect each other, will in the near future make this the tourist-town of the Arkansas Valley. Ten-Mile Cafion lies midway between the passes on the grand conti- nental Divide, covering a distance of perhaps twenty miles. The railroad projected from Georgetown to Leadville will pass through it. To the tourist the views hereabout will be at once entrancing and bewildering, for here Nature has grouped her wonders into a scene of lavish and pic- turesque confusion. The canon is destined in the near future to be one of the most popular resorts in the mountains. The landscape is singularly broken and strikingly picturesque. A writer in describing this cafion, of which comparatively little is known, says : " What a storm is to the ele- ments the canon is to the surrounding scene. It stands alone and apart from all the rest — a rugged defile dropped in the midst of the rugged mountains. Led into it by the ripple and flash of foam-crested waters, one pauses in the midst of miniature cascades to watch through the spray- laden air the grand ascent of the rocky barriers which shut it in. Thou- sands of feet in air they rise precipitously, not swart and black as other ramparts do, but variegated as the colors in a picture ; on a ground of glittering white are veins of crimson, blue, and gold ; the rocks mirror on their surface all the colors of the rainbow. Artists would call it a mountain-gorge shut in by walls of variegated marble. It looks like layers of distinct and curious formations. But in one rock, a vast mass of veined granite, it catches and reflects every shade of light. Mirrored on its surface, the suji waves back in glittering landscapes of quivering shade. The spray, cast by the dash and splutter of the waters as they foam and lunge over rocky and abrupt declivities, rises like a veil of mist. The sun, glancing from the overhanging crests, mirrors the scene and catches the various shades and lights as in a prism of wonderful and indescribable beauty. Crowning them like a cross, midway the gorge, rise two columns named Loveland Peaks, twin sentinels of the rugged scene. On the summit of a mountain ten thousand feet in air, they shoot up the rugged surface like momentous spires in the midst of deso- late surroundings. Hundreds of feet above the tallest peaks, they stand desolate and grand as Egyptian pyramids — tall columns which catch and COLORADO. 113 reflect every slanting ray of light. Some day the tourist will make this Coloraxlo scene his Mecca, as the Moslem turns to the shrine of his faith, watching in the day's decline the wonderful spectacle of sunshine and shadow, and the weird, rugged sublimity of mountain-gorge, materializing a dream of beauty which far outstrips the achievements of the painter's pencil." These scenic beauties will be open to the tourist world when tlie High Line road reaches out from Georgetown over the range, and opens up the profuse and elaborate scenery to the traveller, mingling the thrilling with the beautiful in the grand panorama of our mountain- attractions. PAKKS AND EIVEES OF COLOEADO. A peculiar feature of the State is its mountain-girt parks. These are great basins, with surface and soil more or less similar to that of the Plains, but surrounded by lofty mountains whose elevation reaches from seven to ten thousand feet above them. These parks are generally well watered, abundantly timbered, and abounding in springs containing mineral waters. There are four great parks, separated from each other by narrow but lofty mountain-ranges. The entire chain can be easily traversed, and as they abound in fish and game, and present some of the most varied, romantic, and beautiful scenery imaginable, it will be seen that they are points of great interest to tourists and hunters. North Park is near the northern boundary of the State. "Within it the North Platte River takes its rise. It is a circular basin some thirty miles in diameter, and is the most timbered and lofty of the parks. It has not, as yet, attracted much attention ; still, its points of interest are not easily excelled elsewhere, and there is a possibility of vast mineral resources lying hidden within the hills that surround it. There are, as yet, but few settlements within its boundaries. It is easily reached from Fort Collins, on the Colorado branch of the Union Pacific Railroad. Middle Park adjoins it, and is very much larger. It has a diameter of about fifty miles. It is drained on the west by Grand River, whose exit is by a caflon of sublime depth and awful grand[eur. Spurs of lofty mountains shoot far out toward its centre. Hot Sulphur Springs in the middle of the park is quite a summer resort. Some considerable settle- ments have been established within the park, and it is reached by a line of stages from Georgetown. South Park, by the advent of the Denver and South Park Railway, that traverses its entire length, is now beginning to be well known. In 8 114 THE GREAT WEST. it the South Platte takes its rise. It is about forty miles wide and seventy miles long. Its central basin is one vast meadow, capable of sustaining millions of cattle. Its rim and its spurs abound in gold- and silver- mines. San Luis Park lies in the extreme southern part of the State, and is the lowest in altitude, while it is the longest in extent, of the four great parks. It is drained by the Rio Grande del Norte, which flows in a southerly direction through it, and thence in a south-easterly course seeks the Gulf of Mexico. This park has always been the favorite place of settlement for the Mexican population of the State, but the advent of the Denver and Rio Grande Railway into it, and the consequent entrance of a thrifty white population, are rapidly driving this shiftless class into New Mexico, and replacing them with the elements that go to strengthen and exalt society and the State. The farming resources of San Luis Valley are vast and of untold value. In the years to come it will be a beehive of agricultural industry. There are hundreds of other parks, varying in size from ten to a thou- sand acres, scattered all over the State. Estes Park, perhaps, might be mentioned as one of the largest of this coterie of cozy nooks hidden in the hills. Through it visitors pass to make the ascent of Long's Peak. In its mountain-streams are abundance of trout, while all kinds of game can also be found in it. It is a favorite resort for tourists, and is reached by rail to Longmont, and thence by an easy coach-ride of five hours. The principal rivers of the Plains region of Colorado are the South Platte and the Arkansas. These have their sources in the mountains, and as they reach the Plains are fed by many small streams. The first drains the South Park and the range from Denver north to the boundary of the State. Its source is near Mount Lincoln, and its principal branches within the park are High, Little, Platte, Trout, and Tarryall Creeks. Its general course is in a north-easterly direction, and after it leaves the caflon its principal affluents are Bear, Turkey, Clear, Ralston, St. Vrain's, Coal, Boulder, Left-Hand, Big and Little Thompson, and the Cache-la-Poudre. The valley of the South Platte, from its exit from the caDon to where it leaves the State, is two hundred and fourteen miles long, with an average width of two miles, containing about four hundred square miles of bottom- land. The main stream, with its branches, is supposed to carry water enough to irrigate about fifteen thousand square miles of arable land, on the supposition that three cubic feet per second will irrigate one square mile. The Arkansas River rises near Tennessee Pass, flows through small COLORADO. 115 valleys and cafions — ^the main one being the celebrated eafion of the Arkansas — in a general southerly direction until it reaches La Junta, where it turns east and leaves the State. A number of short streams contribute to its volume of water in the mountains. The most important of these are Grape, Texas, Chalk, Cottonwood, Elbert, Oil, Currant, Badger, Trout, and the South and East Arkansas. On the Plains it receives the Purgatoire, Apishpa, Huerfano, Cucharas, St. Charles, Green- born, Hardscrabble, Fontairie-qui-Bouille, and Monument. The area of arable land and of its branches has been estimated to be nearly two thou- sand square miles ; these valley-lands are not cultivated so extensively as are those on the South Platte and its branches, but attention is being drawn to them as equally desirable for agricultural and horticultural purposes. The Rio Grande del Norte heads in the heart of the San Juan Moun- tains. From the great snowfields and the abundant rainfall of these high mountains the stream grows rapidly, and when it enters the valley of San Luis Park it is one of the largest streams in the State. Here several good-sized tributaries add to its volume. The principal ones are the Alamosa, La Jara, Conejos, Rio San Antonio, Trinchera, Culebra, and Costilla. The agricultural capabilities of this stream and its branches are measured solely by the supply of water. The soil being of a more sandy nature, a larger amount of water is required than in the northern part of the State, and five cubic feet per second has been allowed in this estimate. About eight hundred square miles of land are capable of being supplied with water enough for cultivation. The San Luis Valley is now mainly given over to grazing, but it is beyond question that it will yet be the garden-spot of the State. The San Juan River drains the southern slopes of the San Juan Moun- tains, and the land capable of being utilized is distributed in narrow belts in. and near the mountains. Its main branches are the Piedra, Los Pinos, Las Animas, La Plata, and Mancos. These have more or less of culti- vated land, supporting a population mainly composed of Mexicans. The Grand River heads among the snowfields of the western slope of the front range in Middle Park. It covers a drainage-area of over tweniy-two thousand square miles. Its principal tributaries in the park are North Fork, Willow, Troublesome, Muddy, Frazer, Williams, and the Blue. All of these are in valleys of more or less width, but contain- ing little arable land, principally lying on the Frazer and the Blue. A succession of short caflons follow until the Gunnison is reached. The Gunnison River heads in the Sawatch range, and has for its tribu- 116 • THE GREAT WEST. taries Tomichi, "White Earth, Lake Fork, CeboUa, Uncompahgre, Dolores, and San Miguel Creeks. All of these branches have more or less irri- gable areas, while the Gunnison proper, in what is known as the Uncom- pahgre Valley, has an abundance of land and water. The White River has its rise in high plateaus which reach the timber- line. Its course is westward, and it flows in a narrow valley limited by cafion-walls. Its arable belt of land is extremely small, except at the point where the White River Agency is located, where it branches out into a belt five miles wide and about the same in length. It has not land enough to use up the flow of water. The Yampah River heads in Egeria Park, flowing north for about thirty miles, then turning to the west. Its main branches are the Little Snake, Elkhead, and Sage. It is stated that there is an arable area of about three hundred and fifty square miles in this valley and its tribu- taries, with an abundance of water for all that can be cultivated. EESOUECES. Arapahoe county includes a strip of country about thirty miles wide and one hundred and seventy-five miles long, with its eastern limit at the Kansas State line, and is entirely upon the Plains. It possesses no min- eral deposits save coal, and but little timber. Its agricultural industries, however, are of great importance, and are likely to become still more so by the completion of a canal of immense size and length called the Platte Canal. The soil is well adapted to the growth of all the cereals and veg- etables, while in the vicinity of Denver considerable attention has been paid to fruit-raising. Denver is the principal city, and as a mercantile, manufacturing, and railway centre contributes greatly to the wealth of the country. Of Denver we treat more fully under a separate head. Littleton, Petersburg, Brighton, Box Elder, and Deer Trail are small villages in Arapahoe county, and the centres of agricultural and stock interests. The amount of land returned last year as in cultivation in the county was 131,424 acres, at a valuation, including improvements, of $2,583,265, but the taxable wealth of the whole county is set down at $31,000,000. Bent county comprises a district sixty-eight miles wide and one hun- dred and eight long, and is one of the great grazing-districfs of the State. It is but sparsely settled, and at present cattle- and sheep-raising are its principal resources. But the Arkansas River runs through the southern half of its limits, and the land is well adapted to cultivation. The Atchison, Topeka, and Santa F^ Railway runs through it, and at La COLORADO. 117 Junta a branch goes down to Trinidad. West Las Animas is the coun- ty-seat and principal town. The Las Animas River empties into the Arkansas at this point, and the lands in this valley are occupied by quite a thrifty class of farmers. The taxable wealth of the county amoimts to $5,000,000. BouLDBB county is part plains and part mountains, the latter predom- inating. It is one of the best developed and richest counties, aside from Arapahoe, in the State. Its fertile valleys are filled with industrious husbandmen, while its hills and mountains are stocked with precious metals. Gold, silver, iron, coal, — ^these are the principal resources. Here, in this county, the first discovery of gold was made (in 1858), and its belt of mines extends the entire length of the county, while its silver- mines include the world-renowned Caribou and others of well-known value. Long's Peak lies within its borders, while the valleys of St. Vrain, Boulder, Left-Hand, and Ralston enrich its eastern limits with extensive tracts of arable land, all well dotted over with the comfortable homes of well-to-do farmers. The coal-beds of Boulder county are no unimportant item of its resources. They underlie the whole eastern strip, and are worked at several points, yielding the finest coal found in the northern part of the State. Fire and potters' clays also exist. An abundance of timber is in the mountains. Excellent water-power, beau- tiful scenery, a healthy climate, vast mineral deposits, unrivalled agricul- tural facilities, — ^these place Boulder county in the front rank of the coun- ties of Colorado, ensuring it a career of future prosperity. At present, its mines, like those of the San Juan, are not attracting the attention they deserve ; but when the carbonate fever is over the lodes in this district will be a permanent source of wealth to their fortunate owners. The area of the county is about nine hundred square miles. The prin- cipal towns are Boulder, Longmont, Valmont, Louisville, Sunshine, Jamestown, Gold Hill, Salina, Ni Wot, and Pella. Farming-lands were returned last year by the assessor at a valuation of a million and a half of dollars on 127,485 acres, while the entire valuation of the county foots up to nearly $7,000,000. Clear Creek county three years ago was the principal silver-produ- cing county in the State. The Leadville district leads in the race now, but the silver-mines of this county are still being worked to a considerable extent, and constitute the principal resources of the district. It is a small- sized county, 15 by 35 miles, full of good water-power and excellent mill-sites, with some little agricultural land ; but mining, milling, man- ufacturing, and grazing are the main reliance of its inhabitants. Clear 118 THE GREAT WEST. Creek is the principal stream, but this has numerous branches, flowing through ranges of mountains traversed by belts of silver- and gold-lodes and covered with timber. Clear Creek Caflon is referred to elsewhere. The principal towns are Georgetown, Idaho Springs, Empire, and Silver Plume. The narrow-gauge system of railway reaches Idaho Springs and Georgetown, and is likely to be extended beyond the latter point, over what is known as the High-Line route, to Leadville. The real estate and personal property of the county foots up to nearly $4,000,000. Chaffee county is one of the latest formed counties in the State, having the Saguache range for its western boundary and the Park range for its eastern. Leadville lies directly north, in the adjoining county of Lake. The Arkansas, River runs through it north and. south. Gulch-, placer-, and lode-mining are carried on to some extent. Some noble mountains, such as Mounts Harvard, Yale, Princeton, and Shavano, are within its boundaries. The town of Buena Yista, founded last year, is attaining considerable prominence as a business-centre, while its nearness to some famous hot springs on the Cottonwood, about ten miles away, will tend to make it a resort for invalids. Cleora and Granite are promising towns in this county. Conejos county is one of the somewhat isolated districts of the State. Railway communication ends at Alamosa on its eastern border, but the bed of the Denver and Rio Grande Railway is graded to Conejos, the county-seat, and the cars will reach it before the year is ended. The re- sources of the county are almost wholly undeveloped. Alamosa is its principal town, and an extensive trading business is carried on with the mountain-regions on the west. It is also the present shipping-point for the trade with New Mexico. The celebrated Pagosa Springs are in the western part. It has a large number of villages of plazas, wherein Mexi- cans cluster. Nearly one-half of the county is forbidden ground for the white man, being in the Ute Reservation. There is a large area of well- watered and arable land, but thrifty and enterprising people are needed to develop the at present hidden resources. The taxable property last year amounted to only $750,000. Costilla county is in the San Luis Valley, and has the Rio Grande del Norte for its western boundary, while the railway runs through it from east to west. It boasts of the highest mountain in the range, Mount Blanca. It has within it several small streams, principally the Costilla, Culebra, Trinchera, and Sangre de Christo, in whose valleys more or less rude agricultural pursuits are followed by the residents, who are mainly Mexicans, and whose principal industry is the raising of a few sheep, COLORADO. 119 horses, goats, asses, and cattle. Fort Garland, an important military post, is in this county. There are large areas of arable land susceptible of cul- tivation for cereals by irrigation-canals from the Rio Grande River, but they must await the coming of a thriftier set of people than the Mexi- cans, who now are in the majority. The taxable wealth of the county is returned at a little over a million of dollars. CuSTEE county has within its borders Silver Cliff, whose importance a.s a mineral district is beginning to be recognized by the outside world. The Sangre de Christo range is its western boundary, while in the south-east rise the Wet Mountains, giving a name to the valley between, whose pas- toral and farming resources are very large, though as yet but scantily developed. Silver Cliff, Rosita, Ula, and Colfax are the principal towns; The mines in the vicinity of the two first named have been demonstrated to be of extraordinary richness, and their development will make the dis- trict a point to which prospectors and capitalists will be directed. Douglas county lies south of Arapahoe, and is traversed by the Den- ver and Rio Grande Railway. In connection with Elbert county, on the east, it takes in what is known as the " Divide " country, a belt of high land separating the valley of the South Platte from that of the Arkansas. It is a timbered region, with some stock-raising and agricultural resources. Farming is carried on here without irrigation, the altitude conducing to frequent rainfalls during the growing season. It is becoming noted as a dairying district, springs and sheltered places abounding on either slope of the Divide. Several small streams course through it, but they furnish no reliable water for irrigating purposes. The principal towns are on the line of the Denver and Rio Grande Railway. Castle Rock is known for its extensive stone-quarries, and furnishes this material in abundance for the Denver market. The iron ore of Douglas county, when developed, will be one of its principal resources. At present stock-raising and agriculture predominate. Elbert county is a cattle county, lying east of Douglas and taking in part of the Divide. The Kansas Pacific Railway runs through it in a south-easterly direction, and the main settlements are along the line of/ the road. Cattle and sheep are the principal industries, though some attention is paid to dairying and farming in the western part. The tax- able wealth of the county is $300,000. A considerable portion of the lands are unsurveyed, and are the roaming-grounds of the antelope and buffalo. El Paso county is the leading sheep-raising district in the State^ returning nearly one hundred and twenty-five thousand in 1879. It has 120 THE GREAT WEST. Pike's Peak, Manitou, Monument Park, the Petrified Forest, Cheyenne Caflon, and the Garden of the Gods as points of interest for tourists. The Fontaine-qui-Bouille, a tributary of the Arkansas, is the main Btream within its borders, and in its valley lie some choice tracts of farming-land. But therie is a general lack of water for irrigation, and this county cannot look forward to any great agricultural development unless artesian wells are demonstrated to be feasible. The western part of the county is mountainous, but there have been, as yet, no discoveries of minerals of any great value. Its wealth is in its plains, where a million sheep could find sustenance, and in its beautiful city of Colorado Springs and the numberless attractions in that vicinity, that draw yearly a steady stream of visitors. The taxable wealth is between five and six millions of dollars. The Denver and Eio Grande Railway runs through it from north to south, and there are several stations — Monument being the principal one — of more or less importance on the line of the road. Fremont county. — The Arkansas River passes through the entire length of this county. It is one of the most promising in the State, comprising as it does within its boundaries coal, gypsum, iron, marble, alum, petroleum, and some of the finest fruit-lands in the State. The coal of Caflon City is a bituminous coal of superior quality, and cannot be mined in sufficient quantities to meet the demand. The Grand Canon of the Arkansas is reached from Caflon City, and is one of the wonders of the Western World. Soda springs abound within its borders. One of the main highways to Leadville runs through it. Considerable atten- tion has been paid to fruit-culture in the valley of the Arkansas east of Caflon City, and it boasts the largest apple-orchard in the State, yielding over two thousand bushels last year. Grapes grow ia abundance, while the foot-hills are full of wild fruit. Fremont county boasts a real and personal property of two and a half millions, which is destined to rapidly increase. Gilpin county is the smallest political subdivision of the State, but one of the most important, and embraces within its limits the richest gold-mining region in the Rocky Mountains, and perhaps in the world. Broken by mountain-ranges and their intervening gulches and chasms, it is rich in the precious metal. Its mountains are covered with forests of pine, and its rugged ravines hide rippling waterfalls and grass-covered bottoms. Central City, Black Hawk, Nevada, and Rollinsville are the principal towns, the two first being surrounded and traversed by belts of gold- mines, while in the immediate vicinity are gulch- and placer-diggings WILLIAMS CASON, COLORADO SPRINGS. BY THOMAS MORAS. COLORADO. 121 that have yielded millions of dollars' worth, and will yet yield millions of dollars' worth more. The mercantile and commercial interests of the county are important, and are skilfully managed by a class of merchants and business-men possessing unusual enterprise and ability. The alti- tude of Central City is eight thousand three hundred feet, while the average of the county reaches nine thousand. The climate of the district is mild and healthy. Railway communication is had by the narrow- gauge system, and the ride from Black Hawk to Central, where several miles are traversed to gain one in distance, is one. of the grandest in the world. Grand county lies in the northern part of the State, between Larimer and Routt. It comprises within its borders North and Middle Parks and the Rabbit Ear range of mountains, in which some silver-veins have bean discovered. The famous Hot Sulphur Springs are in the last-named park. The North Fork of the Grande, the North Platte, and the Cache- la-Poudre Rivers have their rise in the centre of the county. It is a region of vast possibilities, and may yet become renowned for its mineral deposits. Middle Park and the Hot Sulphur Springs are reached by coach from Georgetown — North Park from Fort Collins, on the Cheyenne branch of the Colorado Central Railroad. Gunnison county. — "To Gunnison?" is to be the rallying-cry of thousands this season, who hope to find fabulotis wealth within its hidden defiles and bosky dells. It has within its boundaries noble rivers of which but little is known, while countless smaller streams traverse the valleys of this comparatively terra incognita of Colorado. To reach it a lofty range of mountains, whose passes are always full of snow, must be crossed. The Elk Mountains are on the eastern boundary, while stretch- ing far to the west are mighty ranges whose resources will not be defi- nitely known until the Indians are driven out of the country and white men allowed to enter and explore them. In a number of districts bor- dering on the reservation mineral veins of value have been found, but tiieir richness and importance have not been thoroughly demonstrated. Hinsdale county is part and parcel of the San Juan country, and is a region laboring under the general disadvantages made up of difficult mountain-ranges, remoteness from railway communication, and want of confidence of capitalists to invest in mines at such a distant point. But the county is undeniably rich in mineral wealth, and Lake City, its cap- ital, is the centre of an important silver-producing district. Smelting- works have been put in, and are in successful operation. The taxable wealth of the county is set down at $1,000,000. 122 THE GREAT WEST. Htjeefano county lies in the southern part of the State, and takes its name from the river that runs through it, and which, with the Cucharas and Apache, gives valleys in which about forty thousand acres of choice agricultural land await a better development than the present population — ^which is mainly of Mexican descent — is likely to give it. At present cattle- and sheep-raising is followed. Corn can be grown in 'great abun- dance, and the soil seems to be admirably adapted to its cultivation. Am- ber cane would be a good crop, and will probably be one of the important industries of the county in the near future. The Spanish Peaks are on its southern line, and on these some silver-mines are being worked to good advantage ; but it cannot be said that much attention is being paid to the metals that may exist in the mountainous portion of the county. Considerable coal is mined at Walsenburg, one of its principal towns. La Veta, Cucharas, and Santa Clara are the other most important towns. On the western border rises the great Sangre de Christo range, with Veta Pass and Muleshoe Bend to attract tourists over the line of the Denver and Eio Grande Railway, which enters the county from the north and runs through it in a southerly direction to El Moro, while the main line turns at Cucharas for La Veta Valley, climbing the celebrated pass and running down into the San Luis Valley. The present valuation of the real and personal property of Huerfano county is $2,000,000. Jefferson county is part plains-land and part foot-hills, running north and south, with the valley of the South Platte traversing its eastern boundary. Its agriculture is its main feature, though fire-clay, gypsum, potter's clay, building-stone, and coal abound. There is but little un- occupied land in this county. It possesses an abundance of cheap fuel in its mines of coal ; inexhaustible supplies of excellent building material in its stone ; superior water-powers ; large tracts of timber afford good lumber in unlimited quantities. The Colorado Central gives ample trans- portation for the products of the county to Denver and the markets of the State, and places it in direct communication with all the commercial centres of the country. Golden is the principal city and the county-seat, the home of manu- factures, mines, mercantile enterprises, educational and religious institu- tions. Morrison, famous for its quarries of stone, is reached by the Denver and South Park road, and is a cozy little nook hidden in the hills. There is still ample room for thousands of industrious farmers, artisans, and miners within the limits of Jefferson county. Lake county has Leadville for its principal attraction. The county, originally one of the largest in the State, is now one of the smallest in COLORADO. 123 extent, and illustrates the axiom that whatever is most precious is small in size. It is full of gulches that were once the centre of attraction for thousands of miners who were drawn to it in the early days of Colorado's history, then abandoned, but are now the Mecca toward which a steady tide of human beings are flowing in search of carbonates. Mining is the only industry of the county, but as the output of the present year is likely to amount to $25,000,000, it will readily be seen that these mines are a suiiicient attraction in themselves, and Lake county needs no other. The name of Leadville is a synonym for imtold riches that lie hidden in the vast mineral areas of the district. Mounts Massive and Elbert lift their stately summits to the clouds within its borders, while those gems of liquid beauty, the Twin Lakes, will be a point of interest for tourists for all time to come. Now that railroad communication has reached the Carbonate Camp, no visitor to the State can afibrd to leave it without a look at Leadville, to which we devote a special heading elsewhere. La Plata county lies west of Conejos, in the extreme south-west corner of the State. It borders New Mexico, Utah, and Arizona, and is rich in coal, silver-veins, and gold-placers, and contains many fine fertile valleys. Within this county are the celebrated ruins now so well known through the reports of Hayden's surveys, and to which reference is made in these pages. The coal-lands of this county are estimated at over six hundred square miles, and will be a source of immense wealth when railroads shall reach this far-ofi^ corner of Colorado and reveal its wonders, its mineral wealth, and its agricultural resources to the world. Larimer county is one of the three principal agricultural counties, lying in the northern part of the State, and borders on Wyoming. Its western part is extremely mountainous, while beyond it lies North Park, to which it is the natural highway. The Cache-la-Poudre, one of the most reliable streams on the eastern slope, runs through it in a south- easterly direction. An abundance of timber and magnificent water-power in the foot-hills and mountains give it an assured present and a magnificent future career of prosperity. But it is as an agricultural district that the county is best known at present, and its farming resources are limited only by the amount of water that can be made available. The first large irrigating canal in the State — ^that constructed by the Union Colony at Greeley — heads in this county, as also does the extensive canal of the Weld and Larimer Canal Company. But most of the arable areas cov- ered by these canals lie in the adjoining county of Weld. Still, enough is covered by these and numerous other canals to make agriculture one of the main resources of the county. Last year the returns showed sixty 124 THE GREAT WEST. thousand acres of improved lands, with a valuation of $300,000, while the entire taxable wealth of the county is about $3,000,000. The Col- orado Central branch of the Union Pacific Railway gives direct com- munication with Denver and the mountain-towns, while Cheyenne and the east and west are reached on the north. Fort Collins, Loveland, Livermore, and Wheatland are the principal towns. Las Animas county lies along the southern boundary of Colorado. Its principal stream is that from which the county is named, and the valley of " The Spirits " forms one of the most magnificent tracts of farming-land in the State. The Denver and Rio Grande and the Atchison, Topeka, and Santa F6 Railways traverse it, while Trinidad and El Moro are its principal towns. At these points a vast and expanding industry has been established : hundreds of coke-ovens are burning night and day. The coal in this vicinity makes excellent cok§, for which, of course, the mines furnish a ready market. There is no mining done in this county, but the extensive table-lands furnish unequalled grazing-grounds fbr sheep, of which the county has over one hundred thousand. The coal- mines are a source of constant revenue, and the valley is capable of sus- taining a large farming community whenever a thrifty class enters and occupies the fertile soil. OiXKAY county lies west of San Juan, and is part of the San Juan mineral belt of country, full of mountains, ravines, and gorges in which precious rnetals abound, but with which communication, especially in the winter season, is difficult. This remoteness from civilization has tended to retard its progress, but there is a possibility of a railroad reaching this distant point at an early day, and then a rapid advancement may be looked for. Ouray is the main tqwn in the district. The Dolores plateau, lying west of the belt of mountains traversing the eastern borders of the county, is believed to be capable of agricultural development, but this is not likely to occur at an early day in the history of Colorado. Park county. — This is the famous South Park country. It lies in a kind of basin, having mighty mountain-ranges for its rim on three sides, while its eastern border is a series of spurs broken by small streams that feed the South Platte River. It is the most centrally-located county in the State, full of mineral springs, salt springs, carbonate deposits, and coal. Within its borders Mount Lincoln rears its lofty head. From its eastern slope the South Platte River starts on its journey to the Plains, while on its western edge its waters seek the Pacific through the channels of the Blue and the Grand Rivers. The Denver and South Park Railway courses through it, and all along its line towns are springing up, to be- COLORADO. 125 come of more or less importance in future years. Stock-raising is a prominent feature in the industries of tilis county, the vast area of the park being capable of sustaining countless herds of cattle. Fairplay and Alma are its principal towns. Pueblo county is a valley-county, lying on each side of the Arkansas River. The Denver and Rio Grande Railway runs through it north and south, and a branch at Pueblo runs west to Caflon City. The Atchison, Topeka, and Santa F^ road enters it from the east, so that Pueblo, the principal town in the county, is an important railroad-point. It is one of the finest agricultural districts in the State, but stock-raising at present predominates. Nearly a hundred thousand cattle and sheep are herded on the plains, while the Arkansas Valley contains two hundred thousand acres of arable land. The Fontaine-qui-Bouille, St. Charles, Chico, and Greenhorn are the principal tributaries to the main river running through it, in whose valleys more or less farming is carried on. It could be made a great fruit-raising section if attention was paid to this industry. The terminus of the Atchison, Topeka, and Santa Fg Railway being at Pueblo for the present, makes it quite a commercial centre, and the city is in a thriving condition. The taxable wealth of the county, in live-stock, real estate, personal property, and railway-tracks, amounts to nearly seven million dollars. There are some extensive cattle- and sheep-ranches here, where Mexican labor is wholly employed, yet but a tithe of its twelve hundred square miles of fertile land is in cultivation. Rio Geande lies between Conejos and Saguache, and is partly moun- tainous, with large breadths of plains-land. The Rio Grande del Norte runs along its western border, and San Luis Park lies partly within it. There are several small tributaries feeding the main stream, whose valleys are lined with cultivated farms ; but for the most part the vast area of arable land is unoccupied,, waiting the coming of those who are to till the. productive soil and feed the myriads who will throng the mining districts to the west and north. Routt county, in the extreme north-west corner of the State, is covered with mountain-ranges and spurs, and with river-valleys in which grazing and agricultural pursuits to some extent could be successfully carried on. Egeria Park is in its south-east corner ; Yampah River courses through it from east to west ; and the Elkhead range of mountains are the prin- cipal ones within its borders. On the head-waters of the Snake and Elk Rivers there are some extensive placer-lands from which considerable gold has been taken, and where flumes and ditches have been constructed. Steamboat Springs are in the eastern part. The county at present is 126 THE GREAT WEST. attracting but little attention, but when communication can be had with it easier than at present it will be found capable of supporting a vast population. Saguache county occupies the northern extremity of San Luis Valley, and has considerable settlements within it, but is capable of sustaining many more. It has a fertile and finely-watered region, scarcely equalled anywhere, whose numerous valleys are great natural meadows covered with vegetation, and whose table-lands afibrd abundant pasture for sheep and cattle. Perhaps one hundred and fifty thousand acres of land are improved. The taxable wealth of the county is $1,000,000. In addition to its pastoral resources, it contains some of the finest scenery in the State, being hemmed in on the east, north, and west by the Sangre de Christo, Saguache, and Cochetopa Hills. It is a district with great natural attrac- tions and boundless resources, and has an era of prosperity before it whose dawn already casts its light upon the horizon. San Juan county is a small but exceedingly rich section of country in the south-western part of the State, and is full of mining districts in which thousands of lodes are located, and many of them worked. The dis- coveries and developments that are constantly in progress, despite the amount of interest excited by Leadville, vindicate the conviction that the great natural resources of the San Juan country are not likely to be forgotten. Indeed, these silver-ribbed rocks can hardly be overlooked. Silverton is the principal town, and one that is steadily growing. A good wagon-road connects it with Ouray, Lake City, and the outside world. The gulches in this district contain many very productive mines, but the wealth that has thus far been brought to light is but trifling to what will yet be realized when capital concentrates at this point. San Juan county has no agricultural resources. Summit county is one of the extreme north-west counties, lying west of the summit of the Main Range. It is a region as yet undeveloped on its eastern borders, where it is rich in silver-lodes and gold-placers. In the western part of the county coal is said to exist in immense deposits. Some eight millions in gold, silver, and lead have been taken out of this district since Colorado was first settled. New and important mining dis- tricts now being developed are attracting some attention. Ten-Mile dis- trict has some rich galena-veins that have been lately opened. Eagle River, the Blue, Snake, Swan, and their tributaries, are all likely to be- come famous points, as they are the last discovered in the extensive min- eral regions lying west of the range. The Mountain of the Holy Cross, the subject of J. Harrison Mills's celebrated painting, is in this county, COLORADO. 127 while Mount Lincoln is on its south-east boundary and Mount Powell on the north. The blood-stained White River Agency lies within it. Weld county is one of the largest in the State, and lies in the north- east corner. The South Platte River runs through its entire length, while the Denver Pacific Railway passes down its western edge. It is wholly a cattle-raising and agricultural county. Within it Hes Greeley, the first farming-town established in the State, and the success of which led. to the establishment of so many others. It is believed that coal underlies a good part of the western portion, but this is only conjecture, save in the extreme south-west corner, at Erie, where mines are worked. The valley of the South Platte is one capable of raising, by systematic and economic irrigation, food enough to supply the wants of the people of the entire State. Out on the Plains, beyond Greeley, some attention is paid tb sheep-raising, and there are large herds of cattle kept between the river and the Territory of Wyoming on the north. When the railway system of the country reaches and occupies the South Platte Valley, it will open up a splendid country and develop the resources of this county to a very large extent. The principal towns are Greeley, Evans, Platteville, and Erie. The taxable property reaches $7,000,000. The construction of the Weld and Larimer County Canal throws open thousands of acres to cultivation, and when these are utilized Weld will stand in the front rank as a county whose agricultural resources are unbounded save by the volume of water in its streams. THE ELOEA. OF COLOEADO. The flora of the State is full of interest to the casual observer, the lover of flowers, and the botanist. For many months in the year the plains, ■ the foot-hills, the very sides of the mountains, are covered with the com- mon wild flowers that luxuriate in the bright sunshine and dry air. Here is not found such wealth of foliage as abounds in moister climates ; the blossoms predominate to a remarkable degree. The botanist, wandering through the Sangre de Christo range, tramples down whole fields of white and blue larkspur and delicate mertensia. The summits are crowned with phlox and forge<>me-nots. The fields of Wet Mountain Valley are full of clover, iris, and lilies. Wild roses bloom along the banks of every stream, great or small. . Ipomea covers the mesa.s, abronias whiten innu- merable acres of land, while the large, conspicuous flowers of the Mira- bilis multiflora are seen opening their petals late in the afternoon and show- ing fresh, bright faces to the passer-by. .The syringa grows wherever it can find a foothold, the cafions are alive with fallugia, while wherever little 128 " THE GREAT WEST. streams of water dash over the rocks in the foot-hills and lose themselves in mist the golden columbine and aquilegia grow to perfection. The scarlet and the blue pentstemon, the brilliant gillia, spireas, and hosts of less showy but equally interesting plants occupy every available spot. Especially in Southern Colorado is the flora of the Plains and foot-hills remarkable for abundance, variety, and brilliance. The low elevation of the Arkansas Valley and its tributaries has induced many of the most noticeable and beautiful specimens, whose home is in New Mexico, to find a rasting-place here and to grow abundantly. The parks are dotted with the tree-cactus and the frankenia, while at least thirteen species of cactus abound, from the familiar prickly-pear with long flat joints and sharp thorns and handsome yellow flowers, up to the tree-cactus with its large purple flowers and sharp thorns, growing twelve feet in height in favor- able localities. Here and there solitary cones of Cereus fenaleri can oc- casionally be found, bearing two or three large purple-flaming blossoms, while up on the mountain-sides flourish in great abundance hemispherical masses of Cereus phwnious, scarlet with a hundred blossoms and bristling with a thousand spines. A world of floral beauty, it may therefore be said, is open to all be- holders in this State, so rich in resources in its valleys, plains, hills, and clifis. It may be called the "Wonderland of America, and its flora will be an irresistible attraction during the summer and fall months for all who have an eye to the beauties of Nature unchanged by human art. WILD ANIMALS. Middle Park may be taken as a fair type of the fauna of the moun- tain-regions of Colorado. As it contains lakes and streams, plains and hills, it may be looked upon as a miniature State, and in describing the animals of this section we describe those of all Colorado. The following have been seen or killed in the park or on the moun- tains that surround it: Of the bear family ( DroBMs) : The common black {americanus); brown or cinnamon {arctus); grizzly (ferox). Of the wolf family (Lupus) : The common (cants) ; prairie (latros) ; wolverine (Gulo Iugus). Of the fox family ( Vulpus) : The common red (vulgaris) ; black (alo- pex); silver (argenteus). Of the deer family: The common (Cervus virginianus) ; the antelope RESTORED TOWER AND CLIFF-HOUSES. COLORADO. 129 (Antilocapra cervicapra) ; the elk or moose {Aled amerioanua) • the moun- tain-sheep {Ovis montana, resembling the Caprovis nmsimon of Europe). In addition to these may be named : The cougar or panther, generally called the Rocky Mountain lion. This fierce animal is found all through the Rocky Mountains. The lynx (Felia canadensis), very common in the parks. It is called the wild-cat, and sometimes, erroneously, the catamount. The pole-cat {Putorius vulgaris of the naturalists, and seems to be a cosmopolite). The mink [Putorius vison), valued for its skin, being covered with fine fur. The beaver [Ckistor americanvs). This is perhaps the .same as the Eu- ropean Castor fiber. Its fur is well known. The otter {Lutra canadensis or Lutra mollis, so called on account of the softness of its fur). It is an aquatic animal, and found only in lakes and streams. The muskrat (Fiber zibethieus), a genuine native American, and found in no other part of the world. The woodchuck (Arctomys monax), sometimes called the ground-hog, and found all over the country. ANdBNT KTTINS. South-western Colorado is one vast network of ruins, indicating an age in the far past when its valleys and mountains were filled with an enterprising people. It is asserted that there is scarcely a square mile in six thousand examined by the Hayden Expedition that does not furnish evidence of previous occupation by a race totally distinct from the no- madic savages who hold it now, and which must have been in many ways superior to the latter. These ruins are in a great measure the remnants of stone structures, some of them of large dimensions, and have been classed under general heads : Lowland or agricultural settlements ; cave- dwellings ; cliff-houses or fortresses. The first of these are on the river- bottoms, close to water; the second are excavations in the bluffs; the third are built high up in steep, almost inaccessible, cliffs. Rock-inscrip- tions are numerous, both engraved and painted on the clifis. Remains of pottery and flint-chips are abundant. The number of these ruins pre- cludes the possibility of mentioning them save in a general way. The section of country in which they are principally found is that drained by the San Juan River, reaching from the Sierra Abajo on the north to Choco Cafion on the south, and covering an area of some twenty s 130 THE GREAT WEST. thousand square miles. Evidences of a once thickly-inhabited country abound throughout its entire length. At some time in the distant past a pre-historic race of people existed in the fastnesses of the south-western portion of Colorado, whose life and history are only hinted at in the vast accumulations of remains that are left behind them. Of the habits of these people we know but little. The general absence of human remains, and the fact that few if any burial-places have been uncovered, would seem to indicate that other methods than those used in our day to hide the remains of the dead were practised. Indeed, the heaps of ashes mingled with charred wood lead us to believe that cremation was not an unknown art with them. As to the era in which this extinct race existed, there is no positive data. . The towns are now as they were hundreds of years ago, for these ruins were seen and described by Spanish explorers, who accounted them Aztec ruins. It may be that time and more extended research may open up the story of the people who once flourished — as did the Egyptians of old in all their grandeur upon the banks of the Nile — among the cliffs of Colorado, but who have been swept away from their rock-hewn castles on the cliff-sides and their valley-towns, leaving noth- ing behind to tell the story of the ages in which they flourished. It would seem as though these ruins would indicate races of ancient culture flourishing here thousands of years ago, and that America may yet be established to be the Old instead of the New World. In this vast area of land — still far away from civilization, but into which the feet of the tourist will in a few short years wander, while the hearts of the beholders will be hushed with awe and their eyes grow round with wonder — ^will be found new fields of study and research that will be more puzzling than the secrets of the Nile have ever been. The Dolores, San Juan, Mancos, La Plata, De los Pinos, De los Animas, De Chelley, — ^these will be Meccas for the geologists, archaeologists, ethnolo- gists, who will find, in unfolding the secrets of the cliffs, full occupation for their skill. Then, perhaps, the hieroglyphics upon the walls will tell a story at which a civilized world will wonder. As to the causes that destroyed such an immense nation as evidently once inhabited this country, we can only conjecture. It is among the possibilities that they were once similar to the people who inhabited the valleys of the Mississippi and Missouri, and who were driven westward by the ancestors of the present race of savages still lingering in our midst, and that they were eventually destroyed in their mountain-fastnesses by these and the Spaniards of earlier days. The present Pueblo Indians are supposed to be a remnant of the ancient race of Cliff-dwellers. COLORADO. 131 AGEICULTUEB. Agriculture in Colorado is an entirely different pursuit from that prac- tised in the East, and the farmer who comes to the State and enters upon the cultivation of the soil in the style l^e has been accustomed to, will find that failure is more likely to crown his endeavors than success. He has much to unlearn. It is best to abandon old notions and begin anew. Dependent upon irrigation for the growth of his crops, he must study the methods and meet the requirements of the climate. With a fixed pur- pose, in his mind to overcome all the obstacles that will daily present themselves to him, it will not be long before the new order of things will become familiar, and, once understanding the methods, he may rely upon Nature for the rest. Bountiful harvests will crown his efforts, and excellent prices will cheer his heart and fill his pocket. Irrigation is dreaded because it is not understood. Yet it is almost as old as civiliza- tion, and Oriental countries have depended upon it for uncounted ages. The records of ancient history are full of it, and to-day in India, Chi- na, and elsewhere in Asia long and expensive irrigating-canals are the reliance of millions to whom a failure of water would be starvation and death. In the early history of Colorado small ditches by individuals were constructed, covering only the meadow- or bottom-lands. But the selec- tion of Union Colony (in 1870) of Colorado for the settlement of a new town caused the construction of the first large canal to cover the plains proper, or uplands, running several miles back from the stream. This successful enterprise was followed by others of like corporate nature, and now a large amount of English capital is being spent in the construction of canals covering from thirty thousand to seventy-five thousand acres of land. An immense impetus has been given to the agricultural devel- opment of the country by these companies, and the rapid increase of population keeps up a demand that the farmers are not able to supply, neither will they be for a number of years. Hence good prices will be the rule, while bad seasons are the exception, in the experience of farmers. The agriculture of the State is confined to the valleys, of which we mention the principal : The Cache-la-Poudre, a valley thirty-five miles long, with an abundant supply of water ; the Big and Little Thompson, the St. Vrain, Left-Hand, and Boulder, in Boulder county ; Ealston, Clear Creek, and South Platte. These are the principal agricultural valleys in Northern Colorado, and here two-thirds of the grain and veg- etables of the State are raised. Something like three-quarters of a mil- 132 THE GREAT WEST. lion bushels of wheat, and about the same quantity of oats, barley, rye, corn, and potatoes, are raised. South of Denver the main producing valleys are the Fontaine-qui- Bouille, Arkansas, Las Animas, and Rio Grande. In these not so much progress has been made in turning their countless acres into cultivated fields and gardens ; but attention of late has been attracted to this part of the State, and the next few years will see a rapid progress in the development of Southern Colorado, not only in agriculture, but in horticulture. The price of land and water combined averages twenty dollars per acre in the north, but there are thousands upon thousands of acres to be had at nominal prices in the south ; and to these the coming farmers must go to lay the firm foundations of future prosperity for themselves, their posterity, and the State. The cost of raising general crops under a system of irrigation is sup- posed, by those not familiar with it, to be very expensive. But this is not really so, as the experience of Colorado farmers goes to prove. Wheat can be raised at 40 cents per bushel, or $8 per acre ; taking the low average of yield to be but twenty bushels per acre, at $1 per bushel, it leaves a profit of $12 to the acre. Oats can be raised at an expense of $10 per acre, leaving the profit $12.60. Corn can be raised for $6.75, leaving a margin of profit of $14.75. Potatoes can be grown at a cost of $20, and in average seasons give $60 profit to the acre. Amber cane can be raised at an expense about equal to corn, but yielding a return of $20 per acre. It will easily be seen that in these figures, based upon actual itemized accounts kept during the season of 1879, there is a good margin of profit ; and while there may be seasons when scant snowfalls in the winter on the mountains give short supply of water in the sum- mer, or untimely frost or grasshopper visitation may occasionally curtail the harvest, yet these are less frequent than the violent storms, the severe drouths, and the destructive insects that visit the fields of Eastern and Southern farmers. There is nothing to discourage the cultivators of the soil in the peculiar conditions that are required to make the harvest in Colorado a sure and profitable one. There is abundant room for thou- sands of them, still open at figures within reach of the poorest ; for even if one comes almost penniless, he can still find land ofiered him for the occupancy thereof by government ; and though it may not be a wise policy for individuals to go too far from settled communities, still small colonies can combine their capital, co-operate in building canals, and so create settlements that will eventually grow into thriving towns. Not COLORADO. 133 one-tenth part of the land susceptible of cultivation has been placed under canals, and of this not one-third is occupied. Every variety of grain and all kinds of vegetables can be grown profitably, and the yield is enormous compared with that of the older States. The soil seems inexhaustible in the constituents of cereal crops. Wheat has been raised running eighty bushels to the acre, while the average can be set down at twenty-five. Barley is a sure crop, with a ready market for the grain on Siicconnt of its superior malting qualities. The yield is from twenty-five to forty bushels to the acre. Oats are easily grown, and yield about the same as barley, while the supply has never yet been equal to the demand, and Kansas and Nebraska are largely drawn upon for the deficiency. Corn is beginning to be considered a staple crop, though at first it was supposed the general altitude of the country, and the consequent coolness of the nights, formed a hinderance to success. But late years have proved that there can be as good corn raised here as in any of the North- ern States. Especially is this so in Southern Colorado. Amber cane has been found to be peculiarly adapted to the soil, and a cane is grown rich in the qualities that produce good syrup and sugar. Rye is but little raised, but more attention is being paid to it each year. Potatoes, especially in the foot-hills and on the Divide, yield immense crops. Many of the uplands, especially on the north side of the Cache-la-Poudre, are also suited to the successful cultivation of this tuber. As for vegetables, all kinds, down to the tenderest, are grown with remarkable success. While agriculture is an established success, it is being conclusively shown that horticulture will yet become a prominent pursuit in the State. Strawberries are one of the most certain and profitable of crops. One acre can be cultivated and the crop marketed at a cost of $150, while the profit from 1800 quarts at 25 cents per quart — ^which was the wholesale rate during the summer of 1879 in the Denver market — leaves a profit of $300 per acre. Blackberries, raspberries, currants, and gooseberries range from 20 to 50 cents per quart at wholesale, while the expense of cultiva- tion is perhaps one-third less than for strawberries. Grapes grow in great abundance, and tons of them are annually put upon the market and find ready sale. Peaches, pears, and cherries are grown in various localities in sheltered locations, and it would seem as though — in Southern Colorado, at least — ^these fruits would yet be successfully cultivated to a limited ex- tent. Apples of the more hardy varieties are now raised in both sections of the State. One orchard yielded two thousand bushels last season ; it is located in the Arkansas Valley, near the town of Caflon City. Of course there have been many failures in the past, and will be in the future, 134 THE GREAT WEST. in these pursuits, until time and experience determine the varieties suited to the peculiar climate. But such discouragements have been met with elsewhere, and in States that are now recognized as great fruit-growing States. Colorado horticulturists have no cause to be discouraged. The general outlook for agriculture and horticulture, therefore, may be said to be good, though they cannot be expected to keep pace with the mining progress ; but this fact is in the farmer's favor, not against him. The building of extensive irrigating-canals, the economical use of water, the introduction of all the improved kinds of machinery, the intelligent system of cultivation, the sure cash-market that exists, and the inexhaus- tible richness of the soil, — these are safe warrants for the assertion that " Colorado agriculture is sure to be remunerative, as well as ennobling, to all who pursue it, and who bring to it that intelligence, industry, economy, and perseverance which is demanded for success in other avocations of life." CATTLE — SHEEP DAIEYING. The rapid increase and general prosperity of the stock interest of the State confirm its character of peculiar attractiveness and adaptability for the successful pursuit of this and kindred industries. The mildness of its climate and the nutritious character of its native grasses not only tend to the highest development and perfection of breeds, but enable the stock- owner to meet the expense of long transportation and compete in the markets of Chicago and New York with cattle-growing regions more accessible to market, but less favored in conditions of climate and vast extent of native and inexpensive pasturage. With the advantages which these two conditions of climate and food so abundantly offer, stock-raising is destined to continue to be a leading — in fact, the second great — industry of Colorado, and a prominent element in its wealth. The grazing-grounds of the State extend from its eastern borders to the line where farming begins — say, a strip twenty miles wide from the base of the foot-hills. From, the Arkansas to the Platte, and along the streams which are tributary to these rivers, on the head-waters of the Republican, and in fact wherever upon the Plains water can be found in sufficient quantities for stock, there is probably an area of forty thousand square miles where cattle, sheep, and horses can range, feeding upon nutritious grasses, and costing their owners a nominal sum only for herding or the expense of the annual " round-up." The yearly losses are very small from storms, exposures, and other causes, and do not exceed five per cent. It is supposed, especially by those engaged in the business, that there COLORADO. 135 are enough cattle and sheep in Colorado for the land that is open to sus- tain them. But this is an erroneous impression, calculated to injure the growth of this important element of wealth. There are still immense areas of pasturage, especially in the southern and south-western portions of the country, where cattle can be kept and where sheep can be made a source of immense revenue. These lands for a long time to come are not likely to be made available for agriculture, and consequently can be used for grazing purposes. The very great profit there is in cattle and sheep lies in the important item of free feeding, and is likely to continue to be the source from which their owners will draw princely revenues for many years to come. A movement was lately inaugurated by the Stock-Growers' Association of Southern Colorado to memorialize Congress on the subject of offering for sale these so-called arid lands at a graduated price per acre, by which extensive tracts which are only suitable for grazing purposes might be purchased at a low valuation, believing that such a course would add to the taxable wealth of the State, while it would be of material service in building up the permanent stock interest. But it is a question if the pas- sage of such a law would not result in the establishment of a few immense ranches, to the exclusion of the large proportion of small cattle-growers now holding the ground by the right of occupancy. The grasses on the Plains are mainly of three kinds : the gamma-grass, growing about ten inches high, in a single round stock, with two oblong heads at the top of it ; then comes the buffalo-grass, growing about four inches high, which is curly in its character and lies close to the ground ; then there is what is called bunch-grass, which keeps green at the roots nearly all winter. On these cattle and sheep subsist the year roimd, and grow fat. The five leading counties of the State wherein cattle predominate are Weld and Arapahoe in Northern, and Bent, Elbert, and Pueblo in Southern Colorado. The number returned last jeat was 502,293. The counties returning the largest number of sheep are Weld, Larimer, and Arapahoe in the north, and El Paso, Huerfano, Las Animas, Conejos, Bent, and Pueblo in the south. The number returned last year was 779,991. But few horses, comparatively, are raised in the State, 61,506 being reported altogether; the five counties having the largest number are Weld, Arapahoe, El Paso, Larimer, and Boulder. The assessment returns of live-stock for some counties are believed to be far too low to give any correct idea of the extent of this industry. It 136 THE GREAT WEST. is believed by competent judges that there are nearly nine hundred thou- sand hdad of cattle and two million sheep in the State, and that the total value of the live-stock upon the range will foot up $15,000,000. The shipment of cattle out of the State has reached over one hundred thousand head yearly, and at an average price of twenty-five dollars per head it will be seen that Colorado realizes no inconsiderable income from this source, it footing up two million five hundred thousand dollars, while the amount realized from the sale of tallow and hides and the dairy prod- ucts adds one million more to these figures. The quality of cattle is constantly improving, there having been introduced within the last few years a large number of short-horns, Herefords, Jerseys, and Devons. A State Board of Cattle Inspection Commissioners is provided for by statute. There are two State Stock Associations, holding annual sessions. In the spring occurs the " round-up," when all the cattle spread over the various grazing-ytracts of country are driven together in one vast herd, and, with their increase, separated and driven to their respective ranges by their various owners. These "round-ups" cover sixteen districts, and are governed by well-established rules and regulations. The growth of the sheep interest has been uniform and rapid. Ten years ago there were not twenty thousand in the State ; now there are two million, and the industry is increasing eaxjh year both in quantity and (by the introduction of thoroughbred Merinos) quality. The wool-clip of last year was over 5,500,000 pounds, valued at $1,400,000. Sheep-raising is very profitable. The estimates of outlay and profit on sheep-farming for three years can be easily given from the actual ex- perience of those engaged in the business : Outlay. — One thousand sheep, twenty rams, wagon-team, harness, ranche, house, corral, herders' wages, and provisions : , First year, $4660; second year, $1225; third year, $2050; total, $7935. Profits. — From the wool : First year, $1790; second year, $2710; third year, $3940; total, $8640. It will be seen, therefore, that the proceeds from the sale of wool more than cover the first cost of the sheep and the herding outfit and expenses, leaving a balance in favor of the raiser of $705. At the end of the three years he has therefore his entire flock in hand, numbering 4200, free of cost. The value of these may be set down at $2.50 per head, or $10,000, while his ranche, corral, and team, worth about $1000, are still to be taken into consideration. This shows a profit of over two hundred COLORADO. 137 per cent, upon his original investment, and the next two or three years the ratio of percentage will increase. One man can attend to from one thousand to two thousand sheep with ease, except at lambing-time, when the services of two men are required for one month. Those who intend to enter this business, however, are advised to go cautiously at first. Learn the ways of the country and the methods of caring for sheep requisite for success by engaging with those who have had experience for at least one season. The knowledge thus gained will be of incalculable value. A careful selection of land for a range is necessary ; some sheep-men have two ranges — one for summer, on the plains, and one for winter, within the shelter of the foot-hills. Good sheep in the start pay better than a poor grade. A close attention to business will enable even those who are novices at it to build up a respecta;ble fortune in a very few years by sheep-raising. In this connection a few words about dairying may not be out of place. For this industry Colorado presents many excellent advantages. The native grass is rich and nutritious ; the water is pure, abundant, and cold ; the soil produces in greatest profusion all kinds of roots adapted for winter-feed for new milch cows. All these are items which the dairy- farmer will readily recognize as important factors in an industry for the products of which there is a constant home-market, where butter brings a good price. The demand for this article has always been greater than the supply, the price ranging from twenty-fi.ve to forty-five cents. We give in this connection a demonstration of what dairymen can do in Colorado, and of the profit there is in the business, from figures kept by one engaged in it : Twenty cows from January 1st to December 1st yielded 2640 pounds of butter, or an average of 132 pounds to the cow, which, selling at 30 cents — a low average price — gave a total of $792, or an average of $39.60 per cow for the season. In addition, the .calVes brought $5 each, making the total from each cow $45.60. The expenses figured up as follows : help, $300 ; salt, $20 ; hay, $80 ; bran and feed, $20 ; total, $420 — leaving a balance of $372 profit at the end of the season, or $18.60 per cow. There are excellent locations for dairying on the Divide south of Denver and within the first range of mountains, from ten to twenty miles from the Plains. These localities are small valleys or parks, varying in size from twenty to two hundred acres, surrounded by mountains, full of beautiful streams of water. Pine, cottonwood, and willows furnish timber and shade, while in the valleys considerable hay can be cut and stored for 138 THE GREAT WEST. winter use. Here the grass is rich and sweet, even far up the mountain- slopes, and usually so little snow falls that pasturage can be had almost every day in the year. Some of these parks are immediately connected with others, making a series of valleys where a few families form a pleasant neighborhood and live in rural quiet and prosperity TOWNS AND VILLAGES. The cities of Denver and Leadville being described under separate headings, we now group together brief descriptive sketches of some of the other principal towns and villages of the State, following the lines of railway : Golden is the county-seat of Jefferson county and the point of junc- tion of the broad- and narrow-gauge divisions of the Colorado Central Railroad ; population, about 3000. This is a manufacturing and coal- mining centre, and is one of the oldest and most prosperous of the cities of Colorado. It was founded in 1859 by gulch-miners, and was at one time the rival of Denver and the capital of the State. It lies on Clear Creek, where a rapid stream, with a fall of sixty feet to the mile, gives the town an immense water-power. Extensive smelting-works have been erected in the valley adjoining the town, and the advantages for manufacturing industries at this point are numerous. Golden is iifteen miles west of Denver, and has an elevation of 5882 feet. The State School of Miues is located here. Two weekly journals, the Transcript and Globe, are pub- lished. Its location is somewhat remarkable for its surroundings, being hemmed in on all sides by mountains, except, at the opening made/ by the debouching of Clear Creek from the foot-hills on its way to the Plains. Idaho Springs is a point of interest as a popular summer resort, where the hot springs annually attract a large number of invalids, while the beauty of the canon draws thither tourists from all directions. The springs vary in temperature from 60° to 110°. The Iris, an excellent local journal, is published weekly. Georgetown is the principal town and the county-seat of Clear Creek county, lying at the very base of the IV&in Range. It was founded in 1860, is surrounded by lofty mountains ribbed with silver-veins, and has a population of 2500. It boasts of waterworks, a fire department, five churches, two newspapers — the Miner and the Courier — ^two banks, and business-houses equal to any town of its size in the State. There are reduction-works, concentrating-mills, sampling and ore-buying establish- ments, all in active operation. Mining is carried on very extensively in the immediate neighborhood. Near by lies the celebrated Green Lake, a COLORADO. 139 ■very attractive spot for tourists and sportsmen, while Gray's and Irving's Peaks tower above it. The elevation of the town is 8452 feet. Black Hawk was first, settled as a mining-camp in 1859, and the present town is built irregularly along the gulches and against the moun- tain-sides. Its appearance, therefore, as viewed from one of the adjoin- ing hills, is very peculiar. The principal industries of the place are gold-mining and milling and reducing ores. Some of the oldest and best- developed gold- and silver-mines of the State are in the immediate vicinity, making Black Hawk a busy, prosperous town of about 1000 inhabitants. It has one weekly journal, the Post. Altitude, 7955 feet. Central City is the business-centre of the gold-mining districts of Gilpin county, its principal city and the county-seat. ' The streets are narrow, steep, and rugged, the result of the peculiar conformation of the ground ; they run on each side of the gulches and on the slopes of the surrounding mountains. It is a terminus of the narrow-gauge system of the Colorado branch .of the Union Pacific Railroad, Georgetown being the other, has a population of 2000, and supports an excellent daily paper, the Register- Call. Distance from Denver, 40 miles. Louisville. — From Golden the broad-gauge track extends northward, passing the town of Louisville, built within the last two years. In its neighborhood is the Welch mine, yielding the best coal found in Northern Colorado, and giving employment to a large number of people. Popula- tion, 500. BotTLDER is the principal town and the county-seat of Boulder county, and is located in a beautiful valley close to the foot-hills. In earlier years it was the head-quarters of an extensive mining district, and is still prominent in this respect. Its site and surroundings, its manufacturing "advantages, the mineral and agricultural wealth of the county, will yet place Boulder in the front rank of thriving cities. Its coal-mines are no unimportant factor in its elements of prosperity. Boulder Cafion (de- scribed elsewhere) is unexcelled in the State for the weird grandeur of its scenery. The State University is located here. There are two banks, six churches, three newspapers, and an excellent graded school employing eight teachers. Population, about 2000. Elevation, 5536 feet. LoNGMONT. — Continuing along the line of the railway, fourteen miles north of Boulder we come to the town of Longmont, located in the very centre of the agricultural portion of Northern Colorado. It is not a large town, but it is an exceedingly prosperous one, being surrounded on all sides for a distance of from seven to twelve miles with cultivated farms. It was settled by a colony in 1872, and relies entirely for its business 140 THE GREAT WEST. upon its agricultural surroundings. Lying on tJie north bank of the St. Vrain, it has a beautiful location, with Long's Peak, from which it was named, looming in the distance. The road to Estes Peak, now attract- ing attention as a summer resort, is from this point. When a system of waterworks, now projected, is established, Longmont will become one of the most pleasant country towns in the State. LovELAND lies seventeen miles north, on the bank of the Big Thomp- son. This town is of recent growth, but bids fair to be the centre of a thriving and industrious farming community. FoET Collins is the county-seat of Larimer county, and, located as it is near the foot-hills, obtains, in addition to the trade of the extensive farming settlements lying all around it, the entire trade of the mountain- districts directly west of it. The road to North Park leads from this point. The State Agricultural College is located on 240 acres of land just south of the town. A splendid brick schoolhouse marks the intel- ligence of the community. Within the last year or two the town has grown rapidly, and bids fair to become the largest in that section. Greeley is a town known all over the Union as the one founded by Horace Greeley, in connection with N. C. Meeker, in 1870, at which time several hundred families left the Eastern States to establish in the West a temperance settlement. At first, many things conspired to dis- courage the colonists, and perhaps four-fifths of the original ones left the place and country in disgust. But now, ten years after its settlement, a thriving town of 2000 inhabitants attests the wisdom of its founders. The streets are of generous breadth, lined with shade trees. The inhab- itants are, as a class, very intelligent. A magnificent school-building was erected six years ago. A canal about forty miles long furnishes water for sixty thousand acres of land enclosed in a common fence. Farming in this neighborhood is the occupation of three-fourths of the people, and the wheat-crop raised each year is about one-fifth of what is raised in the State. Two banks, two newspapers, and churches of all denominations are here and thriving, indicating that the society is of the best in the State. The science of farming is better understood and practised here than anywhere else in Colorado. Greeley is on the line of the Denver Pacific Railway, fifty miles south of Cheyenne. Evans lies south of Greeley, four miles away. It is on the north side of the South Platte River, and boasts an enterprising and thrifty community. Considerable farming is done on the lands lying south of the stream, but there is room for more, as water is abundant. A colony settled here in 1872, and though not as successful as some others, still the COLORADO. 141 result is gratifying, as there is a pleasant little settlement of perhaps 500 people, with a newspaper, schools, churches, flouring-mill, and stores of all kinds. Erie is a coal-mining town in the centre of the coal-producing districts, and is reached by the Boulder Yalley Eailroad, branching off at Brighton, a station on the Denver Pacific. There are five extensive coal-banks in the neighborhood, giving employment to a large number of men. Some farming is done in the vicinity. Population, about 500. Platteville was originally founded by the Platte River Colony in 1873, but has not developed much. It is pleasantly located, however, and surrounded by excellent agricultural land. It has a population of 200. It is a station on the Denver Pacific, about 35 miles from Denver. Littleton is the first principal station on the Denver and Rio Grande Railway, and is 10 miles south of Denver. Pleasantly located on the east bank of the Platte River, it will eventually become a prosperous suburb of the capital, as both the Denver and Rio Grande and the Den- ver and South Park Railways pass by it. Castle Rock is the county-seat of Douglas county, and is beginning to be famous for its excellent building-stone, which is extensively used in Denver and elsewhere. It has not a very large population ; settlements in the vicinity are scattered, but still it supports a newspaper, school, churches, and a number of stores. Monument lies about 20 miles north of Colorado Springs, just over the crest of the Divide, and is the centre of a rapidly-growing district. It draws the trade of a section of country stretching east over twenty miles, where farming can be carried on without irrigation. There is also a good dairying district in the neighborhood, for, though streams are few and scanty, yet an abundance of springs that never run dry give it an advantage in this respect over other portions of the State. CoLOEADO Springs is the Saratoga of the "West. Founded in 1871 under the auspices of the railway company, it soon came into prominence as a favorite resort for invalids, while its close proximity to Monument Park, the Garden of the Gods, Glen Eyrie, Manitou, Pike's Peak, Chey- enne £!anon, and other attractive points soon made it a place toward which tourists from all parts of the East tended. The streets and avenues are broad, and lined with trees of uniform size planted by the town company in the early days of its organization ; these have now grown to a large size, and make the city look like a forest during the summer season. Outside of Denver, it has the handsomest residences of any town in the State, and is attracting to it the wealthy and influential classes to such a degree 142 THE GREAT WEST. that it bids fair to become, socially and intellectually, the most desirable residence-city in Colorado. Waterworlts and gasworks give quite a metropolitan tone to it. Business is good, and constantly increasing in volume. The population is set . down at 6000, but it is difficult to establish it definitely, as it ha.s, and always will have, a shifting popu- lation, drawn to it by the natural advantages of the town for invalids and pleasure-seekers. An irrigating-canal supplies extensive tracts of land with water for gardening purposes, but no large breadths of farm- ing-lands can ever be cultivated in the immediate vicinity, as the waters of the Fontaine-qui-Bouille are not of sufficient volume to warrant the construction of any large canal. An excellent daily journal, the Gazette, is published here, and one weekly. Colorado College, a Congrega- tional institution, is located here, and has been liberally endowed. A stone schoolhouse was early erected, but three buildings are now required for the educational needs of the residents. The State Deaf and Dumb Institution is located just east of the town, on rising ground commanding a beautiful view of the mountains. Colorado Springs can be considered the third city in size in the State, but in proportion to its population it does not fall behind Denver in social position. Pueblo, the principal town and the county-seat of Pueblo county, is located in the valley of the Arkansas, near the confluence of that stream with the Fontaine-qui-Bouille. It is surrounded with good grazing-lands and many hundred square miles of fertile agricultural land, but the un- certainty of the current and the shifting sands that constantly wash into it make large canals somewhat expensive to keep in good working order. Originally, Pueblo was quite a distributing-point for the South and West, and a rendezvoas for the various stage-lines running in these directions ; but the advent of the railroads changed these, and it is now something of a railway-town, it being the terminus of the Atchison, Topeka, and Santa F6 and a highway for the Denver and Rio Grande, which latter also has a branch road running from it to Caflon City, 35 miles west. An excel- lent daily newspaper is published here, also a weekly ; the town is well supplied with schools, churches, public buildings, and is the seat of the Insane Asylum of the State. CaSon City is the county-seat of Fremont county, and boasts a popu- lation of 1200, with banks, newspaper, churches, and schools. The State Penitentiary is located here, built of granite quarried from the adjoining hills. The town is located just where the Arkansas leaves the foot-hills, boasts of mineral springs, both hot and cold, and undeniably possesses some superior natural advantages. There are some singularly beautiful COLORADO. 143 cafions near by, while the Royal Gorge is but a few miles distant, and is soon to be traversed by the iron horse as it steams en route to the great carbonate city of Leadville. (These cafions are mentioned elsewhere.) Near Caflon City considerable attention has been paid to fruit-culture, and the results have been gratifying in the extreme. Between Caflon City and Pueblo, a distance of 35 miles, some farming- is carried on. The city has advantages that cannot fail to ensure it a prosperous growth, Trinidad. — This town is situated near the base of a spur of the Rocky Mountains, a few miles from Raton Peak ; it lies on the Las Animas River, a stream whose valley, about 150 miles in length, em- braces some of the most fertile lands in Colorado. Inexhaustible beds of coal are in the immediate vicinity, and hundreds of ovens are engaged in making coke, the demand for which is greater than can be supplied. Copper and iron ores have been discovered in the neighborhood, while the plains east of the town are covered with cattle. In fact, Las Animas county, of which it is the seat, is fast coming to the front as the leading stock-county of the State. The town has had the New Mexican trade to a large extent of late years. Perhaps one-quarter of the people are Mexicans in a population of 2000. The Atchison, Topeka, and Santa F6 road reaches the town from the east, and the Denver and Rio Grande from the north. Its growth within the last few years has been very rapid and healthy, and Trinidad, though almost on the southern line of the boundary of the State, being only 14 miles from the New Mexican line, has a promising future before it. The Raton Pass, aptly denom- inated the gateway to New Mexico, is but 15 miles from the town. It supports two daily newspapers, schools, churches, and other adjuncts of civilized society. BuENA Vista was founded only last year, but its peculiar location has already brought it into prominence, and it seems likely to be a thriving town. It rests in the delta formed by Cottonwood Creek at its junction with the Arkansas River, and the site i^ pronounced to be one of the finest in the State. Its nearness to Leadville, being only about 35 miles from that city, makes it a place where the business-men of that populous but unhealthy city could easily reside, now that railroad communication is to be established between the two places. Near by are the famous Cot- tonwood Springs, becoming known as a resort for invalids troubled with rheumatism. There is said to be a large body of land suitable for agri- cultural purposes in the neighborhood, but the town is more likely to become celebrated as a great watering-place, and may yet rival Colorado Springs in attractions. 144 THE GREAT WEST. Alamosa. — This town has been for two or three years the south-west- ern terminus of the Denver and Rio Grande Railway, and has grown into some importance as the point from which to reach Del Norte, Silver- ton, Ouray, and the San Juan country. It has a population of about 800. Some large forwarding-houses are established here, and an exten- sive trade is carried on with the settlements west and south of it. It is beautifully laid out on the west bank of the Rio Grande del Norte, and is in the centre of San Luis Park. The town is entirely surrounded with majestic mountain-ranges, and presents a very attractive appearance. Overlooking the site rises Sierra Blanca, its snow-crowned crest stretch- ing skyward to an altitude of 14,472 feet. Its snowy mantle is peren- nial, and its lofty crest, like the pyramids of the Egyptian dynasties, is gilded at each sunrise with the first flushing touches of the coming morn. There are many points contiguous to Alamosa that will yet tempt the artist to reproduce them. The extension of the railroad south to Conejos may take away most of the southern trade from the town, but it will still be the main distributing-point for the mining districts to the west of it. The Independent is a sprightly local paper, published weekly. Saguache is the county-seat of Saguache county, and lies in the north-west corner of San Luis Park. It is the business-centre of a large and constantly-increasing agricultural and live-stock region, and was first settled in 1874. It has a population of 500, and while its growth has not been as noticeable as that of towns in mining districts, still it has been steady and the business transacted is of a substantial nature. Lead- ville has proven a very profitable market for all those engaged in pur- suits connected with the soil, and the impetus thus given to the industries of Saguache is not now likely to retrograde. One weekly journal, the Chronicle, is published, while the town has the usual supply of chiurches and schools. SiLVEETON is the county-seat of San Juan county, and is a growing and prosperous town. Lofty mountains overhang the lovely little park in which the town is located, and in these lie hidden numberless silver- veins of varying richness. The great depth of the snow in winter makes tlie approaches to this town almost impassable for several months in the year, hence it labors under great disadvantages. The elevation, too, is somewhat high, being 9400 feet. In summer coaches connect it with Lake City and the outside world. Silver Cliff, — This town is hardly two years old, but has sprung to a sudden prominence in the mining history of the State that promises to be enduring. It is located on the eastern slope of Wet Mountain Val- COLORADO. 145 ley. Two daily papers are already published here, and the fame of the mines is likely to make the town one of the most important among the many that are rising into prominence in the mineral-bearing sections of the State. It is 30 miles from Cafion City, mth. which point it makes daily connection by coach. Mills of various kinds have been erected, and the undoubted richness of the mines in the vicinity- will ensure a steady development of business. Lake City is the county-seat of Hinsdale, and the principal town in it.' It is one of the most promising towns in the San Juan country, At present it does not control the trade it had in 1876 and 1877, before the discovery of carbonates, at which time it was the distributing-point for the Sierra country, as San Juan was called ; but it can look forward en- couragingly to the future, when attention will be again drawn to the in- exhaustible fissure-;y^eins that rib the mountains and indicate the untold wealth that lies in them. It is surrounded by 'these, and has a situation bordering on the wildly picturesque. Del Noete. — This town lies along the banks of the Rio Grande River, and is the county-seat of Rio Grande county and the entrance- way to the mines of San Juan, The gold-mining excitement of 1874 created it, and it has now a population of about 1200, sustains a bank, a weekly journal, churches, schools, many large stores and warehoiises. It is 34 miles from railway communication, its nearest point being Alamosa. While not at present presenting any prominence among the towns of the State, it may be said to enjoy a present fair share of prosperity, with an assured future before it when the San Juan mines are worked. LBADVILLE AND THE ADJACENT CAMPS. ■ Three years ago Leadville had no existence. It is now a city of giant proportions, and challenges the world to produce its superior in all that embodies the features of present wealth and future greatness. It lies under the deep shadows of the continental Divide, a very Golconda of riches within the hills that encircle it, clothed with the majesty of a metropolis, and inhabited by a people active in all the industries con- nected with professional and commercial life. To a newcomer, this city, the creation of three years, preseiits . a fresh and startling aspect when compared with the old-established cities whose position is the result of decades of growth. Fifty thousand people where but a short time ago there were not fifty is an indication of the strength of that thirst for gold that first sent Coronado in search of the Seven Cities of Cibola in the country to the south of the Carbonate Camp,, and 10 146 THE GREAT WEST. that has in our day gathered together the people of all nations and coun- tries, all professions and trades, of all ages and conditions. The reported richness of the camp took them in by hundreds daily last year in all manner of conveyances and by Nature's own method of transportation. Many sought for wealth in a day, and, finding it not, left for other fields. But those who remained in more or less measure of success have had their persistence crowned with the reward of well-doing. Hardly a week passes, even now, without heralding the discovery of new mines of fabulous value, while the possibilities of the future are almost suf- ficient to turn the brain of the most clear and cool-headed of mankind. One hundred and seventy-five producing mines, and thousands more possessing good prospects, are a base of calculation for the growth of Leadville that no other place in history has ever presented. The man who put up the first shop in the town,^on Chestnut street, refused to give one hundred dollars for it when the owner of the lot on which the shop stood demanded that amount. Within ninety days he saw the same lot sold for three thousand dollars. Hundreds, like him, have hesitated, and lost small fortunes by their hesitation. High as are the figures asked now for business and residence lots in choice locations, these prices are more likely to advance than recede. But the era of wild speculation has passed away, and real-estate transactions are on a solid basis. Fortunes are y6t to be made, but capital will be re- quired in larger amounts than heretofore. The climate of Leadville cannot be said to be one conducive to the restoration or preservation of health. It is in a region of altitude where vegetation is limited, the air of an extreme rarity and full of the delete- rious vapors from a score or more of smelting and other works located in the very heart of the city. The prevailing diseases are pneumonia, pleurisy, diphtheria, cardiac affections, erysipelas, and bronchitis. Acute rheumatism also prevails, while lead-poisoning is frequent among those employed in the smelting-works. The sanitary condition of the city is yet imperfect, and prejudicial to health. There is no system of sewerage, and the emanations from the smelting-works fill the atmosphere with sulphurous fumes and carbonic-acid gases. A great deal of sickness, however, is the result of exposure and imprudence or ignorance on the part of newcomers. The sudden entrance into a higher altitude always affects those who are not acclimated. Care must be taken to guard the body against the sudden changes of the weather. Heavy woollen under- garm'ents are an absolute necessity in summer as well as winter, as the setting of the sun is always followed by a marked change in the ther- COLORADO. 147 mometer. All exposures and imprudences are to be avoided, and what might at a lower altitude be a simple cold, not needing any care or atten- tion, in Leadville will speedily develop into a serious case unless prompt- ly attended to. It does not get well of itself, as elsewhere. A proper sanitary provision will ultimately remedy some of the evils here men- tioned : a careful attention to hygienic laws on the part of those who reside there will tend to decrease the number of cases of sickness, and the time may come when Leadville will enjoy what it certainly does not do now — a good reputation as a healthy city. The altitude is ten thousand two hundred feet above the level of the sea, and. the city is located on a broad plateau of land sloping toward the Arkansas Valley, and is surrounded by towering mountain-ranges. Its supply of water is brought frOm a distance by means of ditches and pipes, while an immense reservoir has been built near by to hold a reserve. The water is pure, wholesome, ample, and never-failing. The winters are severe and long, while even in summer the nights are cold. Hotel accommodations range from one to four dollars per day. Board in pri- vate houses is ten dollars per week. Rents are high, close to business- streets averaging twenty dollars per month for a single room, running down to five dollars on streets a few blocks away. There are some build- ings yielding in two months' rent what it cost to build them. Lumber is mostly used for building purposes. Native costs $30 ]per thousand feet ; Chicago A stock, $125 ; Chicago .siding, $50 ; shingles, $7 ;- doors and sash, from $2,50 to $5. Brick is scarce, bringing $20 per 1000. The most successful prospectors are those who know comparatively little about minerals. Pluck, perseverance, and a pick are the three requisites to success, supplemented by pork and provender. The time has gone by when men with small capital can enter into business success- fully in Leadville. There are no Chinese ; they were once introduced into the gulch, but immediately notified to leave, and since then have not ventured to intrude. The articles needed by a prospector depend upon his bringing-up and the length of his purse. As one has said, " If he is well fixed " he may buy a burro for $25, and on the back of the diminu- tive beast pack his tent, pick, shovel, sack of flour, side of bacon, blankets, frying-pan, coffee-pot, sugar, coffee, and baking-powder, and start off on his venture, comparatively " well fixed." A Sharp's rifle is a handy thing to have — ^not because there is anything or anybody to fear, but elk, ante- lope, and Utes are to be met with, and are excellent — when dead. Men looking for soft positions as clerks and bookkeepers are not wanted. Wages of carpenters, bricklayers, miners, and laborers range from five 148 THE GREAT WEST. to two dollars per day. The working or building season is from May to October. The town is full of professional men, but here, as elsewhere, " there is always room at the top." Insurance rates rule high on account of the buildings being mostly of wood. The cost of living may be estimated from the following figures ; of course there is a constant fluctuation, according to the season and the abun- dance of stocks in the market, but a good idea can be had from the prices given : Flour, $6.75 per 100 pounds ; potatoes, 6 cents a pound ; sugar, 15 ; lard, 15 ; coffee, 30 ; hams, 15 ; bacon, 15 ; tea, 50 cents to $1 ; salt, 5 cents ; syrup, $1.50 per gallon ; vinegar, 75 cents ; coal oil, $1 ; candles, 25 cents a pound ; corn meal, 5 cents ; Graham flour, 6 ; raisins, 20 ; cod- fish, 12 ; mackerel, 10 ; dried fruits, from 10 to 45 ; beans, 8 ; barley, 12 ; hominy, 10 ; crackers, 12 ; butter, 40 to 50 ; cheese, 25 ; soap, 8 ; eggs, 45 cents a dozen ; poultry, 25 cents a pound ; oat meal, .8 ; mincemeat, 20; dried beef, 20; white fish and mackerel, $2 per kitt; buckwheat flour, 10 cents a pound ; New Orleans molasses, $1.25 a gallon ; canned goods, from 25 to 75 cents a can; beef, 15 cents a pound; mutton, 15; pork, 20 ; wild meats in their season, 20 ; prairie-chickens and grouse, 60 to 75 cents a pair; quail, 50 cents a pair; trout, 60 cents a pound; lake and sea fish, 35 to 60. A trade-report of over twenty million dollars in a city but three years old, with a certainty that even this enormous amount does not include the whole of the business, presents a statement challenging comparison with any Eastern city of three times its size. We group together the different branches of trade as proof positive of the marvellous enterprise displayed by its business-men and of the activity exhibited in a city built ten thou- sand feet above sea-level. If no other evidence was at hand of the num- ber of people in and about Leadville, the fact that their necessities de- manded such a wave of business would be amply sufficient : Assaying, $45,000 ; auction, $260,000 ; barber-shops, $40,000 ; bakers and confec- tioners, $310,000; books and stationery, $75,000; bath-houses, $35,000; blacksmiths, $900,000; boots and shoes, $165,000; clothing, $650,000 ; cigars and tobacco, $100,000; dry goods, $1,100,000; drugs, $235,000; fruits, $25,000; furniture, $175,000; glass and queensware, $25,000; groceries and provisions, $3,500,000; hats and furs, $45,000; harness and saddles, $30,000 ; hardware, $750,000 ; hay, flour, feed, and grain, $850,000; hotels, $450,000; jewelry, $210,000; lumber, $750,000; livery and sales stables, $500,000 ; millinery and dressmaking, $75,000 ; meat and vegetables, $600,000; manufactures, $400,000; tailors, $30,000; commissions on mining and real estate, $600,000; news d6p6ts, $35,000; COLORADO. 149 oysters, fish, game, and eggs, $40,000 ; plumbing, $75,000 ; painting and papering, $55,000; restaurants, $550,000; sewing-machines, $10,000; loans, $4,500,000 ; surveying, $85,000 ; shingle-mills, $200,000 ; storage and commissions, $125,000; theatres, $500,000; wood, $60,000 ; liquors, $885,000. Grand total, $20,120,000. These figures tell their own story. The " boom of business," as it is called, is no way lessening ; on the con- trary, it is constantly increasing, and the business of the present year will without doubt figure up $30,000,000. The first public school organized in Leadville was in July, 1877. In the fall of that year a Board of Education was formed and school-terms were established. There is now a high school, two intermediate and four primary schools, and the last census of the district showed 1230 scholars. Nine teachers are employed, whose salaries range from $60 to $125 per month. The school property of the district cost about $10,000. It may be said that the educational interests of the city are in a fair way to be properly taken care of, and that the rising generation will receive all the advantages that a liberal-minded policy can give them. Already school privileges are of a pronounced and healthy character, while there is no doubt that the future will provide all that is necessary to render the system more complete. Six religious denominations have church buildings — ^the Presbyterians," Methodists, Christians, Roman Catholics, Congregationalists, and Episco- palians. The pastors of these churches are doing a good and effective work in society, and are upheld by a large moral sentiment outside of their respective organizations. The Leadville bar compares favorably with that of any city of its size, and has in its ranks men who are distinguished for legal lore and elo- quence. Of course these representative men have come from every State in the Union ; some have grown gray through long years of study and experience in other fields, and now bring to their new arena of labor the ripe fruits of years of toil. The field, like that in all mining camps, is a lucrative one, on account of unsettled titles and conflicts of claims and interests. Hence, while some mines make their legal owners rich, other mines make the legal advisers of the owners feel that bonanzas are not entirely confined to the glittering soil, but are also hidden in the " glitter- ing generalities " of the law. Leadville was incorporated as a city in March, 1879, and is run at an ex- pense of nearly five thousand dollars per month. It has a mayor, aldermen, clerk, solicitor, physician, engineer, surveyor, street commissioner, fire- warden, marshal, and twenty policemen. The salaries of these city officials 150 THE GREAT WEST. range from $250 per month down to $75. A revenue of nearly $200,000 is derived from licenses and fines, while the expenses are largely under that amount ; hence the financial affairs of the corporation may be said to be in a healthy condition. But it is a sad and suggestive comment upon the morals of Leadville that the arrests from which fines are received average two hundred per month, and the great majority of these are traced directly to intemperance. An excellent fire department is in effective service. Time and money were early given toward the organization and support of a fire-service. There are one hook-and-ladder and two hose companies, fully equipped and uniformed. There are fifty-nine hydrants or fire- plugs through the streets, having a head or pressure of water sufficient for all practical piu-poses, while the Gamewell system of fire-alarm tele- graph is in active working order. So it will be seen that full provision has been made against the spread of fire. The mineral fields of Leadville cover many gulches and mountains, and seem to defy all laws of mining deposits. The class is termed car- bonates, which is defined by Webster as a salt formed by the union of carbolic acid with a base. In working, the first thing found is the drift, debris, boulders, and gravel that floods and fires have rounded into hills and valleys. These go down a few feet, when a light-colored chalk rock is met with ; this is porphyry, and overlies the iron, which is the cap-rock of the ore, and is called the " contact." When iron is reached and carbonates found beneath it, a mine has value, not before ; for some- times no mineral is found beneath the iron. The bed-rock is usually blue limestone of an undulating character, and the ore follows the uncer- tain course of the wall, and is rich in the depressions and more barren in the elevations. There are two theories extant as to the placement of the carbonates in the position in which they are found. One is, that they were washed into their resting-place ; the other, that internal commotion forced the bed-rock and the cap-rock apart, using the carbonates as a lever, where they cooled and remained. The weight of opinion is on the side, of the last supposition. Sixteen extensive establishments smelt the gold and silver output. These have all been built since September, 1878. The entire value of bullion produced by them for the year 1879 reached a grand total of $9,250,000, the four principal smelters producing more than one-half of the above amount. There are two sampling-works where ores are crushed, assayed, and mill-runs made ; these do quite an extensive business in buying and shipping ores to foreign smelting companies and base bullion for ship- ment to the refineries, the value of the ore they ship out figuring over COLORADO. 151 one and a quarter million of dollars. Taking the amount of bullion-prod- uct from the smelting-works, value of ore shipped out by sampling-works, the amount sent by private parties to foreign smelters, and the gold-yield from placer-mines, a grand total of nearly thirteen millions of dollars for one year presents figures for the world to wonder at. The amount of mining transfers during the last year gives a good in- dication of the wave of prosperity now flowing over the camp. In this estimate is omitted all transfers where the amount was less than five him- dred dollars, but includes the sales of placer-mines as well. All sums named in considerations which are known to be purely nominal have not been taken into account. This grand total of mining transfers for the year foots up to $35,350,940. One of the most important mining tributaries to Leadville is that comprised in the district known as the " Eagle River country," about twenty-five miles north-west, where all the elements of a prosperous min- ing district seem to be concentrated. Outside of the Carbonate Camp proper there is no section of the mineral regions of Colorado, as far as known, so full of genuine promise as this ; and its favorable showing, and the rapidity with which energetic prospectors are developing a re- gion running for fifteen miles up and down the Eagle River, entitle it to rank among the best in the State. Before the year is over it may be that Eagle City will be no mean rival to Leadville. " The Gunnison country," as it is called, is reached from Leadville over the Red Mountain Trail through Lake Creek Canon, one of the most beautiful of all Colorado's caflons. This silver land beyond the Snowy Range is likely to be the Mecca of thousands of prospectors during the present season, as fabulous stories of its richness in the precious metals have been circulated, and will have their due effect upon the minds of those who seek Colorado for a fortune. In addition, the Elk Mountain region, on the edge of the Ute Reservation, has given substantial indica- tions of silver in true fissure-veins varying in length from one to two feet. The town of Gothic has already been founded at this point, and the country explored for miles around it. The only drawback to the im- mediate development of this country is the Ute question. If this is sat- isfactorily settled, the vast resources of this entirely undeveloped region will be opened up, and we may expect that the Elk Mountains and the reservation will become one of the most populous mining camps, and possibly the richest, in the State. Ruby Camp is in the Gunnison country, and was organized in June, 1879. It comprises the section embraced by Coal, Ohio, and Anthracite 152 THE GREAT WEST. Creeks and the North Fork of the Gunnison River, and may be said to be a tributary to Leadville. Although young, the camp has an apparent- ly bright future before it. The mines thus far discovered are all true fissures, and where shafts have been sunk a high-grade mineral has been reached, composed of brittle ruby, chloride, and black sulphurets of sil- ver. Sometimes native and wire silver have been found. About fifty mines have been more or less developed, but it is probable that the camp during the present season will present a lively appearance, as saw-mills, smelters, and roasters are to be taken into the district this spring. The Denver and South Park Railway is pointing in this direction. It is said that in addition to its mineral prospects there is a large deposit of bitu- minous coal about ten miles distant, which excels even the Trinidad coal for coking purposes. The main town in this district is named Silver Gate, and is beautifully located. Ten Mile is an important mining district about fifteen miles from Leadville, on the western slope of the range, and is in a valley of the same name lying about eleven hundred feet above the sea-level and from three-fourths to one and a half miles wide. There are three towns, named Kokomo, Carbonateville, and Ten-Mile City, in close proximity to each other. The district has three smelters, and it is said shows more mineral than Leadville did two years ago ; but capitalists have not invested here as yet to any great extent, though there are scores of mines giving abundant promise. The valley is said to be far more healthy than Leadville, while it also possesses some of the most magnificent scenery in the country in Ten-Mile Caflon, of which notice is made elsewhere. DENVEE. In June, 1858, the first party of prospectors (from Georgia, led by Green Russell) reached Cherry Creek. In September of the same year a town was established on the present site of Denver, and called St. Charles. In October a rival town, called Auraria, was located on the west side of the creek. In November the Denver City Town Company was organ- ized and the site of St. Charles occupied. Considerable rivalry existed between the two towns until the year 1861, when Auraria began to lose ground. Early in 1859 a hotel, blacksmith-shop, bakery, and carpenter-shop were erected, and in April the Rocky Mountain News was issued by Wil- liam N. Byers & Co. In the same month a convention was held to form a government for a State that was to be called Jefferson. In May a post- COLORADO. 153 'office was established. In June, Horace Greeley arrived by coach, en route to California, and addressed the citizens of the town before visiting the mines. In December the first mayor was elected, under a city char- ter granted by the provisional Legislature. In October, O. J. Goldrick opened the first school. By New Year's Day, 1860, Denver had two hundred houses, while Auraria had almost twice that number, the com- bined city census giving a population of over one thousand people, rep- resenting all classes, creeds, and nationalities. In April, 1860, the towns of Auraria and Denver were consolidated. On the Fourth of July the patriotic pioneers celebrated the day in a grove close by. The close of the year found about four thousand people in the town, with three day schools, five churches, and three newspapers. During the winter of 1860-61 a stampede was made by hundreds of the inhabitants of Denver and the adjoining mining camps to the San Juan Mountains, whose reported discoveries were shortly pronounced a hum- bug. In April news of the rebellion reached Denver, and by August recruiting was going on for the first regiment of volunteers. For the next few years the rebellion, the big fire of 1863, and the Indian war of 1864 blockaded the route to the States, paralyzed the industries of the town, and threatened danger in every direction. Dull times prevailed until 1866, when a reaction set in. In that year over three hundred new buildings were erected, and the census showed a bond fide population of four thousand, with perhaps half as many as transients. In 1867 a Board of Trade was organized, and through its efforts the first attempt at building a railroad to connect the embryo City of the Plains with Cheyenne, and so obtain railway communication with the East and West, was made, and by 1870 the project had been successfully carried out. The Denver Pacific Railway reached the "bity, and it was no longer an isolated point apart from civilization, but part and parcel of the great overland highway from the Atlantic coast to the Pacific. Such is the brief epitome of the first eleven years of the history of Denver, but it might be well to give some statistics in connection with its commercial prosperity at that time, in order that its present position may be the better placed in contrast. The place was well and solidly built up, many of its banks, churches, public buildings, and principal business-blocks comparing favorably with those of much older and larger cities in the East. It contained at that time about fifteen hundred build- ings, with a population of nine thousand. The sales of general mer- chandise footed up $8,500,000 for the year, while coal, lumber, land sales to new settlers, live-stock and beef, flour and the value of new buildings. 154 THE GREAT WEST. increased the total to nearly twelve millions. The banks carried an aver- age of $1,500,000 in deposits, and the shipment of bullion was nearly $6,000,000. Four lines of railway were built or building, centring in Denver — the Kansas Pacific, Denver Pacific, Colorado Central, and Boulder Valley. The Denver and Rio Grande, leading southward, was being graded, and the narrow-gauge system from Golden to the moun- tains projected. One woollen-mill, two flouring-mills, an iron-foundry, two planing-mills, a terra-cotta factory, a carriage-factory, several wagon- factories, a turning-shop, and other industrial enterprises marked the prog- ress the town was making in the department of manufactures. A branch of the United States Mint was in operation, while a theatre gladdened the pleasure-loving public with its nightly attractions. The business of the town was on a solid basis, and the outlook exceedingly favorable. From 1870 to the present time the growth of Denver has been steady, while to-day the city enjoys the flood-tide of prosperity consequent upon the rapid settling, up of the country. During the year 1879 the arrivals averaged two thousand per week, filling the hotels to their utmost capacity and taxing the ingenuity of landlords, while private houses for boarding were filled to repletion. To-day there is no more beautiful and attractive city than is Denver. She has proven her title to the name of the " Queen City of the Plains," and as a thriving trade-centre, great thoroughfare, and pleasure resort she has become known all over the Union. For a hundred and fifty miles the eye can take in the outlying foot-hills and the Snowy Range, forming a landscape of whose never-ending beauty the eye cannot grow weary. The streets are broad, solid, and cleanly, lined with massive business- blocks, elegant residences, and cozy cottages, while shade trees and lawns abound. ' A review of the trade of Denver for the year 1879 will give some idea of the advance during the last ten years. Twenty-six millions of dollars' worth of business was done in the leading branches, while those not enumerated will swell the figures up to thirty millions. The banking business is a safe index to the growth and prosperity of a community. Four national and One private bank, with a combined capital of $600,000, show total deposits amounting to $5,875,665, and loans and discounts to $2,721,125. The amount of exchange drawn was $36,500,000. The building of the reduction-works at Argo within the last two years has materially aided the growth of the city. Removed from Black Hawk early in 1879, active operations have been carried on and a large amount of bullion produced, amounting in gold, silver, and copper to $3,000,000. COLORADO. 155 Eeal-estate transfers have been unusually active of late, and an advance in prices of nearly fifty per cent, has gladdened the hearts and filled the purses of fortunate owners. The records of the Recorder's office show transfers amounting to about two thousand in number, with a considera- tion of nearly three million dollars. This is an excellent showing for one year, but the present season will probably double it, both in the number of transfers and amount of values, thereby proving the existence of a healthy financial condition, the confidence of capitalists in the assured growth of the city, and establishing beyond question the fact that it is to be the largest and most important commercial centre between the Missouri River and the Pacific Ocean. The number of buildings erected during the last year is without pre- cedent in the history of the city. Yet the demand for them has far ex- ceeded the supply, rapid as it has been, and there seems to be no likelihood of any cessation of building operations during the present or the next few years. Denver seems to possess peculiar attractions for those who are making fortunes in the mining districts, and is yet to become famous as the residence of a score or more of " bonanza kings," M'ho are putting their surplus moneys into splendid business-blocks and superb private residences. Probably five hundred new buildings were erected last year, costing $2,250,000. Among the most prominent of these may be men- tioned the Grand Hotel, costing $250,000 ; the Tabor Block, $180,000 Glenarm Hotel, $40,000 ; Twenty-fourth street public school, $24,000 Wentworth House, $30,000 ; Senator Hill's private residence, $20,000 Washington Terrace, $18,000. Scores of elegant residences, costing from $3000 to $10,000, have been put up, while the number of tenement- houses, containing from four to six rooms, has not been half equal to the demand. It may be that for several years to come this remarkable growth can be looked for, as there seems to be no diminution in the arrival of strangers and no abatement in the influx of capital. The street-railway system, of late years fully equal to the requirements of business, is now hardly adequate. The number of ears put on has been doubled during the year. There are only eight miles of road in operation, but the widening of the area of residences, and their exten- sion into the suburbs east and west and south, will necessitate new branches to accommodate the needs of the residents of these points for rapid transportation from their places of business to their homes. During the year two telephone systems have been in operation, with nearly a thousand connections. These lines reach out to the neighboring towns of Golden, Central, Black Hawk, and other points. A consolida- 156 THE GREAT WEST. tion of the two companies was made early in the present year, and they are now practically under one management, doing a very efficient service and coming more and more into popular favor. The branch mint at Denver purchased over six hundred thousand dol- lars' worth of the precious metal. It is believed that additional facilities will shortly be provided for manipulating the minerals of the country. The posf>-office business has doubled during the last year. There is now a carrier service in operation. The money-order department issued orders amounting to $325,000, and received from other offices $1,112,000. It paid out on domestic and foreign orders $435,000, and remitted nearly $1,000,000 to other points. In the registry department 12,000 letters and packages were sent, and 16,500 received. The total expense of con- ducting the office was about $21,000, while the receipts from the sale of stamps and envelopes, box-rents, unpaid letters, and waste paper was $82,000. The city is supplied with water for fire, domestic, and manufacturing purposes by the Denver Water Company, with works constructed on the Holly system. Three million gallons were furnished in 1878, double the quantity of last year, and the limits of the works thereby reached. But new works, costing a quarter of a million of dollars, have been constructed, a large reservoir or lake established a short distance from the corporate limits, and in future the people are ensured an abundant supply of pure water, the capacity of the new works being from six to eight million gallons every twenty-four hours, supposed to be equal to the needs of a city of seventy-five thousand inhabitants. Thirty miles of mains have been laid, and more are being extended in directions where they are needed. The city government is composed of a mayor, clerk, treasurer, engineer, chief of police, attorney, police justice, street commissioners, chief of fire department, and twelve aldermen, two from each ward. The fire depart- ment includes four fire and hose and two hook-and-ladder companies. There are the county hospital and St. Vincent's and St. Joseph's Homes, in charge of the Sisters of Charity. Three express companies have general offices — the Kansas Pacific, Adams, and Leadville. The Western Union Telegraph has its general Western office here. Of newspapers and periodicals we enumerate the following : Daily. — Rochy Mountain News, Tribune, JRepublioan, Post, Hotel Reporter, and Times ; each of these issues a weekly edition. Weeldy. — Farmer, Hei'ald, Journal, Mining Review, Financial Era, and Gazette- Advocate. Month- ly. — The Antelope and The Colonist. COLORADO. 157 The churches of Denver are well sustained, and some of the edifices are an adornment to the city. The pastors, as a rule, are faithful in the performance of their duty ; some of them are quite talented and draw " full houses " — if the term may be allowed — every Sabbath day. Two services are generally held — one in the morning and one in the evening — with Sabbath-school in the afternoon. Wednesday evening of each week is devoted by all the denominations to a meeting for prayer. During the annual week of prayer union services are generally held. Between the pastors of the various churches a good feeling of harmony prevails. Each in his own immediate circle finds his head, heart, and hands fully employed ; hence sectarian squabbles are hardly known. The influence of the pas- tors of the churches is felt on every hand in every kind of public enter- prise having reform for its base. Especially in temperance-work have they been active. They, aided by the Good Templars, inaugurated the Blue Ribbon movement in the State three years ago, which has been so effectual in the reformation of hundreds who are now sober and indus- trious citizens. The first preaching and praying ever done in the State of Colorado was done in Denver as early in its history as December, 1859, when the voice of one George Washington Fisher was heard preaching in the wil- derness, and from that day onward religious privileges have not been lacking for those who are so inclined ; and the proof that a large pro- portion of the community is a church-going class is found in the twenty- six churches and religious organizations that now exist in Denver. The Baptists have three — Zion, First Baptist, and Antioch. The first and the last of these are colored. The second is presided over by Rev. F. M. Ellis, an eloquent divine. The Catholic element sustains St. Mary's Cathedral, Church of the Sacred Heart, and St. Elizabeth's church. Two are Congregational — ^the First and the Second. The Episcopalians have four — St. John's, Trinity Memorial, Emmanuel, and All Saints'. There are two Jewish — ^the Emmanuel and the Ohawi Emune. The Methodists are numerically the strongest denomination in Denver. They sustain seven churches, as follows: African Methodist Episcopal, California Street Methodist, German Episcopal, Lawrence Street, M. E. Church South, St. James, and Evans Mission Chapel. The Rev. Earl Cranston is the bright and shining light of this branch of Zion. The Presbyterians have three churches — the Central, St. Paul's, and Seventeenth Street. Rev. H. C. Westwood, a distinguished divine lately from Philadelphia, presides over the first, which has the most pretentious church-edifice in the city. There are one Second Christian, one Reformed, one Unitarian 158 THE GREAT WEST. church, and a railroad mission-school ; in this last named all the churches are interested, and unite in sustaining it. It will be seen that thus far the religious facilities have been ample for the needs of the people ; but the rapid influx of population has filled all the churches to overflowing, and either larger edifices must shortly be built or new societies organized around which can crystallize the new- comers who are making homes for themselves in the beautiful and attrac- tive " City of the Plains." Of secret and benevolent societies the following are in successful opera- tion, earnestly working in their respective fields of labor : Masonic. — Grand Lodge A. F. and A. M., with an annual session in September; Grand Royal Arch Chapter; Grand Commandery K. T. ; Denver, No. 5, A. F. and A. M. ; Union, No. 7, A. F. and A. M. ; Den- ver Chapter, No. 2, E. A. M. ; Colorado Commandery, No. 1, K. T. ; Pentalpha, No. 5, F. and A. A. ; Delta Lodge of Perfection, No. 1 ; Mackay Chapter of Rose Croix, No. 1. Knights of Pythias. — Colorado Lodge, No. 1 ; Damon, No. 2 ; the Endowment Rank, K. of P. Odd Fellows. — Grand Lodge, with annual session in October ; Union, No. 1; Denver, No. 4; Germania, No. 14; Denver Encampment, No. 2; Humboldt, No. 6 ; Arapahoe, No. 10 ; Colorado Degree Lodge, No. 1 ; Samaritan Lodge, No. 5. Champions of the Red Cross. — Pioneer Encampment, No. 1. Good Templars. — Denver, No. 12; Harmony, No. 4; Happy Home, No. 21. Benevolent Societies. — Denver Lodge, No. 171, I. O. B. B. ; Denver Lodge, No. 2, A. O. U. W. ; Standard Lodge, No. 3, A. O. U. W. ; Colo- rado Lodge, Knights of Honor ; Gruetli Verein (Swiss) ; Skandia Bene- ficial Socieiy ; Firemen's Relief Association ; St. Vincent de Paul Society; Denver Irish Progressive Society; Ancient Order of Hibernians; St. Joseph's Total Abstinence Society. The school system of Denver is well established, thoroughly classified, and under excellent superintendence. Eleven schools, including the high school, are open, but cannot meet the demands upon them ; in several of them sessions of half a day only are allowed to certain classes. But this condition of things is not likely to last long. A noticeable feature, establishing the recognition Denver has received in the East and in England, is the introduction of companies controlling large amounts of capital, which is used in developing the industries of tlie country at large. Two years ago the advent of the Colorado Land and COLORADO. 159 Investment Company of London (limited) marked a new era in the finan- cial history of Denver. Making the city its head-quarters, money was loaned, especially throughout the farming section, at a rate fifty per cent, lower than had prevailed at banking institutions and with private indi- viduals. A drop of from twenty-four and eighteen per cent, to twelve per cent, per annum made a vast difference to a large class of people on whom grasshopper visitations had fallen heavily. The relief came at an opportune season for these in the establishment of this new company. The success attending this company has led to the establishment of others, based on foreign capital, for the construction of canals, the sale of lands under them, the erection of hotels, and other enterprises involving the outlay of vast sums of money. The Weld and Larimer Irrigating Canal in the northern part of the State is one of these, under the manage- ment of the same parties interested in the loan company. This canal is nearly finished, and will prove of incalculable benefit. But a greater enterprise still, in the same line, has been inaugurated by which Denver will be directly benefited, though the whole State will ulti- mately feel its wholesome influence. This is the Platte Canal, by which hundreds of thousands of acres in the immediate vicinity of Denver will be thrown open to cultivation. The arable lauds of the country will be increased twenty per cent, by this canal, and be capable of meeting the tome demand for the products of the soil. A system of reservoirs in connection with the, canals is contemplated, by which water running to waste in seasons when no irrigation is going on will be stowed away, to be drawn upon in emergencies. The effect of such an agricultural development near Denver will give an impetus to its growth that as yet cannot be realized to its fullest extent. The canal is now in course of construction, and before the year 1881 closes will be completed. Denver will derive immediate benefit while its construction is going on, but when the lands are settled it will increase its business, its real-estate values, and its importance in no small degree. SOCIETY AND CHUECHES. Everywhere in Colorado — the mining camps being no exception — good society may be said to exist. Moral and religious teachings are observed with the same strictness as in any of the established cities of the Eastern States. Indeed, why should they not? The inhabitants of the State have come from every part of the Union, bringing their culture, their intelligence, their thrift, with them. While there is much that may be denominated rude and uncouth on the general surface of society, there is 160 THE GREAT WEST. an undercurrent that is strong and deep and ceaseless, for ever flowing in channels that conserve society, elevate its tone, and lift it upon a plane of civilization worthy the respect and recognition of the most reiined and cultured minds in the Union. It can no longer be said of society in Colorado that it is rude and rough ; during the last ten years a great progress has been made in toning down frontier traits, rounding the sharp angles of character, and mould- ing the peculiarities of the adventurous classes who were first tempted hither by a thirst for gold ; and now the rapid building of cities and towns, the establishment upon a permanent basis of schools of learning and religion, the accumulation of material wealth, and the constant acces- sion made to the population by the wealthy, the cultured, the renowned of other States, places Colorado on an equality with her older sisters in respect to all the privileges that are peculiar to older and more densely populated sections of the country. It is not to be imagined, therefore, that Colorado is inhabited by a half- civilized race of beings. All over the State are to be found communities of orderly and ambitious citizens, around whom are clustered all the re- fining influences of the family circle. In the cities and larger towns entertainments, concerts, lectures, festivals, balls, and other amusements are quite as frequent and as creditably managed as in other places of like population. The public-school system will compare favorably with that of any other State, and in addition to this there are, educational institu- tions of an advanced character, now firmly established, at which thorough and complete academical and collegiate courses can be pursued if desired. Throughout the State all the religious denominations are well represented. There is not a town, and indeed hardly a village, in the State that has not its place of worship, and the sound of the church-going bell is as familiar to the ear as it was in years gone by in valleys lying far away down the slopes of the Prairies, among distant villages by the sides of the great lakes or the still greater sea. There is no lack of religious privileges for those who desire and take them into account as they canvass the possibil- ities of a future home in the Great West. EDUCATIONAL. The public-school system is based upon that adopted by Illinois. The people of Colorado have always been interested in the educational inter- ests of the State, and there have been erected a number of large and ex- pensive school-buildings that would do no discredit to towns three times as large in more settled communities. A (iLLMl'SI'; (IF llKNVKIt, COLdRADO. COLORADO. 161 The schools are maintained by a direct tax, averaging three mills to the dollar, on all the taxable property of the State, and by the proceeds of the lease or sale of school-lands, while the residents of each school dis'' trict have a right to levy taxes for special purposes within their own jurisdiction. The fund arising from the leasing or sale of school-lands thus far has not been large, but the rapid increase of population will ia time make the revenue derived from this source quite a respectable sum, and aid ia keeping at low figures the general tax, which by law has for its minimum two mills on the dollar. The school law makes it the duty of county superintendents to examine all persons who present themselves at the quarterly examination, and to grant certificates to such as are deemed worthy ; and it is further pro- vided that no person shall be paid out of the public fund for teaching unless such person holds a certificate of competency signed by the said superintendent. A series of uniform questions has been prepared by the State superintendent by order of the State Board of Education, and three grades of certificates are issued, as follows : Fiest-Gbade Certificate. — First Group. — Average, 90 per cent.; no branch below 75 per cent. Second Group. — Average, 75 per cent. ; no branch below 60 per cent. Second-Gra.db Ceetificate. — First Group. — Average, 75 per cent. ; no branch below 60 per cent. Second Group. — Average, 60 per cent. ; no branch below 40 per cent. Thikd-Gkade Cektificate. — First Group. — Average, 60 per cent. ; no branch below 50 per cent. Second Gi-oup. — Average, 50 per cent. ; no branch below 40 per cent. The topics are divided into two groups, to -wit : First Group — Arith- metic, United States history and Constitution, reading, orthography, gram- mar, theory and practice, and geography. Second Group — Physiology and laws of health, school law, botany, and other natural sciences. The State law also provides that State diplomas of perpetual validity may be issued by the State Board of Education to applicants who have taught two years or more in this State with eminent success, and who pass a satisfactory examination or who have received a diploma else- where. By the last biennial report of the State superintendent we find that the number of persons in 1878 between the ages of six and twenty-one was 26,473, with an average percentage of enrollment of 63 ; number of school districts in the State, 372 ; number of schoolhouses, 249 ; value of schoolhouses and property, $474,771 ; number of male teachers, 226 ; 11 162 THE GREAT WEST. number of female teachers, 341 ; average wages of male teachers, $49.90 per raonth — of female teachers, |46.95 ; average cost per month for each pupil, $2.72. The table of wages shows a decrease of ten per cent, from the preceding year, but it will be observed that the wages of male and female teachers are nearer an equality than in many other States. When the wages of female teachers in Massachusetts average one-half less than male teachers, it is gratifying to note that more are employed than males, showing that the sex is recognized as better instructors for the young. As yet public-school libraries are few in number ; there are not over four thousand volumes in the various libraries. There is a State university located at Boulder, with a preparatory and a normal department, the average age of the pupils, of whom one hun- dred are in attendance, being eighteen years. In the preparatory departs ment Greek, Latin, German, French, geometry, algebra, physics, and chemistry are the branches taught ; in the normal department, geog- raphy, arithmetic, English grammar. United States history, reading with phonetic analysis, and spelling. The university is supported at an ex- pense of about $15,000 per annum. There is a college at Colorado Springs, where there are four courses of instruction — ^for the degree of bachelor of arts, preparatory school, nor- mal school, mining and metallurgy. This college was founded in 1874, and is open to students of all denominations at a cost for tuition of $25 per year, so that the institution is practically free to all. There are four terms in each year. The State Agricultural College is located at Fort Collins. The lead- ing object of this institution is to impart a thorough and practical know- ledge of all those branches and sciences that pertain to agriculture and the mechanic arts. Lectures on practical agriculture, weekly exercises in English composition and declamation, contemporaneous history, lessons in free-hand, industrial, and perspective drawing, are continued through- out the entire course. The course embraces three terms of four years. The calendar is made to conform to the necessities of an agricultural col- lege. Its vacation is in winter, but this interval between the autumn and spring terms is employed by the faculty in visiting and lecturing on topics connected with their departments in various portions of the State. Last winter a series of farmers' institutes was held with great success. Tuition is free to all within the State. There are a number of private institutions of learning at different points through the State, so that it is to be said of Colorado that the needs of the rising generation are recognized and liberally provided for, COLORADO. 163 considering the scattered nature of its settlements and the constant changes going on within its borders. The progress in this direction made during the last few years is extremely gratifying to the most ardent educational enthusiasts. It is the boast of Denver that her public schools are equal to the best in the country. PROSPECTING. PROSPECTING is simply hunting for mineral — ^in this case one of the precious metals — ^where the mineral lies in fissure-veins deeply- imbedded in granite, gneissoid, or rock of like density. The work not only requires muscle, courage, and patience, but a considerable knowledge of geology and mineralogy. The prosjiector must have some idea of the external indication of the presence of veins which may be hundreds of feet below and thousands of feet distant from the point where the " blos- som" is found. First, the prospector seeks the " blossom " which indicates the presence of the mineral, and then he next tries to find out where it comes from. He examines carefully the topography of the country, turns over loose stones, peers into and along beds of streams, and is perhaps at last re- warded by finding the " blossom "-rock. He carefully turns it over. If its edges are sharp and defined and the fracture evidently of recent date, he is satisfied the vein is near at hand. If, on the contrary, the corners are rounded and the fracture of remote date, he is satisfied it must have travelled a considerable distance. In either case, he must hunt patiently, and often for a long time, before he strikes the prize. But prospecting at Leadville is quite another affair. The carbonate mineral, instead of being found in vertical lines, held in the strong em- brace of the solid rock, which must be drilled and blasted and tunnelled before the mineral is reached, occupies a more nearly horizontal position, varying with the dip of the surface. Up to the present time there are no certain superficial evidences of the existence of the mineral. From the day the first carbonate-mine was struck down to the present time the pro- spector has worked in the dark until his spade struck the ore. Proximity to a known body of ore is perhaps the only " guide." If a person gets a claim near a mine in which mineral is known to exist, he has reasonable as.surance of a valuable claim. And it being a determined fact that car- bonate ore exists in large and paying quantities not only at Leadville, but 164 PROSPECTING. 165 in varions directions for fifty miles around, the prospector who starts in to-day has every advantage over those whose luck alone brought to light the first carbonate ore in the Leadville district. Pay ore is found at Leadville on Fryer, Carbonate, and Iron Hills, in all the gulches above the timber-line, across the valley of the Arkansas, at Oro, Malta, near the grass-roots and hundreds of feet below the surface. The same conditions obtain at Ten Mile, Eagle Eiver, on Elk Mountains, at Twin Lakes, beyond the Saguache, in the Gunnison country, at Chalk Mountain, Tin Cup — shafts being sunk and new paying mines being con- stantly found. If these facts mean anything, they mean that inasmuch as the prospector who goes in now has the benefit of all who have gone in before, and a knowledge of the great extent of the carbonate deposit to guide him to the best location, he stands a better chance of speedy and sure success than he would have stood a year ago. The pioneers have " blazed " the way, and it is an easy matter for any man with provisions for a few months, a level head, and vigorous muscle to follow a path already marked out. In prospecting three men should go together. They need each a pick, costing $1.60, a shovel, $1.50; they are then fully equipped, so far as tools are concerned, for commencing a shaft, which should be about four feet by six. After going down a few feet they need a bucket, costing $5, windlass and rope, at say $25, drills and hammers, fuse and blasting-powder, at $10 — making a total cost for outfit of $49. If working some distance from town a burro will be needed, and can be obtained at from fifteen to thirty dollars. Provisions for a party of three would not cost above thirty dollars a month, and a temporary shanty can be built in a short time, at no cost save labor. Thus a prospecting-tour of two months can be made at a total expenditure of less than one hun- dred dollars. Many of the most valuable mines were discovered on a less expenditure than this, and what has been done will be repeated hundreds of times before the summer is over. There remains after getting the out- fit nothing to do but " dig." A grub-stake is a prospecting outfit furnished by men of wealth — i. e. those who can command a hundred dollars or so — ^to impecunious miners. For instance, A and B desire to prospect, and, not having the means to procure the necessary outfit, or perhaps having sunk shafts until their means are exhausted, C comes along and gives them a " grub-stake " for an in- terest in whatever they may find. In other words, he " mines by proxy." 166 THE GREAT WEST. A grub-stake of less than fifty dollars got Governor Tabor one-half of the Little Pittsburg and made him a millionaire, and grub-stakes, properly placed and followed up, are to-day as good investments as any man ought to wish. LOCATING A MINE. The process of coming into possession of a mine is this : A man stakes out his claim — ^three hundred by fifteen hundred feet. To do this he sets up a stake three inches in diameter, square at the top, and if his name be John Smith writes in pencil upon the four sides, " John Smith's Lode, Corner No. 1." He steps off the distance and sets up such a stake on each corner, marking each stake in succession, as " Corner No. 2," and so on. Then he begins to sink his shaft. Two men work the windlass and one digs, and the three take turns in digging. Sometimes a fourth man cuts the timber to be used in "timbering" the shaft; that is, walling it up to prevent its caving in. Good saplings adapted for the purpose grow on the mountain-side, and it takes all the trees on fifteen acres to timber the average shaft. Thus it happens that the original owners of a claim often number four men, and almost always number three. The shaft is usually four feet wide and six feet long. Three men working at such a shaft can go down through the first fifty feet at the rate of from three to five feet per day, timbering as they go, and through the next fifty feet, two and a half to three and a half feet per day ; that will probably bring them to rock, through which they must blast, and they cannot go faster than two feet per day, and even that is good work. On a contract the first fifty feet will cost $3.50 per foot, the next fifty, $5.50 per foot, and after that it will cost from $8 to $15 per foot to go down, according to the hardness and depth of the rock. The contract-price for sinking a shaft averages $4.50 to $6 per foot, including curbing. Thus the diggers go down through the wash and the porphyry — and the rock and the iron if they find the last two — ^until they come to the " contact." The depth which they have to go varies, as I have said. Li the Adelaide Mines mineral is in some places but four feet imder the sur- face ; in the Morning Star it is two hundred and fifty feet. On an aver- age it is one hundred feet down. Even the most experienced miner can- not tell, by looking at what is before him, whether the stuff has mineral in it or not. So he has it assayed. This costs from $1.50 to $5, and takes from two hours to a day. If he finds he has mineral, he goes for a United States surveyor and has his claim surveyed and recorded, and he writes on his four stakes the date when the survey was made. He PROSPECTING. 167 now owns the claim. It is his without having to pay the government anything, as the latter gives the claim to the man who finds the mineral. It is a disputed point whether iron is " mineral " in the sense contem- plated by the law, but the custom here is to have surveys made on finds of iron. In staldng out his claim the owner is not compelled to run his survey over the claim that he first staked out. He can shift his lines in any di- rection that he chooses, determining that by the pitch and direction of his own vein or deposit. It will often happen that he will thus take in the shaft which is being sunk by another man near him — ^will " survey him in," as it is called — and that other man has no recourse. Suppose several men have claims staked out near his, and have shafts started. As soon as the first man strikes mineral the others feel that their chances for striking it are good, and they all go to work with might and main to be the next to strike it, for that man is the lucky one, since he has the next choice of land. Additional " shifts " of men are put on, the work goes forward night and day, a horse is used to turn the wind- lass if it can be so arranged, and the race is as if for dear life. When the next man finds mineral he makes a break for a surveyor ; and if two strike it at the same time they race like mad for one, for the claim first surveyed is the one that holds the land. It often happens that the mineral found has such a direction that a survey has to be made over a claim already surveyed. In that case the ne^f survey can hold the land within its claim and outside the other claim, but that part lying within the first claim remains to the owners of the first claim. However, if the second claim is a rich one, the overlapping por- tions have enough mineral in them to satisfy any man ; but in any case the new claimant yields with good grace. Surveys are always made one hundred and fifty feet each way to the side-lines from the discovery-shaft; they cannot be made two hundred feet one way and one hundred feet the other, nor be divided up unevenly ; therefore it happens often that a man cannot get a " full claim " — ^that is, one three hundred feet wide — ^but has to be content with what he can get, "bonding a mine" is a process needing explanation. After a set of men have found mineral it frequently happens that they bond it to some one to sell — ^that is, they execute an instrument setting forth that, in consideration of the bonder putting up so much of a forfeit, he shall have a certain number of days — thirty, sixty, or ninety — ^within which he may sell the mine at what- 168 THE GREAT WEST. ever he can get for it, with the understanding that if the sale is made the owners of the mine are to receive a stipulated price. For example, the Little Giant had a half interest bonded for $110,000. The bonder was at liberty to sell that half interest for as much more as he could get for it within the time agreed upon. If he failed to sell it within that time he lost his forfeit — ^forfeits range from one to five thousand dollars — and the control of the mine reverted to the owners. "WAGES. The wages paid to good miners here have steadily kept at $3 a day ; foremen, $100 to $125 a month. Surface common labor is paid from $2.25 to $2.50 a day. The roads from all mines, except those located on Iowa Gulch, are of continuous down-grade. At hauling ore teamsters load fully four thousand pounds per trip, and their contracts are so made as to give them from nine to ten dollars daily gross earnings. From Little Pittsburg to Harrison or Grant's smelter they receive from $1.75 to $2 per ton ; from the Adelaide Consolidated Mine of Malta, $2.25 per ton. These prices make it cost about one dollar per ton to get the ore " on the dump " — ^that is, on the pile at the mouth of the mine — and one dollar per ton more to deliver it to the smelter. Very little blasting is required in the mines, most of the mineral being capable of extraction with a pick and shovel. DEFINITIONS OP MINING TEEMS. The newcomer into a mining camp will hear and read of many things totally unknown to any other kind of business, and he will find a know- ledge of the various mining terms of no little benefit as well as pleasure. He would not want a " stope " for his dinner, nor to regard " country rock " as necessarily remote from a populous city, nor would he desire in a mining camp to always regard a " horse " as a good " feeder." " Stamps " he will not find so easily .transported as our national currency, nor a " whim " possessing any "human eccentricity. By carefully looking over this compendium of mining terms the reader will be able to read and talk more intelligently, and therefore more satis- factorily : Adit. — A level, a horizontal drift or passage from the surface into a mine. Alluvium. — A deposit of loose gravel between the superficial covering of vegetable mould and the subjacent rock. Apex. — The top or highest point of mineral. Argentiferous. — Containing silver. PROSPECTING. 169 Assay. — To test ores by chemical or blowpipe examination. Auriferous. — Containing gold. Bed. — ^A horizontal seam or deposit of mineral. Blende. — ^An ore of zinc consisting of zinc and sulphur. Boiianza. — Fair weather ; a mine is said to en bonanza when it is yield- ing a profit. Breast. — The face of a tunnel or drift. Cap. — A vein is in the " cap " when it is much contracted. Carbonates. — Soft carbonates : salts containing carbonic acid, with a base of lead. Hard carbonates : the same with iron for a base. Cheek. — The side or wall of a vein. Chimneys. — The richer spots in lodes as distinguished from poorer ones. Claim. — The space of ground located and worked under the laws. Chlorides. — A compound of chlorine and silver. Contact. — A touching, meeting, or junction of two substances, as rocks. Contact-vein. — A vein along the contact-plane of, or between, two dis- similar rock-masses. Country. — The ground traversed by a vein. Country rooh. — The rock-masses on each side of a vein. Crevice. — A narrow opening, resulting from a split or crack ; a fissure. Cribbing. — The timber or plank lining of a shaft ; the confining of the wall-rock. Cropping out. — The rising of layers of rock to the surface. Cross-cut. — ^A level driven across the course of a vein. Cut. — ^To intersect a vein ; open cut, a level without a covering driven across the course of a vein. Dike. — A wall-like mass of mineral matter filling fissures. Diluvium. — A deposit of superficial sand, loam, pebbles, gravel, etc. Dip. — The slope, pitch, or angle which a vein makes with the plane of the horizon. Drift. — ^A horizontal passage underground. Dump. — A place for deposit of tailings or waste rock. Face. — The end of a drift or tunnel. Fault. — ^A displacement of strata or veins, so that they are not continuous. Feeder. — A small vein joining a larger one. Fissure-^ein. — ^A fissure or crack in the earth's crust filled with mineral matter. Float. — ^Loose rock or isolated masses of ore, or ore detached from the original formation. FootrwaU. — The layer of rock immediately under the vein. 170 THE GREAT WEST. Gangue. — The substance enclosing and accompanying the ore in a vein. Gash-vein. — A vein wide above and narrow below. Hanging-wall. — The layer of rock or wall over a lode. Heading. — The vein above the drift. Horse. — A mass of rock-matter occurring in or between the branches of a' vein. Incline drift. — An inclined passage underground. In place. — ^A vein or lode enclosed on both sides by fixed and immovable rock. Lagging. — The timber over and upon the sides of a drift. Level. — A horizontal passage or drift into a mine from a shaft. Lode. — Aggregations of mineral matter containing ores in fissures. Matrix. — The rock or earthy matter containing a mineral or metallic ore. Mill-run. — A test of a quantity of ore after reduction. Outcrop. — That portion of a vein appearing at the surface. Patch. — A small placer-claim. Placer. — A gravelly place where gold is found — includes all forms of mineral deposits excepting veins in place. (Sec. 2329 Pev. Stat. U. S.) Pocket. — A rich spot in a vein or deposit. Prospecting. — Searching for new deposits ; also preliminary explorations to test the value of lodes or placers. Piffle-blocks. — Wooden blocks set on end in a sluice, with interstices for catching gold. Selvage. — Thin band of earthy matter between the vein and walls. Shaft. — ^A well-like excavation in the earth. Shift. — The time for a miner's work, in one day or night. Sluices. — Boxes joined together, set with riffle-blocks, through which is washed auriferous earth. Smelting. — ^Reducing the ores in furnaces to metals. Stamps. — Machines for crushing ores. Slope. — One of a series of steps into which the upper surface of an ex- cavation is cut ; to excavate in the form of steps above a drift. Sloping. — ^The act of stoping or breaking down the surface of an excava- tion with a pick. Strike. — The extension of a lode in a horizontal direction. Stulls. — A framework covered with timber or planks to support rubbish in working a stope. Sump. — That part of the shaft below the platform used for receiving water. PROSPECTING. 171 Tailings. — The refuse matter discharged from the end of a sluice. Tunnel. — ^A level driven at right angles to the vein, which ite object is to reach. Vein. — ^Aggregations of mineral matter in fissures of rocks. Walls. — ^The sides next to the lode. Whim. — A machine for raising ores and refuse. Winze. — A shaft sunk from one level to another. NEBRASKA AND ITS RESOURCES. rNTEODUOrOEY. IiN" folk-lore there is this story : There was a man tired of the patient cultivation of his little farm, and who desired to be rich without labor. Lacking wealth, life had become " stale, flat, and improfitable." Three times he dreamed there was treasure hid under the earth in his old orchard, which for years had been barren of fruit. Three is the regular tion number that makes a dream true ; and so, iu an ecstasy of excitement, he revealed the secret to his wife, and began to dig. Rotrnd one tree he dug a mound of earth, and round another, until there was not a gnarled trunk about whose roots he had not let in the vitalizing air. But there was no treasure. Of course he grew angry over his wasted labor, and he had a sorry time when his neighbors hung on his fence and laughed at his folly. Spring-time, however, came, and the trees blossomed. Autumn followed, and they were loaded with fruit. Years went on, the old orchard yielding a rich revenue ; and so the man found there was golden treasure hid in the earth after all, and he grumbled no more because his farm was not a literal gold-mine, but worked it with vim, and his land made him as wealthy as a man has need to be. Our fathers, who composed this parable, knew what they were talking about quite as well as the old Greeks when they made the myth about exhausted Hercules renewing his strength at the touch of the Earth-mother. Gold is good, but it usually costs the miner as much to win it as it is worth. The produc- tions of the soil are better in the long run, for it is on these that all life must base. In her agricultural productions Nebraska is rich, and will be richer. She boasts soil that is nowhere excelled, a climate favorable to production, and pure water in abundance. 172 NEBRASKA AND ITS RESOURCES. 17a GEOGKAPHY OF NEBEASKA. The area of the State comprises 75,995 square miles, or 46,636,800 acres — roughly speaking, as large as all the New England States, or all Pennsylvania and half of New York. Its length is 412 miles and its width about 200. It is between the parallels of 40° and 43° north, thus placing the whole State in the latitude of Pennsylvania, Southern New York, Northern California, and Southern Oregon; and between 18° and 27° west from Washington or 95° and 104° west of Greenwich. The State is called prairie. So it is, in the sense of the word which means meadow, but not in that secondary sense which implies a land of uniform flatness. In real truth, Nebraska is a part of the lowest eastern grass- clothed slope of the Rocky Mountains. The eye alone will make no observer aware of this fact. Nevertheless, from the eastern to the west- ern boundary of Nebraska there is a gradual and uninterrupted rise of the land of about seven feet to the mile in Eastern Nebraska, and from that to ten feet in Western ; and thus it comes that while the land on the eastern boundary is 910 feet above sea-level, on the western boundary it is about 5000. The surface-form of the State is, of course, made by the rivers. The eastern front of the country shows bold, wooded bluffs to the Missouri, their outlines being cut and scarped into fantastic and picturesque forms by the washing water. West of the Missouri bluJBfe, except on the table-lands, there is no flat, but a land of many changing forms — ^now broad bottoms bounded by low hills, now picturesque bluffi, and, especially in the grazing-region, ravines sometimes as rugged as the gulches in the gold-fields. Now and again a river flows fall to the bank, from which the bottom — ^from a mile to four or more miles wide — spreads out on either hand ; but generally the streams run in deep beds, the high, steep banks and the narrow first bench being thickly clothed with timber. The general ascending lay of the land is broken west to east by three main drainage-channels. On the northern boundary of the State are the Niobrara and the Missouri Rivers, of which latter the Niobrara is an affluent. The Platte, a winding, shallow, spreading stream, dotted with numerous islands and rurming over a bed of white sand, flows through the whole length of the State from west to east at a distance of one hun- dred to one hundred and twenty miles south of the Niobrara; and from fifty to eighty miles south of the Platte the Republican River has its channel. These rivers head in or near the mountains. Their flow is west to east, and their drainage-area on the south is limited to a belt of ten to fifteen miles, and the tributary streams from that side are few. 174 THE GREAT WEST. North of each stream, however, its affluents are numerous, and the general flow of their waters is south-east. This is the topography of Nebraska in barest outline, and with the map before him the reader can fill in the details. He can imagine the great plain ascending to higher altitudes as the mountains are approached ; the rivers, west to east, making three great valleys, and two elevated divides separating the valleys; and, finally, the smaller streams exhibiting the land as broken into an almost infinite number of gently-undulating hills and valleys, with great table-lands on the summits, the trend of which is south-east. GEOLOGY OF NEBRASKA. In the south-eastern part of the State, Upper Carboniferous and Per- mian deposits come to the surface, the boundary-line running south-west , from Washington county to about the centre of the southern line of Thayer county. Over one-third of the State west of this line Cretaceous deposits make the surface, and west again the Tertiary. The surface geology of Nebraska represents great periods in the history of the for- mation of the crust of the globe — glacial epochs and ages of time when seas and lakes covered the land, now the centre of the United States. It is for a scientific treatise to describe in detail the accumulated changes of these eras — the grinding of the mills of the gods which produced life and swept away life, ultimately resulting in the fertile Nebraska which is to-day. It is a marvellous story whose record is everywhere written in Nebraska, but in this article there is not space for its telling. The final formative processes are, however, interesting to the farmer, inasmuch as they describe the land he has to till. Toward the close of the last Gla- cial Period the continent slowly uprose, and a portion of this region became dry land. Yet great fresh-water lakes remained, one in Nebras- ka and Iowa being estimated as five hundred miles long and from fifty to two hundred miles wide. There was the Missouri River, then and now the muddiest river in the world. For a thousand miles its course was, and is, through deposits readily friable and easily worn and borne away by the water, especially as at this time, at the sources of the Mis- souri and Yellowstone, the water-action was aided by the erosive action of moving ice-masses. When the river entered the great lake its current ceased, and the suspended sediment dropped to the bottom. The land was now being gradually upheaved. As it rose the waters of the loess lake were drained off by the Missouri, and its bed became a vast marsh. The present broad bottoms of the country were at that time river-beds, and with their waters still came down the muddy debris from the moxm- NEBRASKA AND ITS RESOURCES. 175 tains, which was largely deposited at the bottoms of the great streams. The land was still rising, and as it rose the rivers drained oif the surplus waters. The river-beds were cut deeper into the yielding soil, and the time ultimately came when Nebraska was fixed in the condition which exists at this day — the loess being largely the soil of the uplands, and the alluvial that of the river-valleys. The two deposits are similar in chemical elements, and they form the richest soil in the world, and most valuable for agricultural purposes, ranging in thickness from five to one hundred and fifty, and even two hundred, feet. Careful analyses of the soil show that in the loess over eighty per cent, of the formation is finely- comminuted silica — so fine that its true character can only be detected under a microscope. About ten per cent, of its substance is made up of carbonates and phosphates of lime. There are some small amounts of alkaline matter, iron, and alumina, the result being a soil that can never be exhatisted until every hill and valley which composes it is entirely worn away. Its finely-comminuted silica gives it natural drainage in the highest degree. When torrents of rain come the water soon percolates the soil, which, in its lowest depths, retains it like a huge sponge. "When droughty periods intervene the moisture rises from below by capillary attraction, supplying nearly all the needs of vegetation in the dryest sea- sons. The richer surface-soil overlies the subsoil, and it is from eighteen inches to three and four, and even six, feet thick. It is organically the same as the subsoil, but enriched with organic matter, the growth and decay of innumerable centuries — a garden soil easily cultivated and mak- ing the arable farm as a garden. CLIMATIC CONDITIONS IN NEBEASKA. In the first place, there is water in abundance underground, on the sur- face, and coming from the clouds. At a depth of twenty to sixty feet, and at some places sixty to one hundred, there is a thick layer of clear sand, which in most cases rests upon a bed of rock or clay ; and so abun- dant is the water in this sand that in many places subterranean streams are formed, which are struck in sinking shafts. Everywhere abundant water, above the average in purity, is obtained at the depths named, the cost of a common tube-well being about seventy-five cents per foot. On the surface rivers, creeks, prairie-ponds, and springs abound. No map yet published does justice to the numberless small streams that exist in the State, even the plats of the public surveys failing to indicate them all ; and, indeed, there are large areas in which running water is now found on every section, where there was none when those surveys were 176 THE GREAT WEST. made. The rainfall is ample. The best data accessible are the tables kept by Dr. A. L. Child of Plattsmouth, from which the following is compiled : Year. Season. f Winter . 1866 §P™S Summer . iFaU .-. (Winter . FaU . . 1875 Winter . Spring . Summer , Fall . . f Winter . 1878 |P^°^ Summer . [FaU . . Temperature. 19.99° 1 47.03° 72.78° 49.75° J 22.14°! 46.17° 70.00° 42.64° 15.06' 45.55' 71.67' I 47.31° J °1 o r 33.01°! 62.71° 72.86° 15.98°! Yearly Snow. Yearly Rain and Melted Snow. 11.45 inches. 22.00 inches. 29.26 inches. 31.70 in. 32.10 in. 50.22 in. 43.47 in. The average rainfall for these five years is 32.29, as compared with 34.13, the average of eleven years in Illinois. From the middle of the State, west, the rainfall is somewhat less than the table indicates, but in the eastern half the average is 32, two-thirds of which is during the agricul- tural months, or quite as much rain at the precise time when it is needed as falls during the same months in Missouri, Illinois, Indiana, Ohio, and New York. A peculiarity of the rainfall is that it is mostly at nights, so that the heaviest showers, quickly draining into the land, scarcely inter- fere with work on the farm. The temperature is of the temperate zone, healthful and bracing to man and beast, and in which corn, small grains, apples, and peaches come to rich perfection. NATUEAL PEODUCTIONS. The prairie, clothed only by natural processes, presents its own testi- mony to the riches of the State. Its whole expanse is covered with grasses, there being not fewer than one hundred and fifty species, and the most abundant making the best pasture, showing green at the end of April and affording feed until November. The blue-joint grows every- where except on low bottoms. Under ordinary conditions its growth is NEBRASKA AND ITS RESOURCES. 177 two and a half to four feet, and on cultivated grounds it is found from seven to ten feet high. Wild oats grow on the uplands, mixed with blue- joint. This grass is relished by cattle, and is abundant. The buffalo- grass, low in habit, is now found in the western half of the State. It disappears before cultivation, but it is Nature's provision of food for grain-eating animals during winter on the prairie, Inasmuch as it retains its nutriment all the year round. Among other feed-grasses are several varieties of bunch-grass, and in the low lands a native blue-grass and the spangle-top, which latter makes excellent hay. THE NATIVE TEEEg. The Nebraska prairie is not bare of trees ; in fact, the native trees fur- nish a large list. The river-bluffs are clothed with them, and the banks of the streams. There are two kinds of buckeye, two of maple, two of locust, four of ash, three of hickory, eleven of oak, twelve of willow (eight species being shrubs), three of poplar, one sycamore, black walnut, yellow pine, white cedar, and red cedar. The shrubs include common ju- niper, pawpaw, prickly-ash, five sumacs, red-root, spindle tree, six species of plum, six of currants and gooseberries, five dogwoods, butter-bush, buf- falo-berry, red and white mulberry, hazelnut, and beaked hazelnut. Cedars are found on the islands of the Platte, and along the Loups and the Nio- brara there is a goodly quantity of pine. But the point is heite : this list of trees is proof that trees flourish on the prairie, and that as much tim- ber as is needed, for all uses can be raised on the farm. The prairie, in iis natural condition, presents the aspect the preceding pages sketch — an untilled garden-land, furnishing plenty for its wild den- izens, for man and beast. Looking at it in this year (1879), it is a mar- vel how Fremont and others could have come to regard it as a desert. Nevertheless, they did so regard it; and the nation up to the year 1850 little knew of the rich domain it possessed in the trans-Missouri region — a region which is to be the great grain- and stock-producing area of the continent, THE HISTOEY OF NEBEASKA. The white man knew Nebraska more than twenty-five years ago. Ad- venturous French trappers explored its wastes and fraternized with the Indians, and the conditions remained the same when Astor's American Fur Company collected the furs of the region. This company established trading-posts, the first of all being at Belle Vue (between Omaha and the 12 178 THE GREAT WEST. Platte River), which was under the charge of Colonel Sarpy, a member of a French family well known on the frontier, and himself noted for his enterprise, sagacity, and courage. It matters little to speak of these times, except that when men see a great river it is natural to desire to know its birthplace in the mountains, and it was in these beginnings that Nebraska had its origin. Across its prairies was the way to the west coast and to Utah. Many an "Argonaut " — as the " Forty-niners " are called — ^never saw the sea until he reached the Golden Gate by way of the prairie, and the Mormon roads are still traceable across the Plains. It was the establishment of frontier forts that was the next stage in Nebras- ka's progress. The people there had to be fed and clothed, and the freight- ing system came into being. To meet the needs of this overland trade, there had to be ranches on the way where supplies could be obtained ; and hence at convenient places they were established. By one means or other the land was known to the outside world about 1850, and there was a crowd waiting on the Iowa and Missouri side of the Missouri to "jump" the river as soon as the Territorial act authorizing settlement was passed and proclaimed in 1854. But from Cedar county in the north to Rich- ardson county in the south there was no belief anywhere that any land except the Missouri bottoms was worth occupying j and a decade went by and there were but few farms opened ten miles west of the river, the balance of the State being really the hunting-grounds of the Indians. In 1864, however, the Union Pacific Railroad was commenced from Omaha, and in 1869 the Burlington and Missouri River Railroad from Platts- mouth ; and since then these railroads have been the largest factors in promoting Nebraska's prosperity. In 1867 the State was admitted to the Union, and at that time Lincoln, on the prairie, was located as the capital, and is now, besides being the seat of government , the second city in the State, with a population of ten thousand, while Omaha's pop- ulation numbers twenty-five thousand. This is a brief statement of the dates which go to make up the items in the short history of Nebraska. To fill up the outline sketched would require a book. In brief, the State has become a white man's country. The Indians have yielded possession, the Pawnees quitting their reservation, which has become Nance county, and the Otoe Reservation also is being settled up everywhere. In the agricultural part of the State the traveller meets with splendid farms, and, in the grazing-region west, enormous herds of cattle. The reasons for the prosperity of the State' will be of interest to those who are contemplating moving West, and the principal of these may be briefly stated. NEBRASKA AND ITS RESOURCES. 179 THE GREAT FOOD-BELT OF THE CONTINENT. Men cannot make bread of sand, and so they do not settle in deserts. The United States cover twenty-three degrees of latitude — away to the frozen North and down to the semi-tropic South. But, with all this choice, from the beginning of Western settlement the great current of movement has been within a central belt five or six degrees in width, and " nearly corresponding with the la,titudinal length of the State of Illinois, which lies between 36° 56' and 42° 30'." The proof of this is furnished by the census of 1870, which shows — Fopulation. True Valuation. Wheat, in Bushels. Corn, in Bushels. Immigrants born out of U.S. 11 States and 3 Terrs, in latitude of Illinois 10 States, larger half in lat- 14,019,314 13,211,389 11,327,668 $12,729,954,998 13,105,750,967 4,140,075,345 117,870,054 104,378,646 55,496,926 334,137,865 240,623,912 186,182,772 2,144,000 2,524,538 898,008 Country wholly out of lat- The foregoing table demonstrates a truth most important to be remem- bered by those who are contemplating a change of base. This is the belt in the United States in which industry obtains the most certain and high- est rewards. It is temperate in climate, and a man can here work up to his best. The land is fruitful, and bears in greatest abundance those products which are necessaries of life, and which have value accordingly. " South of Illinois," writes Dr. Butler, " it is too hot for wheat ; north of it is too cold for corn. Accordingly, in the latitude of Illinois — that is, within three degrees north and south of the parallel of 40° — Amer- ican agriculture can be more diversified than anywhere else. Farmers there are not dependent upon any single staple, but raise crops so various that a season which is pernicious to one is profitable to some other. Theirs is the threefold cord which is not quickly broken. NEBEASKA THE BEST PART OF THE BELT. The marvel of Nebraska is, that the progress of Illinois is here ex- celled. Consider the following figures : At the beginning of 1856 the population of Nebraska was 10,716, and at the close of 1875, 259,912, which was a twenty-five-fold increase in twenty years. In 1810, Illinois had a population of 12,282, and in 1830, 167,445, a thirteen-fold in- crease. These figures exhibit the two States in the first period of growth. Starting with about the same population, Nebraska doubles upon won- derful Illinois in the course of twenty years. The reason is, that in 180 THE GREAT WEST. Nebraska the farmer has Nature fully on his side — a fa^ further mani- fested when the productions of the State are considered. Corn, the king of grains, is bountiful in production, and it is not unusual for seventy- pounds of ear to shell sixty to sixty-three pounds, or four to seven pounds over the standard, the general average of production, with fair cultivation, being fifty to sixty bushels per acre. Numerous varieties of wheat are grown, the yield being fifteen to twenty-five bushels per ax;re ; of barley a fair yield is thirty to forty bushels ; of rye, twenty-five to thirty bushels ; and of oats, forty to fifty bushels. Flax returns about twelve bushels per acre, and tame grasses — alfalfa, or California clover, ordinary red and white clover, Hungarian grass, timothy, millet, blue-grass, and orchard- grass — take well to the soil and climate and cut heavy crops of hay. The country which is good for corn, good for small grains, good for grass and hay, and has a favorable climate, must be the location for stock-raising. It is live-stock the civilized world most wants, and in live-stock the farmer finds wealth. If a settler opens a farm in the agricultural part of the State, mixed farming is the best, and he should therefore combine grain- and stock-growing. If a man goes forth to the great pastoral region, then of course the industry he will follow will be that of herdsman or flock-master ; but be he where he will in Nebraska, cattle, horses, sheep, and hogs are what he needs to have about him. There is in Nebraska a wide field for profitable horse-raising, and except the few colts which farmers raise the field is unoccupied, and large numbers of horses are annually imported into the State, which could all be raised here at much less cost than ■ in the States whence they are imported and sold in Nebraska at from eighty to one hundred and twenty dollars each. The farmer who wants to engage in horse-breeding should come to Nebraska. He will find the broken prairie — ^land which, because it is not the best land laid out for the plough, sells at from three to four dollars per acre — ^the best adapted for the purpose. In these lands draws frequently come in from all sides toward a bottom, and wind-shelters are afforded from whatever direction the wind may blow, and water also is ever abundant. In a location of this character a man may establish himself, put up necessary shelters for his stock at a cheap rate, breed horses or mules, and find a ready market in the State and outside of it, for the freight is an exceed- ingly small percentage on the value of a good horse, and the best horses can be raised in Nebraska at a much less cost than in Kentucky. For feed, horses have the native prairie grasses, which are most excellent for both pasturage and hay, and corn, oats, rye, and barley are grown in great abundance and of most excellent quality. NEBRASKA AND ITS RESOURCES. 181 THE CATTLE-FARM. Cattle should be upon every farm — as many as the land will carry or the owner's means afford. Away from the great ranges it is best to have fairly good stock, which it should be the farmer's aim constantly to im- prove. It will be long years before there are too many beef-cattle in the world, and the market for them is as wide as civilization. Let the reader consider the price of beef in the Eastern markets and in England, and contrast that with the price at which cattle can be raised on the Nebraska prairie. In three years, with good stock, the Nebraska farmer can have a steer to weigh fifteen hundred pounds, and he is amply paid selling at three and a half cents per pound. Under conditions like these there is the possibility of an immense trade with the East and with England, though at present Chicago can absorb all of Nebraska's surplus. Im- provements in cattle-cars and in shipping arrangements, however, will extend Nebraska's sales to the most distant markets, landing stock in good condition in London and Liverpool at most for four cents per pound. As an example of possibilities in prepared meats, an English farmer in Seward county two years ago sent a small parcel of hams and bacon, cured in the English fashion, to the Manchester (England) market. The freight on his small shipment amounted to three cents per pound, and his returns were twenty-five cents per pound, and he was informed that any quantity would be received at that price. The dairy produce of Ne- braska may be indefinitely increased. Already a considerable quantity of Nebraska cheese is shipped out of the State east and west, at one cheese-factory in Lancaster county the product averaging four hundred pounds of cheese per head of cattle, and selling at ten cents per pound. In butter-making, dairymen among the hills, where the milk can be kept in a spring-house, are supposed to have had an advantage not obtainable on the prairie. Now, however, " Cooley's Creamer " puts the prairie- dairyman on the same plane as those who live in mountain-regions. The windmill pump, which costs from one hundred and twenty to one hun- dred and sixty dollars, keeps up a constant Jlow of coolest water from the recesses of the earth. The cooler is a large box, zinc-lined, with (between the zinc and the outer wood) a filling of charcoal. Placed beside the pump, the stream from the pump fills the box, and the overflow is carried off through a waste pipe, so that it can be used for watering stock. This " spring-house " for the prairie is a simple apparatus, and not costly. But further : all who are acquainted with cattle know that under favorable conditions — ^and more favorable cannot be found than those of Nebraska 182 THE GREAT WEST. — their increase is marvellous, calculation showing that thirty cows, that would cost, say, twelve hundred dollars, in ten years will develop into a herd worth thirty thousand dollars, allowing ten per cent, for losses and the butter and cheese for the cost of maintenance. This is cattle-famiing, of course, in the agricultural region. In the great pastures west the busi- ness is simpler. There, as yet, dairy products count for nothing, and it is the increase in the herds — cheaply fed and cheaply cared for — which yields the profit. With the cattle raised in this western half of the State there are good opportunities of profitable trade. Small herds can be selected, brought into the eastern parts, pastured on the way, and wintered on cheap corn and hay ; and then they are in splendid condition for the meat-market in the spring. In the farming-region hogs go with cattle ; and Nebraska farmers, with their Chester whites, Polands, and Berk- shires, have as good stock as can be found in any State. Thousands of men find cattle-raising profitable in Nebraska, and thousands of others may engage in the business with equal success. In the west especially the business is an immense one, but statistics are not readily accessible, EXPERIENCE OF PLOCK-MASTEES. Those who devote themselves to sheep speak highly of the results ob- tained. The sheep in its origin is native to the mountains. It likes the dry, pure air of the uplands and avoids marshes. The lay of the land in Nebraska is therefore peculiarly adapted to sheep. On the breesy uplands, richly clothed with grasses, and in the pure, dry air, they are healthy and vigorous; the experience of Nebraska flock-masters, says the Hon. J. D. Jenkins of Fairmont in Fillmore county, who has had large experience, being that, with good management, sheep return a profit of fifty per cent, upon the investment. The pioneer flock-master of Eastern Nebraska is the Hon. Moses Stocking of Saunders county ; and one yearly return he made exhibited on a flock of sixteen hundred and fifty-two merinos — -which breed he prefers, though long-wool breeds are now coming to have partisans — a profit of $3495. In Jefferson county, Messrs. C. and P. Jansen — leaders in the Mennonite settlement there — commenced sheep-farming in 1875, purchasing in Iowa and Wisconsin a flock of fifteen hundred fair merino sheep, and in New York twenty to thirty thoroughbred merino rams. Since that time they have introduced new blood into the herd by importing additional thoroughbred rams, and have otherwise improved the flock by selling off all inferior animals and keeping only the best, so that now they have a flock of 2300 high-class merinos. As an indication of the manner in which sheep improve in NEBRASKA AND ITS RESOURCES. 183 Nebraska, they furnish the following figures as the yield of wool per head of the sheep during the several years : In 1876 the clip averaged 7f pounds per head; in 1877, 8| pounds; in 1878, 9 pounds; and 1879 the enormous figure was reached of 11 pounds and a fraction per head, from which they realized $5060. All through the State from south to north, and away west to the Republican Yalley and the forks of the Loup, ex- amples of successful sheep-farming are found, and information regarding them may be obtained by inquirers. It is not too much to say that the fifty million pounds of foreign wool now imported into the United States could all be raised on these prairies. SUCCESSrUL FETHT-CULTUEE. When the first settlers crossed the Missouri they would not believe that fruit would grow in Nebraska, and some years elapsed before even ex- periments were made. They gathered prolific crops of wild plums, grapes, and gooseberries, but they were slow to learn the lesson of Nature, that where the plum-thicket was prolific of fruit the apple-orchard would also grow. There were among the settlers, however, men of culture, intelli- gence, and enterprise, who knew how to reason and how to act. These were the pioneer orchardists of the river-counties. They planted, and their planting failed ; but they persevered, and the result is a brilliant success. Orchards and vineyards crown the slopes of the hills, and Ne- braska apples and Nebraska peaches vie with the best produced elsewhere. The success is undoubted, and the reason for the success is the co-adapta- bility of soil and climate — the peculiar deposits (before described), says Professor Aughey, making the State "a paradise for fruit-culture, espe- cially for the apple, plum, grape, and all the small fruits of the temperate zones." PISCICrtTIjTUEE. One acre of water stocked with suitable fish is more profitable than the best ten acres of land on which the sun shines. The native fish of Ne- braska are not of high quality, and there are room and verge enough in the home market for extensive piscicultural operations. There are clear rivers and creeks — in some parts small lakes, and everywhere ponds — ^in which certain species of useful fresh-water fish can be made for ever abundant. To show how fish will increase even when left only to their natural fecundity, instance a consignment of perch, bass, and pickerel which a few years ago were being sent over the Union Pacific Railroad to Califor- nia. By an accident the cal- was overturned into the Elkhorn River. 184 THE GREAT WEST. The fry got into the stream,' and there they have multiplied amazingly (notwithstanding illegal netting), and spread into tributary streams and ponds. At a late meeting of the Legislature a fish commission was ap- pointed to assist individuals in fish-culture and to protect their interests. Already many persons have established hatcheries. THE HONEY-BEE AND THE PRAIRIE FLOWERS, A gentleman who has travelled extensively in the Old World and the New World tasted honey in Nebraska, the product of the prairie flowers, and he said, " This is as the honey .of Hybla, the celebrated honey of the Mediterranean countries, with the same aromatic flavor." The honey of the prairie flowers is peculiarly rich, and bees work on the prairie and in the timber-belts on the streams to great profit. To attend to bees — except when the apiary is on a large scale, as it is now and again in Eastern Ne- braska north and south of the Platte — is an avocation for the women of the household — one in which they take delight, and one which not only puts money in the purse, but adds to the luxuries of the home. The bees begin to work on the wild flowers among the timber at the opening of spring, but the true honey season of Nebraska is July, August, and Sep- tember, when the flowers of the prairie — milkwefed, heart's-ease, golden-rod, sunflower, and many others — ^are in their fullest bloom, though by planting rape and other early-blooming honey-flowers May and June are brought into the honey period. In the river-counties of Nebraska large numbers of bees are kept, and in the neighborhood of Omaha alone there are two thousand swarms. THREE DISTRICTS IN NEBRASKA. The foregoing narrative describes Nebraska in general terms, and if the reader will study the following figures he will see the progress and prospects of the State further exemplified, but in a difierent way. A natural division of the State is into three great sections — North-eastern Nebraska, South-eastern Nebraska, and the grazing-region west. Speak- ing broadly of these several areas, it may be said that the western grazing country is somewhat less than half of the area of the State, North-eastern Nebraska being a little larger than South-eastern, though the present western limit of lands in cultivatibn is not so far west in the north as in the south. In the south the agricultural area extends almost to the western boundary of the State ; and, indeed, in what is now the graz- ing-region the processes which have made the eastern half arable are in rapid progress. NEBRASKA AND ITS RESOURCES. 185 NORTH-EASTERN NEBRASKA. Here there are twenty-eight counties, which in 1860 had a population of 10,500 ; in 1870, 51,088 ; and in 1879, 108,264. And wealth has increased with the increasing population. Twenty-five years ago settle- ment began on the Missouri bottoms. On the whole wide prairie there was nothing which civilized man counts as wealth; and yet now the property is assessed at — and assessed values are but as one in three of real values — $30,441,370, Omaha, with its population of twenty-five thousand, contributing several millions. In 1870 the land in cultiva- tion in the whole State was 647,031 acres, but in 1880 in this quarter of the State the figures are 1,168,846 acres. The live-stock now owned by the people numbers 48,963 horses, 4200 mules, 141,281 cattle, 46,769 sheep, and 134,988 swine ; and the wheat and corn product for the year 1879 (estimating for certain counties which have not made returns on the basis of the 1878 returns) is 5,804,749 bushels of wheat and 16,297,598 bushels of corn. Of cultivated timber there are 26,744 acres ; apple trees, 306,143; pears, 5582; peach trees, 39,584; plum trees, 48,564; cherry trees, 31,734 ; grapevines, 49,444 ; and 1104 miles of live hedge. SOUTH-EASTERN NEBRASKA, with twenty-seven counties, has a still more favorable record. The popu- lation of this section in 1860 was 16,539 ; in 1870, 71,731 ; and in 1879, 201,976 ; and in 1880 the assessed valuation of the property in this section is $40,483,979. The land in cultivation is 1,994,458 acres ; the horses number 100,574 ; the mules, 10,367 ; the cattle, 199,146 ; sheep, 70,285 ; swine, 523,683 ; while the wheat product (estimating as befwe for certain counties that have not made returns) is 8,722,105 bushels, and corn 20,698,982 bushels. The acreage in cultivated timber is 62,769, and of fruit there are 967,457 apple trees, 30,445 pear trees, 1,209,957 peach trees, 96,738 plum trees, and 185,485 cherry trees, 158,367 grapevines, and 5497 miles of live hedge. From the grazing-region west the statistics are not sufficiently complete to warrant their setting forth, though here reside the balance of the pop- ulation (the census of the State for 1879 gives the total population as 386,410, against 122,993 in 1870, or an increase during the nine years of 201 per cent., which is something unprecedented in the history of agri- cultural settlement, and most convincing ' testimony to the excellence of the land), the chief industry being the raising of beef-cattle in immense herds, though in the valleys there is considerable farming, and as settle- 186 THE GREAT WEST. ment proceeds and pioneers push westward the whole State will be de- voted to farming. The figures which are given must show those who want homes in the "West that they cannot settle in a better State than Nebraska. There is enougli and to spare for all the people, and an accumulation of wealth marvellous in so young a State. Those who have money to invest largely in stock may go to the grazing plains; those whose means are more moderate should take a farm ; while those who propose to engage ia trade and manufactures will find openings in one or other of the towns. Ne- braska is, and will always be, to a great extent, an agricultural country, deriving its wealth from the soil. But there is. money invested in manu- factures of various kinds, and there is room for more, especially in the manufactures which are connected with agriculture, as wagon- and car- riage-making, agricultural implements, starch, pork-packing, and dairy products. A large field is indeed open, which only needs capital and in- telligence and skill to develop. THE CENTEE OF THE EAILEOADS OF THE COTTNTEY. The railroad system of Nebraska permeates the State and strikes out over the continent, east, west, north, and south, to the seaboard. Wher- ever there is a market for the surplus products of the State, there are railroads to that market. No State at Nebraska's stage of growth has ever before had such railroad, facilities for the development of State com- merce and foreign trade, through the Pacific roads west and through the gate-cities of Omaha, Plattsmouth, and Nebraska City east and south- east. Nor is this all. A new. era of railroad-building seems to have come to the State, and more railroads will still be built, until there shall not be a corner of it which shall not be penetrated by the iron way, the modern highway of nations, and bring all the people, as will be seen is largely the case at present, into direct communication with Lincoln, the State capital. SCHOOL SYSTEM OP THE STATE. Nebraska provides liberally for the education of the young. In the first place, there is the common-school system, which penetrates every- where. There is a normal school for the training of teachers at Peru, in Nemaha county ; and at the head of the State system is the University at Lincoln, where the higher education, after the payment of matriculation- fees, is free to students. The educational endowments, as shown by the statistics presented to the Legislature in January, 1879, comprise common- NEBRASKA AND ITS RESOURCES. 187 school land, 2,443,148 acres; agricultural-college land, 89,452 acres; university land, 45,119 acres; normal-school land, 12,800 acres; and the school fund in money, $2,120,182 ; the revenue applied to common school purposes for the year 1878 amounting to $629,068. The common schools grow with the State, as the following table will show : , GROWTH OF THE SCHOOL SYSTEM. Tears. Av. No. days of School. Districts. Children. Teachers. Value of School Property. 1870 1872 1874 1876 1878 46 79 88 90 92 797 1410 2215 2513 2690 32,789 51,123 72,991 ^ 86,191 104,030 536 1512 2735 3366 3730 $178,604 817,163 1,553,926 1,585,736 1,806,466 Besides the public provision, the Episcopalians have a college for girls, Brownell Hall at Omaha ; and for boys. Bishop Talbot College at Ne- braska City. The Catholics have a noble college at Omaha; the Con- gregationalists, one at Crete, in Saline county ; and the M. E. Church is about to erect a college at York in York county. The State institution for the deaf and dumb is at Omaha, and for the blind at Nebraska City. The sum of the account is, that every child in Nebraska has within reach a sound education which shall fit him or her to perform the duties of life. STATE INSTITUTIONS. The capital is at Lincoln, and work is just now being commenced upon an addition to the present State-house, the Legislature at its latest session having voted $60,000 for the purpose. The University, a fine Italian building, is also in Lincoln, and the State Insane Asylum is about two miles away, located in a charming country ; the penitentiary, which is a castellated structure, is about one and a half miles from Lincoln; the Blind Asylum is at Nebraska City, and a Deaf and Dumb Institute at Omaha; and a reform school is to be erected at Kearney. OPPORTUNITIES FOB ACQUIltiNG LAND. There are millions of acres of government land yet open to pre-emption, homestead, and timber-culture entries in Nebraska, but those who want these will have to go considerably west. All over the State the public- school lands are offered for sale and lease. The quantities are named in 188 THE GREAT WEST. a preceding paragraph, and information with regard to them may be ob- tained by writing to F. M. Davis, State Commissioner of Public Lands and Buildings, at Lincoln, Nebraska. The minimum price at which these lands are sold is seven dollars per acre, on twenty years' time, at six per cent, interest, and leases are on appraised values. During the years 1877 and 1878 the lands sold were 26,819 acres, and leased 100,918, and the sales and leases during this year are doubling upon these figures. VTSIO'S PACirC EAILEOAD LANDS. For detailed information about these lands written or personal appli- cation should be made to the Land Commissioner U. P. E. E,., Omaha, Nebraska. This company owns three million acres of fertile lands in Central and Western Nebraska, which are sold for cash, or on a credit of ten years at six per cent, interest, with gradual payments of principal and interest. The prices range from two to ten dollars per acre, on ten years' credit, "according to quality, location, timber, and nearness to market;" and a deduction of ten per cent, from credit prices is made to cash purchasers. BUELINGTON AND MISSOTTEI EIVEE EAILEOAD LANDS. For detailed information about these lands address or apply to the Land Commissioner B. and M. R. R., Lincoln, Nebraska. This company has remaining of its la!bd grant of more than two million acres about one million acres south of the Platte River, in the rich south-eastern section and in the north-eastern section north of the Platte. The north-eastern lands, of which there are about six hundred and fifty thousand acres, range from one to six dollars per acre, on ten years' time, with discount from these prices on six years' and two years' credit, and for cash. The balance of the B. and M. lands in South-eastern Nebraska are sold at from three to ten dollars on ten years' credit, with discounts off for cash or shorter time of credit. The reader will perceive that there are still opportunities to acquire homes and farms in Nebraska in United States government land. State land, and railroad land, free or on exceed- ingly low terms; but the progress made by the State, as its history demonstrates, is proof enough that only a short time will elapse before the era of cheap lands is closed for ever. NEBRASKA AND ITS RESOURCES. 189 HEALTH. EXTRACTS FROM AN ARTICLE BY GEO. TILDEN, M. D., OF OMAHA. IN a new State the subject of malarial diseases is one of vital import- ance. Prominent among the causes and conditions of this class of affections may be mentioned a fertile soil, luxuriant vegetation, and poor drainage. Our soil is extremely rich and our vegetation most abundant, but the other condition, poor drainage, is not present The atmosphere is very pure and dry, and prevents the pernicious mias- matic effects which usually result from decaying animal and vegetable matter. Nebraska has less malarial disease than any Western or South- western State. Indeed, cases of this class are very rare, and when they do occur are mild in character and yield very readily to simple treat- ment. In regard to epidemics, I think I may very safely assert that there never has been in this State an epidemic of any kind ; even scarlet fever and measles have never appeared here epidemically. The vital statistics of the United States for the year 1870 set forth a fact of the highest importance to us relative to consumption. These statis- tics, together with our own, show with mathematical certainty that this is the most, favorable State in the Union for the prevention, control, and treatment of this great scourge. Here, in proportion to the population. Consumption shows her smallest bills of mortality. But this authoritative statement will not surprise in the least those who have resided here for the last ten or fifteen years and given any attention to the subject. They have stoutly contended that this is the most favorable spot for those pre- disposed to this malady ; and time and observation and the faithful record of facts have more than confirmed their most sanguine expectations and assertions. .... It matters not how warm and oppressive the day may be, the night is cool and delightful. Sleep, the great restorer of the mental and physical energies, is never disturbed by an oppressively warm atmosphere. In fine, the atmosphere of Nebraska is very pure, clear, dry, elastic, and bracing, and prpmotes in a high degree mental and physical axjtivity and development. Take the seasons as they come and go, and average them, and no State can make such goodly promises as this for health, develop- ment, and longevity. NEW MEXICO. BY GEN. LEW WALLACE, GOVERNOR. THERE are three interests in New Mexico worthy consideration — the mineral, the grazing or pastoral, and the agricultural — and they may be said to constitute the resources of the Territory, as manufacturing is confined almost exclusively to jewelry, of which very exquisite work in filigree is produced in Santa F6, mostly from gold and silver native to the Territory. AGEICULTUEE. Agriculture in New Mexico is yet in its primitive condition. The wooden plough of the Mexican fathers holds preference with the majority of farmers. Development is barely suiBcient to serve anticipation. Corn, wheat, oats, barley, and the table vegetables generally are raised with a view to the home market, which is quite limited. Corn is produced best in the valleys along the banks of streams. I have seen wheat- and oat- fields six and seven thousand feet above the sea-level as rich as any in Illinois and Minnesota. It is not possible to state even approximately the area of such productions. All irrigable lands, wherever they may be in the Territory, belong to the productive or farming class. The depth of the soil is something wonderful. With rains as in the Mississippi Valley, the results of intelligent labor would astonish" the world ; as it is, no one thinks of land for cultivation except it be irrigable. In this sense water is king. THE EIO GEANDE VALLEY. The river Rio Grande gives name to the lowlands along its shores, which, running north and south nearly four himdred miles, have an average width of five miles. The soil is light, warm, sandy, and sur- passingly rich. Putting the soil, river, and climate together, the Rio 190 NEW MEXICO. 191 Grande Valley is more nearly a duplication of the region of the Nile than any other of which I have knowledge. Not more than one-tenth of the soil is actually occupied. A consid- erable portion of it is unfortunately covered by grants claimed or con- firmed. , Fruits are favorite articles of production. Peaches, pears, apri- cots, apples, grapes succeed admirably, though in most instances, and notably with exception of the grape, the varieties are the poorest. In- deed, the word " variety " can scarcely be applied to them. The grape is free from disease, and affords wines which are in growing demand abroad. With skilled labor and capital to enable manufacturers to carry their wine a sufficient time, no portion of the country, not excepting California, will surpass this valley in this line of production. In all instances, and whatever the crop, the dependence of the farmer is upon the river, which, when irrigation is thoroughly systematized,' will be found furnishing an ample supply of water. Iron piping will then take the place of the open acequias and the area of planting be vastly increased. The wonder is that more attention has not been given this part of the country by people East seeking investments in landed property. One gentleman I have heard of near Mesilla, in Dofia Ana county, who clears annually quite ten thousand dollars from the fruit-products of twenty acres. Paying vineyards are also to be found at Bernalillo and Albu- querque. THE PECOS EIVEE VALLEY. This valley, deriving its name from the river Pecos, is not so thickly settled as its rival of the Rio Grande. The lands there are almost en- tirely occupied for grazing purposes. A good supply of water is obtain- able from the Pecos River and its tributaries, and every inch to which it can be carried will respond richly to the plough. Its advantage is in the absence of land grants, and, like the Rio Grande, it is blessed with a climate most healthful and delightful. THE MESILLA VALLEY. The beautiful region bearing this name should have a special mention by itself, but, to economize space, I have thought best to treat it as a part of the Rio Grande Valley. Agriculturally considered, it is the same. CATTLE- AND SHEEP-GKAZING. Off the Pecos and Rio Grande Rivers there are vast tracts of table- lands, called mesas, which are to be distinguished from the mountains 192 THE GREAT WEST. and valleys. They are too high for irrigation, yet they yield grasses of the richest kind for subsistence of cattle and sheep — grasses that cure themselves in the standing stalk. The varieiy of these mesa-tops permitting, as on the mountain-sides, the growth only of grass and cedar and pifion trees — the latter invaluable for shelter of animals, particularly in winter — will for ever limit their use to grazing. The ranges they offer cannot be excelled for that purpose ; adding them to the ranges on the mountain-sides, the vastness of accom- modations for feeding cattle, sheep, and horses can be appreciated. The inexpensiveness of the mode is well understood. The old dispute as to which is the more profitable, cattle-raising or sheep-raising, is yet unsettled, each having very intelligent and practical adherents. That New Mexico has not her proper place in the meat- and wool- markets of the United States may be set down to causes now very soon to disappear. They are — first, difficulties with Indians ; second, the in- ferior quality of the stock, no attention whatever having been given by owners to importation of blooded animals ; third, other localities, claim- ing original shipments, have been largely credited with the products due this Territory. I regret not having statistics to enable me to give the quantity of wool produced or the number of cattle and sheep in ownership. The results in either case would be astonishing to those who know little or nothing about New Mexico, who are in the habit of regarding it as chiefly de- sirable on account of its climate. The increase of both sheep and cattle is constant, and the improvement of breeds is becoming more and more noticeable. THE MUSTEEALS OF NEW MEXICO. Notwithstanding the adverse judgment of Lieutenant Wheeler in his very able report for 1876, I am of opinion that New Mexico will come quite up with her neighbors in the yield of precious metals. A variety of causes have heretofore contributed to prevent her thorough explora- tion for such wealth. Both Mexicans and Indians are indifferent to dis- coveries in this line ; in fact, the latter yet make it a capital offence to show a prospector anything of the kind. A Pueblo might be induced to part with his eye-teeth ; no inducement could prevail upon him to take a white man to a mine ; and in the hands of these people the golden keys have been held in tight grip ever since the expulsion of the Span- iards. Hence the ignorance prevalent with respect to the mineral riches NEW MEXICO. • 193 of the Territory, and the heretofore utter failure of attempts at their de- velopment. It is absurd to say that an arbitrary geographical line marks a silver or gold limit. With productive mining districts on the south, west, and north, and with geological formations identically the same, the best of the scientists will be hard put to to give a- reason why New Mex- ico is barren, and Chihuahua, Arizona, and Colorado are rich beyond computation, in gold, silver, copper,' and galena. And now every day is settling the question. The genuine prospector is here, and come to stay. He is in the mountains everywhere. Bugbear stories do not stop him, neither do land grants, rattlesnakes, bears, or painted Indians. He has discovered and adopted the burro as a friend, comrade, and servant. The consequence is new "finds" every day in out-of-the-way places. All mining history is divisible into two parts — the era of prospecting and the era of production. In New Mexico we have just entered upon the former ; five years will bring us to the latter. What can be had cheap to-day will then cost a fortune. Men seeking mining investments are welcome to the hint. There are more traces and signs of ancient mining in New Mexico than in either Colorado or Arizona. Already enough is known to warrant the assertion that the Territory is well stored with gold, silver, iron, copper, lead, zinc, mica, gypsum, coal, marble, precious stones, and stone of every variety for building. EESOUECES OF NEW MEXICO. BY L. BEADFOED PKINCE, CHIEF-JUSTICE OP THE TEEEITOEY. IN writing a general letter to old friends on Long Island on this subject last spring, I said that there was no opening at all for men without some means — ^that mechanics, clerks, and laboring-men could find no ade- quate field of labor. This was based on the fact that the wants of the native population are generally few and easily satisfied, that as a rule they are far from rich, that they have little desire for new houses, and that whatever building was progressing was in adobe, with which our mechan- ics were unacquainted ; and, as to clerks and laborers, that there were more men than places already. This was entirely true then, but the cir- 13 « 194 THE GREAT WEST. cumstances are since somewhat changed by the advance of the railroad. The Atchison, Topeka, and Santa F^ line has now not only reached Las Vegas, but is pressing with all the speed that enterprise and full resources can impart to the Rio Grande, which it is expected to reach by Christmas. It brings with it a new and active population and a great change in con- ditions. Las Vegas is to-day one of the busiest towns in the country — full of active, bustling, restless AWrican life. A hundred and fifty houses have been built in six weeks, and there is a constant struggle now to procure mechanics for rapid future improvements. The haste to build may be exemplified by the fact that I counted twenty-four carpenters on the roof of one half-finished hotel, all busily engaged at the same time in shingling. These circumstances of course present a field for mechanics, and I believe that the advance of the railroad will cause this field to increase rather than diminish for the next two or three years. Carpenters, masons, painters, and plasterers can all find employment in considerable number ; but especially carpenters, as houses must be built, but painting and plaster- ing are matters of not such immediate necessity. A few cabinetmakers, who can make and repair the furniture suitable to a new population, can also find profitable employment. These, I think, constitute all the classes of men without any capital who would do well to come to New Mexico at present. There is no lack of common laborers or of young men fitted ' to be store-clerks. And now for the branches of business in which those with some money can profitably engage. SHBEP-EAISING. I mention this first, because it is the most important industry of the Territory. It extends from the extreme east on the head-waters of the Canadian River to the San Juan coimtry in the far north-west. The sheep of New Mexico are to be counted by the million, and yet there is plenty of room for new enterprises both as to number and quality. To commence the business properly requires a capital of five thousand dol- lars, which will buy two thousand sheep and provide for all necessary ' expenses until a regular income is derived from the flock. No business can be safer, surer, or more healthful ; but, like all others, it requires work and attention, and if any one thinks that sheep-raising is to be conducted profitably by living in town and having flocks roaming the prairies under irresponsible herdsmen, without personal attention, he had better remain at the East. NEW MEXICO. 195 CATTLE-EAISIISrG. An immense field for this branch of industry is still open in New Mexico, and it can be surely successful under the same conditions as with sheep-raising. The profits are greater, but it requires a larger capital at the commencement and a longer period before there are returns of income. PEUIT-EAIBING. The whole valley of the Eio Grande from Santa F6 to Socorro is ad- mirably adapted to fruit-culture, and so are other portions of the Territory. Plums and apricots flourish considerably to the north of Santa F6, and grapes — of which I will speak separately — ^to the extreme south of the Territory. It is only within a few years that fine varieties of fruit have been introduced from the Eastern States, but the perfection in which they can be raised here, and the size which they attain, are extraordinary. The flavor of fruits here appears to be much higher than in California. Until now it has been useless to extend the culture largely, as there was no ade- quate market for the products ; but now that there will soon be direct communication by rail with Kansas and Colorado, the valley of the Rio Grande will become the great orchard of the West. Any good fruit- culturist coming now to New Mexico and establishing orchards in that fertile valley, will find an immense market open by the time his trees are in bearing, and cannot fail to reap a profitable reward. VINEYAEDS AND WINE-MAKING. For years the grapes and vines of El Paso have been celebrated, but this gives but a small idea of the extent of this vineyard-region or of the future importance of this branch of industry. The Eio Grande Valley from Bernalillo down to the Mexican line is naturally a grape-growing region, and vineyards are already in full bearing at all the important points, and at some have existed for more than two hundred years. The finest varieties of both native and foreign grapes succeed admirably, so that raising the fruit for immediate shipment will be a most excellent business within two years, when the railroad shall have made transporta- tion swift and easy. It is none too soon now to arrange the vineyards for this approaching trade, as the demand will be enormous before vines planted this fall or next spring come to bearing. The grape now ordina- rily grown, and of which vineyards of full size can be purchased if de- sired, produces an excellent wine largely used at present in the Territory, and which will no doubt find a market abroad as soon as the railroad is 196 THE GREAT WEST. completed. Unless all reports are false, this is the finest vineyard coun- try in America, the climate allowing the growth of many varieties too tender for the North, while the flavor is higher than in Californian grapes. The present native wine is said to carry more than an ordinary amount of spirits, and to produce an excellent brandy at small cost. It is stated by those whose judgment in such matters is reliable that a com- petent distiller can do a large and profitable business by buying the native wine and distilling brandy therefrom. MAEKET-GAEDENS. While a great proportion of the land in the Territory is adapted to grazing, yet there are beautiful valleys of extraordinary fertility where enormous crops can be raised on small areas. Such are the valleys of Mora and Taos, part of the Pecos Valley, ete. These present just the field adapted to German market-gardeners, for whose products the new hotels and advancing tide of population will make a ready market. And here I will mention one specific want which a few enterprising persons can soon remedy with profit to themselves and benefit to the com- munity. I refer to chickens and eggs. These are very scarce, no one apparently making it a business to raise them ; and any one engaging in the business can find a ready sale for a quantity practically unlimited. WOOLLEN-MILLS. Turning from farm-products to manufactures, the most profitable in- vestment in the latter connection would be a woollen-mill. Wool is the great product of New Mexico. It is here in inexhaustible quantities, and at present is all transported East at a very heavy expense to be man- ufactured. Kansas, Nebraska, Colorado, and New Mexico itself, present a vast market for woollen products, which are now brought from the East- ern factories ; so the wool raised here pays a double freight before it ar- rives at the West again, to be used in the form of blankets, carpets, and clothing. It is obvious that mills on the ground would save all this ex- pense, and that their business could not fail to be profitable. It may be added that in the few manufacturing experiments tried here it has been demonstrated that the native boys make excellent factory-hands. TANNERIES. In this land of hides, sheep-skins, and fancy skins there are no tanner- ies. Everything is sent away for that purpose. The extra freight on the useless weight thus transported is itself a large item. Of fancy skins NEW MEXICO. 197 there is a great variety, including bears, mountain-lions, beavers, red and gray foxes, wolves, minks, etc., all of which when tanned are readily sold and command good prices ; but at present they have to be sent long distances for tanning. I know of two lots very recently sent to New York for that purpose, thus entailing the expense of five thousand miles of transportation to and fro. A tannery established here, where the hides and skins could be brought directly to the door, could not fail to be largely profitable, even though the tanning material had to be brought from other places. BEICKMAKEHS. In various parts of the Territory there is good brick-clay, and from this time forward large quantities of bricks will be wanted. A practical brickmaker cannot fail to be successful. BANKING. By far the finest opportunity for an investment of capital, by those who do not wish hard work, is a bank in Las Vegas. A national bank is greatly wanted there, and would be very profitable. The business of the town is already very large, and as an immense section of country is now and must continue io be tributary to Las Vegas, it will undoubtedly increase. The immediate deposits would be considerable, and the oppor- tunities for safe loans are abundant. The lowest bank-rate in the Terri- tory is one and a half per cent, a month ; and a careful inquiry as to the success of other banks here and the business condition of Las Vegas leads me to say confidently that no such opportunity for a safe and prof- itable investment of capital exists to-day in the whole country as in the establishment of a national bank at that city. MINING. I have reserved this for the last, as it is probably the most interesting topic of this letter. Almost every section of New Mexico abounds in " mineral," and the amount of gold, silver, copper, coal, and mica within its limits may be called incalculable. I will not enumerate all the local- ities, but venture the assertion that in less than five years New Mexico will be the great field of American mining enterprise. All that is wanted now is development. The gold-mines of Colfax county are practically useless until the conclusion of the pending foreclosure of the mortgage on the Maxwell land grant sets free the belt of rich mining-lands within its limits. The same is true of gold, copper, and mica on the Mora grant, 198 THE GREAT WEST. now in process of partition. These two great grants, together containing about two million six hundred thousand acres, have been standing right in the gateway of immigration into the Territory as a kind of barrier, but the next few months will no doubt see the title of each settled, and this vast extent of land, embracing mineral, farming, and grazing dis- tricts, thrown open to American energy and enterprise. All through the Territory excellent prospects exist, but all need development. The pla- cers contain millions of dollars in gold-dust, but in general cannot be worked for want of water, which can only be obtained at considerable expense. By meeting that expense an immense return could be ensured. The Cerillos silver-mines are in a most encouraging condition, but need capital for development. They are situated on the very hillsides from which the Spaniards extracted unknown millions centuries ago, until the enslaved Indians arose and drove them from the land, and endeavored to destroy every trace of their sufferings by filling up the mines in which they had labored. At the Cerillos are dozens of claims showing excellent veins of " min- eral," but very few of the prospectors have the money with which to sink shafts to the distance necessary for profitable results. Around Silver City and Shakespeare there is much mining enterprise, but everywhere there is a necessity for more capital for development. Reports come daily of rich new discoveries, which can no doubt generally be taken with some grains of allowance ; but this much is true, that but a moderate portion of the Territory has been prospected at all, and that the indications are that a short time will develop fields of mining industry which will give profitable employment for thousands of men and millions of capital. Coal is found in large quantities and of excellent quality in several sections of the Territory. The Atchison, Topeka, and Santa Fg Railroad Company recently bought a considerable section of coal-land belonging to the government, but there is still room for plenty of private enter- prise in this direction. THE PROFESSIONS. Many professional men, lawyers and physicians, inquire as to the chances for successful practice here. To these I can only say that there is always plenty of professional business for those who are competent and skilful, who obtain the confidence of the community, and who really mean in good faith to labor zealously in their professions. The bar of New Mexico is second in ability to that of few of the States. No one should come with the idea that he is going to find an inferior degree of NEW MEXICO. 199 talent here, but yet there is room for a few more lawyers of the right kind. The same may be said as to physicians ; with the addition, that the increasing population of course requires more medical attendance, and that there are country towns of considerable size which at present have no qualified physician. Thus I have sketched as briefly as I could some of the business oppor- tunities and something of the industrial situation in New Mexico* I shall add here that the climate, which is altogether the finest in the country, will allow thousands of those who are invalids at the East to ^ engage in active business here. Especially to those ha-ving weak lungs it presents great advantages. Here they can raise vineyards and orchards if they do not care to risk the roughness of life on a ranche. The medicinal and hot springs at Las Vegas, now under control of the rail- road company, which is making rapid improvements, will be a resort giving the advantages of Eastern watering-place life to the families of such residents as desire it before next summer. And — what ls perhaps of the greatest importance to those proposing to locate here, and presents a marked contrast to attempted settlement in the Southern States — they will find the native population polite, generous, and hospitable almost to a fault, with no dislike or distrust of newcomers of the proper class, but inclined to welcome good citizens from wheresoever they come. Con- sidering the circumstances of the case, and the character of some of the first Americans who came to the Territory, it is really surprising that so much goodwill should be felt by the so-called " Mexican " population toward the newcomer ; but it certainly does exist, and those who choose to make New Mexico their home, and who are entitled to respect and con- fidence, will find a welcome anywhere in the Territory, and need have no fear of being branded as " carpet-baggers " or ostracized from society. WYOMING. BY HON. JOHN "W. HOYT, GOVEKNOE. SSENEEY. WYOMING scenery is a subject for poet and painter. One sees much of the poorest of it in travelling over the great Pacific Railroad, and some that is sure to enkindle his enthusiasm. It is much to live in the presence of beautiful and magnificent surroundings, for Nature at her best exerts a most refining and elevating influence. -SIsthetic and moral culture is the priceless product of her teaching. Many a Wyoming herdsman grazes his cattle and many a shepherd watches his flock in the midst of scenery that would challenge the genius of a Turner or Salvator. He is the better for it, and the children who play about his cabin-door and gambol on the bank of the beautiful stream flowing past will be the better citizens for these silent lessons. I cannot here attempt even to locate these glories of the landscape ; one finds them on every mountain-side and in nearly every valley. When better known they wili make of Wyoming, including that "wonderland" the great National Park, a region of resort for pleasure-seekers from every part of the world. POPULATION. A very large proportion of the population consists of former residents of the New England and Middle States. Of the foreign population (not large) the majority are German. In the coal-mines at Evanston and Rock Springs, and the Atlantic City coal-mines, are considerable numbers of Chinese. There are also some persons of this nationality at several of the larger towns along the railway, the whole number in the Territory aggregating four or five hundred. The great majority of the population occupy the sixty-nine towns, villages, and stations along the Union Pacific Railroad. The remainder are found at South Pass, Atlantic, Miners' Delight, Lander — all in the 200 GIANT'S BUTTE, GREEN RIVEE. WYOMING. 201 region of the Wind River Mountains; at Centennial, Douglas Creek, Snowy Range, and other mining points in and about the Medicine Bow and Seminole Mountains; at the several military posts, in the settle- ments on the Bear River and its tributaries in South-western Wy- oming, and on numerous isolated ranches throughout the southern and middle portions of the Territory. The two great branches of industry are the pastoral and mining. The bulk of capital employed is invested in live-stock, though much of the population and a good deal of the mercantile business are in some way connected with the mining industry, manufacturing, and the business of transportation. The Pacific Railroad Company alone has on its pay-rolls and connected with its extensive operations — machine-shops, rolling-mills, stations, and mines included — quite a percentage of the laboring popula- tion. These of course occupy the towns and villages along the line. Of the capitalists engaged in the stock-business and mining, very nearly the whole numbelb also live in the towns, even though their mines or ranches should be two or more hundred miles in the interior. The herd- ers, and they who, as foremen, have immediate oversight of the herds and flocks or mines, live on the' ranches or in the camps of necessity, but the proprietors, with few exceptions, reside upon the railway, and with their teams go and come as interest demands. In the towns they are the men who, with the merchants, prominent men of the trades, and professional men, mould society and govern in public affairs. Hence it is well for the Territory that they are almost universally men of character, intelligence, and foresight ; men who, having the beginnings of fortunes at the East, have come out here to enlarge them more rapidly than was possible there; men of former means and position, who during the financial storms of these recent years suffered partial wreck and sought a field wherein to recuperate their failing fortunes ; young men, members of first families, who feeling the pinch of close quarters in New York, Philadelphia, and Boston, and desiring to breathe the freer air of the great West, have taken a sum modest or large as convenient, and are here for the threefold advantage of increase in wealth, invigoration of health, and the indescri- bable charms of a frontier-life under sunny skies and in the midst of sub- lime surroundings ; ambitious graduates of Dartmouth, Yale, Harvard, and other colleges, who were willing to postpone entrance upon their life- pursuits until they had first felt the inspiring touch of Nature and laid a foundation for future independence ; men also of special culture in litera- ture or science, who, for the time at least, have left the unremunerative life of research, that they may divide a few years of time between the 202 THE GREAT WEST. pleasures of private study and the building of a little fortune. All these are here, and for the greater part are realizing their most sanguine expec- tations. The other classes are common to all communities, though an unusually large proportion of those who compose them are characterized by a special energy, tact, and enterprise. As a matter of simple justice to a people who are still suffering, in the judgment of a remote public, for the sins of unworthy forerunners, whom they long since succeeded, — for this reason and none other I deem it pro- per to represent the present population of Wyoming as being especially characterized not only by courage, keenness, enterprise, and energy, but also by a most commendable love of good order and by a liberality of sentiment rarely found in any community. EEPOET OF THE SUEVEYOE-GENEEAL, EDWAED C. DAVID. GENEEAL DESCEIPTION. THE area of Wyoming is 97,883 square miles, of which 9,000,000 acres are surveyed into sections and 42,638 acres are improved. The real and personal property amoimts to $20,000,000, the population is 30,000, and the towns and villages number 69. There are extensive forests, coal- fields, gold-bearing lands, and mines of silver, copper, iron, graphite and sulphur ; also extensive deposits of soda and inexhaustible springs of pe- troleum. Minerals, timber, and stock constitute the principal resources. A large supply of cattle, horses, sheep, and wool is sold in this Territory or shipped to the East annually. The pure air, dry climate, mild win- ters, and nutritious grasses render the advantages in stock-raising unri- valled, and it is becoming a great soiu'ce of wealth to the settlers. The cattle feed and fatten upon the short but nutritious bunch- and gramma- grasses of the Plains in winter and summer, without shelter, as has been proven during many past winters. The favorite wintering-ground of the herders and shepherds is along the east slope of the Laramie Moun- tains, at an altitude of about four thousand five hundred feet above sea- level, and their herds are generally healthy and fat even in winter. The annual loss in cattle, from all causes, is only two per cent., and the cost per head for keeping a herd of ten thousand is not more than one dollar. A profit of one hundred per cent, has been realized in investments in WYOMING. 203 cattle, and the profits are never less than twenty per cent. Butter and cheese are beginning to be extensively made for the home supply. The number of cattle in Wyoming is 300,000, and yet the wide pastures in Northern Wyoming are unoccupied, though as large as Pennsylvania, and a choice portion of the Territory. Here the valleys are productive and beautiful, and the meadows are of surprising richness and almost endless succession. Thousands of square miles in the valleys of Powder Eiver and its branches are found to be susceptible of producing all the cereals with irrigation, and in many places without irrigation in favorable seasons. For more than one hundred miles there is a succession of crys- tal trout-streams, fringed with timber. The late occupation of this re- gion by the Indians has prevented it from being sooner settled. The number of sheep in Wyoming is 200,000, and they are often wintered by grazing. The number of horses is 20,000. The North Platte basin contains 8,000,000 acres of pasturage, with lasting streams and good shel- ter in the bluffs and canons ; and this area would feed 8,000,000 sheep, yielding 4,000,000 pounds of wool, worth $6,000,000. The Laramie Plains, nearly one hundred miles wide, and once the favorite resort of the buffalo, are now occupied by herders and shepherds in all seasons, and here they are near the great forests of pine and the Union Pacific Rail- road, and- settlers can obtain iron ore, white marble, building-stone, lime- stone, and fire-clay. The shipment of cattle increases largely every year, and many will be required for the Pacific slope and for the home demand. The quality of cattle has been greatly improved by importing thorough- bred Durham stock. The valleys and sloping plains in Northern Wyoming are only of three or four thousand feet altitude, and will prove more desirable to the farmer and stock-raiser than the higher plains along the rail- road. CLIMATE. The climate of Wyoming is very salubrious, and the impression among the inhabitants of lower altitudes that it is hyperborean and chilled by deep snowdrifts for half the year is erroneous. The mean temperature at Fort Laramie for twenty years has been 50°, the annual rainfall eighteen inches, and the snow, which is light and soon disappears, was of the same annual depth. From observations by army officers at Fort Laramie and Cheyenne, from 1855 through a period of seventeen years, it is proven that these localities have a mean annual temperature corresponding to that of Middle Pennsylvania, Ohio, and Indiana, and that the annual and monthly ranges of the thermometer are more moderate than in those 204 THE GREAT WEST. States. The rainfall seems to range from five to nineteen inches per an- num. The force of the wind is diminished greatly by the mountain-ele- vations. From 1850 to 1855 the average temperature was 49°, the same as at Cheyenne since 1871. Army surgeons and physicians here pro- nounce Wyoming one of- the most healthful portions of the world. The air is light and pure, with sufficient oxygen to exhilarate the nervous sys- tem. The thermometrical changes, though sometimes sudden, are of short duration. Fort Eussell in 1869 gave 55°.78J mean temperature, with cool and bracing evenings and mornings during the summer. The isothermal line of 50° annual mean temperature, from Burlington, Iowa, passes through Fort Laramie and thence to Puget Sound, bearing stead- ily north of west from the Mississippi. Strong and frequent winds in fall and winter are an objectionable feature in the climate, but they are not so prevalent in the mountain-valleys, and never increase to a hurri- cane, as in lower countries. TOPOGRAPHY. The general elevation of the plains and valleys of Southern Wyoming is from five to seven thousand feet above the sea, and the mountains are from one to four thousand feet higher. The altitude of Pine Bluffs is 5026 feet ; Cheyenne, 6041 feet ; Sherman, the highest point on the rail- road, 8241 feet ; Laramie City, 7123 ; Medicine Bow, 6550 ; Carbon, 6760; Fort Steele, 6840; Creston, 7030; Green River, 6140; and Wahsatch, five miles west of the Wyoming boundary, 6879 feet. The Union Pacific Railroad, on which the above-mentioned towns are im- portant stations, is the chief resource for transportation over the 488 miles of its length located in Wyoming, and has an average grade of only four feet per mile. The Laramie, North Platte, and Green Rivers flow through a region supposed to have once been the bed of fresh-water lakes, and now producing but a sparse growth of vegetation, mainly artemisia or sage-brush. Bear River, rising in the Uintah Moun- tains, runs north in a monoelinal valley ; and these rivers, with their tributaries, drain the south half of Wyoming. The north half, sloping north and east, is drained principally by Wind River, the Big and Little Horn, Tongue, Powder, and Cheyenne Rivers — all, except the latter, being confluents of the Yellowstone. The Wind River Mountains in the north-west constitute the watershed of the Yellowstone on the north-east, and of Green and Snake Rivers on the south-west, and culminate in the Three Tetons and Fremont's Peak, the latter 13,750 feet high. The Big Horn Mountains are in the central WYOMING. 205 portion of Northern Wyoming, and their highest peaks rise above the snow-line. The Carboniferous limestone resembles the older strata, in which are found the silver and galeniferous ores of Utah. The Triassic sandstone contains salt and gypsum. The coal-fields of Wyoming are in the lower Tertiary beds, and hematite iron ore two to fifteen inches thick is found in the same strata. COAL. The mineral resources of the Territory are vast and varied, and of these coal is the most important. Evanston produces 125,000 tons annually, Eock Springs 144,000, and Carbon 75,000. Coal is found in the Medicine Bow Mountains, Laramie Peak, Separation, the Big Horn Mountains, Eock Creek, Fort Fetterman, Black Buttes, Hallville, Point of Eocks, and at many other points noted by the United States deputy surveyors. Most of the mines extensively worked are on the railroad. The Wyoming coal has but little sulphur, and for domestic use is pre- ferred to the bituminous. It resembles lignite, is brittle, but nearly as compact as anthracite, and is used in Nevada for smelting the silver and lead ores. The Evanston coal has the largest per cent, of carbon, and the stratum is twenty-seven feet thick. On the Missouri Eiver the Wyoming coal is preferred to that of Iowa. There are 267,319 acres of coal-lands already surveyed into sections, and in 1877, 275,000 tons were the product of the mines. Magnetic iron ore, in mountain-masses, yielding seventy-two per cent., is found forty miles west of north from Cheyenne, on the east side of Laramie Mountain, to which an easy railroad grade can be obtained. Eed oxide of iron, used in manufacturing metallic paint and the reduc- tion of silver ores, is found, accompanied with strong indications of cop- per, three miles north of Eawlings, and here considerable capital has been used in paint-works. GOLD. The gold-mines on Douglas Creek in the Medicine Bow Mountains, though yielding only $15 per ton of quartz, are profitably and easily worked, and have valuable improvements. Gold is also found on Eock Creek and in the Big Horn, Wind Eiver, and Seminoe Mountains. The area reported in recent surveys is 31,161 acres of lands containing gold. In the Sweetwater gold-mines the quartz yields $50 per ton, and a choice specimen from the Seminoe Mines yielded $106 per ton. 206 THE GREAT WEST. BODA.. The soda^lakes in the valley of the Sweetwater are about one hundred in number, with areas of twenty to one hundred acres, and contain deposits of sulphate of soda ten to fifteen feet thick, almost chemically pure, having nineteen per cent, of soda and twenty-four per cent, of sulphuric acid, making forty-three per cent, of sulphate of soda. The largest lake has fifty million cubic feet of soda, and one boring of forty feet did not reach the bottom of the deposit. The water containing the salts rises from the bottom and fills any excavation made, thus rendering the supply inexhaustible. The seven million dollars paid by the United States yearly for a foreign article can be earned by these mines, five of which have been surveyed for the claimants. The hot springs in the valley of the North Platte, at the foot of the Medicine Bow Mountains, have been improved as a resort for invalids, and those near Camp Brown are valuable for their medicinal properties. There is an oil-spring on the Popo Agie, near the Shoshone lands, of heavy, non-inflammable lubricating oil, which has been surveyed for the claimant, and this oil is preferred by the railroad company. Crude petroleum is also found on Bear, Green, and Wind Rivers. Three copper-mines surveyed yield ores largely mixed with lead and silver. FOKESTS. The forests of Wyoming will furnish to the settlers the means of cheap improvement, and they cover an area of ten million acres. Saw-mills at various points are converting the logs into lumber, the annual product of which is 5,000,000, shingles 3,000,000, and laths 1,000,000, besides 500,000 railroad ties and 2,000,000 bushels of charcoal. The Snowy Range is covered with vast forests of pine, cedar, fir, spruce, and hemlock, equal to that of Michigan ; and much of this tim- ber is near the railroad. The Medicine Bow, Uintah, Wind River, Big Horn, Wahsatch, and Aspen Mountains are as heavily timbered, and the streams when full in the spring can all be used for rafting saw-logs, wood, ties, posts, and poles to the railroad. The Big and Little Laramie, Rock, Medicine Bow, North Platte, Bear, and Green Rivers and their tributaries can all be utilized for rafting timber to the railroad and for sawing it into lumber, adding prosperity and wealth to the railroad-sta- tions on these streams, and supplying the wants of settlers, of future rail- roads, and of telegraph-lines. There are also pine-lands in the Laramie Mountains and in the north-east and north-west corners of the Territory; WYOMING. 207 350,000 railroad cross-ties, 200,000 cords of wood, 1,000,000 feet of saw- logs, and 40,000 fence-poles were cut in one township, and yet this amount of depredation only consumed one-seventh of the dense growth of timber in that township. Larger bodies of thrifty timber are annually killed by the firing of dry windfalls by ' mischievous Indians, careless hunters, and lightning than in any other way, and the fires this fall have wasted millions in value. AGEICULTTTEE. Where the valleys can be irrigated, wheat, oats, barley, potatoes, cabbage, turnips, beets, onions, etc. can be raised. The loamy soil is very productive, and oats, barley, and potatoes grow finely and ripen at Laramie City, at an altitude of seven thousand two hundred feet, the potatoes yielding four hundred bushels per acre. Potatoes, beets, onions, asparagus, beans, peas, lettuce, radishes, turnips, carrots, parsnips, cab- bage, cauliflower, melons, cucumbers, and squashes are raised at Fort Fetterman. Several thousand acres on the Laramie River are irrigated by a canal twelve feet wide 'and twelve miles long. The valleys of the Lodge Pole, Horse Creek, Chugwater, and Laramie River can all be irrigated and made to grow thirty bushels of wheat per acre, and where streams are wanting water can be raised from wells by windmills, as in California, the water being abundant fifteen to thirty feet below the surface, as in the wells at Cheyenne, generally half full of water. A well two hun- dred feet deep filled to within ten feet of the surface. CITIES, TOWNS, AND VILLAGES. Cheyenne, at the junction of the Denver and Union Pacific Railroads, and near the junction of the Colorado Central, is the capital of Wyoming and the county-seat of Laramie county, and has a population of five thousand and an area of one thousand five hundred acres. It has six churches, a large brick high-school building, two large brick hotels, several extensive wholesale establishments, factories for making wagons and carriages and for the manufacture of jewelry, and there are many fine brick residences. It is supplied with water for irrigation by ditches and reservoirs, and by a steam-pump for security against fire. Its trade with freighters, miners, and stock-raisers, and with Camp Carlin and Fort Russell, near it, is extensive, and it is a division station on the railroad. Its average temperature in 1878-79 was — summer 65°.37, rainfall, 1.88 208 THE GREAT WEST. inches ; autumn, 40°.38, rainfall, 0.33 inch ; winter, 25°.27, rainfall, 0.24 inch; spring, 46°..63, rainfall, 1.13 inches. Laramie City has 2000 inhabitants, four churches, a very fine school- building, a public library, a hospital costing $12,000, and the machine- shops, rolling-mill, and large hotel of the railroad. It is irrigated with water from the mountains. The town of Wyoming has a sawmill for the manufacture of lumber from timber rafted down the Little Laramie. Carbon is a mining town of 800 inhabitants, and ships a large amount of coal. Green River and Eawlings — ^both county-seats — Eock Springs, Hillard, Bitter Creek, Bryan, and Carter are in a coal and iron region, and are important railroad-stations. Evanston has 2000 inhabitants, a public library, water-supply, and saw- mill ; also extensive coal-mines and a thriving lumber-trade. Hamilton, South Pass, and Atlantic Ciiy are near the Sweetwater gold- mines, and have a total of 2000 inhabitants. The seven forts in the Territory have been sufficient to keep the Indians from depredating to any great extent, though the Utes in North Park, near the south boundary, heve lately been hostile. The Shoshones have had a part of their reservation surveyed into sections. The Chinese are peaceable and industrious, but are slow to assimilate with Americdn customs. GAME. Buffalo are becoming scarce, but the hunters still find an abundance of elk, antelope, and beaver, besides mountain-sheep, rabbits, squirrels, par- tridges, grouse, quail, sage-hens, ducks, and geese ; also otter, mink, marten, ermine, and musk-rat. Of the predatory animals we have the fox, coyote, wild-cat, lynx, panther, mountain-lion, and bear. Speckled trout abound in most of the streams of Northern Wyoming. MANTjrACrtrEING EESOTTECES. With abundant water-power in the large streams, with an inexhaust- ible supply of coal, and with railroad transportation through the entire length of the Territory, railroad iron, wrought iron, and heavy cast-iron utensils and machinery can be made in Wyoming. Lumber, leather, and glass can be manufactured, the white marble wrought, and the soda and sulphur refined. WYOMING. 209 ADDENDA. The admirable graded-school system adopted here is similar to that of Michigan. The Territorial library now contains five thousand volumes. The removal of the Sioux from Northern Wyoming has given fresh impulse to settlement in that fertile region. MONTANA. BY EGBERT STEAHOEN. MONTANA, next to the youngest, and one of the largest Territories of the Union, lies between the 45th and 49th degrees of north lati- tude and the 104th and 116th meridians of west longitude. It is bounded on the north by the British possessions, on the south by Idaho and Wy- oming, on the east by Dakota, and on the west by Idaho. GENERAL DESCRIPTION. This magnificent empire of the New North-west contains an area of 150,000 square miles, or nearly 100,000,000 acres. Of this, 16,000,000 acres are fertile farm-lands, a more extensive area than is covered by an entire average Eastern State. It contains 38,000,000 acres of unexcelled grazing-lands, a pasture-field alone larger than the great prairie State of Illinois. Its surface, underlaid with stratum after stratum of coal — largely embraced in the grazing and agricultural area already mentioned — amounts to 60,000 square miles, and would not only cover the giant State of Pennsylvania, but would extend over the boundaries of the commonwealths which encompass that greatest of all our Eastern coal- mining regions. And then the Montana forests, 14,000,000 acres in extent, cover more territory than those of the noted lumbering State of Michigan, whose product in this line reaches a valuation of $40,000,000 per annum. Of the mineral wealth the world knows more, for it is a region whose quartz-veins and sluice-boxes have poured out over $150,000,000 in treasure in the first seventeen years of its ^settlement. In questioning Montana's position and climate, readers should remember that the whole of England, Ireland, Scotland, Belgium, Holland, and some of the most beautiful and fertile portions of sunny France, lie north of the extreme northern boundary of Montana. 210 MONTANA. 211 THE CLIMATE is unexceptionable. It would be a broad sweep to claim that it is the best in the United States, but many citizens claim as much for it, and indeed, according to their liking, they are not idle in their belief. There are cold snaps — ^that is, old Fahrenheit registers the cold at ten to twenty degrees below zero. Yet there is something here, as in all Rocky Mountain re- gions, that tempers the cold to poor humanity — ^the rarity and the dryness of the atmosphere, it is said — and one suifers vastly less during the winter season than he would in the Middle States; besides, these extremes in temperature are infrequent, and last winter, being unusually severe, reg- istered scarcely a day at fifteen degrees below, with very few days at all below. Summer is never sultry or hot, while the U. S. Signal Office at Fort Benton revealed one hundred more clear days during the last year than were observed at Chicago. With very little severity and infrequent extremes, the weather still has variety enough to prevent complaints of it on that score. Naturally, all concede this and such it indisputably is. Notwithstanding theoretical arguments against the Rocky Mountain region as a resort for lung diseases, we can positively aver that all lung affections wherein there is no undue loss of capacity are universally benefited in Montana. Asthma or hay fever there is none, though some persons may confound advanced emphyzema with such. For latent or threatened consumption there is unimpeachable evidence in its favor. The rector of St. Peter's church, Helena, gives in his record of interments the cause of death, and in twenty-six cases, his whole service in the Territory, there was but one death by consumption. Malaria cannot exist here, even though men bring it implanted in every bone. The Missouri River is thoroughly open near Helena a month earlier each spring than at Omaha, with almost unfailing regularity, and signal- service and private observations demonstrate the fact that the mean annual temperature of Helena is the same as that at Santa F^, New Mexico, the latter being some eight hundred and fifty miles south of Montana's capital. It is hardly necessary to state that the extreme of heat is never known in all this great mountain-land. The nights, always cool, are proverbial for their absence of disagreeable dews and damps. In the higher moun- tain-ranges the winters are of course more rigorous, the snowfall far ex- 212 TEE GREAT WEST. ceeding that in the valleys and the weather sometimes growing intensely cold. As a resort for invalids and for those constitutionally deformed we can commend Montana just as heartily. Innumerable springs — ^mineral springs, hot springs, sulphur springs — are scattered about, and so situated that patients can have their choice. That there is virtue in these springs for certain ills, such as are visited upon mankind by the sins of their fathers — ^for constitutional diseases generally — ^is beyond dispute. NATITRAL SCENEEY. The tourist, the pleasure-seeker, the scientist, all will find as happy a friend in Montana as the combination dare hope for in the wide world. In the heart of Montana, four thousand miles from the sea, the Missouri River presents such distinctive features of wildness, grandeur, and beauty as are hardly dreamed of by those witnessing its murky and treacherous meanderings through the prairie States. Here clear as crystal, alive with trout, embowered in beautiful pine-forests, the average citizen of Omaha would never believe it the miserable eyesore he left down there, tearing away Iowa and Nebraska counties so unmercifully. Entering Montana from the south, vid the Union Pacific and Utah and Northern Railroads, the tourist hardly crosses the line ere objects of interest to the purely aesthetic taste plead for attention right and left. Then he may wander all over this marvellously beautiful domain — from the Bad Land region of the lower Missouri and Yellowstone at the extreme east to the grandly- rugged and often iridescent summits of the Bitter Root range at the western boundary — and at the close confess in his bewilderment that Nature charmed so irresistibly at different steps it would be difficult to determine which spot to favor in a second ramble. YELLOWSTONE PARK. The Yellowstone, its great falls and grand cafions, its enchanting scenery and wild rapids, is renowned the world over. The National Park en- chanted land, its lakes and mounts and geysers, "with its variety of phenomena so vastly excelling anything of the kind elsewhere that com- parisons are almost ridiculous," is only bordering Montana, but is the Montanians' summer-resort, watering-place, picnic-ground. To the sporting man we have only to announce everything in his field, from the mountain-lion down to the jack-rabbit, from the wild-goose to the sage-hen, from the mammoth salmon to the brook-trout. The rifle, the fowling-piece, and the fly can be utilized on the same excursion. MONTANA. 213 AGEICULTCTRE. Abounding in noble rivers and possessing the best valley-system to be found in the entire Rocky Mountain plateau, Montana also offers many inducements to the agriculturist. Aside from the Missouri, Yellowstone, and Upper Columbia — each navigable and possessing thrice the volume of the Ohio at Pittsburg — there are within her boundaries a dozen rivers presenting features of size and beauty hardly excelled by the. finest in New York and Pennsylvania. Among these are the Madison, Gallatin, Jefferson, Bitter Root, Beaver Head, Hell Gate, Musselshell, and Flat- head, their valleys ranging in length from one hundred to two hundred miles, and in width from two to twenty miles. Add to these the nearly numberless lateral streams which beautify almost every ravine and valley, and one finds here unlimited water-power and inexhaustible supplies of water for irrigation. Montana Territory was once known to the world as a rich placer- mining country, but, far away from centres of trade and highways of travel, its great resources lying beyond its gold were unobserved. Those early days saw flour sell at one hundred dollars per sack, while the present demonstrates that it was then, and is now, the best wheat district in the Union. There are well-authenticated cases of enormous yields ; among which are these : One field of twenty acres yielded eighty-two bushels per acre ; one lot of a number of acres gave one hxmdred bushels per acre ; and one single acre in one instance produced one hundred and twelve bushels. Oats and barley yield almost proportionately with wheat, while vegetables are grown quite beyond anything observed in a long experience in the East. BIG POTATOES. General Brisbin, commandant at Fort Ellis, gives statistics of twenty- seven acres of vegetables cultivated by soldiers, which at the prevailing prices in Montana amounted to over seven thousand dollars. This last season, he says, the yield has been one-third greater. At the Helena Fair were exhibited potatoes that weighed four pounds each, rutabagas that weighed seventeen pounds each, and turnips one of which weighed forty- two pounds. Farms that yield crops as above are worth from five to twenty-five dollars per acre, depending upon the means to market and upon the im- provements ; but good land may still be had much cheaper, and near enough to market, through the various land acts. Under the Desert 214 THE GREAT WEST. Land Act a settler is allowed six hundred and forty acres anywhere in Montana by paying one-fourth of a dollar per acre on possession, by dig- ging an irrigating-ditch through it within three years, and by paying one dollar per acre by the end of that period. Besides, he is allowed the tract subject to exemption laws in existence elsewhere. Considering the vast extent of territory, no one need entertain a fear that the choicest acres are already located, or that they will be too soon for him. who has a long way to come. Besides all the hardy cereals and vegetables, which are produced in great abundance in the inhabited valleys, we find some farms in the Bitter Root and other sunny basins where apples, plums, grapes, cherries, pears, nearly all small fruits, melons, tomatoes, and even tobacco and pe- cans, are among productions which indicate a not very forbidding clime. IiTigation is considered necessary in most localities, although some large crops were raised this year without it. This is an expense of about fifty eents per annum per acre. STOCK-EAISING. As a stock-raising section Montana is rapidly becoming known to the outside world. Its beef-cattle are the best sent to the Eastern markets from the grazing-regions, and bring the best prices. It is acknowledged the best grazing-land in the world. Cattle live and increase without a shelter other than the broad canopy of the heavens, or food provided ex- cept as it grows and is left for them spread over the great hills and plains they make their homes. Sheep and horses roam through the severest winter, exposed to the climate, compelled to live entirely by grazing. Nothing is expended for them save the services of a herder, who keeps a general survey of the range. Matured steers sell readily at the ranch at an average of twenty-five dollars per head. Marketing them consists of" driving, during the summer, south through Wyoming to the Union Pa- cific ; thence to Chicago by rail. Sheep are worth from two and a half to three dollars per head. The estimates on sheep-raising are that the expense is equal to the wool-product, leaving the increase of flock as profit! Wool is standard at twenty cents per pound. There are no fatal diseases in the Territory to which sheep are subject ; the only af- fliction among them is scab, a curable affection. Can we demonstrate anything plainer to the reader than that a few thousand dollars invested by him who will endure an outdoor life, and a lone one, in stock-raising here, must inevitably make him independent in a few short years? Last winter was the severest within the past fifteen years, and yet the loss of MONTANA. 215 stock was little, if any, above the average loss — from two to three per cent. VAST PASTXTEES, DETAILS OF THE BUSINESS, ETC. There are 38,000,000 acres of grazing-lands, and of these not 10,000,000 have yet been occupied. Heifers produce at two years of age, and the winters are so mild that not one calf in ninety dies. It is unnecessary to put up any hay for stock in winter. It can run out every month in the year. The increase of sheep is one hundred lambs to every hun- dred ewes, and ninety per cent, of the lambs live. The produce of wool is immense, and four to eight pounds of fleece are cut. About 350,000 head of cattle are now owned in Montana, 250,000 head of sheep, 40,000 head of horses, 3000 head of mules, and 10,000 head of hogs. Poultry is very scarce, and turkeys sell for three dollars apiece, chickens from fifty cents to one dollar each. During 1879 over 50,000 head of cattle were driven out of the Territory for beef, and 1,000,000 to 1,500,000 pounds of wool shipped. Sheep yield from thirty to forty per cent, profit, and horses from twenty to thirty per cent. The loss in sheep is one to one and a half per cent., and horses two per cent, per annum. Yearling steers in Montana bring seven to ten dollars ; two-year olds, twelve to twenty dollars ; three-year olds, twenty to twenty-five dollars, and four- year olds, twenty-five to thirty-five dollars. Cows are worth ten to forty dollars, according to their quality. Common sheep are worth two to three dollars, and graded four to five dollars. DAIRYING, POULTRY, ETC. Climate, pasturage, water, and an unequalled market for dairy products combine to render dairying one of the most lucrative pursuits. Cows cost not a dollar for their keeping from one year's end to another, and the product of butter and cheese is by some figured a clear gain, as the increase in stock pays all expenses. The dairymen are numerous in Mon- tana who commenced five or six years ago with rented cows, and no cap- ital but willing hands. To our personal knowledge, a large portion of them are possessed of good ranches, and worth fiom five to ten thousand dollars each, all made by good, honest labor in the corral and milk-house. Over one million pounds of butter and cheese were produced in the Ter- ritory in 1878, and the average prices obtained were forty cents per pound for butter and seventeen cents per pound for cheese. The demands for products of the dairy were never harder to meet than during the past winter, and. those who embark in this industry now can duplicate the ex- 216 THE GREAT WEST. perience of the pioneers with almost absolute certainty. It is almost im- possible to secure eggs or poultry at any price, while no climate could be better for the production of the feathered tribe than this. The average farmer here soon works into the ownership of a nice herd of stock, gets independent of ordinary farm-drudgery, as he calls it, and leaves hundreds of openings for the diversified industry of the Missis- sippi or Missouri Valley. It is these small items of the dairy, the hen- nery, and the truck-patch which hold out the highest inducements to in- dustry, and are yet the most available for poor home-seekers. Many dairymen are going out of the business, simply because their rapidly-in- creasing herds will support them handsomely without work, PEICES OP PEODTJCTS. The following are the prices paid last winter to ranchmen in Montana cities for the offerings of the farm and dairy : Wheat, 2 cents per pound; oats, 2J cents ; hay, $10 to $12 per ton ; potatoes, 1^ cents per pound ; onions, 5 cents ; squashes, 4 cents ; cabbages, 6 cents ; butter, 45 cents ; eggs, 75 to 90 cents per dozen ; turkeys, $3 to $5 each ; chickens, $6 to $7 per dozen. GETTING HOMES, It should be borne in mind that the above prices were obtained for productions of lands which have cost practically nothing but their im- provements; homestead laws apply here as elsewhere. In few of the valleys are one-fourth of the desirable lands taken ; in fact, only 400,000 acres of the vast agricultural area outlined- above are accounted for on the tax-lists. Montana is clearly an empire of itself that offers homes and support for millions of the landless toilers of the crowded East. Nearly all Montana pioneers first built good, comfortable log houses at almost no expense but their own labor. This also applies to fencing and other improvements. Forests being adjacent to nearly all the valleys, the situation remains unchanged to-day, and the man with muscle, and will to exert it, can build for himself a home — better than his forefathers enjoyed in New England — at less expense than in any Eastern or prairie State we know of. Improved farms are very cheap in all the valleys, when their wonderful productiveness and unequalled market are taken in consideration. They can be purchased well fenced, with fair buildings and the necessary ditches and water-rights, for from fifteen to twenty-five dollars per acre. MONTANA. 217 MINING. Mining gold and silver is now, as it ever has been, the chief industry of Montana, though it differs vastly in all particulars from the days when Virginia City and Alder Gulch were notorious. Placer-mining, with the quarrelling, killing, and hanging attending the excitement of rich pans, big pockets, and marvellous finds, has almost entirely given way to quartz-mining, with its attending life, sober, lawful industry, with only the confusion and uproar of the stamp-mill and smelting-furnaces. Mining has indeed been revolutionized, and while the yield of gold has much lessened, it has resolved itself into a legitimate, steady business, through which the Territory is vastly the gainer. With it all there is, within the last year, a reaction in favor of an increased yield, which promises much. In 1877 the amount of gold and silver produced was $3,500,000, compared to $6,700,000 for 1878, and about $8,000,000 this year. Some of the best quartz-mines of the Territory reach the following amounts : The Lexington, near Butte City, last year produced $240,000 ; the Alice Mine, same place, yielded during the summer $45,000 per month ; the Phillipsburg Mine yielded $300,000 last year ; the Penobscot, twenty miles from Helena, yielded $600,000 during the year ;* the Whit- lach Union has had a total yield of $3,500,000. The total yield of the precious metals in Montana during the past six- teen years has been $163,000,000 — more than that of Colorado, Utah, and Idaho combined. About $147,000,000 'of this is gold, placing Mon- tana only second to California in the production of that metal. The fifty-thousand-dollar gold brick of the Penobscot Mine, near Helena, a product of thirty days during the past season, startled readers all over the Union. Ores containing from twenty to sixty per cent, copper, unlimited in quantity, are found in several districts. There have been on exhibition at Helena ores from forty-eight different iron-mines or deposits, running in value from twenty-five to eighty per cent, iron, and representing every conceivable variety of ore. An iron-mountain in Deer Lodge county, larger than the famous deposit of Missouri, averages thirty per cent of that metal. Coal-beds lie within three miles, and an iron-furnace will be built this season. Professor Hayden and others estimate that from fifty to sixty-five thousand square miles of Montana's area are underlaid with coal. Several measures are yielding an excellent quality of fuel. Lead ores, averaging seventy-five per cent, of lead and a proportion of silver, are also frequent. 218 THE GREAT WEST. BUSINESS, WAGES, EXPENSES. The Territory affords fine opportunities for business-men of either large or moderate means who will be content with profits ranging from fifteen to twenty-five per cent, on capital invested. Money is rarely Joaned on any kind of collateral at less than two per cent, per month interest, and from that to three and four per cent. Stock-men claim that they can well afford to borrow money at two per cent, per month, and bankers are of the opinion that the borrower in such cases makes as much as the lender. There has been only one business failure of any magnitude in Montana for years. Business is done generally on a cash basis, and Montana merchants rank among the highest in the country, according to commercial agencies. Montana has never, like some other Western sections, been flooded with labor. The cause is very apparent — from its distance from the railway, and the consequent expense and trouble incurred in getting there. The industrious machinist, carpenter, cook, or bricklayer gets higher wages there than the confidential bookkeeper of a representative Eastern busi- ness-house, and the farm-hand, laborer, or even, herder, who scorns to work morS than ten hours a day, commands more pay than the skilled workman in New York. Mechanics of all kinds command from $4.50 to $7.50 per day. Unskilled labor receives never less than $3 a day. Prices of all necessaries (save meats and flour, which are often cheaper than in the East) are about twenty-five per cent, higher than in the Mid- dle States. Board and lodging at first-class hotels cost from $12 to $16 per week ; at quite comfortable places of less pretension, from $7 to $10. Although 12,000,000 acres of Montana's area are covered with heavy pine forests, the high price of labor makes building material rather ex- pensive. Bough lumber sells at from $20 to $30 per 1000 feet; dressed finished lumber, matched flooring, etc., at fPom $40 to $50. Good two- horse teams can be bought in any of the agricultural districts at from $150 to $225; oxen, from $80 to $100 a yoke. Farming implements, wagons, etc. will average twentyrfive per cent, higher than at points east of the Missouri. ABOUT THE TOWNS. Helena, the capital of Montana, is located in the central part of the Territory, and has a population of 5000 inhabitants. It has many fine public and private buildings, and employs a cash capital of $5,000,000. Virginia is in the southern part of the Territory, and has a population of MONTANA. 219 1500. It is near the famous Alder Gulch, which still produces annually $500,000 in gold. Butte is a beautiful town, and already second to Htlena. It has a population of 3000 souls. Bozeman is at the head of the famous Gallatin Valley, and is surrounded by the richest farming- region in the West. It has a population of 1000, and is rapidly increas- ing. Deer Lodge, Missoula, Bannack, Benton, Radersburg, Vestal, and Phillipsburg are also fine and growing towns. The Yellowstone Valley is in Montana, and has two towns — Miles City and Sherman. The popu- lation of the Territory is about 40,000 ; assessed valuation, $14,000,000. Yellowstone Valley is capable of sustaining twenty-five thousand farmers, and the settlements have just been founded. We have ridden up and down the valley several times, and its upper portion has few superiors in the United States. Montana has indeed a wonderful future before it, and we know of no place where the farmer, manufacturer, or professional man can enter with a greater assurance of prosperity. Telegraph-lines have already been established to many parts of the Territory, and there are four daily and ten weekly papers, giving all the news. The isolation of the Territory has heretofore prevented ma'ny persons from seeking it, but now that this rich and unknown land is connected with the outside world by railroads, it will soon be filled up and become a prosperous commonwealth. EAILEOADS. Montana has always been far off — in miles, in time, in facilities for getting there — and it is not hard to comprehend that, rich as it is in re- sources, it is almost an outside world. At present, home-seekers can reach its boundary by rail. There is only one route available from all points and the year round — ^by the Union Pacific Railroad to Ogden, Utah, and north over the Utah and Northern Railway, 275 miles, to Beaver Cafion, its present terminus ; thence to various points by daily stage. One can thus go to within a thirty-six-hour stage-ride of most Montana towns, and the Utah and Northern will imdoubtedly be extended farther north- ward in the spring. The time from Omaha to Helena at present is less than five days, and the fare very reasonable, considering the distance. MONTANA POINTS are reached by Gilmer, Salisbury & Co.'s daily stages in from twenty- three to forty hours from Beaver Caflon. The rates of fare now in force from Omaha to the most important places in Montana are given below, 220 THE GREAT WEST. with the distances and stage-time from Beaver Cafion, present terminus of the Utah and Northern Railway : First Second ■p„-„..„t Distance, Stage-time, Class. Class, ■^'"'g'o.ni. ^^^^^_ ^^^^^_ Lovell's $100 $75 $45 118 23 Virginia City 100 75 45 193 28 Butte 100 75 45 208 82 Deer Lodge 100 75 45 235 38 Helena 100 75 45 245 40 Holders of second-class and emigrant tickets, vid Gilmer, Salisbury & Co.'s line, will be carried from the railway terminus to destination in covered mail-wagons — one hundred pounds of baggage free by rail ; forty pounds free by stage, on first-class ; fifty pounds free by wagon, on second- class and emigrant; extra baggage on stage- and wagon-lines, fifteen cents per pound. Stages and wagons run daily. The travel to Montana is increasing wonderfully, and the through rail- route vid Omaha, Ogden, and the Utah Northern Railway, carries it, as it deserves to. In addition to the already splendid equipment of the stage-line between the Utah and Northern terminus and Montana cities, coaches that will carry thirty passengers have been ordered by Gilmer & Salisbury to run between those points, and will be put on the route this winter. B. F. POTTS, GOVEENOE OF MONTANA, SAYS: " The farmer, the miner, the -merchant, the tradesman, and in short all classes of our people, are prosperous and contented. Capital yields satis- factory returns, and labor is liberally rewarded. " The Utah Northern Railroad, a branch of the Union Pacific Rail- road, has been built into the Territory during the present year. The completion of this road will enable the landless citizens of the Eastern States to reach Montana, where homes can be obtained more advantageously than in almost any section of the country." MONTANA. 221 MINEKAL EESOUKCES. BY Z. L. WHITE. THE chief resources of Montana's mineral wealth have heretofore been her rich placers, which are estimated to have yielded about one hundred and forty million dollars' worth of gold-dust. The placer-ground in most of the gulches was originally worked over with pick and shovel at a time when wages were high and no one could afford to wash the gravel with very great care. Now much of this old ground has fallen into the hands of men who are able to spend large sums in new water- ditches and bed-rock flumes, enabling them by means of Chinese labor to work over by the hydraulic process and ground-sluicing not only the old tailings, but also the " lean " ground that was left before. Besides this, some of the old gulches have never been worked out, and new ones are discovered almost every year. During the past summer there has been a stampede to the Judith Basin, where there are unquestionably good placers. The eastern portion of the Territory, which has only recently been opened, has never been thoroughly prospected, and new diggings will undoubtedly be discovered in many parts of it. I am therefore of opinion that although the product of the placers of Montana will not in the future be as great as it was in the first few seasons after the discovery of gold here, it will continue to be several millions a year for a long time to come. The gold quartz-mines of this Territory which have been developed are not very numerous, and have been operated with varying degrees of success. The Whitlach Union Min^e, near Helena, after yielding three or four millions, has suspended. There is a divisioii of opinion as to the cause of its present condition, some holding that it is due to bad mining and the failure to open new ground while the old was being stripped, and others declaring that the vein has been worked out. The Atlantic Cable, in Deer Lodge county, has been, and perhaps still is, a very promising mine, but has been involved in litigation for ten years, which has not only sucked the life-blood out of it, but prevented the investment of capital in its proper development. The mines in the Silver Creek dis- trict (the Lexington, Belmont, Hickey, and others) are excellent proper- ties, now producing about fifty thousand dollars a month, with a prob- ability of an increase. The Lexington, the largest and best known in 222 THE GREAT WEST. the district, will probably begin to pay dividends at the opening of the new year, but whether it will be able to pay high rates of interest on the enormous price at which the mine was bought and the cost of the expen- sive improvements that have been necessary, remains to be proved. I have no doubt that its monthly product will be a large and increasing one. I think there are some excellent openings for the investment of capital in gold quartz-mines in Montana, but in order to ensure success it ought to be associated with the best and most experienced mining skill. New leads are constantly being discovered, and some of them will undoubtedly be developed into good mines. The two successful silver camps in this Territory to-day are Butte and Glendale. The former, I believe, will offer unrivalled inducements to capital and enterprise, and I look to see it become one of the " boom- ing " camps of the West. At Phillipsburg and Wickes preparations are being made for the mining and milling of large quantities of ore, and the former of these camps is now sending some silver bars to market. There are hundreds of silver-mines in Montana that are only waiting for the advent of capital and cheap transportation to be converted into first- class properties. It is unnecessary to warn Eastern people against wild-cat schemes. No man or company can afford to expend capital in the purchase and develop- ment of a mine and in the erection of reduction- works until the property has been examined and reported favorably upon by a competent, disinter- ested expert. A disregard of this fundamental rule has been the cause of more than one disastrous failure in Montana. A wild-cat scheme cannot be foisted upon capitalists if proper precautions are taken ; if they are neglected, mining operations become lotteries in which one may draw a prize, but is very much more likely to get a blank. The reduction of silver ores is a process requiring a knowledge of chemistry and metallurgy, and practical experience in the application of scientific principles to the treatment of different kinds of rock. The failure of the Montana Company at Jefferson a year ago was confessedly due to a neglect to observe this axiomatic rule. Other silver-mining enterprises in this Territory have failed for the same reason. The losses incurred in these cases will probably serve as a warning to those who inaugurate new enterprises in the future. Mining as a legitimate business has been brought into discredit in Montana, as in other Territories, by the dishonest management of some officers and superintendents. Mining is no longer a legitimate enterprise, but an outrageous swindle, when it is managed for the purpose of raising MONTANA. 223 or depressing the value of the stock in the interest of a clique of specu- lators ; and yet too many concerns are operated in this way. If it is desired to bull the stock, it is very easy for a superintendent to strip his mine of the ore that has been made accessible by previous developments work, thus greatly increasing the product for a few months without increasing the working expenses. In the same way a cotton-manufac- turer in New England might divide among his stockholders all the money he received for his fabrics, without retaining any with which to purchase fresh material or to keep his machinery in order. A time would soon come when he would either have to make an asse,ssment upon his stockholders, borrow money, or stop, but in the mean time, if his method was kept secret, the price of his stock might be enormously advanced. On the other hand, a superintendent may keep his entire force at work for months in sinking new shafts and driving new levels without pro- ducing ore, until a number of dividends have been passed and the stock is greatly depreciated, although the mine may be growing better and better all the time. It is as though the manager of the cotton-mill should go on month after month spending his entire receipts for new material, secretly piling it up in his storehouse, and reporting no profits. I could name good mines in Montana that have been ruined by this sort of management. For a few months they have paid large dividends, and the stockholders have supposed they owned a bonanza. But all at once production has stopped, there has been no ore in sight, and the mine must close unless money to pay current expenses is obtained either by an assessment or by a loan. Honest people will do well to give a wide berth to any company whose stock is suspected of being the football of speculators. The richest bonanza in the country cannot make such an enterprise a safe one to invest in. The revival of popular interest in gold- and silver-mining has caused the owners of undeveloped properties, and even investors in the East, to have an exaggerated estimate of the value of mines and pros- pect-holes. It is an axiom among conservative miners that no mine is worth more than the actual value of the ore in sight. Even then th6 purchaser takes the risk of finding enough new ore to pay for the expense of taking it out and the interest on his money invested. This is a pretty safe rule to be governed by in making purchases. Thoroughly-developed mines on strong, well-defined veins are undoubtedly in many instances worth much more than the value of the ore in sight, but in a new mine the man who buys ore in posse gambles on an uncertainty. - 224 THE GREAT WEST. I do not wish, by anything I have said, to dLsparage the mines of Montana or throw discredit upon their management. I believe the mineral resources of this Territory to be wonderful in their extent and richness, and that the failures in mining enterprises have generally been due to lack of capital, and experience and the isolation heretofore of Montana from the remainder of the country, rather than to dishonesty. At the same time, I have written what I believe every man in the East who thinks of investing in mines ought to know, and what he is not likely to learn except by spending a season among mines and miners, as I have done. STOCK-RAISING IN MONTANA. MONTANA is the best grazing-country in the world. I know that this is a bold assertion to make, but after seeing something during the past summer of the best cattle-ranges of Kansas, Nebraska, Colorado, Dakota, Wyoming, and Utah, which States and Territories furnish so large a proportion of the beef consumed in this country, and talking with stock-men, army officers, and others whose acquaintance with the West is far more extensive than my own, and whose experience gives to their opinion great weight, I am certain that it is not an exaggeration. There may be portions of South America where cattle, sheep, and horses can be raised at less expense than in Montana, but there certainly is no part of the United States where the same grade of animals, ready for market, cost the ranchmen less money, while the price which they command is many times greater than in any of the Spanish-American republics, and but very little below that obtained in the less remote States and Territories this side of the Missouri River. ^ No one can spend a week in any part of Montana without hearing some of the most marvellous reports about the profits that have been realized during the last few years in the business of stock-raising in this Territory. These stories, many of which have reached the East recently in enthusiastic newspaper letters and pamphlets published in the interest of Western railroad companies, are true, so far as I have been able to verify them ; but while, as a rule, they relate only to the exceptionally successful ventures — -just as the wonderful yield of a bonanza-mine in a MONTANA. 225 camp is heralded from one end of the country to the other, while the hundred prospect-holes which have been failures are never heard of — the unvarnished truth about the average profits of the business will seem al- most incredible to Eastern people. It is only now and then that a herd of cattle, sheep, or horses yields a net income of from forty to sixty, or even one hundred, per cent, per annum ; but I doubt if there is a single instance in which, taking a series of years together, the profits on stock- raising have not been from twenty to thirty per cent, on the original in- vestment; and that, too, in cases where the animals have suffered severely from unusual cold and snow in the winter or from disease. In the first place, the grass is better and more abundant than in any other of the Western States and Territories. In previous pages I have mentioned the fact that the bunch-grass grows not only all over the val- leys and the benches, but on the foot-hills, and even on many of the mountains themselves. The supply of it is inexhaustible. Even in the older settled portions of the Territory, where improved farms are frequent, often adjoining each other in the valleys, the cattle, sheep, and horses do not begin to eat down the grass, and although the ranges for several miles on each side of the valleys may be nominally taken up, they are still ca- pable of sustaining many times as many animals as now graze upon them. No one who intends to raise stock on a large scale or to make that his chief business would think of driving his animals to these particular hills near the settlements, but the farmers whose flocks and herds are now feeding upon them, and who want their cattle near at home, may increase the size of their herds almost indefinitely before there will be any scarcity of feed. But it is not in those portions of the Territory that have been longest settled that stock-raising is most profitable. The valley of the Yellow- stone River from near the National Park to its mouth is six hundred and fifty miles long, and on an average from ten to twelve miles wide. All of this land can be easily irrigated and placed under cultivation. Hun- dreds of families have settled there this year. On either side for almost the entire length of this valley are benches, foot-hills, and prairies cov- ered with bunch-grass and amply watered by small streams. Nor is this all. There flow into the Yellowstone from the south the Powder River, the Tongue River, Big Horn River, Clarke's Fork, and almost innumer- able smaller streams, the valley of each of which is from thirty to one hundred miles in length, and nearly every one afibrds as good pasturage as is to be found in the world. Nearly the whole of this country has been inaccessible until within the last eighteen months or two years, and 15 226 THE GREAT WEST. the tide of immigration has only just begun to flow in. A few herds of cattle have been driven into the valleys of all the streams I have named, but it is safe to say that there is not one steer there to-day where there is feed for a thousand. Even the extensive ranges that are more accessible are far from being occupied. Thousands of cattle have been driven this summer to the Sun River country and to the sparsely-settled sections north and north-east of Helena, and even there the ranges are so large that in riding over them one would have difficulty, except for the trails, to select the lands upon which the cattle have been feeding from those which have not been touched. I should not dare to make an estimate of the number of ani- mals that Montana can sustain, but I am perfectly safe in saying that hundreds can graze in her valleys and on her hills where now there is one, and that it will be many years before it will be possible for the stock to begin to be crowded. I said that the grass in this Territory is better than it is elsewhere. It is bunch-grass, that grows from one to two or three feet high. In most places the bunches stand close together, and cure early in the summer. In August and after, until the next spring, the grass has a color some- what similar to that of ripe wheat, although the yellow is not quite as bright, and the country looks like one vast field of grain nearly ready for the harvest. This grass is wonderfully sweet and nutritious. Cattle fatten upon it quicker and keep in better condition than those which feed on the blue-grass of Kentucky and South-western Virginia or the buifalo- grass of Nebraska and Colorado. The beef is remarkably sweet, tender, and juicy, as I can testify from having eaten of it every day for more than a month. The proprietor of the two most popular hotels in Salt Lake City also told me that Montana beef, of which he had occasionally obtained some, was far superior to any other he could get, and equal in quality to the best stall-fed beef in the East. The chief fault I have heard found with it both here and in Salt Lake has been that in summer it is too fat. In winter even cattle that are on sheltered ranges keep in excellent condition. Very few of the stock-men of Montana make any provisions for feed- ing their cattle in the winter, and there is no herding in the summer, as in Nebraska, Colorado, and Wyoming. Old cattle-owners say that a herd that is fed occasionally when a heavy storm comes will not winter as well as one that is not fed. The cattle which receive hay once are likely to remain in the immediate vicinity of the ranch, even after the feed there has become short, and if driven away will return. As it is impossible MONTANA. 227 to feed them all the time, they grow lean, while if they stay out on the range, where the grazing is better, they will keep in good condition. The grass is stiff, and on the hillsides is rarely entirely covered with snow. The loss from exposure is said to be not more than one or two per cent. Whether there is force in this reasoning or not, it is certain that some of the most careful and most successful stock-men are begin- ning to put up hay as a precaution against severe cold and deep snows. They say that the cost of the hay, which is cut with- machines in the natural meadows along the river-bottoms, is only from fifty cents to one dollar a ton, and that in the long run, by being prepared to feed their cattle a little in the winter if it is necessary, they save more than enough animals that would otherwise perish to pay for their trouble and expense. The customary way of managing a herd of cattle in Montana is simply to brand them and turn them out upon the range. Some stock-owners give no more attention to their cattle until the next spring, when they round them up, brand the calves, select those they intend to sell, and turn the remainder out again. Under this careless management they are sure to lose some steers, which stray away or are stolen. The more care- ful managers employ oile man for every fifteen hundred or two thousand head of cattle, whose duty it is to ride about the outskirts of the range, follow any trails leading away and drive the cattle back, and to go among neighboring herds, if there are any, looking for stray animals and driving them home. At the spring round-up a few extra men have to be em- ployed for .several weeks. In starting a new herd, cows, bulls, and yearlings are bought. The older cattle of ordinary grade (they are all American — no long-horned Texahs) cost from fifteen to twenty-five dollars a head, the calves under one year old running with the herd not being counted. Yearlings may be obtained for from five to seven dollars each. The average cost of raising a steer, not counting interest on capital invested, is from sixty cents to one dollar a year, so that a four-year-old steer raised from a calf and ready for market costs about four dollars. He is worth, on the ranch, about twenty dollars, and if driven to Fort Benton or to the rail- road in Wyoming, at least twenty-five dollars. A herd consisting of yearlings, cows, and bulls will have no steers ready for the market in less than two or three years. Taking into account the loss of interest on capital invested before returns are received, all expenses, and ordinary losses, the average profit of raising cattle in Montana during the last few years has been at least thirty per cent, per annum. Some well-informed cattle-men estimate it at forty to forty-five per cent. 228 THE GREAT WEST. A large and increasing percentage of the cattle and sheep of Montana are owned bv persons who do not manage them themselves, and some of ■whom do not reside in this Territory. Xearly all the leading merchants and bankers of Helena own interests in herds of stock, and lawyers, doctors, and Federal officers are following their example, and investing either their own money or that of their friends in the East in cattle, sheep, or hors«. A man who desires to invest in stock, and who has not the time or inclination to attend to the business himself, takes as an associate some man of experience and int^rity, but destitute of capital (of whom there are many in Montana), and gives him entire charge of the herd. This man selects the range, cuts the hay that is necessary, moves the animals when necessary, attends to the roimding-np, and drives those that are sold to the place of delivery, paying all expenses and being entirely responsible for the management of the business. For this he receives one-half of the increase of the herd, the man who furnishes the capital taking the other half. The returns which capitalists obtain on their money invested in this plan in a herd of cattle are never less than fifteen per cent, in a flock of sheep twenty- per cent, and upward, and in a band of horses much greater than in either. • A new plan for dividing the profits in this business between capitalists and managers has lately been suggested, and will probably be tried next year. The manager is to take the heid purchased with the money fur- nished by his partners — ^the latter retaining the title to the animals — find a suitable range, and pay all the expenses of the enterprise, until from the profits he has paid back to the investor a sum of money equal to that which he at first put in. Then the manager is to become the owner of one-third of the business and to receive thereafter one-third of the profits, the expenses being paid out of the receipts. It is proposed by responsible men in ^lontana to organize stock companies in tlie East for the purpose of conducting the cattle- and sheep-raising business on this plan, and, with ordinary precautions in the selection of a proper man to mana2:e such an enterprise I can imagine no undertaking in which the security can be better or the certainty of large profits greater. The management of sheep is of com-se different from that of cattle, A flock of sheep containing one thousand and upward, in good condition and free from disease, may be bought here this season for thi-ee to three dollars and a quarter a head. They must be herded summer and winter in sep- arate flocks of not more than two or three thousand each, corralled every night, and guarded against the depredations of dogs and wild animals. Some hay must be provided with which to feed them when there are deep MONTANA. 229 snows, and sheds ought to be erected to protect them from the most severe storms. Cattle and sheep cannot live together on the same range. The latter not only eat down the grass so closely that nothing is left for the cattle, but they also leave an odor which is very offensive to steers. Although the cost of managing sheep is greater than that of handling cattle, the returns are quicker and larger. While a herd of young cattle begins to yield an income only at the expiration of three years, sheep yield a crop of wool the first summer after they are driven upon a range, and the increase of the flock is much greater than that of cattle, being from seventy-five to one hundred per cent, a year. The wool is of good quality, free from burrs, not washed, and brings a good price on the ranch, the competition between buyers sent out here from Eastern cities to obtain it being very great. Many thousand sheep have been driven into this Territory this year from California, Oregon, and Washington Territory, and every flock that has arrived has been gobbled up by men eager to increase their flocks or to start new ones. It is not my purpose to mislead any reader by reciting the cases in which unusual profits have been realized in the business of stock-raising, but it may be interesting to know what has occasionally been done in cases where all the conditions have been favorable, just as we like to hear of the rich refairns which bonanza-mines sometimes give. The following is an example : Judge Davenport of this Territory four years ago last July purchased one thousand ewes, which cost him in the nisighborhood of three thousand dollars. These he put in charge of a young man, who was to take them on a range, care for them, pay all the expenses of the flock, and to receive as his share one-half the wool produced and one- half the increase of the flock. At the end of four years a settlement was to be made, and Judge Davenport was then to receive back one thousand of the best ewes which the flock contained. The settlement was made last July. In the mean time, Judge Davenport had received for his share of the proceeds of the wool |6500, and for his share of the increase $8000. The profits of his investment of $3000 for four years were, therefore, $14,500, or $3626 (or 121f per cent.) a year! During the same year other men made only fifty or sixty per cent, on their sheep, and some, who from inexperience or bad fortune met with heavy losses, perhaps not more than twenty-five per cent. ; but I have never heard of a single instance in which there has been an absolute loss in a period of, say, three or four years. One man, driving a large flock of sheep from the South a year or two ago, was caught by the winter in an unfavorable place and lost one-half or two-thirds of his flock, but at the end of three 230 THE GREAT WEST. years, when he came to balance his books, he found that the remnant of his flock had done so well that his profits had been about twenty-five per cent, a year on his original investment. The number of cattle now in the Territory is estimated at 500,000, and the number of sheep 250,000. The wool-clip this year was about 900,000 or 1,000,000 pounds, which sold, on an average, for twenty cents a pound. I have seen no estimate of the number of horses in Mon- tana, but I think there are only a few very large bands. Horses will endure the cold weather and get at the grass if ft is covered by snow much better than cattle, but they are so much more valuable that most owners prefer to have their bands fenced in or herded pretty carefully. The best horse-farms are in valleys ten or twelve miles long, on the sides of which the foot-hills extend up to high mountains. By building a fence across each end of such a valley the horses are prevented from stray- ing from the range. The profits upon the rearing of horses and mules are very great, and there is a ready market for all that are offered. What I have written in this paper will undoubtedly prompt some one to ask, " Can any one from the East, with a capital of a few thousand dollars, go to Montana and engage successfully in the business of stock- raising ?" No, unless he supplements his capital with experience, either of his own or of some one with whom he associates himself. A man reared in an Eastern city or town to professional, mercantile, or manufac- turing pursuits would be as helpless with a herd of several thousand head of stock on his hands as a Western ranchman would be in a cotton- mill. But with an experienced partner even a city man would soon learn the business. The first thing to be done in entering the stock business is to select a good range, and to do this requires a pretty thorough knowledge of the country and of what constitutes a desirable location. Foot-hills from which the snow will be likely to blow off, exposing the bunch-grass, good water, cafions in which the animals may seek shelter from storms, and natural meadows if hay is to be cut, are all considered essential. The greater the distance from other ranges, the less trouble there will be from the mixture of the animals of other herds and the less the expense of rounding-up. Of course the ranges are all government land, to which no title can be obtained, but the right of the first occupant to the land he uses is universally recognized. Cattle and sheep are subject to diseases which the herder must know how to treat. Young cattle, yearlings, and two-year-old steers have suf- fered severely in some parts of Montana this year from the " black leg," MONTANA. 231 a coDgestive disease, which has destroyed from one to two or three per cent, of the flocks on some ranges, and greatly alarmed the owners. The cause of this distemper is not known, but it has proved fatal in every case. The disease known as scab has been brought into Montana by sheep from California, Oregon, and Washington Territory, and it has been spread among many of the flocks that before were healthy. This disease can be cured by proper treatment, but the losses from it have been considerable. In conclusion, I can only repeat what I have already said — ^that Mon- tana is the best grazing-country in the United States ; that stock-raising here, when intelligently conducted, is a safer business and more profitable than any other I know of; and that more people are going into the busi- ness and investing more capital in it than are turning their attention to any other of the industries of the Territory. HINTS TO MEN WITHOUT CAPITAL. THERE are room enough and work enough in Montana for all the people who may desire to make it their home for years to come, and who are willing at the same time to forego for a season a few of the luxuries which make life in the older States so attractive, and to adapt themselves meanwhile to the conditions which they will find existing here. I have written very briefly about the grazing and agricultural resources of the Territory. They are simply wonderful, and in their development offer to thousands of people from the East the opportunities for gaining a competency, if not a fortune. The remoteness of Montana, not only from the Eastern States, but from the lines of railroad which connect the other far Western States and Territories with them, has thus far been a barrier against a large immigration into its beautiful valleys. Men will go to the ends of the earth in search of the precious metals ; they will deny themselves all the comforts of life, defy savages and wild beasts, and face dangers before which almost any other class of people would turn back. But the farmer who intends to make his home on the land which he reclaims and cultivates (the prospector or miner is only a bird of passage, who always calls his home " a camp " even after it has become a solid, permanent town) must have a cei-tain degree of security for himself and family and a market for his surplus products. 232 THE GREAT WEST. The farmers of Montana have, as a rule, been hardy fellows, fond of adventure, who have established themselves near the military posts and successful mining camps or along the great lines of travel, and very many of them have lived as the miners and prospectors do, without families or the comforts and refinements which the presence of women only can give. All this is now changing. People are hearing about the wonderful nat- ural resources of the Territory, and are seeking new homes here, intending to make Montana their permanent residence. Any one who has capital needs no suggestion in regard to settlement in these valleys of the Rocky Mountains. He has the means of learning where the best lands are, and how to obtain them, and he can make a personal inspection of the coun- try, and, if he desii:es, purchase an improved farm. With a poor man it is different, and it is for the benefit of this class that I d&sire to give a few hints. The cost of reaching Helena from any of the Atlantic States is a little more than one hundred dollars. To make the journey for this sum one must travel in emigrant-trains to the terminus of the railroad, and thence to Helena by the " fast freight " line ; that is, in ordinary farm-wagons with spring seats and canvas covers. The journey from New York will occupy between two and three weeks. In addition to the fare, the trav- eller has, of course, to supply his own provisions, and unless he sleeps out of doors in his blankets his bed will cost him fifty cents a night on the wagon-journey. The expense of reaching Montana by first-class trains and in the stage-coaches will of course be considerably greater. A man who comes to this Territory early in the spring will have no trouble in securing employment on a ranche at the rate of from thirty to forty dollars a month and board. One season's work on a Montana farm gives a stranger an opportunity to become acquainted with the methods of cultivation prevalent here, and to look about for a place on which to settle. I have seen several men who have come here from the East, leav- ing their families at their old homes ; they found immediate employment, have taken up during the first season a quarter section of land, and put up a house for the shelter of their wives and children on their arrival. I met on the stage-road one day a family consisting of a mother, a daugh- ter about fourteen years of age, and three smaller children, who were making the journey alone from one of the counties of Central New York to the Jefferson Valley in this Territory. The lady told me that her husl)and and son had come to Montana last year, and had found employ- ment on neighboring ranches. In the spring they sent for the eldest daughter, who had, since her arrival, been engaged in teaching school, MONTANA. 233 and last month the remainder of the family when I met them were on their way to their new home. When a man has become sufficiently established on his new ranche to have raised one crop of wheat or oats and to have got a few head of stock, he need have no fear for the future. Patient industry brings swift and great rewards. In going to PhillipsbuTg a week or two ago I rode twen- ty-five miles with a Scotchman who has a farm in Deer Lodge county, near New Chicago. He told me that he had taken up one hundred and sixty acres of land about four years ago. At the time he had no capital, but was master of a good trade — that of a carpenter — and had two sons old enough to assist in the farm-work. The old gentleman had worked several months each year at his trade, earning five dollars a day, " And," he said, " I hardly know how it came about, but we have to-day a finely- improved farm, a good house, about fifty head of cattle, and seven good horses, five of them good Americans three years old. I have spent very ■ little money for stock, and all that we have is the result of only four yeare' work. We sell enough butter, chickens, and eggs to pay our gro- cery-bills, and are now saving some money, besides what goes to improve our place. I have been twenty years in the Western States, and I have never seen a place where a poor man can get a start as easily as here." A stranger who desires to work into the stock-raising business will find in Montana opportunities to do so, even though he may not have capital to invest in sheep or cattle. One who has been accustomed to the care of stock in other sections of the coimtry will, of course, get better wages on the ranges than one who is totally unacquaiuted with the bus- iness ; but so many new herds of cattle and sheep will be driven out upon new ranges next spring that any one who is willing to work and anxious to learn will have no difficulty in obtaining employment. In Colorado and Nebraska a man working by the month with a " cord out- fit," as a herd is called there, has the privilege of having a few cattle of his own on his employer's range, and the same arrangement could un- doubtedly be made here. The profits of stock-raising have been so great iu Montana that almost all business-men here, as well as many who have never seen the Territory, are anxious to invest some money in it, while many of them do not desire to manage the flocks or herds themselves. There are, therefore, mimerous opportunities for responsible men, known to be experienced in the care of sheep and cattle and honest in their deal- ings, to become partners in the stock-raising business with the investment of little or no capital. If one man furnishes all the money and another takes the entire care and management of a stock of sheep or cattle, it is 234 THE GREAT WEST. customary to divide the annual increase and the wool that is cut from the sheep equally between the two. Some of the most successful stock-men in Montana have got their start by taking flocks and herds to manage on such terms as I have described. Of course, farming and stock-raising in Montana are subject to the same vicissitudes which sometimes cause failure elsewhere. A farm that is properly irrigated will never suffer from drouth, but the grasshoppers may sometimes injure or destroy the crops, and other noxious insects may appear, as they do in the older States. So, also, disease may appear among animals, or some of them may perish during an unusually severe winter ; but these are risks which have to be taken everywhere, and are no greater here than in any other new country. Skilled mechanics are in great demand in Montana. Carpenters earn five dollars a day, and many more could have found employment in He- lena and about the principal mining camps during the past summer if they had been here. I have known of several instances in which important building operations were delayed because carpenters could not be obtained. In Helena and Butte bricklayers and stonemasons have no trouble in find- ing employment, but in most of the other towns the buildings are all of wood. Good blacksmiths find plenty of work, not only in the towns, but at the mines, every one of which is obliged to employ several when in operation. Almost all of the machinery in Montana is built in the East, so that there is as yet little work here for moulders and machinists. A few engineers are needed at every large mine, and one or two machinists are employed to make small repairs on pumps, hoisting-machinery, and mill-work. Skilled miners earn from three to four dollars a day, the latter price being paid only to those who work in wet or dangerous places; and common, unskilled laborers are paid from two and a half to three dollars a day. Nobody is idle who is willing to work, and tramps and beggars are unknown. Perhaps there is no want that is as keenly felt in Montana as that of. good domestic help. A few years ago good house-servants, cooks, were paid sixty dollars per mdnth, and even now a white girl who knows how to do housework receives from twenty-five to forty dollars a month — the former of these rates being paid only to servants of a very inferior kind. Both in Helena and Butte it is generally impossible to obtain white ser- vants at any price, and the greater part of the housework in families is perform.ed by Chinamen, who receive, on an average, about thirty dollars a month. The early settlers of Montana were exclusively men who were hunting for gold, and never expected to remain in the Territory after the MONTANA. 235 mines first discovered failed to pay. "When the population began to be- come permanent the few who had families sent for them, but the majority were unmarried men who had no families. For the last fifteen years, too, Montana has been so remote that comparatively few women have come here expecting to go out to service in families, and those who have come have almost invariably been married within a few months after their arrival. Some of the experiences of young women who have been brought to Montana in the capacity of servants have been very amusing. A lady who brought a maid from Chicago two or three years ago' told me that the young woman had five offers of marriage while travelling a week on a stage-coach between Corinne and Helena, part of them from passengers and part from stage-drivers. I have no doubt that several hundred good servants could now find employment in Helena, Butte, and other towns at the wages I have named, and that the majority of them would find good husbands within a year if they wished to marry. The professions seem generally to be well filled in Montana, and clerk- ships in stores or offices are not very plenty. I have heard less about mining litigation in Montana than in any other place where mining opera- tions are going on, and the lawyers, while in most cases making a living, are probably able to attend to all the business that offers. A few good physicians might make an opening for themselves here, and as the popu- lation increases their practice would of course become greater. Montana has many good schools, and tl^y are generally in the hands of competent teachers, who are engaged in the States. There are frequent changes among the lady-teachers, because a large proportion of the whole corps in the Territory is married every year. The merchants of Montana are, almost without exception, men of con- siderable capital. Until this ye^r no one else could do business here, be- cause the freight-lines were all closed in the winter, and it was necessary to carry a stock of goods large enough to last about nine months. Now that the Utah and Northern Railroad will be opened across the mountains next month, goods can be imported every month in the year, but as freights will always be higher during the season when the Missouri River is closed, merchants will continue to purchase goods during the spring and summer in sufficient quantities to last until the next summer, and will be able to undersell those who purchase in smaller quantities and pay higher rates for transportation. The tide of immigration into this Territory has already received a new impetus, and next year a large increase of population is expected. 236 THE GREAT WEST. DISTANCES, TIME, FAKE, BAGGAGE ALLOWED, EXTEA BAGGAGE, AND HOUSEHOLD GOODS. FAKES FEOM OMAHA. THE fares to Lovell's, Yirginia City, Butte, Deer Lodge, Helena, and other central points in Montana are as follows : First class, $100 ; second class, $75 ; emigrant, $45. On the cars children five years old and under twelve, half fare in any of these classes ; under five years old, free ; on stages children under twelve and over three years old, half fare ; under three, free. Passengers holding first-class tickets will be carried from the Utah and Northern Railway terminus by Gilmer, Salisbury & Co.'s stage-line with 40 pounds of baggage free. Holders of second-class and emigrant tickets will be "transported from the Utah and North- ern terminus by Gilmer, Salisbury & Co.'s line of covered wagons — car- rying the United States mail — and will be allowed 50 pounds of bag- gage free. EXTEA BAGGAGE AND HOUSEHOLD GOODS. Extra baggage by stage or mail-wagon from the terminus of the Utah and Northern Railway to points named above will be charged fifteen cents per pound, but it may be forwarded ]^ freight-wagons at a cost of from two to three cents, its transportation in this way, how'^er, requiring considerably more time. Freights on household goods {well boxed) from Omaha to Utah and Northern Railway terminus, $4.05 per hundred pounds, or double that rate if carried in trunks. Freight rates from the railway terminus to Montana points above named are from $1.50 to $2.50 per hundred pounds. Stages run day and night, making connections with Utah and Northern Railway trains daily. Mail-wagons also run daily. First-class eating- stations along the stage-road furnish meals or lunch at reasonable rates. Telegraphic stations are established at frequent intervals along the stage- road. All streams are well bridged, and the entire equipment of the stage-line is the finest in the West. The Utah and Northern Railway, completed to Beaver Canon, Idaho, 274 miles north of Ogden, in Sep- tember, 1879, is being rapidly extended northward into Montana. Unless winter opens unusually early, it will no doubt reach Red Rock, Montana, 30 miles north of Beaver Cafion, in December, 1879, reducing stage- MONTANA. 237 travel to the more distant points named below to thirty-six hours. Fol- lowing are the distances and the stage-time from Beaver Caflon to the prin- cipal points, as well as rates of fare from Omaha in force November 1, 1879: First Class. Second Class. Emierant. Distance. Stage-time. Lovell's, Montana, $100 $75 $45 118 miles. 23 hours. Virginia City, " 100 75 45 193 " 28 '• Butte, 100 75 45 208 " 32 " Deer Lodge, " 100 75 45 235 " 38 " Helena, 100 75 45 245 " 40 " DISTANCES AND FAEES IN THE TEEEITOEY. The following are carefully-compiled tables of distances from Helena, Deer Lodge, and other points to all stations in Montana, with stage-fares in effect in June, 1879. Stages on nearly all routes run daily, making an average of over one hundred miles in twenty-four hours : RODTB TO Utah and Northern Railway— (jamer Total in 1875 . . Total in 1878 . . 207,376 274,450 $9,875,245.12 16,467,000.00 24,964 40,564 $1,622,660.00 3,042,300.00 225,028 286,241 $5,747,215.12 7,442,266.00 Increase . . . 67,074 $6,591,754.88 15,600 $1,419,640.00 61,213 $1,695,050.88 Per cent, of in- 1 crease in 5 yrs. J 32.34 54.47 57.20 Otheh Cattle. Sheep. Swine. to .1= 1 6 > o S a fe5 1 > 1 a i "d Total in 1875 . . Total in 1878 . . 478,295 586,002 $9,039,775.50 12,423,242.40 106,224 243,760 $247,501.92 731,280.00 292,658 1,195,044 $2,077,871.80 6,094,724.40 Increase . . . 107,707 $3,383,466.90 137,536 $483,778.08 902,386 $4,016,852.60 Per cent, of in- \ crease in 5 yrs. / 22.52 129.48 308.34 In the eleven years from 1866 to 1876 the following changes occurred in the positions of the States: New York, first in 1866, and also first in 1876 ; Ohio, from second to third ; Pennsylvania, third to fourth ; Illinois, fourth to second ; Indiana, fifth to sixth ; Iowa, sixth to fifth ; Michigan, seventh to ninth ; Wisconsin, eighth to eleventh ; Kentucky, ninth to twelfth ; Missouri, tenth to eighth ; Tennessee, eleventh to thir- teenth; Texas, twelfth to seventh; Virginia, thirteenth to sixteenth; Georgia, fourteenth to fifteenth ; New Jersey, fifteenth to twenty-second ; Alabama, sixteenth to twenty-first; Vermont, seventeenth to twenty- seventh ; Mississippi, eighteenth and eighteenth ; North Carolina, nine- 268 THE GREAT WEST. teenth and nineteenth; Maine, twentieth to twenty-fourth; Maryland, twenty-first to twenty-sixth ; Massachusetts, twenty-second to twentieth ; Connecticut, twenty-third to thirty-first; Minnesota, twenty-fourth to fourteenth; Arkansas, twenty-fifth to twenty-third; New Hampshire, twenty-sixth to thirty-second ; South Carolina, twenty-seventh to twenty- ninth; Louisiana, twenty-eighth to thirtieth; Kansas, twenty-ninth to seventeenth ; Florida, thirtieth to thirty-fourth ; Nebraska, thirty-first to twenty-eighth; Delaware, thirty-second to thirty-fifth, Rhode Island, thirty-third to thirty-sixth. Thus it will be noted that the advance made by Kansas in the period named was beyond all question the most striking among all the States of the Union, ascending on an average to one place higher each year. Minnesota is the only State approaching her, but while she was doubling her aggregate of valuation Kansas trebled hers, and at the end had within four million dollars the valuation of Minnesota. New York, though leading in 1876 as in 1866, had $36,000,000 less valuation. Ohio losing $17,000,000 and Pennsylvania $8,000,000, Kan- sas had $30,000,000 in 1876 to $10,000,000 in 1868. LOCATION OP BEST FARMING LANDS. This question cannot be satisfactorily answered unless the exact wants of the interrogator are made known in each case. Only a very general answer can be given. There is probably no State in the Union where there is so small an acreage of waste land as in Kansas. The bottom- lands of our beautiful valleys are what are commonly known as " second bottoms," which very seldom contain ponds of stagnant water, and which are, in this respect, unlike most of the bottom-lands in most of the Western States. Skirting and distinctively bounding the valleys are picturesque bluffs, varying in form and size, sometimes gently undulating, and then bold and abrupt, and in most cases clad with verdure. Stretching out on either hand from the skirtings of the valleys are the gently-undulating prairies, or uplands, until other valleys are reached. Bottom-lands are preferable for hemp and tobacco, and are equally good for other crops, un- less it be for fruit. It is thought by many fruit-growers that the growth in the bottoms is too rank and soft, and that the fruit is not as fair nor as highly flavored ; others think this is compensated largely by the protec- tion given from the high wincjs of the prairies. Sometimes wheat and other small grains grow so very rank in the valleys as to lodge badly, and wheat is a little more inclined to rust than on the high prairies. The whole State, including the yet unorganized counties, embracing what has been familiarly known as the " Plains of Kansas," is well adapted to stock- KANSAS. 269 growing; this designation, which carries with it the idea of a country " without elevations or depressions," is as erroneous as that formerly ap- plied, within our memory, to all Kansas — ^the " Great American Desert." While many watercourses have their source east of this region, a reference to the Kansas map will disclose the fact that the following rivers have their sources west of the State : the Cimarron River in the extreme south- west; the Arkansas some sixty-five miles north of the former; the Smoky Hill in the central portion ; and the Republican in the north-west. It will also show that, as these rivers flow eastwardly, the feeders are nu- merous and important, webbing the unorganized counties with a network of watercourses which will enable sheep-husbandry and grazing of horses, cattle, and mules to be carried on to an unlimited extent. To rely upon this portion of the State, however, at the present time, for diversified farm industries would be disastrous — only a " potter's field " for all capital in- vested. The advantages for sheep-raising are equally as good until you reach the sixth principal meridian, and east of here through Kansas, in the ordinary method of keeping a limited number ; but west of this line the range is unlimited, and the deep abrupt walls or bluffs in many locali- ties, where small streams and ravines zigzag to the larger ones, guarantee ample protection from the severity of the winds of winter, and at the same time furnish, in the bottom of the miniature valleys and often on the sides of the bluffs, a good growth of wild grass which furnishes nutritious food. There are winters where stock, especially sheep, will go through with very little care or food beyond what has been named. The failures which have hitherto occurred in these industries in the extreme West are owing to the fact that an impression has gone abroad that because stock will occa- sionally stand this kind of treatment, it may be tried with impunity at any time. TJiis is an egregious mistake; stock any and everywhere in Kansas need more or less care, protection, food, and water — more than they can obtain if allowed to roam at large. It is believed, however, that the mortality which often occurs is owing to thirst ; streams become frozen, and the poor creatures become mad with thirst, and start out in all kinds of weather in quest of water, thereby exposing themselves to the inclemency of the weather when their systems are in the worst pos- sible condition to repel cold, and when they would otherwise be huddled together behind Nature's wind-breaks and feeding upon native grasses, without " going out in the cold " for them. There are two conditions precedent to a successful outcome in raising farm animals on a large scale. These are the adaptability of the climate and soil for the production of corn and the amount of grasses fit for pas- 270 THE GREAT WEST. tare and hay. The figures in the progress of the corn-culture eloquently establish the claims of that cereal to the title of king of farm-products in Kansas. The extreme western organized counties are not as good for corn as those in the eastern part of the State, and it is questionable whether it can be grown with profit at all except in the river- and creek- bottoms. It can be brought by rail from eastern counties at less cost than it can be raised in the western, or stock can be taken farther east to winter. Corn last fall and though the winter has sold on the line of the railroad at from twenty-two to twenty-five cents. But stock can be driven a distance from railroad communication, where corn is cheaper. As to grasses, the unlimited pastures of Kansas produce a superabun- dance of the most nutritious wild or native varieties — the common prairie grasses in the east, and the buffalo and blue-stem in the west, taking the lead. As the buifaloes recede from the fast-encroaching settlements, the blue-stem, a variety which often grows from eight to ten feet high, reaches westward, and in turn will undoubtedly be followed by the smaller and more desirable prairie-grass, which obtains throughout all Eastern and Middle Kansas — ^that is, in the organized counties. Then, as the settle- ments become older and farms become fenced, timothy, clover, and blue- grass pastures and meadows have been established with ease, all taking kindly to the soil and promising the best of results. In the west — in fact, throughout Kansas — alfalfa promises to be eminently successful. Especially in the west, where rainfall is variable to some extent, and less than in the east, its determined, fibrous roots descend to a great depth, and it flourishes beyond all expectation. Millet and Hungarian also do well throughout the State. Spring wheat gives the best results in the north-west, but is being fast superseded by its stronger rival. While we have not been sufficiently definite to answer any one partic- ular question, we have endeavored to furnish a fair statement of the rela- tive capabilities and possibilities of the different parts of the State, with- out narrowing down to county or district lines. In this connection we would be recreant to every sense of duty if we did not spt forth a little more in detail the advantages and disadvantages of the eastern and west- ern portions of the State, PRICES OF IMPROVED AND UNIMPROVED FARMS. The enthusiastic immigrant, when he leaves his more Eastern home, seeks cheap lands in the extreme West. He takes no more notice of the beautiful farms of Eastern Kansas and the improvements on every hand #ian if they did not exist. And yet these are among the most fertile KANSAS. 271 and productive in the West. They have the advantage of having a most admirable network of railroads, which furnish convenient markets for their products; elegant school-houses and church edifices, dotting hills and valleys; modern bridges spanning the numerous streams; court- houses and other public buildings erected ; fields under a high state of cultivation ; orchards and vineyards in full bearing with all kinds of fruit grown in this latitude — apples, pears, peaches, apricots, nectarines, cher- ries, plums, grapes, together with the whole army of small fruits. To accomplish such results has required the pluck and energy of an enter- prising people for the last twenty or more years. The transformation of the homestead region from a boundless prairie waste, beautiful but wild, into a land teeming with the foregoing evidences of wealth, prosperity, and civilization will require another twenty or more years. The western portion of the State is bewitchingly inviting to all of small means, whose only hope for a farm and home of their own is government land. It is equally so to those of larger means, who wish to prosecute farm industries on a large scale with the least possible outlay : especially is this true of stock-raising. But there is another class throughout the Eastern States, who possess from one to fifteen thousand dollars each, and whose little capital, owing to shrinkage in values, general business prostration, and want of confidence, is either idle or earning a very low rate of interest. These men are among the best, and are signalling the West for infor- mation to enable them to make safe investments in land and to establish new homes and business relations. In the East, with land from one to two hundred dollars per acre, their Outlook is gloomy. In Eastern Kansas we find an anomalous state of things — wild lands at about the same prices for which they can be had from private parties in the West, while improved farms can be purchased for less than the cost of the improvements ; and this in a region unexcelled in fertility, with no parallel in the history of material development and substantial pros- perity. It is no discredit to the country producing these apparent con- tradictions, but greatly in her favor. In the early settlement of the State, when immigration was exceedingly large, and when, as now, immigrants had to purchase largely the first year, the soil yielded so abundantly, and the market at each farmer's door for every bushel of grain, every pound of butter, every dozen of eggs, and everything else which he could pro- duce, was so good, with prices so extraordinarily high, he considered it would be only a question of a few years when he would have all the surroundings that affluenpe could bring. Following quickly upon this glittering picture of future wealth, while land-speculation beset and upset 272 THE GREAT WEST. even the old stagers who had passed through in the East the severe ordeal of 1836 to 1840, church-spires sprang up like magic, built with money largely sent by the various denominations in the older States ; school dis- tricts vied with each other in the erection of elegant school-edifices ; court- houses, bridges, and other public improvements were carried on ; railroads were being pushed ahead with unexampled and unexpected celerity. The money for all these improvements was spent in the State, of which the farmers received a goodly share. This additional source of prosperity begat a new spirit of land-speculation, from which it was impossible for any class possessed of the ordinary frailties of human nature to escape. Farmers, being the most prosperous, outdid all others in the mania for land, which they purchased at fabulous prices, making small down-pay- ments, giving notes for the balance secured by mortgage on all their real possessions. While these seemingly inexhaustible sources of monetary supply con- tinued, with real estate constantly appreciating, an Utopian future was presented to the mental vision. But in a day, as it were, all these cher- ished hopes were dissipated. Values depreciated ; the various improve- ments herein named stopped ; bonds which had been issued for railroads, expensive school-houses, bridges, court-houses, etc. called for a tax-levy for annual interest, and for a sinking fund for their final redemption ; and interest had to be paid or defaulted on mortgages covering real estate largely undeveloped. Shrinkages occurred in everything except mort- gages ; these soon became malignant, cancerous growths, which not only consumed the profits of the farmers, but the farms themselves. Hence it is that a train of circumstances has conspired to bring financial dis- aster upon one class of farmers, while the prosperity of those who are out of debt, and the rapid advancement of the country in material greatness, clearly vindicate the statement that it is no fault of Kansas, of her soil or climate, that this state of things, nearly always incidental to the rapid settlement and development of a new country, exists. These overladen farmers, with pleasant surroundings, the accumulated labor of years, must give up their homes, save all they can, and commence anew in the West, where government lands can be had without price. It is to these farms, which can be had at great bargains, that the attention of the new- comer is called who has the means to gratify his inclination and taste. KANSAS. 273 POPULATION OF KANSAS. rriHE following tables show the population of Kansas, by counties and -L principal cities, as returned by the assessors, through the county clerks, to the State Board of Agriculture, March 1, 1879 : POPITLATION BY COUNTIES. Enamera- Enamera. Enomera- Ennmera. tloD uf in- habitanM, 1878. tion of in. habitaou, 1879. lacr. Deer. Couimss. tioD of iD- habitants, 1878. tioD or in. babitaots, 1879. iDcr. Deer. Allen 8,964 10,116 1,152 Marion . . . 8,306 10,154 1,848 Anderson . . . 6,000 6,616 616 Marshall . . 12,270 17,129 4,859 * Atchison . . 20,600 21,700 1,100 McPherson . 11,291 13,196 1,905 Barbour . . . . 1,388 2,016 628 Miami . . . 14,4:« 15,161 728 Barton . . . 8,231 12,333 4,082 Mitchell . . 8,673 14,034 3,361 Bourbon . . . 17,741 18,310 569 Montgomery . 16,468 15,979 489 Brown . . . . 10,446 10,790 344 Morris . . . 6,656 7,197 l,'54'l Kutler . . . 14,175 17,006 2,831 Nemaha . . . 8,876 10,267 1,.391 Chautauqua . . 9,246 10,537 1,291 Neosho 11,055 13,694 2.339 Chase 3,798 4,743 945 Norton . , 1,865 4,797 2,942 Cherokee . . . 17,770 18,635 765 Osage .... 12,618 15,369 2,761 Clay . . . . 8,759 10,658 1,899 Osborne , . . 6,125 9,445 3,320 Cloud . . . 10,183 12,6.16 2,473 Ottawa . . . 6,664 8,757 2,093 Coffey 8,599 10,077 1,478 Pawnee . . . 6,114 7,023 909 Cowley . . . . 15,390 18,157 2,767 Philips . . . 5,436 7,956 2,.520 Crawford . . . 12,759 14,622 1,863 Pottawatt'mie 11,196 13,791 2,695 Davis 6,382 6,087 705 tPratt (o) . . 2,084 2,084 Dickinson . . . 10,850 13,003 2,166 Ueno . . . 11,528 12,042 614 Doniphan . . . 15,122 15,459 337 Republic . . 10,132 12,193 2,061 Douglas . . . , 18,931 20,630 1,599 Rice . . . 6,149 7,601 1,332 Edwards , 1,700 2,801 1,101 t Riley . . . 7,419 7,419 Elk 8,218 8,787 569 Rooks . . . 2,100 5,104 3,004 Ellis 2,437 5,240 2,803 Rush .... 2,794 6,282 2,488 Ellsworth . . . 5,057 6,741 1,684 Russell . . . 3,239 6,521 3,282 Ford . . 2,160 2,832 672 Saline .... 9,330 12,424 2,894 Franklin . . . 12,381 14,073 1,692 Sedgwick 15,220 17,613 2,393 Greenwood . . 7,658 8,202 554 Shawnee 19,114 22,632 3,318 fllarper . 2,1,58 2,l,i8 Smith .... 8,313 11,498 3,183 Harvey . . . . 8,107 10,440 2,333 t Stafford (6). 2,364 2,364 tHodgeman . . 1,738 1,738 Sumner . . 12,078 15,090 3,012 Jackson . . . . 7,930 8,732 802 t Trego . . . 2,310 2,310 Jefferson . . 12,471 13,872 1,401 Wabaunsee . 5,386 6,245 859 Jewell . . . . 11,388 14,161 2,773 Washington . 10,319 11,900 1,681 Johnson . 18,139 16,012 2,127 Wilson . . 11,760 11,901 141 Kingman . . . 2,399 2,599 Woodson . . 5,514 6,038 544 Labette . . . . 17,196 18,171 975 Wyandotte . 13,161 13,046 1,886 Leavenworth . 28,544 30,283 1,739 ♦Unorganized Lincoln .... Linn 4,611 ■ 13,228 7,448 2,837 counties . . 8,500 13,000 6,600 14,686 1,358 Lyon 13,634 15,073 1,439 Total . . . 708,497 849,978 144,097 2,616| Actual increase during the year ending March 1, 1879, 141,431. * Estimated by assessors. t Harper organized August 5, 1878 ; Hodgemirn organized March 29, 1879 ; Stafford organized June 30, 1879 ; Pratt organized July 25, 1879 ; Trego organized June 21, 1879 — which accounts for no official returns for 1878. t Returns for 1878; no enumeration for 1879. (a) In 1878, Pratt county, then unorganized, was attached to Eeno as a township thereof, and to which the enumeration was made. Population, March 1, 1878, 2180. (6) At the time of the reinstatement of Stafford county by decision of the Supreme Court, June, 1879, Barton county extended to the south line of township 23. By said decision twelve townships were taken from the south part of Barton and added to Stafford. As the enumeration of inhabitants for Bartou was taken March 1, 1879, the returus for said twelve townshi|3a appear in the Barton county returns, and show a population of 23S7, or 197 to each of the Congressional townships. June, 1879, at time of said decision, the population of Stafford county was 4731. Deducting the population returned to Barton county (twelve townsliips), 2367, from that of Stafford county (4731), we have left 2364 for the remainder of the territory of Stafford county. 18 274 THE GREAT WEST. Population of the Pbincipai, Cities, in the Obdeb op Eank, coMMENciNa WITH THE Highest. Leavenworth, Leavenworth county . 16,643 Topeka, Shawnee county 11,204 Atchison, Atchison county 11,000 Lawrence, Douglas county 8,478 Wichita, Sedgwick county 5,235 Fort Scott, Bourbon county .... 5,010 Wyandotte, Wyandotte county . . . 4,612 Emporia, Lyon county 4,061 Ottawa, Franklin county 3,507 Salina, Saline county 3,383 Parsons, Labette county 3,130 Independence, Montgomery county . 2,829 Newton, Harvey county 2,539 Junction City, Davis county .... 2,345 Olathe, Johnson county 2,260 Beloit, Mitchell county 2,194 Winfield, Cowley county 2,103 Osage City, Osage county 2,003 Paola, Miami county ....••• 1,973 ^Burlington, CoflFey county 1,740 Hutchinson, Eeno county 1,709 Clay Centre, Clay county 1,600 Manhattan, Riley county 1,593 Empire City, Cherokee county . . . 1,591 Mound City, Linn county 1,497 Humboldt, Allen county . . Concordia, Cloud county . . Great Bend, Barton county . Marysville, Marshall county . Garnett, Anderson county . . Osage Mission, Neosho county Girard, Crawford county . . Hiawatha, Brown county . . Wamego, Pottawattamie county Baxter Springs, Cherokee county Minneapolis, Ottawa county Holton, Jackson county . Seneca, Nemaha county . Earned, Pawnee county . lola, Allen county . . . Eureka, Greenwood county Oswego, Labette county . Chetopa, Labette county Fredonia, Wilson county Sabetha, Nemaha county Neosho Falls, Woodson county Washington, Washington county Brookville, Saline county . . . Cottonwood Falls, Chase county Louisville, Pottawattamie county 1,456 1,441 1,430 1,420 1,252 1,216 1,184 1,078 1,071 1,069 1,045 1,044 1,036 1,031 966 880 759 745 720 706 669 656 485 472 363 With few exceptions, throughout the State the same person performs the duty of assessor for his township and the city or town therein. We have given in the above list the population of the cities and towns of the State, so far as assessors made separate enumeration of township and city population. Where the population of township and city is aggregated, an estimate only of either could be given, and injustice might be done. TEXAS. AEEA. THIS State is bounded on the south-west by Mexico, from which it is separated by the Rio Grande, and on the east by Arkansas and Louisiana. It has an area of 237,504 square miles. The reader should remember that this vast region is equal in extent to all New England, together with New York, Pennsylvania, Ohio, and half of Indiana. HISTORY. In 1687, La Salle, the well-known French explorer, erected a fort on Matagorda Bay. In 1715 the country was settled by Spaniards, and sev- eral new missions were established, but the Camanche and Apache Indians, among the most warlike in America, and still troublesome to the border settlements, hindered the progress of the country. In 1 803, Texas, claimed by both Spain and the United States, became a disputed territory. From 1806 to 1816 settlements were formed, and several attempts made to wrest the country from Spain. In one of these, in 1813, two thousand five hun- dred Americans and Mexicans were killed, among them seven hundred inhabitants of San Antonio. Mina, a Spanish refugee, gained some suc- cess, but was defeated and shot. In 1819 the river Sabine was established as the boundary. In 1820, Moses Austin, an American, got a large grant of land in Texas from the Mexican government, and began a settlement which rapidly increased, but many of the settlers were of so lawless a character that in 1830 the gov- ernment forbade any more Americans coming into Texas. In 1833 a convention of settlers, now twenty thousand in number, made an unsuc- cessful attempt to form an independent Mexican state, and in 1835 a pro- visional government was formed, Sam Houston chosen commander-in- chief, and the Mexicans driven out of Texas. Santa Anna, president of Mexico, invading the country with an army of seven thousand iive hundred, 275 276 THE GREAT WEST. after some successes was entirely routed at San Jacinto, April 21, and Texas became an independent republic, acknowledged in 1837 by the United States, and in 1840 by England, France, and Belgium. In De- cember, 1845, Texas, at her own request, was annexed to the United States, but was invaded by Mexico, which had never acknowledged its independence, and thus originated the war with the United States. PHYSICAL FEATUKES. The country near the Gulf is level, with a gradual ascent toward the north. The coast-region is formed of alluvial beds of sand or gravel. The whole of Eastern Texas, embracing a territory larger than Ohio, consists of pine-barrens, called " cross timbers," interspersed with prairies which give it a park-like and delightful aspect. The little arable land of Eastern Texas is confined to the valleys of the streams. Out of the valleys the soil is sandy, and would not pay to clear and cultivate. This region, it would seem, is not destined to become thickly peopled. It now supports a scanty population of lumbermen, and some poor farmers who cultivate little patches along the creek-bottoms. The larger streams are bordered by narrow tracts of good soil, where there are some large cotton-plantations. This part of the State is not a new country, and except on the opening of the lumber industry by the building of a railroad it has had no growth in recent years. Something might be done with fruit-culture ; a few peach-orchards at Palestine have proved remarkably profitable, their product bringing an extremely high price in the St. Louis market; but the population lacks enterprise to develop any new branch of industry. The middle region of Texas, or that portion lying west of the above-described pine-barrens, stretching from the Red River southward almost to the Gulf, and having an aver- age width of about two hundred miles, consists of beautiful rolling prai- ries, which are unexcelled in fertility and productiveness. This region may be roughly compared in area to the State of Illinois. Farther west is a broad belt of hilly or rolling country, consisting of prairies and post-oak or black-jack openings, that is too dry for agricul- ture, but is well adapted to grazing. This is the great cattle-region of Texas. It stretches from the Red River to the Rio Grande and the Gulf. Some portions of this region may eventually be cultivated if the rainfall, which is now insufficient, should increase by climatic changes, which are said to be going on along the eastern border of the whole arid region from Montana down to Mexico. Still farther west is an immense arid region, comprising about three- TEXAS. 277 fifths of the whole surface of the State. This region is in the nature of a high table-land, and the salt and " Staked Plains " (so called from the great abundance of yucca-stems, resembling stakes), elevated from three to /our thousand feet above the sea, Avithout trees or grass, destitute of vegetation, may be allied to a vast desert. There are a few small moun- tains in the west, spurs of the Rocky Mountains. The river-bottoms are well timbered. CLIMATE. The climate of Texas is variable, from semi-tropical to moderately temperate. Snow and ice are seldom seen in the central portion, and rarely if ever in the extreme south. In the northern part one or two snowfalls during the winter, of from one to three inches in depth, are usually expected ; occasionally a much heavier fall of snow is had, and ice from one to two inches in thickness is sometimes made. The mer- cury rarely falls more than three or four degrees below the freezing- jjoint, and seldom continues that low more than two or three days at a time. Stock graze all winter ; field-work can be done at all seasons of the year ; and February is regarded as the time for planting corn and other cereals. The extreme heat of the summer is 90° to 95°, rarely rising to 100°, while in some of the Northern States in the latitude of St. Louis it not unfrequently rises to 104°, and even higher. The summer heat is so tempered by cool and refreshing breezes from the sea-coast and the light winds which blow almost continually from the south and west as to render it far less oppressive than in the Northern States. The nights are delightfully cool and pleasant. Sunstroke, so frequent at the North and East, is almost unknown here. inWEEALS. In this State are found "fine marbles and some deposits of lead and copper. AGRICULTUEAL PRODUCTS. The soil is of great fertility, the coast producing the finest cotton and sugar, and the interior wheat, corn, and fruits of all kinds, with immense pasturage, making it one of the finest cattle-raising countries in the world. Central Texas is }irobably the best cotton country in the South, and is now producing one-sixth of the whole cotton crop of the United States. It is not nearly as good a corn country as Illinois and Kentucky, and for the production of wheat no part of it can compare with Minnesota, Iowa, and Kansas. Root-crops, as a rule, do not succeed ; the product, though 278 THE GREAT WEST. large and apparently well developed, is coarse and watery. Some fruits do tolerably well, particularly the peach and pear, but little attention is given to raising them. Apples are brought from the North. Central Texas is declared to be a paradise, with excellent soil, and a climate which brings visitors for profit, pleasure, and health from all parts of the world. Stock-raising, for which Texas is especially adapted, yields to the diligent herdsman a bounteous remuneration for his services. The vegetation is in the greatest variety, from the oak, cedar, and pine to the palmetto, mezquite, and nopal, which latter feeds the cochineal insect; also figs, oranges, grapes, vanilla, and flowers in wonderful profusion. ANIMALS. The prairies abound in buffalo and immense herds of wild horses, and the forests with deer. There are also the puma, jaguar, black bear, and the wolf. MISCELLANEOUS. The State deaf and dumb, orphan, blind, and lunatic asylums have each an endowment of 100,000 acres of State lands. There is a State school fund of $2,500,000, and each county has 17,712 acres of land for educational purposes. The tide of immigration into the State is immense, and there is every prospect that during the present year it will be veiy large. The taxable property of the State in 1850 was $51,000,000 ; in 1860, $294,000,000; in 1870, $174,000,000; in 1875, $275,000,000; while it is believed that in 1879 the figures reached will be nearly $325,000,000. Though the country is generally level, it is not destitute of wild and grand scenery. In some parts of the State are found gigantic animal fossils and silicified trees, which are objects of wonder and admiration to the scientist and antiquarian. Austin, the capital, is a thriving town. The metropolis and most im- portant seaport in the State is Galveston. Other towns of importance are Houston, Marshall, Indianola, and Corpus Christi. IDAHO. BY WILLIAM P. CHANDLER, SUEVEYOR-GENEEAL. THERE is a succession of mountains extending over a large part of the northern half of this Territory, the soil of which is generally- sandy and rocky. The mountain-sides are covered with pine, fir, and cedar timber. In the southern part the Goose Creek and Owyhee ranges extend to the southern and western boundaries, with similar soil and a growth of juniper timber. The soil of the lower hills is composed largely of decomposed granite and sandstone, and in its natural state produces a luxuriant growth of bunch-grass, affording abundant grazing for stock. The soil of the table-lands is much the same, except considerable tracts in which fine rich loam is intermixed, and when irrigated produces large crops of grain. Sage-brush grows on all the table-lands interspersed with grass. In the valleys of the streams and along the bases of many of the mountain-ranges the soil is a dark, sandy loam, finely pulverized, and mellow and well adapted to the growth of cereals and vegetables. There is a large volcanic plateau near the centre of the southern half of the Territory, inaccessible and unexplored, destitute of soil or vege- tation. CLIMATE. This Territory, extending from the 42d degree of north latitude to the 49th, and its surface broken up into undulating plains, high rolling hills, and rugged mountain-ranges, has a varied climate. The valleys are mild and equable, sufficiently warm in summer to mature the crops of the farmer, and rarely visited by severe storms or deep snows in winter. In the high and mountainous regions the winters are long, deep snows cover the ground, but owing to the purity and dryness of the atmosphere they are endured without great discomfort. The dry, cool air of the moun- tains, the pure streams of cold water, the game for the hunter and trout 279 280 THS GREAT WEST. for the angler, render life in the mountain-region in summer a perpetual attraction to the tourist and invalid. The temperature of Boise City, the capital, in latitude 43° 37' north and longitude 116° 12' west, 2880 feet above sea-level, is mild, the lowest point during the winter of 1878-79 being 5° above zero in January, and the highest, 103°, August 9. The rainfall was as follows : Seasons, Inches. Autumn, 1878 1.10 Winter, 1878-79 5.87 Spring, 1879 4.38 Summer, 1879 1.46 Total 12.31 AGRICULTURE. In considering the agricultural resources and productions of Idaho reference must be made to its altitude and surface. Its elevation is from two thousand feet above sea-level, in the lower Snake River Valley, to nine thousand feet on the top of its mountain- peaks, a large part lying above the altitude of four thousand feet. The higher portions are broken up into a succession of mountain-ranges, in many places very steep and rugged. Below these are high, rolling hills, upon which nutritious grasses are found, affording vast pasture- lands for stock. Still lower are the table- or " sage-brush " lands, rich in soil, and when properly irrigated and cultivated producing large crops of cereals and vegetables, and favorable to the growth of fruits common to this latitude. The valleys of the streams are fertile, and in the northern portion of the Territory (where the rainfalls are sufficient in spring and early summer) excellent crops of cereals are raised without artificial irri- gation. In the central and southern parts irrigation is essential to sure and good crops, although there are occasional small tracts lying near the level of the streams on which grain-crops may do well without. The mountain-valleys and plateaus, lying not to exceed five thousand feet above sea-level, produce large crops of oats and the hardier vegetables, and yield hay abundantly when sufficiently watered. The agricultural lands are found along the valleys, and include the table-lands lying lower than the sources of the streams flowing through them, from which water can be brought for irrigation. The aggregate amount of such land is large, but is distributed in com- paratively small tracts throughout the whole Territory wherever there are streams of running water, but mostly in the northern and southern IDAHO. 281 portions. In the northern, along the valleys of the Spokane, Palouse, and Clearwater Rivers and their tributaries, successful and quite exten- sive farming is carried on, the surplus products finding a ready market down the Snake and Columbia Rivers, which are navigable to Lewiston, the county-seat of Nez Perc6 county. Salmon River, south of the Clearwatei-, is a large and rapid stream. Its source is in the western slope of the Rocky Mountains and along the Saw-Tooth Range near the centre of the Territory, and it courses through its entire breadth from ea.st to west, and unites with the Snake near latitude 46° north. This stream rises in and runs through the most rugged and mountainous part of the Territory, with but little agricultu- ral land along its narrow valley. Bonanza City, in latitude 44° 35' north, longitude 114° 30' west, altitude sixty-four hundred feet, is sit- uated on its head-waters, and is surrounded by high and rugged moun- tains whose peaks tower into the regions of perpetual snow. A large area of the interior of the Territory is covered by mountains, which extend across it from the Rocky Mountain range on the eastern boundary to the Snake River on the western. Weiser and Payette Rivers rise in the westerly spurs of this mountain-range, and flow west- erly into Snake River near latitude 44° north, the valleys of which con- tain many acres of very fertile land, upon which there are good farms ; and many more will be taken up and cultivated when the settler can feel assured that he will not be exposed to the annual raids of maraud- ing Indians. Boise River takes its rise in the south-easterly spurs of the same mountain-range, flows north-westwardly, and joins the Snake in latitude 43° 40' north, longitude 117° west. The valley of this stream, for a distance of sixty miles from its confluence with Snake River to where it debouches from the mountains, contains a large area of the most produc- tive land, the valley being at some points several miles in width, with many farms in a high state of cultivation. The stream falls in its course through the valley at the rate of about ten feet per mile. The banks are low, and water is easily diverted from its channel to irrigating- ditches. Snake River takes its rise in the mountainous regions of Wyoming, and. its various branches, flowing westwardly into the Territory, unite in one grand stream twenty-five miles north of Taylor's Bridge, about fifty miles from the east boundary of Idaho. Thence its course for a distance of one hundred and sixty miles is to the south-west ; thence north-west- wardly about the same distance to the western boundary of the Territory ; 282 THE GREAT WEST. thence north along the western boundary about three hundred and fifty miles to Lewiston, where it passes into Washington Territory. At the point of junction of the several streams forming the Snake there is a large tract of rich bottom-land, mostly above high water, and to which many settlers have removed this season, feeling confident they will suc- ceed in their efforts to cultivate successfully this valley, although the alti- tude is nearly five thousand feet above sea-level. The stream from this point for a distance of one hundred and fifty miles runs through a broad valley of rich land. In many places the banks are low and favorable to the construction of irrigating-ditches. Below this point for seventy-five miles the river courses through a deep rocky canon, in which is situated the Shoshone Falls, equal to the Falls of Niagara in height and volume of water and far exceeding them in natural scenery. After leaving the caflon the river flows with a gentle current through an open rolling country about two hundred miles, when the mountains on both sides close in, and its course is confined to a narrow rocky channel or caflon until it leaves the Territory near Lewiston. The valley of Snake River contains most of the table-lands in the Ter- ritory, and the water of the stream is ample for irrigating millions of acres of as productive land as can be found in any country. Running into the Snake from the south are several small streams, the valleys of which contain considerable tracts of agricultural lands. Com- mencing with the Bruneau, thence following up the stream, are Goose and Marsh Creeks, Raft River, Fall, Rock, and Bannock Creeks, Port^ neuf, Ross's Fork, and Blackfoot Rivers. There are settlements in the valleys of all these streams, but the more considerable are along Goose and Marsh Creeks, Raft River and its tributaries, and Blackfoot. In the south-eastern portion of the Territory, along the Malade and Bear Rivers and their branches, are large settlements of prosperous farmers. I have only called attention to the most important agricultural sections of the Territory, leaving out the many small valleys containing small areas of very productive land and more or less occupied by the farmer and herder. Any estimate of the number of acres of the various classes of lands in this Territory, so broken in its surface and varied in its climate and altitude, can be only approximate. Of its total area of 55,228,160 acres, I believe 12,000,000 acres to be agricultural, either in its natural state or as it may be reclaimed by irrigation with the Available water now IDAHO. 283 flowing in the streams ; 25,000,000 acres pasture-lands ; 10,000,000 acres timber-land; and the remainder, 8,228,160 acres, may be considered worthless, consisting of inaccessible mountain-peaks and lava-beds. The development of the agricultural interests of the Territory has been slow, owing to its inland and isolated position, lying outside of all railroad lines until the building of the Utah and Northern Railroad through the eastern part during, last year, with no navigable waters except at Lewiston, at the head of steamboat navigation on Snake River, just as it leaves the Territory. Transportation by teams is so expensive that but little profitable farming can be done beyond a supply of the home market, which is found at the mining camps principally, where remunerative prices are obtained. The yield of cereals is large ; twenty-five to forty bushels of wheat and barley, and fifty to eighty bushels of oats, per acre, is a fair average yield. Where the ground is properly irrigated and cultivated failure of crops has never been known. All the vegetables grown in this latitude are produced in abundant quantities for the wants of the people. Loss of crops at harvest-time, catised by rains, is unknown. I have been unable to find any statistics showing the number of acres in cultivation, number of cattle, horses, etc. ; but through the kindness of Joseph Perault, Esq., Territorial Auditor, have been furnished with the total assessed value of property for taxation, as follows : 1877 $4,319,958.75 1878 4,520,800.50 The present year has been a prosperous one for the farmer, large crops of all kinds having been raised. MINING. The mineral wealth of Idaho is its largest resource. Extensive and rich lodes of gold-, silver-, and copper-bearing ores are known to exist in various parts of the Territory. The production of the precious metals is the most important and leading branch of industry. The field for en- terprise in this direction is almost without limit, but the development of its mines has been retarded by the high price of labor and the great cost of transporting supplies and machinery to the centre of the mountainous regions in which the mines are mostly situated. The building of the Utah and Northern Railroad through its eastern border, and the expectation of the early construction of a line from near Blackfoot to the Columbia River, running through the centre of the Ter- 284 THE GREAT WEST. ritory, has stimulated prospecting, and many rich lodes of gold- and silver- bearing ores have been discovered within the year. Placer-mining is carried on successfully in many places, but the yearly exhaustion of surface-diggings reduces the annual production from that source. Gold too fine to be separated from the earth by the old process of wash- ing is found in Snake River Valley through its whole distance in the Territory, and heretofore it has baffled the skill of the miner to save it. During the present season several parties have been working claims along the river with silver electro-plated machines with satisfactory re- sults. Should this system of mining prove successful, it will open up a large field of operations. The area of land containing this fine or "float" gold may be counted by thousands of acres. I have no means of ascertaining the annual production of the various mines in this Territory, but from the printed statement of Wells, Fargo & Co. find the total shipments of gold-dust, bullion, and ore for the year 1878 to be $1,868,122. To obtain information regarding the condition of mining interests, I addressed letters of inquiry to several United States deputy mineral sur- veyors, requesting statements of the development and production of the mines in their localities. I also requested A. Walters, Esq., United States Assayer at Boise City, to furnish a brief outline of the mineral resources of the Tetritory. His official relation with miners gives hhn facilities to obtain the most reliable information, which is contained in his able and intelligent statement, and which I have the pleasure to introduce : " UxiTED States Assay Office, "I " Boise City, Idaho, October 3, 1879. J " Sir : Agreeably to request, I have the honor to herewith give you a brief outline of the mineral resources of Idaho Territory and the past and prospective production of her mines. " Until five or six years ago by far the largest portion of the precious metals produced in the Territory was derived from the placer-mines, and it is safe to credit to that source of supply at least three-fourths of the sixty-five millions produced up to 1873. Since then most of the rich alluvial deposits have been exhausted, and, with few exceptions, placer- mining is entirely in the hands of Chinese, who, on account of their more than frugal habits and mode of living, manage to realize (to them) large profits from claims which would not yield the lowest wages to a white laborer. While during the most productive seasons these placers yielded IDAHO. 285 as high as five and six millions per annum, less than one million has been taken out annually for the last few years, principally derived from the placers of Boise Basin. There being a large amount of poor — or so-called Chinese — diggings, this production -will probably continue "for quite a number of years, but as the whole country has been prettj' thoroughly prospected for placers, it is hardly probable that any more rich diggings will be found that are extensive enough to cut a figure in the bullion pro- duction of the Territory. " The gradual exhaustion of the placers naturally led miners to look for the source whence these gravel-deposits came, and numerous gold- and silver-bearing veins were thereby discovered, especially during the last three years. " The first lodes discovered were those of Owyhee county, the Atlanta and others in Alturas, and the Gold Hill in Boise county ; but, though great excitement was created for a while by the enormously rich and ex- tensive silver-lodes found in the former, reckless mismanagement and 'the working of the mines in the interest of stock manipulations, coupled with the high price of machinery and rate of wages, soon resulted in the same disastrous consequences experienced to a greater or less extent by all the Pacific coast mining States and Territories in their earlier history. " The revival of quartz-mining dates from the successful operations of the Gold HiU Mining Company, which, through good and economical management, succeeded in realizing large profits from ore which, I believe, on an average yields less than ten dollars per ton. Since that time many of the old Alturas and Owyhee mines have come to the front again, new ones have been steadily discovered, and for several years the lode-mining interest has decidedly overbalanced that of placer-miuing. " The largest amount of bullion has undoubtedly been produced by the Owyhee mines, and the fact that they have been comparatively idle since 1876 is almost exclusively due to the almost simultaneous absconding of the secretaries of the Mahogany, Ida Elmore, and Poorman companies with all their available funds, and the suspension of the Bank of Califor- nia, aggravated by the fact that nearly all the incorporated companies worked their mines for the sole purpose of bulling and bearing stocks in San Francisco. The latter is also the cause of the sudden collapse of one of the best base-metal camps of the coast. South Mountain. In that dis- trict are found numerous veins of argentiferous galena, the finest carbon- ates, unusually rich in silver, good iron ore for fluxing — in short, every- thing necessary to make the camps flourishing and prosperous — but, 286 THE GREAT WEST. nevertheless, bad management succeeded in ruining the camp, and nothing has been done until this summer. " The mines of Alturas county have not produced as much this year as before, a large number of her miners having left to prospect in Lemhi county, where remarkably rich and extensive veins have been discovered during the last few years. " The lodes of Rocky Bar district are exceptionally rich, but narrow, varying generally from three to six feet in width, and the miners are laboring under great disadvantage in not having a good quartz-mill which will work their ores cheaply and to the best advantage. The Atlanta mines have been doing well, and the discoveries in Queen's River and Lake districts, and those on Wood River, will undoubtedly materially increase the production of the county next year. " Great excitement has been and still is prevailing about the discovery of remarkably rich lodes in the Yankee Fork district, Lemhi county. The veins in that camp are of an unusual width and richness, but so far the production has been small, as the absence of a wagon-road made it impossible to bring in heavy milling machinery, and outside of the richest ores, shipped principally to Salt Lake City for reduction, the working of ore has been carried on only in the two arrastras of Mr. Norton, owner of the Charles Dickens lode. A few weeks ago a wagon-road was com- pleted, and next year at least one good mill will be erected ; and as there is an enormous amount of ore in sight, Lemhi county mines will probably furnish the largest amount of precious metals during the next few years. " In Boise county, the Elmira Company, working the Wolverine, Crown Point, and Banner lodes in Banner district, has been steadily at work, taking out a large amount of silver, and, with some needed improvements in their reduction-works, they will be large producers next year. The Gold Hill Mining Company of Quartzburg has also, as usual, been work- ing their mill to its utmost capacity, and some of the late discoveries on CaBon Creek, near Placerville, have produced some very rich ore. In the southern part of the county, eight to twelve miles from Boise City, quite a number of gold-bearing quartz-lodes have been discovered during the last year. So far, operations have been in most cases confined to pros- pecting and dead work, and as the ore is not very rich it requires the erection of a good riiill, like that of the Gold Hill Company, to ensure profitable working ipf the same. " Northern Idaho, especially Idaho county, possesses a large number of gold- and silver-bearing veins, but there are no mills to work the ore, and not even a wagon-road to bring in machinery, and consequently they all IDAHO. 287 lie idle ; the owners, being poor men, are unable to work and develop lodes without a market for their ore. " In Ada county several veins carrying exceedingly rich copper have been found, and some work done on them this year. There are also good silver- and galena-lodes in Mineral district, but little work has been done so far on account of the isolated situation of the camp. " It is impossible to furnish approximately correct data of the bullion production of all these mines, many of the owners refusing to give any information, but I think it perfectly safe to place it at not less than a mil- lion dollars. This looks little, but lode-mining in this Territory is still in its infancy, and surrounded by difficulties and drawbacks experienced in no other State or Territory, except perhaps Arizona. We have no railroad communication so far, many mining districts being even without a wagon-road, and consequently wages are high. Mining and milling machinery costs here two and three times as much as in more favored localities, and its absence in many districts makes the working of the mines beyond mere annual representation an impossibility for the poor owners ; but as it seems now to be a finally settled fact that the Utah Northern Railroad will traverse the Territory in close proximity to the principal mining districts, there is no doubt in ray mind that the mines of Idaho in the course of a few years after the completion of this railroad will give her one of the leading positions among the bullion-producing States and Territories of the Union. " I have the honor to be, very respectfully, "A. Walters, United States Assayer. "Hon. Wm. p. Chandler, Surveyor-General of Idaho." The following items respecting the development of the mines in the Yankee Fork mining district have been kindly furnished at my solicita- tion by Walter S. Shannon, Esq., United States deputy mineral surveyor and mining engineer, which I beg leave to present : The mines of Yankee Fork are principally gold-bearing quartz. The working of these did not commence until early last spring. Morrison's placer has been worked for some years with great success ; nuggets have frequently been found as large as hens' eggs. Over thirty-five thousand dollars have been expended during the last four years in constructing ditches, dams, etc. At present it is paying |1.25 per pan. This placer- mine is situated at the mouth of Jordan Creek, which empties into Yankee Fork River. The Custer mine is situated on the side of Mount Custer, nineteen 288 THE GREAT WEST. hundred feet above Yankee Fork River and three miles north-east of Bonanza City. The ledge is between three and four hundred feet wide, and runs from top to bottom of the mountain, the ore assaying from $450 to $650 per ton. The owners, Messrs. Heggin, Tevis, Hurst, and Pfieffer (Pfieffer superintendent), are working the mine, running a tunnel, so that the miners will be protected from snow in winter. A forty-stamp mill is in process of construction in San Francisco, which will be placed in position early the following spring. The Unknown mine, owned by the same parties, including Mr. Greorge Grayson, is situated on the east side of the Custer mine, and is a con- tinuation of the Custer ledge, but containing rock which assays from $900 to $1000 per ton. There are other mines situated on Mount Custer, but of a lower grade. Mount Estis mines, which are seven miles north-west of Bonanza City, are of a different formation from the Custer rock, being less flinty. The Montana mine is the principal one, owned by Captain Varney, who has a tunnel fifty feet from the surface. This rock assays from $6000 to $7000 per ton, all free gold. The ledge between hanging-wall and foot- wall is eight feet. The captain has been shipping rock to the quartz- mill at Atlanta during the past summer. Estis mine, owned by Estis Bros., is situated near the Montana mine, and is estimated at the same value. The ledge is seven feet wide. Their rock at present is worked by an arrastra. Charles Dickens mine is situated on the forks of Jordan Creek and Yankee Fork River, on the east side of the hill, four hundred feet above the river. The tunnel follows the ledge sixty feet. The rock assays between $300 and $400 per ton. They have an arrastra, which is worked night and day. This mine is owned by William Norton, Esq. The rock from these mines, excepting the Montana and Estis, is roasting ore. As soon as stamp-mills are erected the owners of mines will commence work in earnest. At present the number of miners employed does not exceed three hundred, who command five dollars per day. The seasons are very short for mining purposes, and the want of a wagon-road has retarded the development of the mines. The Wood River district is situated south-easterly from Bonanza City, about sixty-five miles. The hills around the head of Wood River are a spur of Saw-Tooth range. The principal mines are situated at the head of Wood River, better known as " Ketchem's Camp." The character is chloride, and consists principally of silver and galena. All the rock from this district carries seventy-three per cent, of galena, and no mine IDAHO. 289 assays less than $165 per ton of silver. Gold is very seldom found. The principal mines are the White Oloud, Pilgrim, Shamrock, Quimby, and Occident, which all assay more than $200 per ton, and as high as $900. Messrs. Ketchem & Shannon intend to put up a smelter early next spring. The altitude of this district is eight thousand four hundred feet above sea-level. A wagon-road is to be built next spring to the emigrant wagon-road, which is twenty miles south of Ketchem's Camp. Major Robert ]VJ. McDowell, United States deputy mineral surveyor and mining engineer of Banner district, in response to my request, fur- nishes the following statement relating to the mining interests in that and adjoining districts : The placer-grounds at Idaho Ciiy, and in the cafions leading thereto, for a radius of fifteen miles, as a matter of history have been among the richest in the world. These are flanked by rich deposits of gold-rock in the Quartzburg district, where shafts have been sunk on the trend of the lode, one to the depth of seven hundred feet from the surface and two hundred and fifty feet below water-level, which is a greater depth than has been attained by any similar work north of Snake River. A number of valuable gold-mines, mostly operated by adits and tunnels (with quartz- mills), are located in the above last-named district and Summit Flats, and all are yielding profitably. The character of this quartz-carrying sul- phuret is free, and milling and reduction " kind " and inexpensive, cost- ing only from $5 to $6 per ton and yielding from $8 to $100 per ton. The deposits of pay ore, though located mainly in chimneys (ledge-mat- ter), are nevertheless easily traced, in most instances being confined be- tween walls of granite and gangue. Sometimes their courses are inter- cepted by porphyry-dikes. Of the mines in successful operation are Gold Hill, Sub Rosa, Ebenezer, and Balshaza. During the present year a rich gold-lode has been discovered on Moore's Creek Summit, eighteen miles eastwardly from Idaho City. A clean-up of fifteen tons gave a result of $110 per ton. Some eighty miles from Idaho City the great Saw-Tooth range, run- ning in a north-east and south-west course, towering far above lesser ele- vations called mountains, and having an approximate altitude of nine thousand feet above sea-level, with its imbedded strata of silver and gold quartz, invites labor and capital. Indians have prevented advances in that direction this season, but next year rich discoveries are anticipated. Banner district, Boise county, twenty-eight miles from Idaho City, north-east, in latitude 44° 30', is essentially a silver-mining region, and 19 290 THE GREAT WEST. rapidly developing as such. In 1875 a twenty-stamp dry-crushing quartz- mill, roasting-furnace, shop, assay-office, etc. were erected, but owing to a deficiency in the skill of properly chloridizing the ore, and from other causes, no successful progress was made until within the past year, when it was purchased by the Elmira Silver Mining Company, capitalists from Elmira, New York. The production has been 3900 pounds of silver bul- lion, assaying 920 fine, from the 1st day of July last to the 1st day of October. About fifty men are employed in all departments, and the average yield of ore mined is from $75 to $85 per ton, by milling pro- cess. The absence of bases in these ores is notable, as shown by the following analysis: Silica (quartz) 92.4 Sulphur 1.0 Iron 6.0 Arsenic 0.6 Zinc traces 0.0 100. Banner district yields chlorides (black sulphurets rarely), antimonial, arsenic, ruby, and native silver. The general direction of all the ledges thus far prospected or developed is north-east and south-west. Identifica- tion is not easy, as the ledges do not often outcrop upon the surface ; yet the silver-belt has been traced some ten miles, and has a width of less than a half mile. Some fifty claims are located, and while by assays some specimens have shown as high as $6000 and upward, from $50 to $100 is probably near the figure to be relied upon in actual milling process on chlorination up among the nineties. The veins do not seem to be continuous, but in pockets or chimneys, and are encased within granite and gangue of a white or light-yellow tinge, and are almost invariably accompanied with manganese, which as- sumes the thickness of half an inch to two inches, and is always indica- tive of a well-defined paying ledge. The ledges in this locality have not been sunk upon to sufficient depth to ascertain trend and dip as a gen- eral rule. Veins located on parallel ridges having the same course dip toward each other, and it is contended by miners and experts that each vein will preserve its identity to an inexhaustible depth. Many theories are advanced, but only actual sinking can demonstrate their nature. The Elmira Silver Mining Company have possessory titles to upward of twenty lodes, but are prosecuting work upon only three of the number — viz. Crown Point, AVolverine, and Banner. The first-named two have been entered by three shafts and two tunnels, and a well-defined vein IDAHO. 291 averaging two feet in thiclmess (milling $85 per ton) developed from the surface-croppings down to a depth of two hundred feet. POPULATION. The isolated and inland situation of Idaho and the want of easy com- munication to its borders have prevented any rapid increase in population. Since the Territorial organization only the census of 1870 has been taken. The number shown by that enumeration was 20,588. Since that time there has been a steady and healthy growth, and the number may now reasonably be estimated at 27,000. TRANSPORTATION. Lying outside of all the great routes of travel and commerce, the only means of communication hitherto has been by tedious and toilsome jour- neys over unimproved roads, except the outlet by Snake and Columbia Rivers — navigable for light-draught steamboats — to one point in North- ern Idaho for a few months in each year. During the past and present year the Utah and Northern Railroad has been constructed from Franklin, at the southern boundary of the Terri- tory, through its eastern border, a distance of one hundred and fifty miles to Camas Station, its present terminus. This road will be extended to Montana at an early day. Surveys have been made during the present season for a line to the Columbia River vid Boise City, to connect with this road at or near Blackfoot Station. Freights are high and commercial intercourse restricted. Rates from Kelton — on the Central Pacific Railroad, the nearest railroad point — are from three to five dollars per hundredweight to Boise City, and much inore to most of the mining camps. The mountain-formation extending across the Territory near latitude 44° north divides it into two parts as regards communication. There are no roads in the Territory connecting its northern and southern portions, and it seems to be an undertaking too expensive for the local authorities to build a wagon-road through this region, although the physical obstacles are not great. STOCK-GROWING. This interest is large and constantly increasing. The facilities afforded by pasture-ranges, covered with a luxuriant growth of bunch and other grasses indigenous to this soil and climate, limited only by accessibility to watering-places, early attracted the attention of the herdsman. Cattle and horses in numerous and extensive herds subsist the whole year 292 THE GREAT WEST. through on these natural grasses, supplemented in winter by white sage, sweet and nutritious after being touched by the frosts of autumn. The herds are usually driven to the hills and mountain-slopes during summer, reserving the feed along the foot-hills and valleys, where but little snow falls and the temperature is moderate, for winter. Most stock- growers find their winter range near natural meadow-lands, where hay enough is secured to feed through the exceptional seasons when deep snows cover the ground. These winters are liable to occur once in from four to six years. The beef produced is of an excellent quality, and stall-feeding never resorted to. There being no statistics of stock made in the Territory, I will not attempt to state the number owned and herded within its bounds. It is estimated that twenty thousand cattle have been sold for the Eastern mar- kets this season from the western part of the Territory, and probably an equal or greater number from the northern and eastern portions. Wool-growing has not yet received much attention, although the soil and climate are well adapted to that interest. There are several flocks of sheep owned in the Territory, but the number is not large. Horses enough are raised to supply the increasing wants of the people. The profits to the careful and judicious stock-grower are large, and stated by one in the business to be not less than thirty-three and a third per cent, per annum on the capital invested. EESOUECES. The geographical position of Idaho is such that the various branches of industry depend more largely upon each other than in most States. Lying outside and beyond the main thoroughfares of commerce and travel, the siu-face broken into many high mountain-ranges, traversed by numerous rapid streams flowing in deep valleys, thus making the con- struction of roads costly and difficult, communication has been slow and tedious, and each settlement almost a community by itself and depending upon itself. The discovery of gold along the valleys of the streams first brought the miner, whose wants were supplied by pack-trains, bringing the barest necessaries of life at fabulous prices to the mining camps situated in its mountain-fastnesses. Following, came the agriculturist, seeking out the nearest arable valley to raise such vegetables as were indispen- sable to the miner; and gradually, as the mining interest increased and spread over the various parts of the Territory where the precious metals IDAHO. 293 were found, so gradually grew the agricultural interest to supply the local demand only, followed by the mercantile to supply both, thus making all to hinge upon the mining interest. As it was at the early settlement of the Territory, so it is in a great measure now. Manufacturing, which might reasonably have been expected to follow, has not ; one of the reasons for which may be the high price of labor, mechanics commanding from four to eight dollars per day. Another may be found in the fact that there is no centre of trade or commerce for any considerable portion of the Territory, each community or settlement sup- plying itself from the nearest business-point, either within or without the Territory as most convenient. Flour-mills sufficient to manufacture flour for local demands are estab- lished at various points, and also saw-mills to cut the lumber required for home use by the settler. Near Boise City three considerable irrigating-ditches have been con- structed, for which water is taken from Boise River and distributed over nearly sixty thousand acres of most productive land, which without irri- gation was barren and worthless. Many other ditches have been con- structed and large quantities of land reclaimed, but mostly by each farmer for his own use. No systematic and organized effiirt has yet been made for the construction of large and expensive ditches to reclaim the thousands of acres lying along the valleys of the streams, that need only the fertilizing touch of water to make that which is now an arid desert laugh with bounteous harvests. The subject of irrigation and the reclamation of the irrigable lands in this Territory is one of vast importance to its future growth and pros- perity, and seems worthy the early attention of the government. There are yet small tracts of vacant land lying along the smaller streams that are available for the settler of small means, and the present laws for their disposal appear applicable; but there are large plateaus of irri- gable land lying in Snake River Ytilley that will require a larger capital to reclaim than private parties under the present land laws will care to invest. Either large tracts should be sold to parties who would construct and maintain ditches, and depend upon the sale of the lands for their remuneration, or some general system should be adopted by the govern- ment, and the construction carried on by it as the needs of the country require. The land classed as grazing- or pasture-land is worthless for any other purpose, and unsurveyed, and if ever disposed of must be in extensive tracts. Much of the timber used for fuel is found along the borders of the 294 THE GREAT WEST. streams, and consists principally of cottonwood, poplar, and willow, is taken from land owned by the parties using it, and is very limited in quantity. The fir and pine timber, valuable for building and commerce, grows on the mountain-land, and much of it is found on steep, craggy hillsides and in inaccessible mountain-valleys, and is so difficult of access and so distant from the farm-lands that no more is cut than the actual necessities of the settlers require. During the summer fires rage over extensive tracts, destroying immense quantities. The material advance of Idaho is not rapid, but steady and continuous. The advantages from the building of the Utah and Northern Railroad on its eastern border are already seen in the settlement of large tracts of land along its route and a great increase in mining activity in that part of the Territory. The principal exports from the Territory are gold and silver from its mines and cattle from its hills. Products of the farm, even if in excess of the wants of the people, could not pay cost of transporta- tion to other markets and compete with them in price. The hostility of the Indians in this and the past two years has done much to retard im- migration and prevent the settlement of remote and isolated valleys. Notwithstanding all the drawbacks heretofore encountered, the prosperity of the people appears to be satisfactory. Better buildings are being erected both in town and country, and general thrift and contentment seem to prevail. IDAHO. BY M. BEAYMAN, GOVEENOE. THIS year (1879) has been one of general thrift and prosperity. Ag- riculture has been remunerative. Mining has developed with remark- able success in various parts. Many thousands have been added to our pop- ulation. Schools are encouraged. General health has prevailed. In the administration of justice and the management of public affiiirs great advances have been made, and the interests of the government and Terri- tory cared for with improving economy and fidelity. With the advent of railroaxJs, and the improvement of highways now in progress and in prospect, a large immigration may be looked for, and the facilities for bring- ing in machinery and supplies will cheapen transportation and give life IDAHO. 295 to enterprise. The mild climate of Idaho, its rich resources, its health- fulness, its soil capable of such rich returns, will in time, under favorable legislation, make it the home of a vigorous and enlightened people. BOUNDAEIES. The Territory of Idaho, from its southern base upon Nevada and Utah, in latitude 42° north, to the British possessions at 49°, covers a length of about four hundred and ten miles. In width it is two hundred and fifty-seven miles at its southern and sixty miles at its northern limit. It is separated from the State of Oregon and the Territory of Washington on the west by a direct meridian line, broken by the course of Snake River, which forms its western boundary for about one hundred and fifty miles. On the east its wide base lies against the Territory of Wy- oming, while the Bitter Root, an almost impassable range of mountains forming a natural boundary, separates it from the Territory of Montana. This peculiarity of conformation accounts for the inconvenient shape of the Territory. Since the organization of Idaho, under provision of the act of March 3, 1863, its area has been reduced to form other Territories, until it now comprises 86,294 square miles, equal to 65,228,160 acres. An approxi- mate estimate of the quality of these lands will aiford — suitable for culti- vation in their natural state, 15,000,000 acres; capable of reclamation by irrigation, 12,000,000 acres ; grazing-lands, 5,000,000 acres ; timber- lands, 10,000,000 acres; mining tracts, 8,000,000 acres; the 4,228,160 acres of desert toe destitute of timber and minerals and beyond the reach of irrigation. Large portions of the mining tracts bear timber also. ARIZONA. BY GENERAL JOHN 0. FREMONT, GOVEENOE. ARIZONA has remained shut up and barred out from progress by its inaccessibility. There were neither railroads to it nor in it, nor any roads other than those afforded by the natural surface of the ground, and these are rendered more than ordinarily difficult by the hot, dry, and sandy or stony ground over which lie the approaches to the Territory. In the Territorial laws these are spoken of as desert roads. Lately it has been made possible to reach Arizona on rail from the East by travelling along the 42d parallel of latitude down to San Fran- cisco, in longitude 122°, and thence south-eastwardly backward 720 miles to Yuma, east of longitude 115° and south of latitude 33°. This isola- tion has kept it shut out from immigration and precluded the develop- ment which its great resources would otherwise have commanded. The language habitually applied to it is very descriptive of its remoteness. Californians and Arizonians alike speak of going outside when travelling to Arizona, and inside when returning to the surrounding territory. Broken ranges of mountains, swelling occasionally into lofty peaks and pine-covered masses, and alternating evenly with elevated valleys or mountain-basins of greater or less size, represent in general terms the face of the country in Arizona. Its water-ways are the Colorado and Gila Rivers with their tributaries, of which none enter either stream in the lower part of its course. The valley of the Colorado, between its river-hills or bordering mountains, is dry, stony, and barren, the moun- tains naked rock. Crossing these in journeying from Ehrenberg east- ward, a traveller in spring would find this country covered with bloom, the shrubs and trees being represented mainly by acacias and cacti, and the ground covered with low-flowering plants among grasses growing thinly. Except for some shrub-like trees and gigantic cactus [Sagua7-a), ocotiUo, and yucca trees, the ridges herealong are still of naked, glisten- 296 ARIZONA. 297 ing, and black or barren rock, showing no signs of water. The acacias, Palo verde, and other trees crowd down into the dry stream-beds, reaching after the water below the sands, but the oootillo and the tree-cactus delight in the stony and dry mountain-sides. In the rainy season these stream- beds are short-lived torrents. This is the country traversed by the desert roads. But this character of desert, applied to the valleys, comes only from the heated air and absence of water, and not absence of vegeta- tion. A running stream would make anywhere here a garden. After some seventy miles, as the crow flies, over such country, what may be called fertile mountains are reached ; that is to say, mountains more or less covered with shrubs and grass, and having springs and running streams, and affording good cattle-rangea. Continuing eastward, the country in this respect steadily improves, until, after travelling over about a hundred miles of air-distance from Ehrenberg, scattering ju- nipers of very sturdy growth appear several feet in diameter, with here and there small oaks and locust trees; and presently the road enters among pines, which thenceforward generally cover the more upland parts of the country to the eastward. The elevation here is probably 5000 feet in the valleys, the surround- ing mountains rising several thousand feet higher. On the higher ranges, such as the San Francisco and MogoUon, these open woodlands become extensive forests, where the pines reach sometimes a solid growth of six feet in diameter. From Prescott the San Francisco Mountains show grandly in the horizon of hills, some sixty-five miles away to the north- east, and 12,700 feet above the sea. These and the Mogollon Mountains are the principal water-sheds of Arizona, rising from elevated plateaus of 6000 or 7000 feet into peaks between 9000 and 13,000 feet above the sea. In contradistinction to the Eastern States, where the streams maintain themselves in gathering strength from mountain to sea, dryness is one of the striking features of this whole elevated region. Streams and springs are few and far apart. The larger streams gather no affluents, but waste iiiemselves in absorption and evaporation, and the smaller ones usually sink and disappear under the first valley which they enter, where the soil is generally light and loose enough to absorb them. But the water can there always be found — in the lower country at variable depths of fifty to two hundred and fifty feet, and usually only a few feet below the surface in many of the upland valleys. This may give the necessary provision of water for the farms in the valleys, while the mountains fur- nish it sufficiently for stock. There are two seasons of falling weather — the heavy summer rains, when the washes and stream-beds become tem- 298 THE GREAT WEST. poraiy torrents, and the winter season of rains and snow. Now, at the end of October, the falling weather of the winter has not yet commenced except in the high mountains. The days are warm, the sky is unin- terruptedly cloudless, but ice makes at night, and a light snow has just fallen on the San Francisco Mountain. The grass there is be- ginning to dry up, and the northern face of the mountain is probably covered with snow. The Little Colorado and Salt River regions are reported to be the granaries of the Territory. Their valleys are becoming garden-spots, and the bordering mountains great stock-ranges, where the cattle are sometimes too fat to be driven. Like California, the country is favor- able to animal life. In the Salt River Valley there are probably 100,000 acres under cultivation ; in the Gila Valley, between the Pima villages and the mouth of the canon, about 50,000 ; in the Santa Cruz Valley, about 25,000 ; and 25,000 more in all the southern district. In the Salt River Valley the amount under cultivation is being rapidly augmented to the full extent of the water-supply. On the San Pedro River the land is sparsely occupied, and mostly for grazing ; and farther to the east- ward the countiiy is better adapted to grazing than agriculture. Many years ago I found on the San Pedro and in the neighboring country many wild cattle which had belonged to ranches now deserted, where the people had been killed or driven off by Indians. So far as my present know- ledge goes, the grazing and farming lands comprehend an area about equal to that of the State of New York. The climate of Arizona depends of course upon latitude and elevation. Heat is the dominant feature, and this in the lower country is of an inten- sity seemingly not due to the latitude alone. In the dry, naked valley of the Colorado River the summer heat is intense, and the season of summer encroaches largely upon spring and autumn. Over the eastern part of Southern Arizona it is the same. North of the Gila River, and fifty miles east of the Colorado, the heat is already tempered by the elevation, and farther into the interior the increased elevation and wood-covered mountains make a pleasant and healthy climate. South of the Gila the open, low, dry, and hot region extends farther to the eastward, but the eastern half offers a fine country, increasing in good character to the south up to and beyond the boundary-line. Generally speaking, the climate is noticeably healthy. The heat of the sun does not produce the fatal effects of extreme heat in the moist climates of the Atlantic coast, and though the countiy itself may be said to have regular chill and fever, varying usually in temperature more than 30° between three o'clock in ARIZONA. 299 the afternoon and three o'clock in the morning, this disease is almost un- known to its people. No instance of it has been known on the Colo- rado River, and though there is something of intermittent fever at Tucson, it is thought due rather to the alternate wetting and drying of the ground by irrigation than to any climatic influence. But the chief industry of Arizona — that upon which the others will mainly depend, and that upon which, in fact, the Territory depends for value — consists in the development of its mineral wealth. It is pre-emi- nently a mineral region, capable of sustaining a great mining populktion. Without enumerating others, silver, gold, and copper seem to be the ores most generally diifused throughout the Territory, and among these silver is the charaderistiG. Silver, in combination with gold, copper, lead, and other metals, extends in numerous veins of greater or less size and value from the Colorado River on the west to the eastern boundary-line of the Territory. These have been partly resolved into districts, where, up to this time, mines or lodes of greater value have been discovered grouped together in belts or basins. The Mineral Park district has a belt of this kind which is reported to be nearly a hundred miles long, carrying between porphyry walls a mile and a half breadth of productive ore-matter, which is interspersed with veins, principally chlorides of silver. These are said to be very rich, reaching several hundred dollars the ton. The whole mass is said to carry silver. The Bradshaw district is said to be full of large, permanent veins, upon som,e of which mines have been opened that are producing ores of extra- ordinary value. I mention these as having come more particularly to my knowledge since my arrival, but similar reports are coming in from other parts of the Territory, and more especially from the south-eastern ex- tremity, where veins have been opened which give promise of greater richness in gold and silver than any hitherto discovered. In the imme- diate neighborhood of Prescott are rich mines. Want of transportation, and consequent want of population and money, together with the sense of insecurity still existing, have prevented a full knowledge of these lodes as well as a development of those already known. Left to themselves in the mean time, many settlers, instead of becoming farmers in grain, have become small formers in gold and silver, locating veins or placer-grounds which they work themselves. These gold or silver farms, as they may be called, yield a small but sure product, for which any town is the market. In Arizona are fouiid the only instances within my knowledge where three or four men work- 300 THE GREAT WEST. ing together, without money or outside aid, have managed to develop veins into regular silver-mines, which have already yielded several hun- dred thousand dollars, with a promise of still greater success. But these are the solitary examples of opening large mines without money. The " silver farms," as I have designated them, are smaller enterprises. By a moderate use of money in directing and aiding this kind of labor the general government might come in aid of this industry, and open out a prospect for employment to the large class who of late years have been suffering from want of it, and the utmost exertion of whose skill and in- telligence has not been able to command a support. Aided by the gov- ernment in a way which might be indicated, any man might here find room for his labor, needing only his own resolute, stout work to pick for- tune from the earth. Gold in veins and placers is variously found throughout the Territory. Like Missouri and Utah, Arizona has her Iron Mountain, and copper ores of rich character, carrying with them silver and gold, are found in great force. A large percentage of copper is found in the upper work- ings of silver ores. Many years ago, and before our occupation of the country, I found in Southern Arizona the trail of wagons engaged in transporting copper ore from the Upper Gila to the city of Chihuahua, the silver and gold found in the copper being sufficient to defray the cost cff the long and hazardous journey. Notwithstanding the desultory work- ing of the mines, the actual weekly shipment of bullion, by way of Yuma, to California, is about one hundred thousand dollars. There is a Territorial prison supported by the Territory, and located by law at Yuma. It is managed by a board of Territorial penitentiary directors, who audit claims and make such rules and regulations as they think proper for the discipline and management of the penitentiary. The Legislative Assembly of Arizona meets biennially at the capital on the first Monday in January. Eepresentation is apportioned according to population, and the members of the Assembly are elected by counties at the general election held throughout the Territory every two years on the Tuesday after the first Monday in November. Every male citizen of the United States, and every male citizen of Mexico who shall have elected to become a citizen of the United States under the treaiy of peace exchanged and ratified at QuerStaro in 1848 and the Gadsden treaty of 1854, and every male person who shall have declared on oath before a competent court of record his intention to be- come a citizen of the United States, and shall have taken an oath to support the Constitution and government of the United States, of the ARIZONA. 301 age of twenty-one years, who shall have been a resident of the Territory one year next preceding the election, and of the county or precinct in which he claims his vote ten days, and whose name is enrolled on the great register of such county, shall be entitled to vote at all elections which are now or may be hereafter authorized by law. AKIZONA. BY JOHN "WASSON, 8UKVEY0R-GENEEAL. ACCORDING to departmental estimate made some years ago, Ari- zona contains just about 73,000,000 acres of land, 5,000,000 of which are surveyed. The general character of the topography, soil, pro- portion of arable land, productions, pasturage, minerals, timber, water, etc. is the same as that of New Mexico, Colorado, Utah, Nevada, and Idaho. The Territory was created by act of Congress approved in Feb- ruary, 1863. For ten years its progress was slow, because of the con- stant hostilities of the Indians, its isolation, and lack of speedy and cheap transportation. The United States census of 1870 showed a pop- ulation of 9658, exclusive of Indians, but owing to the danger of Indian attacks and the refusal of the military authorities to furnish the marshal with available assistance, he made no effort to enumerate some settle- ments. Under authority of Territorial law a census was taken in 1876, showing about 30,000, exclusive of Indians ; but the enumeration was made by and under special direction of the several counties, and as legis- lative representation was based thereon, and the location of the capital depended on the action of the legislature thus formed, the said census was made to show a much larger population than existed. Conserva- tive estimates place the present population, exclusive of Indians, at from 30,000 to 33,000, with a steady and rapid increase. The population of nearly all the towns is visibly increasing, and new towns and mining camps have sprung up during this year. There are three marked divisions of surface-land in Arizona — ^viz. val- ley, mountain and mesa, or table — ^their areas rating in the order named. NEVADA. HISTORY. "VTEYADA is a part of the territory ceded to the United States by -Li Mexico in the treaty of Guadalupe Hidalgo, February 22, 1848. It was at first a part of California Territory, and was subsequently at- tached to Utah. It was constituted a Territory in March, 1861, with somewhat smaller boundaries than at present. Its admission as a State was discussed in 1863, and a convention called to form a constitution ; but the cxjnstitution was rejected, on the ground that the population was insufficient for the maintenance of a State government. In 1864 an enabling act was passed, under which a constitutional convention was called, met July 4, 1864, and agreed upon a constitution, under which the State is still governed. The constitution was ratified, and Nevada admitted into the Union as a State October 31, 1864. Additions were made to its territory by Congressional enactment in 1866. Its immense mineral wealth foreshadows for it a brilliant future. This State has an area of about 81,539 square miles, or 52,194,960 acres. PHYSICAL FEATURES. The greater portion of Nevada is included in what is known as the Great American Basin, which has for its surroundings the Sierra Nevada on the west and the Wahsatch Mountains on the east. It is bounded north and south by cross-ranges, and has no outlet for its waters. This vast region is a table-land about four thousand feet above the sea, and the mountains in this vicinity rise from one to eight thousand feet above the level of the sea. About twelve thousand square miles in the south- east of the State are outside of this basin, and belong to the Colorado River Basin, whose lofty table-lands and deep caflons have been else- where described. The Sierra Nevada Mountains constitute the western boundary of the State, their eastern slopes only being included within it. Most of the mountain-ranges are parallel to each other, and have a gen- 302 NEVADA. 303 eral course from north to south. In the south-west is an isolated range, the White Mountains. The eastern slope of the Sierra Nevada and the Humboldt, East Humboldt, and Toyable ranges have a considerable num- ber of streams, which, however, disappear very suddenly from the sur- face, and reappear as lakes or pools farther on. The valleys watered by these streams are in part fertile, but their lowest portions are occupied by muddy pools, impassable in winter from the depth of the mud. The agricultural lands of Nevada are estimated at 17,608,960 acres ; reclaimable swamp-lands, 74,880 acres ; mountain-range land, only avail- able for grazing, and that during only a part of the year, 21,520,280 acres ; and barren, sandy, and worthless lands, 2,151,680 acres. It is doubtful if there are, or have been within the last hundred years or more, any active volcanoes in Nevada, though some of the peaks have shown symptoms threatening eruption ; but no one can traverse its mountains and valleys without finding abundant evidence of the great extent of vol- canic action in the past. The surface of the valleys and plains is almost entirely Tertiary, Quaternary, or Alluvial in some of the lower portions of the valleys, but everywhere the numerous mountain-ranges have"a uniform constitution, the Azoic and metamorphic rocks being upheaved, granite or gneiss and trachyte, rhyolite, and basalt above, and every ridge is crowned with Silurian rocks, limestone, sandstone, etc., all crystallized by the intense heat through which they have passed. On many of the bleak and bare mountain-sides, utterly devoid of vegetation, the lava is still visible, though of course changed by the lapse of time. This Great Basin must have been in ancient geologic times the bed of a vast sea until the sub- sequent upheaval, which may have been aided by some subterranean drainage of the waters. The region outside this Great Basin, belonging to the Colorado Basin, is Eozoic and Silurian in about equal areas. There are marked evidences of volcanic action. MINEEALS. Gold, except in combination with silver, is not abundant, but some of the argentiferous ores contain a large amount of gold in combination, and this seems to increase with the depth of the mines. The Comstock Lode and Consolidation companies, since the great progress made in Sutro Tunnel, are yielding increased amounts of gold, much free gold being found in the ore-veins. In the Humboldt and Walker River regions gold quartz-veins of considerable promise have been discovered. Silver is, however, the staple mineral product of Nevada, and the yield of this 304 THE GREAT WEST. metal is increasing with great rapidity. The silver-lodes are found in almost every part of the State, some yielding from $65 to $100 to the ton, others ranging from $450 to $2500 or more to the ton. The number of mines in this State is very large, and new mines are constantly being opened. In the autumn of 1874 the number of mines was 243 in twelve counties, and the product of gold and silver for that year was $35,402,263, of which $22,000,000 came from Comstock Lode. The Sutro Tunnel is three miles and a half in length, and passes through all the ramifications of the Comstock Lode in Virginia City and Gold Hill, draining the mines at a depth of nearly three thousand feet. The other minerals of Nevada are lead, copper, and iron in various forms. There are numerous mineral springs and some geysera in the State. AGEICULTUEE. While Nevada will never be largely agricultural, it possesses a suffi- ciency of arable lands to supply, with the aid of irrigation, possibly the needs of such a population as it is destined to have, and its mountain- slopes and some of its valleys will prove to be among the best grazing- lands of the Pacific region. Its timber-lands proper, those on which grew the lofty pines of the Sierras, are of very moderate extent, not ex- ceeding 400,000 acres, and much of this is being cut off to supply the demands of the mining districts. The flora of the State, except on the Sierras, differs materially from that of California. Of the sixty-five natural families of plants catalogued in the State, many are repre- sented by a large number of genera and species. AinMALS. The animals are those of the Pacific slope — ^the grizzly bear, the Mex- ican bear, cougar, wild-cat, lynx. Rocky Mountain sheep, antelope, deer (two or three species) ; and most of the smaller game, including the sage- hare, sage-grouse, are the most characteristic mammals. The larger lakes are stocked with trout, salmon-trout, etc., but in the shallow lakes these do not succeed well. CLIMATE. The climate of Nevada is characterized by great extremes. In winter snow falls upon the summit of the mountains, though there is not much in the valleys. The air ls dry, the winds strong, and, though the sun- shine is bright and pleasant at midday, the nights are often intensely cold. In January the mercury falls to from 10° to 16° below zero in the valleys, and much lower in the mountains ; but this severe cold lasts but a few NEVADA. 305 days, though it may be repeated. About the last of February the ap- proach of spring is announced, though there may be piercing winds and sharp frosts, chilling rain and snow, in March, and even April. Thunder- storms of great severity occur in April and May, and into June. When these have passed away the dry season prevails until October throughout the western, central, and northern parts of the State. The air becomes heated, and whirlwinds and spiral columns of dust are raised to great heights. The temperature rises to 100° or 106°, but usually only for a few days. It falls every night to between 70° and 80°, and does not average in August more than 90° at midday. In the eastern part of the State there are frequent thunderstorms in summer and till September 15, and the heat is longer continued and more oppressive. There is less intense cold, with very little snow or frost in winter, in South-eastern Nevada, and the culture of cotton and the sugar-cane has been attempted there. The climate is remarkably healthy and invigorating. EDUCATION. Education is carefully looked after, public schools generally being ac- cessible to all. The State University, located at Elko, affords oppor- tunities for higher education. Among the State eleemosynary institutions may be named the Orphans' Home at Carson, which, though yet in its infancy, constitutes the germ of a commendable institution. Carson City, the capital, had in 1870 a population of 3042. Virginia City, the largest city in the State, had in 1879 an estimated population of 26,000. The principal towns are Grold Hill and Hamilton, each having from four to five thousand inhabitants. THE SUTKO TUNNEL. BY ADOLPH SUTEO. IN the construction of this tunnel we had a severe struggle to get along. On the one hand we had people opposing us, and on the other hand we encountered the difficulty of raising money sufficient to carry on the work ; and that was about the " toughest job " of all. But stiU we suc- ceeded. There were some gentlemen who took broad views of the mat- 20 306 THE GREAT WEST. ter, and, partly through their influence and aid, the money was forthcom- ing, and after that we got along reasonably well. In one way and another, we encountered many difficulties in doing the work. We had to work our way inch by inch through solid rock. In these tunnelling operations we had first to drill a dozen or twenty holes, charge* them with giant-powder, explode the blast, then wait for the smoke of the powder to disappear before we could commence loading the debris on the cars for removal. Under the circumstances one cannot get ahead very fast ; but, altogether, we made quite as rapid progress as has ever been made in any similar undertaking. In fact, our progress was more rapid than was the construction of the Hoosac, the Mont Cenis, the St. Gothard, or any other tunnel. A CHAPTER ON MULES. Up to the present time, all the transportation has been done by means of mules. We found it more convenient to use mules than to use steam, because under ground steam is fatal to life. We are now preparing to use compressed-air motors, built on the same plan as those in use on* Sec- ond Avenue in New York. We have now two motors building in Eng- land. We have been using mules for years, and have found out that they are tolerably good animals ; but there is a prejudice against mules, though they are very intelligent. I think that I could write a chapter on their traits, as I have had a very extensive experience with them. It has been said that they have a strong propensity for kicking, but I have never seen them kick when in the tunnel. They become very tame under ground ; in fact, they become the miners' pets. The men become quite attached to them, and as the shift-mules pass along by the men at lunch they will often receive from one a piece of pie, from another a cup of coffee, etc. When a signal is given to fire a blast the mules understand the signal, and will try to get out of the way of it, just as the men do. Of course, under ground it is very dark, and the mules become so ac- customed to the darkness that when they go out into the sunlight they cannot see very well, and when they go back from the sunlight into the mine they cannot see at all. So we are in the habit of covering one eye with a piece of cloth whenever they go out, and keep the covering over the eye until they go into the tunnel again ; we then remove the cloth ; so they have one good eye to see with. We had to adopt this plan for preserving their sight, because the mule is so stubborn that he will not pull unless he can see his way ahead. We have found out another thing about mules. We tried horses at first, but we found that whenever NEVADA. 307 anything touched the ears of a horse he would throw up his head and break his skull against the overhanging rock ; but if you touch a mule's ears he drops his head. For that reason we could not use horses ; we employed mules, and they have answered very well. OBSTACLES TO PEOGEESS. In carrying on a work of this kind we meet all sorts of difficulties. Now and then we would get indications of water. The men would put in a blast, and the water would pour out in a perfect torrent, and the men would have, at times, to quit temporarily to escape it, and wait until the water had subsided sufficiently, so that they could go to drilling again. Every now and then we would come to a clay that would swell and cave, so as to reduce our progress of one hundred and fifty feet (and afterward with improved machinery of three hundred feet) per month to less than fifty feet per month. Sometimes we could not keep the roof up. As soon as we would get started a little way in our work of excavation the rock would yield, and hundreds of feet would come pressing down on the timbers with such force that it was almost impossible to resist it. The worst ground that we came to was the swelling ground. This is some- times clay, and sometimes it is rock. The moment you dig into it, it swells out, and no matter what size of timbers you use, it will snap them off as if they were but matches. Nothing will resist it. You must let it swell. In one place the swelling was so great that the track swelled up a foot or two seven different times, and each time we had to cut it down. The timbers used are a post and a cap. The pressure on this cap would be so great that the post would be pressed through the cap in twenty-four hours, just as though the cap were a piece of cheese. The only way to keep the timbers from breaking in such ground was to em- ploy men to ease up the ground behind the timbers. That is to say, they would take away the rock or clay from behind the posts from time to time, until, after a year or so, the ground settles down to its natural state and does not swell any longer. We have very little trouble of that sort now ; but I suppose that we shall encounter it every now and then as we go on with the lateral tunnels. BAD AIR. The greatest obstacle encountered by us was the heat and the poor air. Our last opening to the surface was at Shaft No. 2, about nine thousand feet from the tunnel-entrance. From there we had to go to the Comstock Lode, a distance of eleven thousand feet, without any natural air connec- 308 THE GREAT WEST. tion. After we got in to a distance of seventeen thousand feet from the mouth of the tunnel the heat became so intense and the air so bad that it was almost impossible to keep the air suificiently cool and pure to sustain life. There was not oxygen enough in the air to make our candles burn. Although we blew in air by means of blowers and air-compressors, still at times there was not sufficient air to enable the men to work. In the place where the men were at work we could generally manage to keep the air sufficiently pure, but at some distance back from the face of the tunnel the air was so bad that one could hardly exist. In fact, in going through these portions of the tunnel the men would often give out ; and as for the mules, we could not get them there at all. A mule would make straight for the air-pipe, and you could not get him away. "We had one mule that would not go away from the air-pipe at all. They beat him, but it was of no use. He had to be carried out, and that mule escaped; he never went into the tunnel again. A shift-mule would always want to go to where the stream of air was rushing in, and he would monopolize it all to himself. He would never leave it ; but would stand there, and as he bobbed his head up and down past the pipe you would hear the air whistling by him. ACCIDENTS. "We had some sad accidents happen. The air-pipes are made of gal- vanized iron, and the leakage is prevented by wrapping the joints with canvas, which is covered with tar or with white-lead. I recollect that one day after a blast had been fired one Garnett, the man whose duty it was to keep these joints wrapped, went forward (he was nearly fainting) to the end of the air-pipe near the face of the tunnel, but before he got there he fell down in a swoon. When the blaster went forward to ex- amine the blast which had just been made, he found that two of the holes had not gone off, and so he re-connected • them and fired the blast while this poor man was lying on the ground. It did not kill him, although he was riddled with rocks. He had about a hundred large and small pieces of rock in him, one being in the back of his head. I thought that he could not live for ten minutes, but he is alive now and as well as ever. The most curious part of it is, that for a long time previous this man had been in ill-health, and that application of rocks cured him. He has told me often since, "That confounded thing cured me." It was rather a severe cure, but it was efieetual. As we approached Shaft No. 2, nine thousand feet from the tunnel-en- trance, which had been abandoned some time previous because it had JfEVADA. 309 filled by a great influx of water to the depth of about nine hundred feet, we bored a diamond drill-hole into it, and the pressure of that column of water, nine hundred feet high, was so great that it threw out the drill-rod and cast it a distance of several hundred feet, although the rod weighed several hundred pounds. CAEES. Not long ago some timbers broke down, and the report came to me that a man had been killed. We found, however, that he was not injured,, but that he had been caved on and could not get out. I started in with the doctor to see how he was getting on. We found that all the work had stopped, and that the man, who had been working in the ditch which we were then constructing in the floor of the tunnel for the purpose of carrying off the hot water, had been caved on and become surrounded by a lot of loose, fine gravel up to his chest, and that the water running in around this gravel had packed it so tightly that the man could not move. We had to get him out in some way, and so three or four men (which were as many as could get into the confined space) got down alongside of him and tried to dig him out ; but as fast as they would dig the gravel would cave in again. When I reached the place the man had been fast for three or four hours. The miners had built dams above in the tunnel to stop the water from flowing down, for if the water had been permitted to come down it would soon have risen to his mouth, and would have drowned him. He was so fast that he could only move the upper part of his body a little. I urged the men to work away with all their might at the dam to keep the water back ; but after a while they reported that it was of no use — that the water was rising above the dam. We did not want to see the man killed, and used every effort to rescue him. I told the men to pass a rope under his legs and try to pull him out. - We thought we had better pull him out, even if it should injure him some- what, rather than let him drown ; but as soon as we began to pull he commenced to cry out, so that we had to give that plan up. Then the men dug again for a while, until ,the foreman came and said that if W3 did not get him out within ten minutes the water would be down in such volume as to drown him. Then the men worked again with the rope for dear life. At last they got one leg out ; then they gave another jerk, and brought the man out. HOSPITAL. As I have remarked, we employ a surgeon. There were many accidents, althousrh we had less than there were in other works. In the Hoosac o Tunnel one hundred and eighty-five men were killed in the construction 310 THE GREAT WEST. of the work. In our tunnel but twelve men were killed, and I do not think that of the twelve more than three or four were killed by anything actually happening in the tunnel itself. I told our men several years ago that every man employed by the company must pay three dollars per month toward a hospital fund — ^that the company could not afford to give the men all the attention that they ought to receive in case of accidents. The men remonstrated a good deal against this ; they did not wish to spend their money in that way ; each one thought that no accidents would happen to himself; but I made this payment compulsory, and after a while the men became reconciled to it. We employed a physician and opened a drug-store. If a man was injured he received every attention. He had the care of nurses, physicians, and medicine. But these miners are all members of an association, the Miners' Union, which does not per- mit any man to work a shift of eight hours under four dollars per day. All the mine-managers have agreed to yield to their wishes, and I think a man working in these hot places well earns his four dollars. But sometimes the Union will interfere with us where it should not. They sent a deputation to me not long ago to say that we were not pay- ing our men four dollars per day. I said that we were. They said that we deducted three dollars per month for the hospital, and that therefore the men only received one hundred and twenty-seven dollars per month, which was not four dollars per day. I replied that that was for the benefit of the men themselves ; that it was a work of benevolence ; that I had inaugurated it solely for the benefit of the men. They insisted that the men should not be compelled to pay anything to that fund ; and as we had to complete a certain amount of work at a given time, and could not afford to get into any trouble with the men, we had to yield in this matter. STARTING A GEAVEYAED. One labors under all sorts of difficulties in dealing with the men. It seems ridiculous, but the most difficult thing we had to do was to start a graveyard. It took some three years to start it. Whenever a man got killed or died the men would get up a big funeral, and go off to Virginia City or some other place to bury the man. All work had to be stopped for one or two shifts. They would each lose their four dollars for wages, would pay three or four hundred dollars more for teams, and some would drink so freely as to be unfit for work the following day. I was deter- mined to put a stop to that. So said I to the men, " Why can we not have a graveyard of our own, and bury our men here ?" I had a grave dug for the next man that died. The dead man's friends came and said NEVADA. 311 that they would not have the man buried there. I asked them why. They said that it would be too lonely for the poor fellow. This seems ridiculous, but it is a fact. I did not wish to have any trouble over the matter, and so I let them bury the man where they chose. Every time a man died we had just the same trouble again. At last two miners got killed who had not paid their fees to the Miners' Union, and had been discarded. They had no friends there to object, and so we buried them there, and thus were able at last to start our own graveyard. ADVANTAGES OF THE SUTEO TUITNEL. The first great advantage of the Sutro Tunnel is that it creates a new base of operations. We open a new surface for mining operations — a surface which is in fact a better surface than the original one. We are down seventeen hundred feet from the surface, and can introduce water through the shafts, and thus get a fall of seventeen hundred feet; or we can take the water which exists at some point between the surface and the tunnel and let it flow down to run the machinery, which is placed at the tunnel-level. We thus could get an abundant water-power. A very small stream of water with a pressure of seventeen hundred feet will give an immense power. The time will come in the working of these mines when they will economize all of the water. In fact, the water which is brought in pipes from the Sierra Nevada Mountains can be most profit- ably used for that purpose, and the time will come when it will be so used extensively. You can readily perceive that a new surface at that point adds just so much to the working possibility of the Comstock Lode. The lode extends down indefinitely, and the ore-bodies recur in differ- ent places ; we cannot tell exactly how or where, because their distribu- tion seems not to be governed by any known law. This tunnel adds to the working possibility of that lode certainly sixteen hundred and forty feet, which is the level at the point where the Savage Shaft is intercepted by our tunnel, and that shaft is away down the hill. This is, of course, an incalculable advantage, for those sixteen hundred and forty feet are surely added to the working possibility of the Comstock Lode, and ought to be worth to it a great many millions of dollars, perhaps hundreds of millions. The Comstock Lode has already yielded something like four hundred million dollars, and there is in it an enormous quantity of low-grade ore which has not been taken out. UTAH. WHEN Utah was first settled by the Mormons in 1847, it was a ter- ritory belonging to Mexico, but by the treaty of Guadalupe Hi- dalgo in March, 1840, was ceded to the United States, with New Mexico and the whole of Upper California. The government did not promptly assume sway over this newly-acquired territory, and the Mormons estab- lished a government for themselves under the name of the State of Des- eret. Congress, refusing to recognize this government of the Mormons, organized the Territory of Utah on September 9, 1850. Brigham Young was appointed governor. AEEA. Utah Territory is situated north of Arizona, east of Nevada, south of Idaho, and west of Colorado, and is between the 37th and 42d parallels of north latitude and the 109th and 114th meridians west from Green- wich. It has a maximum length of 325 miles by a breadth of 300 ; area, 84,476 square miles ; population, estimated at 130,000. It is intersected from north to south by the Wahsatch Mountains, dividing it nearly equally between the Great Basin and the basin of the Bio Colorado. The altitude of the surface on both sides of this mountain-range is about the same — the valleys four to six thousand feet above sea-level; the mountains, six to thirteen thousand. West of the Wahsatch the drainage is into lakes and sinks which have no outlet, the largest of which is Great Salt Lake, with an elevation of 4260 feet, a shore-line of 350 miles, and an area of three to four thousand square miles. It receives the Bear and Weber and many smaller streams, and also the discharge from Utah Lake through the river Jordan. The latter is sweet water, about ten by thirty miles in extent, the receptacle of American, Provo, and Spanish Rivers. There are numerous valleys, the lowest of them higher than the average summit of the AUeghanies. 312 ECHO CaSoN, UTAH. VTAH. 313 TOPOGEAPHY AND GENERAL FEATUEBS. The settled part of Utah lies along the western base of the Wahsatch Mountains, which run through the heart of the Territory from north to south, reaching their greatest altitude near Salt Lake City (where they abut on the Uintah range coming from the east, forming the cross-bar of a T), and almost losing themselves in the sandstone plateau of the Rio Colorado in the south. Abreast of Salt Lake City the Wahsatch range is ten to twelve thousand feet in altitude. Here, within a small area, rise the Bear and Weber Rivers, which empty into Salt Lake; the Provo, which empties into Utah Lake ; and some of the main affluents of the Green River, which, with the Grand, become the Rio Colorado lower down. It is in the vicinity of the heads of these rivers that the Emma, the Flagstaff, the Vallejo, the Ontario, McHenry, and various other well-known mines are situated. Nearly one-half of the Territory lies south of the Uintah range and east of the Wahsatch range proper, and is drained by the Green and Colorado Rivers and their tributaries. Its general altitude along these streams is between four and five thousand feet ; it is much broken by mountains, and is but partially explored, and not settled at all. It contains many thousand square miles of fine graz- ing country above the Grand Caflon, with more or less arable land, and no one yet knows what mineral treasures. It is believed that the Atchi- son, Topeka, and Santa FS Railroad, after being drawn to the head of the river Arkansas by the mineral attractions of Leadville, will find an easy way through this region, entering the Great Basin vid some of the feasible railroad-passes of the Wahsatch. A wide strip of the western part of the Territory is lake, sink, mountain, or desert. The inhabited part is chiefly a narrow belt, watered by the streams of the western slope of the Wahsatch range, which lose themselves in inland lakes or basins. The largest and best known of these is the Great Salt Lake Basin. GREAT SALT LAKE BASIN. Including the valley of Bear River up to the Gates on the north, and the Utah Basin on the south, whose waters are discharged into Great Salt Lake through Jordan River, this basin is 200 miles in length by 40 or 60 in width. The principal streams which are lost in Great Salt Lake are the Malade and Bear — the latter 300 miles long — on the north ; Box Elder and Willow Creeks, Ogden and Weber Rivers, on the east ; and City, Mill, and Cottonwood Creeks and the river Jordan on the south. Into Utah Lake flow the American, Provo, and Spanish Forks — ^though 314 THE GREAT WEST. these are not forks, but independent mountain-streams — and Salt Creek. All of them but the Malade have in the Wahsatch range their sources, which collect the snows in winter that give them life and being. Where they emerge from their caflons settlements have been made on them, and their waters appropriated, so far as it can be cheaply done, for the pur- poses of irrigation, and in some cases of furnishing power for mills. Of these settlements, the largest is Salt Lake City, located about centrally, as regards the length of the entire basin, at the base of the Wahsatch range, ten or twelve miles from the south-east shore of Salt Lake, and • containing a population of about twenty-five thousand. The city is sup- plied with water by City Creek. It is laid out with broad streets and sidewalks, and is built up more or less for two miles square, shade and fruit trees largely hiding the buildings in the summer season. It has ample hotel accommodations, gas, water, and street-cars ; is peaceful and orderly; is connected with the outside world and adjacent points of interest or business by rail. Enjoying the most healthy and agreeable climate of perhaps any large town in the United States ; with street-cars running to the famous Warm Springs, and the bathing-shores of Salt Lake but a half hour's ride distant on the rail ; with peaks of the Wah- satch, the Oquirrh, and other ranges ruiHing the clouds at every point of the horizon ; with picturesque mountain-canons threaded by trout-streams accessible by rail, — it is one of the most attractive places of summer resort for tourists seeking health or pleasure in all the world. The eastern edge of Salt Lake Basin is dotted with settlements, and is highly cultivated wherever water can be got on the ground. These are North String, Bear River City, Corinne, Brigham City, Willard, North Ogden, Ogden, Kaysville, Farmington, Centreville, Bountiful, Salt Lake City, the Cottonwoods, Sandy, West Jordan, Deweyville, Lehi, American Fork, Pleasant Grove, Provo, Springville, Spanish Fork, Salem, Payson, San- taquin, Mona, Nephi, and Levan. Ogden, at the intersection of the east and west and north and south railroads, is the town next in importance to Salt Lake City, the capital. It is in the forks of Ogden and Weber Rivers, is within a short drive of fine fishing and mountain-scenery, and is rapidly improving. Great Salt Lake Basin at large has an altitude of about forty-five hundred feet above the sea, and is the paradise of the farmer, the horticulturist, and the grower of fruit. Cut off from it by a low range, now surmounted by the Utah and Northern Railway, toward the north-east is Cache Valley, UTAH. 315 CACHE, SAN PETE, AND SEVIER VALLEYS. Cache Valley is oval in shape, perhaps ten by fifty miles in extent, watered by Logan and Blacksmith Forks of Bear Kiver, and by the latter itself, and sustaining a settlement wherever a stream breaks out of the enclosing mountains. Logan is the principal town of Cache Valley, and thence one drives eastward through Logan Canon forty or fifty miles to Bear Lake Valley, Bear Eiver here flowing toward the north. Farther on it bends to the west and southward, and, flowing down through Cache Valley, finds its way to Salt Lake. Cache and Bear Lake Valleys have, a score of towns and fifteen thousand inhabitants. To the south-east of Salt Lake Basin, and to be connected with it by rail through Salt Creek or Nephi Canon this season, lies San Pete Valley, called the granary of Utah, surrounded by mountains except on the south, where the San Pete River breaks through into the Sevier, and sustain- ing eight thriving towns, all still in their infancy, though founded several years ago. San Pete and Cache Valleys are fine grain-growing sections, but, having colder winters, are not so well adapted to fruit-raising as the Salt Lake Basin. Next southward is the Sevier River, which has its source in Fish (Indian, Panguitch) Lake, near the southern boundary of the Territory, and runs, like Bear River, a long way north before it finds a way out of the mountains, and turning to the south-west is finally lost in Sevier Lake. Most of the streams in the south-west lose themselves in small lakes or sinks ; that is, such as rise to the northward of the divide between the Great Basin and the Rio Colorado country. The Sevier River Valley is occupied, like all the other Utah valleys (and there are many in the re- cesses of the Wahsatch, and some outlying and disconnected with that range, although of minor importance, which have not been particularly noticed) where a strisam breaks out of the adjoining mountains, by a settle- ment ; but, like the other streams, the full capacity of the Sevier River for irrigation has not yet been called into requisition. GREAT SALT LAKE VALLEY. The western third of the Territory from end to end is an alternation of mountain, desert, sink, and lake, with few oases of arable or grazing lands. Great Salt Lake covers an area of three to four thousand square miles, and the desert west of it a still larger area. The Sevier, Preuss, and Little Salt Lakes, all together, are small in comparison. Formerly, a mighty river flowed northward from the vicinity of Sevier Lake to the ^316 THE GREAT WEST. "westward of Great Salt Lake, the dry bed of which, nearly a mile in width, must be crossed in going west from Salt Lake City to Deep Creek, Since it dried up hills and spurs of mountains have been upheaved in its course, but the old channel continues on its way up hill and down, and over them all. Divided off from Great Salt Lake by a sort of causeway eight hundred feet high is Rush Valley, containing a lake covering twenty to thirty square miles, where twenty years ago there was hay-land and a military reservation. This, as well as the accompanying filling up of the Great Salt Lake, shows a decided aqueous increase in Salt Lake Basin within that time. Rush Valley has mining and agricultural settlements, but much more pastoral than arable land ; and so has Skull Valley to the westward. But from these south to the rim of the basin there are only occasional habitable spots, and they are due to springs. THE MOUNTAINS. The mountains are the source of the wealth of Utah, present and pros- pective, which consists in water and metals. They gather the snows in winter which feed the streams in summer. In the northern part of the Territory the Wahsatch range attains in general a high altitude, with a mass in proportion. There is a large accumulation of snow in winter, and the streams are correspondingly large and numerous. In the southern part of the Territory the main range is lower and less massive ; the average temperature is higher, of course; there is less snow, smaller and fewer streams, and more desert in proportion. This part of the Territory is not rich in agricultural resources. The isolated ranges in the Great Basin seldom give rise to streams of much magnitude, and the interven- ing valleys partake more of the desert character. But all the mountains, so far as known, are full of minerals, and there is generally water enough for the purposes of mining and reducing them. AGEICCLTUEE. Down to June 30, 1878, there were surveyed of public land in Utah 8,178,819 acires of arable, timbered, coal, and mineral land. It is im- possible to tell from any accessible data what proportion of it is arable land — ^probably not more than one-fourth, or 2,000,000 acres. Irrigation is much used, and is almost an indispensable element in farming. The scarcity of water compels settlement along the streams and by the borders of lakes ; but that Utah is productive in the various cereal crops can be realized from the fact that the yield of wheat in one year (1875) was 1,418,783 bushels, while the total value in that year of the UTAH. 317 various crops was $7,500,000. Improved lands are held at from twenty- five to one hundred dollars an acre, according to location. There are, however, large bodies of government and railroad lands which can be obtained at low rates. But it is more advantageous to colonies than to in- dividuals to purchase these latter, as irrigation can thereby be obtained by the construction of canals at very low cost. Fruits thrive abundantly in Utah, as apples, pears, peaches, plums, apricots, cherries, and grapes. STOCK-RAISING. This is one of the great resources of Utah. The grazing-lands are almost unlimited, including the second tables of the river-courses, the slopes of the foot-hills and lesser ranges not too far from water, the shores of sinks and lakes, and the coves and valleys of the mountains. In the elevated portions of the Territory stock requires shelter, but in the Salt Lake Basin and farther south it generally thrives without much if any protection through the winter. It is estimated by stock-growers and drivers that the Territory turns out yearly forty thousand head of stock from one to four years old, averaging in value $15 a head — ^a total of $600,000. The wool-clip for 1878 was 1,600,000 pounds. The Mormon popula- tion is chiefly engaged in agriculture, and the wonderful development of the mineral resources is mainly due to the Gentile population, who are really dependent upon the mines for their support. MINERALS. Mines were known to exist in Utah, and some attempts were made to open and work them, during the five years next preceding the completion of the Pacific Railroad, but the conditions were not favorable, and little was accomplished. On the consummation of that enterprise, however, attention was recalled to them, and within eighteen months thereafter the streets of Salt Lake City were thronged with wagons and teams bringing ore from almost every point of the compass and from twenty to two hun- dred miles distant. Rude mining camps, gradually growing into towns, mills, sampling-works, and smelters, began to appear as if by magic. From the end of 1870 to the end of 1878, as appears from the books of the Utah Central Railroad Company, there were shipped from Salt Lake City 76,912 tons of ore, 109,276 tons of argentiferous lead-bullion, and 8197 tons of lead — ^worth, in the aggregate, quite $40,000,000. For the last three years the value of Utah's mineral output has been 318 THE GREAT WEST. $18,558,805.48. Most of the ores so far worked have been argentiferous galena, but the present depression in the price of lead decreases the profits realized from that kind of ores. Lead represents only $5,379,446 of the product of the last three years, against $13,137,033 of the precious metals, and of last year but $811,068, against $5,224,580, or less than six- teen per cent. And, further, as the profit on lead has decreased, mines producing gold and silver ores proper have been discovered or have risen into prominence. Such are the Ontario, which has paid forty-two con- secutive dividends of $50,000 each ; the mines of Silver Reef, which, first discovered two years ago, are now producing fine bullion at the rate of $100,000 per month ; and the gold-mines in Bingham Caflon, the ores of which, though of comparatively low grade, are very ch-eaply mined and milled, and occur, so far as work has shown, in veins or deposits of extraordinary size and strength. There is not a county in the Territory where mines have not been located and mining districts in greater or lesser number organized. Froiseth's new map of Utah shows eighty of these new mining districts, covering more than one million acres, crowding each other most in Salt Lake, Utah, Juab, and Beaver counties. Box Elder, Tooele, Millard, Piute, and Iron counties have a plentiful sprinkling of them. Wherever there are mountains the prospector has been, and left his footprints in the shape of mining districts. Very many of them are abandoned, it is true, but this is more often on account of ina