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^ til- o • • , •* .''V;* o •n*.o< <^ ''TT.* <&^ ..♦ .A> <> *'7V.* ,6 K* J' \. •A* oil** ^^ O"^ .•"•♦ ^O A* o-JJ"* ^ a5°^ .1 .T* .A V .'^ ... C-" ♦'. "'V'-^-/ %'^^'/ "°^^^-/ V*^'^*,^*' "o^^ {% V.^^^ :M£'^ ^^..^^ ;,^^\ V..^^ .^iJ^fA'o U..^"^ y^^\ % ,0* *o. ' • • • \" x< ."i.^ . . • . - <» ^•^..^^ .-afo'v \/ .'^'o %,^^ .-a^--, "^.^ ^^ "K ^. HISTORY M X mm ^^ MBRCBR COITIB MISSOURI From the Earliest Time to the Present; TOGBTHHR WITH Sundry Personal, Eusiness and Protesslonal SJ^etclies AND FAMILY RECORDS, Bbsides a Condensed History of the State OF Missouri, Etc. HjHitTSTE-A-TEX). ^t- st. louis and chicago: Thb Goodsfebd Publishing Co. CHICAGO. JOHN MORRIS COMPANY, PRINTERS. cii^-lO^^^'^ rr PREFACE. This volume has been prepared in response to the prevailing and popular demand for the preservation of local history and biography. The method of preparation followed is the most successful and the most satisfactory yet devised — the most successful in the enormous number of volumes circulated, and the most satisfactory in the general preservation of personal biography and family record conjointly with local history. The number of volumes now being distributed seems fabulous. Careful estimates place the number circulated in Ohio at 50,000 volumes; Pennsylvania, 60,000; New York, 75,000; Indiana 40,000; Illinois, 40,000; Iowa, 35,000; Missouri, 25,000; Minnesota, 15,000; Nebraska, 15,000, and all the other States at the same pro- portionate rate. The southern half of Missoui'i has as yet scarcely been touched by the historian, but is now being rapidly written. The design of the present extensive historical and biographical research is more to gather and preserve in attractive form, while fresh with the evidence of truth, the enormous fund of perishing occiUTence, than to abstract from insufficient contemporaneous data remote, doubt- ful or incorrect conclusions. The true perspective of the landscape of life can only be seen from the distance that lends enchantment to the view. It is asserted that no person is competent to write a philo- sophical history of his own time; that, owing to imperfect and conflicting circumstantial evidence, that yet conceals instead of reveals the truth, he cannot take that correct, unprejudiced, logical, luminous and comprehensive view of passing events that will enable him to di-aw accurate and enduring conclusions. The duty, then, of a histo- rian of his own time is to collect, classify and preserve the material for the final historian of the future. The present historian deals in fact; the future historian in conclusion. The work of the former is statistical ; of the latter, philosophical. To him who has not attempted the collection of historical data, the obstacles to be surmounted are unknown. Doubtful traditions, conflicting statements, imperfect records, inaccurate public and private coiTespondence, the bias or untruthfulness of informers, and the gen- eral obscurity which, more or less, envelops all passing events, com- bine to bewilder and mislead. The publishers of this volume, fully aware of their inability to furnish a perfect history, an accomplishment vouchsafed to the imagination only of the dreamer or the theorist, make no pretension of having prepared a work devoid of blemish. They feel assui-ed that all thoughtful people, at present and in future, will recognize and appreciate the importance of their undertaking, and the great public benefit that has been accomplished. QO IT PEEFACE. To the county officials of both Harrison and Mercer Counties and the J d putles, t^ .vhom the publishers are indebted for nmform cu- tesy and material aid in research, ^e offer expressions of gratitude to the gentlemen of the press, our hearty thanks for the ^^^^^^]^'^l their endorsement: to the clerks or secretaries of varM^us educations , itera^ secret, benevolent, military and municipal ^-^^-p-}^jf^'^,' acknow edcmekts, and to all the people, to whose cordial and mtel^ Ugent co-operation the success of th^s work is due- -^ J^f^^f' *^«^ hSpe and belief that the history of their county will prove authentic and be acceptable. Much valuable information has been gathered from Hon ff J. Heaston, to whom, among others, the publishers feel specially indebted. With the assurance that our promises have been more than fulfilled, we tender this fine volume to oui- patrons. THE PUBLISHERS. rEBBUAEY, 1888. CONTENTS. PART I.— HISTORY OF MISSOURI. PAGE. Attitude of Missouri before the War 94 ArticIeXV 147 Amendments to the State Constitution 149 Attorney Generals 164 Auditors of Public Accounts 165 Boone's Lick (."ouulry 61 Black Hawk War 67 Beginning of Civil War 92 Boonville 113 Belmont 126 Battle of Pea Ridge 127 Battle of Kirksville 130 Battle at Independence 131 Battles of Lone Jack and Newtonia 132 Battle of Cane Hill 133 Battles of Springfield, Hartsville and Cape Girardeau 133 Battles in Missouri, List of. 142 Baptist Church 159 Clay Compromise, The 65 Constitutional Convention of 1845 74 Campaign of 1861 113 Carthage. 115 Capture of Lexington , 123 Campaign of 1862 127 Compton's Ferry 131 Campaign of 1863 133 Campaign of 1864 137 Centralia Massacre 140 Churches 159 Christian Church 159 Congregational Church 160 Conclusion 197 Dred t^cott Decision, The 87 Death of Bill Anderson 141 Drake Constitution, The 143 Divisions in the Republican Party 147 Dates of Organization of Counties with Origin of ^ames. etc 181 Early Discoveries and Explorers 44 Early Settlements „ 47 Earthquakes at New Madrid 58 Enterprise and Advancement 62 Events Preceding the Civil War 89 Efforts toward Conciliation 104 Emancipation Proclamation and XHIth Amendment Ill Execution of Rebel Prisoners 132 Election of I8S4, The 156 Early Courts, The 157 Episcopal Church 160 French and Indian War 48 Founding of St. Louis, The 49 From 1785 to 1800 65 First General Assembly 66 Fremont in the Field 125 Friends' Church 160 Fire at St. Louis, The Great 79 Geology 12 Gov. Jackson and the Missouri Legislature 97 Gov. Crittenden's AdmiDistration 151 Governors 163 PAGE. Hannibal and St. Joseph Railroad Contro- versies 152 Indian and Other Races 42 Israelite Church 160 Jackson Resolutions, The 80 Judges of Supreme Court 165 La Salle 46 Louisiana. District and Territory of 56 Louisiana Purchased by the United Slates.. 55 Lewis and Clark's Expedition 57 Lutheran Church 161 Lieutenant-Governors '. 164 Minerals and Mineral Springs 23-38 Manufacturing 39 Marquette 45 Missouri a Territory 69 Mormons and Mormon War, The 71 Mexican War, The 75 ^lartial Law Declared 123 Murders at Gun City 149 Methodist Episcopal Church 161 Methodist Episcopal Church South 162 Missouri's Delegation in the Confederate Congress 168 Organization of Kansas and Nebraska 82 Operations against Guerrillas 129 Order No. 11 134 Officers Previous to State Organization 162 Officers of State Government 163 Pontiac, Death of 51 Public and Private Schools 157 Presidential Elections 169 Proclamation by Gov. Jackson 105 Resources 11 Rock Formation 15 Railroads 40 Revision of the State Constitution 150 Representatives to Congress 166 Rebel Governors 169 Soils, Clays, etc 13 State Organization 63 State Convention 64 Seminole War 68 Secession 90 Surrender of Camp Jackson 98 Slate Convention, The 109 Springfield , 125 Shelby's Raid 137 State Constitutional Convention 143 Secretaries of State 164 State Treasurers 164 Salaries of State Officers 181 I'niteri States Senators 166 Votes by Counties at Presidential Elections from IS36 to 1884 171-181 Wealth 41 War of the Revolution, The 52 War with Great Britain in 1812 60 Western Department, The 117 Wilson Creek 118 Year of the Great Waters 54 VI CONTENTS. PART II.— HISTORY OF HARRISON COUNTY. PAGE. Andover ||2 Akron ^'r Bloody Deed of an Insane Man 285 Bethany Schools 319 Bethany, History of 339 Bethany's Growth and Development 349 Blytbedale 376 Blue Ridge 380 Brooklyn °1" Bolton 383 Bridgeport ^»J Cereals of Harrison County 20C County Organization 233 County Court and Proceedings, The 234 County Seat and Public Buildings 239 Census and Statistics 250 Courts and Bench and Bar 25o Crimes and Casualties 283 Churches of Bethany p99 Churches of Cainesville 305 Churches of Eagleville and Vicinity 308 Churches of Rid^eway 311 Churches of Blytbedale 312 Churches of Mount Moriah 313 Churches of New Hampton 313 County Schools 317 Cainesville Schools o-^ Civil War, Preparation for 326 Cities and Towns 838 Cainesville, History of 357 Early Settlement 209 Early Mills 215 Early and Subsequent Boundaries 233 Early Records 248 Elliott Fratricide, The 284 Educational 315 Enrolled Missouri Militia 337 EagleviUe 366 First Settlers 209 First County Court Officials 238 Fatal Accidents 297 Gardner 38- Hallock Murder, The 289 Incidents of Early Days 217 Indian Trading 220 Infantry and Cavalry Regiments 333-337 Jacksonville 382 Killvan War, The 223 and 323 Killing of Charles Burger 284 Killing of John Garrison 285 Killing of McCullum 285 Killing of Isaac Moore ^te* ^^^ Killing of Jacob Fanster ■'•^P- ^*'' Liind Opened for Entry 4>- --' Lorraine 378 Mormon War, The 227 and 325 Mysterious Death of a Young Lady 287 Murder of Albert Hines 288 Military History 322 " Merrill's Horse" 332 Mount Moriah 370 Martinsville 377 Mitchellville 383 New Hampton ■■- 381 Official Directory 2.'>2 Physical Features 203 Prairie 205 Paupers - 248 Press, Elections and Railroads 272 Pleasant Ridge 383 Relocation of County Seat Considered 263 Religious History 299 Ridgeway 373 Streams ^^* Stone, Coal and Mineral Water 206 Settlements, Where Made 215 Stabbing of Jacob Mitchell 284 Sundry (?rimes 286 Suicides ■ 295 Sundry Churches 309 and 315 Topography 203 Timber ^"3 "The.Firsts" " 232 Townships Created 244 Township Organization 247 Twenty-third' Regiment 330 Volunteer Troops for Civil War 328 HISTORY OF MERCER COUNTY. PAGE. Agricultural Association 438 Boundary, Topography and Soil 386 Bench and Bar j21 Baptist Churches 469 County Formation and Organization 401 County Buildings *11 County Officials 411 County Court, The *13 Court Proceedings 414 Clyde Case, The 41' Chipps Homicide, The 420 Christian Churches 468 Catholic Churches 469 Era of Settlement 387 Early Settlements, Circumstance of. 388 Electious, Early and Recent 405 Early Indictments for Crimes 416 Educational History 469 Early Schools of Mercer County 4il First Settlements, The 395 Financial Affairs of the County 408 Goshen 446 Heatherly War, The -iSs Halleck Case, The 418 Homicide of Graves 420 Half Rock 445 Indians, The 394 PAGE. Indictment against Beniamin Smothers 414 Infantry and Cavalry Regiments 448 Killing of Frank Cox 418 Killing of Davis 420 Mullinax Case, The 41» Mercer County Medical Society 438 Modena or Madisonville 4*4 Mill Grove *** Middlebury 445 Mercer County before the War 447 Methodist Episcopal Church 46.J Organization •■■.■ 401 f)rganization of School Townships 472 Physical Features ™5 Population and Nativity • 401 Princeton, Origin and Early Development of 4i3 Princeton, Subsequent History of 423 Princeton's Present Business Interests 425 Protestant Methodist Churches 464 Pauper Schools 469 l'i6sourccs ....■...........•........•••■■■•-•••■■" "O*^ Railroad Bonds and Stock 408 RaiuesCase, The 419 R.avanna, History of 440 Religious History 45J State Boundary tjuestion .■■.■■ 404 Sketch of Military Organizations in County 448 CONTENTS. VII PAQE. School Statistics * 473 Schools of PrincetOD 474 Timber, Agricultural Products, etc 386 Township Settlements 397 PAGE. Township Formation and Organization 403 Towns of the County 423 The Great Rebellion 447 United Brethren Church 468 BIOGEAPHICAL APPENDIX. '"'"""f """•""""' ^ POETKAITS. Gen. B.M. Prentiss 249 Hon. W.P. Robinson 313 Hon. D. J. Heaston 377 D.S. AlTord 479 Joseph Webb 644 PART I. HISTORY OF MISSOURI. History of Missouri, INTRODUCTOEY. MISSOURI, the eighth State of the Union in size, the seventh in wealth, and the fifth in population and politi- cal power, lies in the very heart of the Mississippi Valley. Extend- ing from the thirty-sixth nearly to the forty-first degree of north latitude, it has considerable diversity both of soil and climate. Its eastern limit is marked from north to south by the great " Father of Waters," and the Missouri washes its western bound- ary, from the northwest corner southward about 250 miles to the mouth of the Kansas, and thence flows south of east through the heart of the State, and joins its muddy torreft^ with the waters of the Mississippi. These two mighty rivers have many tributaries which are, to a greater or less extent, navigable for steamboats, keelboats and barges. The extreme length of the State is 328 miles; the extreme breadth, in the southern part, is 280 miles; and the average breadth 250 miles. Missouri has an area of 65,350 square miles, or 41,82-i,000 acres. It has 18,350 more square miles than the State of New York, is nearly nine times the size of Massachusetts, and exceeds in extent all of the New England States combined. There is no State in the Union which surpasses Missouri in respect to geographical situation and natural resources. Other Note.— In the compilation of the State History the authors consulted, an^ong others, the followiug authorities: "State Geological Reports;" "Charlevoix's Journal of a Voyage to North America in 1721;*' Stoddard's ''Historical Sketches of Louisiana;" Schoolcraft's " Narrative Jour- nal;" Breckenridge; Pike's "Expedition;" .Switzler's "History of Missouri;" Bradbury's "Trav- els;" " Lillimau'a JoutbhI;" " American Cyclopedia;" Beck's '■ Gazetteer of Indiana and "Missouri," 1823; Wetmore's " Gazetteer of Missouri," 18.^7; Shehaid's "Early History of St. I.ouis and Mis- souri;" Parker's " Missouri As It Is in 18G7;" Davis & Durrie's " History of Missouri," 1876. 12 HISTOBY OF MISSOURI. regions may boast of delightful climate, rich and productive soil, abundant timber, or inexhaustible mineral deposits, but Mis- souri has all of these. She has more and better iron than England and quite as much coal, while her lead deposits are rivaled by that of no other country of equal area upon the globe. The population of the State, according to the census of 1880, was 2,168,380, showing an increase of 25.9 per cent within the preceding decade. GEOLOGY. The stratified rocks of Missouri may be classified as follows, enumerating them from the surface downward: /. Quaternary or Post Tertiary. — Alluvium, 30 feet thick. Soils — Pebbles and sand, clays, vegetable mold or humus, bog iron ore, calcareous tufa, stalactites and stalagmites, marls; bot- tom prairie, 35 feet thick; bluff, 200 feet thick; drift. 155 feet thick. II. Tertiary. — Clays, shales, iron ores, sandstone, fine and coarse sands. ///. Cretaceous. — No. 1, 13 feet, argillaceous variegated sandstone; No. 2^20 feet, soft bluish brown sandy slate, con- taining quantiti^of iron pyrites; No. 3, 25 feet, whitish brown impure sandstone, banded with purple and pink; No. 4, 45 feet, slate, like No. 2; No. 5, 45 feet, fine white siliceous clay, inter- stratified with white flint, more or less spotted and banded with pink and purple ; No. 6, 10 feet, purple red and blue clays. En- tire thickness, 158 feet. IV. Carboniferous. — Upper carboniferous or coal measures, sandstone, limestone, shales, clays, marls, spathic iron ores, coals. Lower carboniferous or mountain limestone, upper Archimedes limestone, 200 feet; ferruginous sandstone, 195 feet; middle Ar- chimedes limestone, 50 feet; St. Louis limestone, 250 feet; oolitic limestone, 25 feet; lower Archimedes limestone, 350 feet; encrinital limestone, 500 feet. V. Devonian. — Chemung group: Chouteau limestone, 85 feet; vermicular sandstone, 75 feet; lithographic limestone, 12.5 feet. Hamilton group: Blue shales, 40 feet; semi-crystalline limestone, 107 feet; Onondaga limestone, Oriskany sandstone. HISTORY OF MISSOURI. 13 VI. Silurian. — Upper silurian: Lower Helderberg, 350 feet; Niagara group, 200 feet; Cape Girardeau limestone, 60 feet. Lower silurian: Hudson Eiver group, 220 feet; Trenton limestone, 350 feet; Black River and Birdseye limestone, 75 feet; first magnesian limestone, 200 feet; saccharoidal sandstone, 125 feet; second magnesian limestone, 230 feet; second sand- stone, 115 feet; third magnesian limestone, 350 feet; third sand- stone, 60 feet; fourth magnesian limestone, 300 feet. VII. Azoic Eocks. The Quaternary rocks, the most recent of all the formations, contain the entire geological record of all the cycles from the end of the Tertiary period to the present time; and their economical value is also greater than that of all the other formations com- bined. This system comprises the drift and all the deposits above it. There are, within the system, four distinct and strongly defined formations in the State, namely; Alluvium, bottom prairie, bluff and drift. SOILS. Soils are a compound of pulverized and decomposed mineral substances, mingled with decayed vegetable and animal re- mains, and containing all the ingredients necessary to the sus- tenance of the vegetable kingdom. The soils of Missouri have been produced by the mixing of organic matter with the pulver- ized marls, clays and sands of the Quaternary deposits which are found in great abundance in nearly all parts of the State, and are of material best designed for their rapid formation. For this cause the soils of the State are marvelously deep and pro- ductive, except in a few localities where the materials of the Qua- ternary sti'ata are very coarse, or entirely wanting. CLAYS. Clays are dark, bluish-gray strata, more or less mixed with particles of flint, limestone and decomposed organic matter. When the floods of the Mississippi and the Missouri subside, lagoons, sloughs and lakes are left full of turbid water. The coarser substances soon subside into a stratum of sand, but the finer particles settle more slowly and form the silico-calcareous 14 HISTORY OF MISSOURI. cluys of the alluvial bottom. Thus, after each flood, strata of sand and clay are deposited, until the lakes and lagoons are filled up. Then a stratum of humus, or decayed vegetable matter, is formed by the decomposition of the annual growth and of the foreign matter which falls into the water, and every succeeding crop of vegetation adds another such stratum. Thus are rapidly formed thick beds of vegetable mold, yielding support to the magnificent forest trees which grow upon the sites of those ancient lakes and morasses. In this manner have been formed the vast, alluvial plains bordering upon the Missouri and Missis- sippi Eivers, which comprise about 4,000,000 acres of land, based upon these strata of sand, clays, marls and humus. The soil formed upon these alluvial beds is deep, rich and light almost beyond comparison, and is constantly increasing by the filling up of lakes and sloughs as above described. THE BLUFF OB LOESS. This occurs in the Missouri bluffs forming a belt of several miles in width, extending from the mouth of the Missouri to the northwest corner of the State, where it is found just beneath the soil, and also in the bluffs of the Mississippi fi-om Dubuque to the mouth of the Ohio. Thus while the bottom prairie occupies a higher geological horizon, the bluff is usually several hundred feet above it topographically. The latter is generally a finely comminuted, siliceous marl, of a light, brown color, and often weathers into perpendicular escarpments. Concretions of lime- stone are often found, and to the marly character of these clays may be ascribed the richness of the overlying soil. It is to this formation that the Central Mississippi and Southern Missouri valleys owe their superiority in agriculture. Where it is best developed in Western Missouri the soil is equal to any in the country. DRIFT. This formation exists throughout Northern Missouri. The upper members consist of stiff, tenacious, brown, drab and blue clays, often mottled and sometimes containing rounded pebbles, HISTORY OF MISSOUBI. 15 chiefly of granite rocks. The lower division includes beds of dark blue clay, often hardening on exposure, frequently overlaid and sometimes interstratified with beds and pockets of sand, sometimes inclosing leaves and remains of trees. Good springs originate in these sand beds, and when they are ferruginous the springs are chalybeate. TEBTIAET SYSTEM. There is a formation made up of clays, shales, iron ores, sandstone, and a variety of fine and coarse sand, extending along the bluffs, and skirting the bottoms, from Commerce, in Scott County, westward to Stoddard, and thence south to the Chalk Bluffs in Arkansas. The iron ore of these beds is very abundant, and exceedingly valuable. The spathic ore has been found in no other locality in Southeastern Missouri, so that the large quantity and excel- lent quality of these beds will render them very valuable for the various purposes to which this ore is peculiarly adapted. The white sand of these beds is available for glass making, and for the composition of mortars and cements. The clays are well adapted to the manufacture of pottery and stoneware. CRETACEOUS ROCKS. These strata are very much disturbed, fractured, upheaved and tilted, so as to form various faults and axes, anticlinal and synclinal; while the. strata, above described as tertiary, are in their natural position, and rest nonconformably upon these beds. In these so called cretaceous rocks no fossils have been observed. CARBONIFEROUS ROCKS. This system presents two important divisions: The upper carboniferous, or coal measures ; and the lower carboniferous or mountain limestone. The coal measures, as seen by the table, are composed of nu- merous strata of sandstone, limestone, shales, clays, marls, spathic iron ores and coals. Aboiit 2,000 feet of these coal measures have been found to contain numerous beds of iron ore, and at least eight or ten beds of good, workable coal. Investigation shows 16 HISTORY OF MISSOURI. a greater downward thickness of the coal formation in Southwest Missouri, including beds whose position is probably below those of the northern part of the State. These rocks, with the accom- panying beds of coal and iron, cover an area of more than 27,000 square miles in Missouri alone. The geological map of the State shows that if a line were roughly drawn from Clark County on the northeast to Jasper County in the southwest, most of the counties northwest of this line, together with Audrain, Howard and Boone, would be included in the coal measure. There are also extensive coal beds in Cole, Moniteau, St. Charles, St. Louis and Callaway Counties. The Missouri coal basin is one of the largest in the world, including besides the 27,000 square miles in Missouri, 10,000 in Nebraska; .12,000 in Kansas ; 20,000 in Iowa, and 30,000 in Illi- nois ; making a total of about 100,000 square miles. The fossils of the coal measure are numerous, and distinct from those of any other formation. This latter fact has led to the discovery of the existence of coal measures and the coal beds contained in them, over an area of many thousand miles, where it had been supposed that no coal measures and no coal existed. Of the lower carboniferous rocks, the upper Archimedes lime- stone is developed in Ste. Genevieve County. The ferruginous sandstone is generally found along the eastern and southern limit of the coal fields, passing beneath the coal formation on the west. It varies from a few feet to 100 feet in thickness. In Callaway it occurs both as a pure white sand- stone, a ferruginous sandstone, and a conglomerate. In Pettis and Howai-d Counties we find it a coarse, whitish sandstone. In Cedar, Dade and Lawrence a very ferruginous sandstone, often containing valuable deposits of iron ore. In Newton County it occurs in useful flaglike layers. The St. Louis limestone, next in descending order, forms the entire group of limestone at St. Louis, where it is well marked and of greater thickness than seen elsewhere in this State. It is more often fine grained, compact or sub-crystalline, sometimes inclosing numerous chert concretions, and the beds are oftea separated by thin, green shale beds. Its stratigraphical position is between the ferruginous sand- HISTORY OF MISSOURI. 17 stone and the Archimedes limestone, as seen near the Des Moines, and near the first tunnel on the Pacific Railroad. It is found in Clark and Lewis Counties, but, as has been said, attains its greatest development at St. Louis — hence its name. The most characteristic fossils yet described are palcechinus TnuUipora, lithostrotion canadense, Echinocrinus nerei, Poterio- crinus longidactylus and Atrypa lingulata. The lower Archimides limestone includes the "arenaceous bed." the " Warsaw or second Archimedes limestone," the mag- nesian limestone, the " Geode bed," the " Keokuk or lower Archim- edes limestone" of Prof. Hall's section, and the lead-bearing rocks of Southwestern Missouri; which last, though different from any of the above beds, are more nearly allied to them than to the encrinital limestone below. All of the above beds are easily recognized in Missouri, except, perhaps, the Warsaw limestone, which is but imperfectly represented in our north- eastern counties, where the "Keokuk limestone," the "Geode beds," and the magnesian limestone are well developed. This formation extends from the northeastern part of the State to the southwest, in an irregular belt, skirting the eastern border of the ferruginous sandstone. The extensive and rich lead deposits of Southwestern Missouri are partly in this forma- tion, these mines occupying an area of more than one hundred square miles, in Jasper, Newton, and the adjoining counties. The upper beds of encrinital limestone are gray and cherty. The top beds in St. Charles County include seventeen feet of thin chert beds with alternate layers of red clay. The middle beds are generally gray and coarse, the lower ones gray and brown with some buff beds. Crinoid stems are common in nearly all the beds, hence it has been appropriately termed encrinital limestone. The lower beds often abound in well preserved crinoidce. This rock occurs at Burlington, Iowa, Quincy, 111., Hannibal and Louisiana, Mo., and is well exposed in most of the counties on the Mississippi River north of St. Louis, and from the western part of St. Charles to Howard County. South of the Missouri River and along its southwest outcrop it is not generally well developed. 18 HISTORY OF MISSOUBI. In Green County it is quite cavernous. It has not been rec- ognized east of Illinois, and is not separated from other carbon- iferous stones of Tennessee. DEVONIAN EOCKS. The devonian rocks occupy a small area in Marion, Ralls, Pike, Callaway, Saline and Ste. Genevieve Counties; also narrow belts along the carboniferous strata to the south and west. In the Chemung group, the Chouteau limestone, when fully developed, is in two divisions. Immediately under the encrinital limestone, at the top of the formation, there are forty or fifty feet of brownish gray, earthy, silico-magnesian limestone in thick beds, which contain scattered masses of white or transparent calcareous spar. The upper division of the Chouteau limestone passes down into a fine, compact, blue or drab, thin-bedded limestone, whose strata are considerably irregular and broken. In the northeast- ern part of the State, the Chouteau limestone is represented only by a few feet of coarse, earthy, crystalline, calcareous rock, like the lower division of the encrinital limestone. THE VEKMICULAR SANDSTONE AND SHALES. The sandstones of this division are generally soft and calca- reous. They are easily recognized, being ramified by irregular windings throughout, resembling the borings of worms. This formation attains a thickness of seventy five feet near Louisiana in Pike County. It is seen in Ralls, Pike, Lincoln, Cedar and Greene. The lithographic limestone is a fine grained, compact lime- stone, breaking with a free conchoidal fracture into sharp, angu- lar fragments. Its color varies from a light drab to the lighter shades of buff and blue. It gives out, when struck with the ham- mer, a sharp, ringing sound, and is therefore called "pot metal" in some parts of the State. It is regularly stratified in beds varying from two to sixteen inches in thickness, and often pre- sents, as in the mural bluffs at Louisiana on the Mississippi, all the regularity of masonry. Where elsewhere seen, it somewhat resembles the upper beds HISTORY OF MISSOUBI. 19 of the group. At Taborville, St. Clair County, it is of a salmon drab color, occurring in thick beds having an open texture, and contains a characteristic fossil — Pentremites RcBtneri. This lime- stone is found in Pike, Ralls, St. Clair, Cedar and Greene Counties. THE HAMILTON GBOUP. This is made up of some forty feet of blue shales, and 107 feet of semi-crystalline limestone, containing Dalmania, CallUe- les, Phacops hufo, Spirifer mucronahis, S. sculptilis, S. Congesta, Chonetes carinata and Favosiies basaltica. The Hamilton group is found in Kails, Pike, Lincoln, Warren, Montgomery, Calla- way, Boone, Cole and probably Moniteau ; also in Perry and Ste. Genevieve. ONONDAGA LIMESTONE. This formation is usually a coarse gray or buff, crystalline, thick bedded and cherty limestone, abounding in Terebraiula, reticularis, Orthis resupinaia, Chonetes nana, Productus subacu- leatus, Spirifer euruieines, Phacops bufo, Cyathophyllum rugosum, Emmonsia hemispherica, and a Pentamerus like galeatus. Gen- erally it is coarse, gray and crystalline; often somewhat com- pact, bhiish and concretionary, having cavities filled with green matter or calspar; occasionally it is a white saccharoidal sand- stone; in a few localities a soft, brown sandstone, and at Louis- iana a pure white oolite. OBISKANY SANDSTONE. In spite of its name, this is a light gray limestone, containing the Spirifer arenosa, Leptoma depressa, and several new species of Spirifer, Chonetes, Illoenns and Lichas. SILURIAN ROCKS. This system is divided into the upper and lower silurian. Of the former are the following: The lower Helderberg group, which is made up of buff, gray, and reddish cherty, and argilla- ceous limestones, blue shales, and dark graptolite slates. The Cape Girardeau limestone, found on the Mississippi River, about a mile above Cape Girardeau, a compact, bluish gray, frangible limestone, with a smooth fracture, in layers from two to six inches in thickness, with thin argillaceous partings. 20 HI8T0BY OP MISSOURI. There are at least ten formations belonging to the lower Silu- rian series. There are three distinct formations of the Hudson River group, as follows: First — Immediately below the oolite of the Onondaga limestone, in the bluffs both above and below St. Louis, there are forty feet of blue, gray and brown argillaceous, magnesian limestone. Above, these shales are in thick beds, showing a dull, conclioidal fracture. Below, the division becomes more argillaceous, and has thin beds of bluish-gray crystalline limestone. Second — -Three and one-half miles northwest of Louisiana, on the Grassy River, some sixty feet of blue and pur- ple shales are exposed below the beds above described. Third • — Under the last named division are, perhaps, twenty feet of ar- gillo-magnesian limestone resembling that in the first division, and interstratified with blue shales. These rocks crop out in Ralls, Pike, Cape Girardeau and Ste. Genevieve Counties. On the Grassy, a thickness of 120 feet is exposed, and they extend to an unknown depth. Trenton Limestone. — The upper portion of this formation comprises thick beds of compact, bluish gray and drab limestone, abounding in irregular cavities, filled with a greenish substance. The lower beds abound in irregular cylindrical pieces, which quickly decompose upon exposure to the air, and leave the rocks perforated with irregular holes, resembling those made in tim- ber by the Toredo navalis. These beds are exposed between Hannibal and New London, north of Salt River, and near Glen- coe, St. Louis County. They are about seventy -five feet thick. Below them are thick strata of impiire, coarse, gray and buff crys- talline magnesian limestone, containing brown, earthy portions, which quickly crumble on exposure to the elements. The bluffs on Salt River are an example of these strata. The lowest part of the Trenton limestone is composed of hard, blue and bluish-gray, semi-compact, silico-magnesian limestone, interstratified with soft, earthy, magnesian beds of a light buff and drab color. Fifty feet of these strata crop out at the quarries south of the plank road bridge over Salt River, and on Spencer's Creek in Ralls County. The middle beds sometimes develop a beautiful white crystalline marble, as at Cape Girardeau and near Glencoe. The Black River and Birdseye limestones are often in even HISTORY OF MISSOURI. 21 layers ; the lower beds have sometimes mottled drab and reddish shades, often afPording a pretty marble. Near the base this rock is often traversed by vermicular cavities and cells. These may be seen from Cape Girardeau to Lincoln, and in St. Charles, Warren and Montgomery Counties, thinning out in the latter. The First Magnesian Limestone is generally a buff, open-tex- tured, thick and even bedded limestone, breaking readily under the hammer, and affording a useful building rock. Shumard es- timated its thickness in Ste. Genevieve County to be about 150 feet. In Warren County, in North Missouri, it is seventy feet thick. It is found in Balls, Pike, Lincoln, St. Charles, Warren, Callaway and Boone. Southwesterly, it is not well marked — in- deed it seems to be absent in some counties where, in regular sequence, it should be found. It occurs in Franklin, St. Louis, and southwardly to Cape Girardeau County. Saccharoidal Sandstone is usually a bed of white friable sand- stone, sometimes slightly tinged with red and brown, which is made up of globular concretions and angular fragments of limpid quartz. The formation is well developed in Lincoln, St. Charles, Warren, Montgomery, Gasconade, Franklin, St. Louis, Jefferson, Ste. Genevieve, Perry and Cape Girardeau Counties. Besides the above, it is also developed in a more attenuated form, in Callaway, Osage, Cole, Moniteau and Boone. This sandstone is probably destined to be one of the most useful rocks found in Missouri. It is generally of a very white color, and the purest sandstone found in the State, and is suitable for making the finest glassware. Its great thickness makes it inexhaustible. In St. Charles and Warren Counties it is 133 feet thick, and in Southeast Missouri over 100 feet thick. The Second Magnesian Limestone occutb in all the river counties south of Pike as far as the swamps of Southeast Missouri, and is more often the surface rock in all the counties south of the Mis- souri and Osage Elvers, to within fifty miles of the western line of the State. It is generally composed of beds of earthy mag- nesian limestone, interstratified with shale beds and layers of white chert, with occasionally thin strata of white sandstone, and, near the lower part, thick cellular silico-magnesian limestone beds. The layers are more often of irregular thickness and not 22 HISTORY OF MISSOUEI. very useful for buildicg purposes. It is often a lead-bearing rock, and most of the lead of Cole County occurs in it. It is from 175 to 200 feet thick. The second sandstone is usually a brown or yellowish brown, fine-grained sandstone, distinctly stratified in regular beds, vary- ing from two to eighteen inches in thickness. The surfaces are often ripple- marked and micaceous. It is sometimes quite fri- able, though generally sufiiciently indurated for building pur- poses. The upper part is often composed of thin strata of light, soft and porous, semi-pulverulent, sandy chert or hornstone, whose cavities are usually lined with limpid crystals of quartz. The Third Magnesian Limestone. — This also is an impor- tant member, occurring in nearly all the counties of Southern Missouri. It jrs generally a thick-bedded, coarsely crystalline bluish gray, or flesh-colored magnesian limestone, with occasional thick chert beds. It is the chief lead-bearing rock of South- east and Southern Missouri. In some counties it is as much as 300 feet thick. The Third Sandstone is a white, saccharoidal sandstone, made up of slightly-cohering, transparent globular and angular par- ticles of silex. It shows but little appearance of stratification. The Fourth Magnesian Limestone. — This formation presents more permanent and uniform lithological characters than any other of the magnesian limestones. It is ordinarily a coarse- grained, crystalline magnesian limestone, grayish-buff in color, containing a few crevices filled with less indurated, siliceous matter. Its thick, uniform beds contain but little chert. The best exposures of this formation are on the Niagara and Osage Eivers. This magnesian limestone series is very interesting, both from a scientific and an economical standpoint. It covers a large part of Southern and Southeastern Missouri, is remarkable for its numerous and important caves and springs, and comprises nearly all the vast deposits of lead, zinc, copper, cobalt, the limi- nite ores of iron, and neai'ly all the marble beds of the State. The lower part of the first magnesian limestone, the saccharoidal sandstone, the second magnesian limestone, the second sand- stone, and the upper part of the third magnesian limestone be- HISTOBY OF MISSOURI. 23 long, without doubt, to the age of the calciferous saud rock; but the remainder of the series to the Potsdam sandstone. AZOIC ROCKS. Below the rocks of the silurian system there is a series of siliceous and other slates, which present no remains of organic life; we therefore refer them to the Azoic age of the geologist. They contain some of the beds of specular iron. In Pilot Knob we have a good exposition of these Azoic strata. The lower fossi- liferous rocks rest non-conformably on these strata. IGNEOUS AND METAMORPHIC ROCKS. Aside from the stratified rocks of Missouri, there is a series of rounded knobs and hills in St. Francois, Iron, Dent and the neighboring counties, which are composed of granite, porphyry, diorite and greenstone. These igneous and metamorphic rocks contain some of those remarkable beds of specular iron, of which Iron and Shepherd Mountains are samples. This iron ore often occurs in regular veins in the porphyry. HISTORICAL GEOLOGY. When the continent of North America began to emerge from the primeval ocean. Pilot Knob, Shepherd Mountain and the neighboring heights were among the first bodies of land that reared themselves above the surrounding waters. When Pilot Knob thus grew into an island, it stood alone in the ocean waste, excejit that to the northwest the Black Hills, to the northeast a part of the Alleghany system, and to the southwest a small cluster of rocks lifted their heads out of the flood. These islands were formed in the Azoic seas by mighty internal convulsions that forced up the porphyry and granite, the slates and iron beds of the great ore mountains of Missouri. COAL. The Missouri coal fields underlie an area of nearly 25,000 square miles, including about 160 square miles in St. Louis County, eight square miles in St. Charles, and some important outliers and pockets, which are mainly "cannel coal, in Lincoln, 24 HISTORY OF MISSOURI. WarreD and Callaway Counties. This area includes about 8,400 square miles of upper coal measures, 2,000 square miles of exposed middle, and about 14,600 square miles of exposed lower measures. The upper coal measures contain about four feet of coal, in- cluding two seams of one foot each in thickness, the others be- ing thin seams or streaks. The middle coal measures contain about seven feet of coal, including two workable seams of twenty-one and twenty-four inches, one other of one foot, that is worked under favorable cir- cumstances, and six thin seams. The lower measures contain about five workable seams of coal, varying in thickness from eighteen inches to four and one half feet, thin seams varying from six to eleven inches, and sev- eral minor seams and streaks, in all, thirteen feet, six inches of coal. We therefore have in Missouri, a total aggregate of twenty- four feet, six inches of coal. The thinner seams are not often mined, except in localities distant from railroad transportation. All beds over eighteen inches thick are workable coals. The area where such may be reached within 200 feet from the surface is about 7,000 square miles. Most of the State under- laid by the coal measure is rich farming land. That under- laid by the upper measure includes the richest, which is equal to any upon the globe. The southeastern boundary of the coal measure has been traced from the mouth of the Des Moines through Clark, Lewis, Scotland, Adair, Macon, Shelby, Monroe, Audrain, Callaway, Boone, Cooper, Pettis, Benton, Henry, St. Clair, Bates. Vernon, Cedar, Dade, Barton and Jasper Counties into the Indian Territory, and every county on the northwest of this line is known to contain more or less coal. Great quantities exist in Johnson, Pettis, Lafayette, Cass, Chariton, Howard, Put- nam and Audrain. Outside the coal fields, as given above, the regular coal rocks also exist in Kails, Montgomery, Warren, St. Charles, Callaway and St. Louis, and local deposits of cannel and bituminous coal in Moniteau, Cole, Morgan, Crawford, Lincoln and Callaway. In 1865 Prof. Swallow estimated the amount of good available coal in the State, at 134,000,000,000 tons. Since then numerous other developments have been made, and that es- timate is found to be far too small. HISTORY OF MISSOURI. 25 LEAD. This mineral occurs in lodes, veins and disseminations, which are, as yet, only partially determined. Enough, however, is known of the number, extent, dip and thickness of these de- posits to show that their range and richness exceed those of any other lead-bearing region in the world. Galena occurs in this State in ferruginous clay, that becomes jointed, or separates into distinct masses, quite regular in form, when taken out and partially dried; also in regular cubes, in gravel beds, or with cherty masses in the clays associated with the same. These cubes in some localities show the action of at- trition, while in others they are entirely unworn. Lead is found in the carboniferous rocks, but perhaps the greater portion is ob- tained from the magnesian rocks of the lower silurian, and in one or two localities galena has been discovered in the rocks of the Azoic period. At Dugals, Reynolds County, lead is found in a disseminated condition in the porphyry. THE SOUTHEAST LEAD DISTRICT. The Mine La Motte region was discovered about 1720 by La Motte and Renault. It was not, however, until this territory was ceded to Spain that any considerable mining for lead was done in this part of Missouri. Moses Austin, of Virginia, secured from the Spanish Government a large grant of land near Potosi, and sunk the first regular shaft ; and, after taking out large quantities of lead, erected, in 1789, the first reverberatory furnace for the reduction of lead ever built in America. In all this region are found crystallized cubes of galena in the tallow clay, occurring as float. In Franklin, Washington and Jefferson Counties galena is found in ferruginous clay and coarse gravel, often associated with small masses of brown hema- tite iron and the sulphuret of iron ; sometimes lying in small cavities or pockets. The Virginia mine in Franklin County has produced by far the greater portion of lead from this section. At the Webster mines, the silicate and carbonate of zinc are found always accompanying the lead. At the Valle mines silicate of zinc and baryta occur, as well as hematite iron ore. The 26 HISTOKY OF MISSOURI. Mammoth mine was a succession of caves, in which millions of pounds of lead were found adhering to the sides and roof, and on the bottom was mixed with clay and baryta. The Frumet or Einstein mines are the most productive ever opened in Jefferson County, and yield also large quantities of zinc ore. There are other valuable mines, in some of which sil- ver has been found. In Washington County lead mining has been carried on un- interruptedly for ■ a greater length of time, and more acres of land have been dug over that have produced lead than in any other county in the State. In St. Francois County, lead deposits are found in the fer- ruginous clay and gravel. These mines formerly produced many millions of pounds, but have not been extensively worked for many yeai's. Over portions of Madison County considerable lead is found in the clay. There is lead in several locations in Iron County. In Wayne, Carter, Reynolds and Crawford Counties lead has been found. Ste. Genevieve has a deposit of lead known as the Avon mines on Mineral Fork, where mining and smelting have been prosecuted for many years. In this vicinity lead has also been found as " float" in several places. Lead exists in the small streams in several places in the western part of Cape Girardeau County. In the region above described at least 2,000 square miles are underlaid with lead, upon which territory galena can be found almost anywhere, either in the clay, gravel openings, or in a disseminated condition. The Central Lead district comprises the counties of Cole, Cooper, Moniteau, Morgan, Miller, Benton, Maries, Camden and Osage. During later years the lead development of Cole County has been more to the northwestern corner, passing into Moniteau and Cooper Counties. In the former several valuable mines have been opened. The West diggings have been extensively developed and proved rich. The mineral is found in connected cubes in lime- stone rock, and lies in lodes and pockets. Lead has been found HISTORY OF MISSOURI. 27 in several places in Cooper and Osage Counties. The later dis- coveries in that vicinity, although not yet fully developed, give promise of great richness. Camden County possesses considerable deposits of lead; a number of mines have been successfully worked, and, as the en- tire northern portion of the county is underlaid with the mag- nesian limestone formation, it may be discovered in many places where its existence has never been suspected. Miller County is particularly rich in galeniferous ore. Paying lead has been found north of the Osage Eiver. On the Gravois, Big Saline, Little Saline and Bush Creeks, and the Fox, Walker, Mount Pleasant and Saline Diggings have yielded millions of pounds of lead. Benton County contains a number of lead deposits, the most important being the Cole Cany mines. Lead has been found as a "float" in many localities. Morgan County, like Washington, can boast of having lead in every township, either as clay, mineral, " float," or in veins, lodes, pockets and caves. The magnesian limestone series of Morgan, in which the lead ores now are, or have all existed, are the most complete and well defined of any in Missouri. The most extensive deposits of lead in Morgan County have been found south of the center of the county, yet in the north- western part are several well known lodes. We can not even name the hundreds of places in the county where lead is found in paying quantities. There seems to be a region, covering 200 square miles, entirely underlaid by lead. These wonderful deposits are as yet but partially worked. The Southern Lead Region of the State comprises the coun- ties of Pulaski, Laclede, Texas, Wright, Webster, Douglas, Ozark and Christian. The mineral deposits of this region are only partially developed. In Pulaski County lead has been discovered in several localities. Laclede County has a number of lead deposits; one about eleven miles from Lebanon, where the ore is found in a disseminated condition in the soft magne- sian limestone. In the southwestern part of Texas County, along the headwaters of the Gasconade River, there are considerable deposits of lead ore. Wright County has a number of lead 28 HISTORY OF MISSOnRI. mines almost unworked, which are situated in the southeastern part of _the county, and are a continuation of the deposits in Texas County. In Douglas County, near the eastern line, and near Swan Creek, are considerable deposits of galena. Ozark and Christian Counties have a number of lead deposits, zinc being invariably found in connection. The Western Lead District comprises Hickory, Dallas, Polk, St. Clair, Cedar and Dade Counties. In Hickory County quite extensive mining has been carried on, the larger deposits having been found near Hermitage. In the northern part of the county and along the Pomme de Terre River, lead occurs as "float," and in the rock formation. The more prominent lodes are found in the second magnesian limestone, with a deposit occurring in the third. The lead deposits of Hickory Coixnty are richer and more fully developed than any other in this district. Dallas County has a few deposits of lead, and float lead has been found in various localities in Polk. In St. Clair County the galeniferous deposits are in the second sandstone, and in the ferruginous clay, with chert, conglomerate and gravel. Cedar County presents a deposit of lead, copper and antimony. Galena is found in the clay and gravel. In Dade County a considerable quantity of galena has been found in the southeastern corner of the county. The Southwest Lead District of Missouri comjM'ises the coun- ties of Jasper, Newton, Lawrence, Stone, Barry and McDonald. The two counties first named produce more than one-half of the pig lead of Missouri, and may well boast their immense deposits of galeniferous wealth. The lead mining resources of Jasper and Newton Counties are simply inexhaustible, and new and rich deposits are continually being found. Lead ore seems to have been obtained here from the earliest recollection, and furnished supplies to the Indians during their occupation. Formerly, smelted lead, merchandise and liquor were the principal return to the miner for his labor, as the distance from market and the general condition of the country precluded enlarged capital and enterprise. Since the war capital has developed the hidden wealth, and systematized labor, and rendered it remunerative. This, with the additional railroad facilities, has brought the county prominently and rapidly before the public as one of the HISTORY OF MISSOURI. 29 most wonderful mining districts of the world. The total produc- tion of lead in Jasper County for the centennial year was, accord- ing to the estimates of the best authorities, over half the entire lead production of the State, and more than the entire lead produc- tion of any other State in the Union. Later statistics show a steady and rapid increase in the yield of these mines. One fact, worthy of notice, is, that Jasper County, the great- est lead producing county of the greatest lead producing State, raises every year, upon her farms, products of more value than the lead dug in any one year from her mines. IRON. In the mining, shipping, smelting and manufacturing of the ores of iron, there is, perhaps, more capital invested and more labor employed than in all the other metal industries of our State combined. There are three principal and important iron regions in Mis- souri, namely: The Eastern Region, composed of the southeastern limonite district, and the Iron Mountain specular ore district. The Central Region, containing principally specular ores. The Western or Osage Region, with its limonites and red hematites. These three principal regions combined form a broad ore belt running across the State from the Mississippi to the Osage, in a direction about parallel to the course of the Mississippi River from southeast to northwest, between the thirtieth and fortieth township lines. The specular ores occupy the middle portion of this belt, the limonites both ends of it. The latter are besides spread over the whole southern half of the State, while these sub- carboniferous hematites occur only along the southern border of the North Missouri coal field, having thus an independent dis- tribution, and being principally represented in Callaway, St. Clair and Henry Counties. Iron Mountain is the greatest exposure of specular iron yet discovered. It is the result of igneous action, and is the purest mass or body of ore known. The work of years has only just un- covered the massive columns of specular ore that seems to pass 30 HISTORY OF MISSOURI. down through the porphyry and granite to the source of their exist- ence. The region about is covered with the ore debris. The broken masses have the same general color and quality as the vein ore of Iron Mountain. The fresh fracture presents a ligli t gray, tinged distinctly with blue. The crystallization is often coarse, presenting an irregular fracture. All the ore is more or less mag- netic. The streak is a bright cherry red, and possesses the hard- ness of 6. Analysis shows it to contain from 65 to 69 per cent of metallic iron. The ore of Shepherd Mountain is called a magnetite. In some portions of the veins it shows itself to be granular, brown in color, and to have a clear black streak. Other portions present all the qualities of a specular ore. In portions of the specular, as well as magnetite, beautiful crystals of micaceous ore are found. The streak of this specular and micaceous is a dark red ; the hardness is about 5, with from 64 to 67 per cent of metallic iron. The magnetic qualities of this ore are quite variable, usually the strongest at or near the surface, but this is not the case in all the veins. The ore of Shepherd Mountain is superior to any yet developed in Missouri, not quite as rich as that of Iron Mountain, but so uniform in character, and devoid of sulphur and phosphoric acid that it may be classed as supe- rior to that, or any other ore that we have. The ore of Pilot Knob is fine grained, very light bluish gray in color, and with a hardness representing 6, with a luster siib- metallic. There is a most undoubted stratification to the deposi- tion, occurring as before indicated. The ore of Pilot Knob gives from 53 to 60 per cent metallic iron, and is almost free from deleterious substances. The ore below the slate seam is much the best, containing only about from 5 to 12 per cent of eilica, while the poorer ores show sometimes as high as 40 per cent. There have been more than 200,000 surface feet of ore de- termined to exist here. The Scotia Iron Banks, located on the Meramec River, in Crawford County, are most remarkable formations. Here the specular ore is a deep, steel gray color, with a metallic luster. The crystals are fine, and quite regular in uniformity. This ore is found in the shape of boulders, sometimes small and sometimes HISTORY OF MISSOUBI. 31 of immense size, resting in soft red hematites, that have been pro- duced by the disintegration of the specular ores. These boulders contain a great number of small cavities in which the ore has as- sumed botryoidal forms ; and upon these, peroxide iron crystalliza- tions are so formed that a most gorgeous show of prismatic colors is presented. The hardness of this ore is about 6 ; the soft red ore, in which it occurs, not more than 2^. In these banks there are some carbonates and ochraceous ores, but not in any quantity to deteriorate or materially change the character of the other ores. Many of the boulders present a soft red mass with a blue specular kernel in the center. This ore is found to be slightly magnetic, and gives from 58 to 69 per cent metallic iron. Simmons Mountain, one-half mile south of Salem, Dent County, is about 100 feet high, and covers nearly forty acres. The second sandstone is the country rock and at the summit is uncovered, and mixed Avitli specular and brown ores. Down the elevation larger masses of ore are met with that have the appear- ance of being drifts from the main deposit higher up. Shafts have been sunk in this elevation determining more than thirty feet of solid ore. The ore is a splendid, close, compact, brilliant epecular, very hard and free from deleterious substances. The ores of this mountain do not show nearly as much metamorphism as many of the other banks in the second sandstone of this re- gion. The ore is quite strongly magnetic, and gives a bright red streak. This is the largest specular iron deposit, with the exception of Iron Mountain, that is known in the State. Some of the most extensive red hematite banks in Missouri are located in Franklin County. Along the Bourbense there are thirteen exposures of fine red hematite iron ore. Near Dry Branch Station is an elevation, capped at the summit with saccha- roidal sandstone, beneath which there is a large body of red and epecular ore. The red hematite, however, predominates, and is remarkably pure and free from sulphur or other deleterious sub- stances. The sinking of a number of shafts upon this hill reaches the deposits in several places, in all of which the red hem- atite shows itself to be the prevailing ore. This ore will be found to work well with the hard specular and ores of the siliceous character, like Pilot Knob. 32 HISTORY OF MISSOURI. In Miller, Maries, Cole and Camden Counties, also in Bol- linger, Stoddard and Butler Counties, along the line of the St. Louis, Iron Mountain & Southern Railroad, there are a number of red hematite banks of considerable promise. There are simi- lar banks in the northern part of Texas and Wright Counties, and in Morgan, Benton, Cedar and Laclede. In Wayne County there are over seventy different limonite ore banks. In Miller, Maries, Camden, Cole, Moniteau and Cal- laway Counties there are very extensive banks of the same kind. In Morgan, Benton, St. Clair, Cedar, Hickory and Vernon Coun- ties, considerable brown hematite has been found. In Franklin, Gasconade, Phelps, Crawford, Laclede, Chris- tian, Webster and Green Counties, large limonite beds have been found. In the Moselle region very large deposits have been opened and worked for many years. In Osage County there are a number of promising brown ore banks, as well as fine specvdar and red hematite. It is impossible, in the brief space at our command, to de- scribe the number of banks, rich in iron ore, which are situated in the above and other counties of our State; but a glance at the tables found in the works of prominent geologists of the State, will give some idea of the resources of Missouri as an iron pro- ducing region. ZINC. The ores of zinc in Missouri are almost as numerous as those of lead. They are distributed throughout almost all the geolog- ical strata, and scattered through nearly every mineral district; but the principal supply of the metal for commercial purposes is obtained from a very few ores, the more important of which are zinc blende (sulphuret of zinc), the silicate of zinc and the carbonate of zinc, and these are furnished by a comparatively few localities. In reference to their geological position, the ores are in two classes: The first class includes all zinc ores which occur in the regular veins of the older rocks, and hence are associated with other metalliferous ores. The second mode of occurrence, and the ore by far of paramount importance in Missouri, is that of the third magnesian limestone of the lower silurian series, where HISTORY OF MISSOURI. 33 it usually occurs in association with galena in the cave formation. Zinc blende abounds at Granby and Joplin, and is found at many other mines of the southwest. It also occurs at the lead mines of Franklin and Washington Counties, and at some other points in Southeast Missouri. The pockets of coal in Central Missouri nearly all contain zinc blende. The lead mines of the same section also sometimes ■carry it. There are quantities of silicate of zinc at Granby and Joplin, and the ore is found at most of the lead mines of the southwest, and occasionally in Central and Southeast Missouri. Carbonate of zinc occurs at Granby, Joplin, Minersville and Valle's mines. It is in the Granby, Joplin and Valle mining districts that zinc ore is principally worked. COPPER. Several varieties of copper ore exist in the Missouri mines. The copper mines of Shannon, Madison and Franklin Counties have been known for a long time. Some of those in Shannon and Franklin were once worked with bright prospects of success, and some in Madison have yielded good results for many years. Deposits of copper have been discovered in Dent, Crawford, IBenton, Maries, Green, Lawrence, Dade, Taney, Dallas, Phelps, Eeynolds and Wright Counties, but the mines in Franklin, Shan- non, Madison, Crawford, Dent and Washington give greater promise of yielding profitable results than any other yet dis- covered. NICKEL AND COBALT. These ores abound at Mine La Motte and the old copper mines in Madison County, and are also found at the St. Joseph mines. Sulphuret of nickel, in beautiful hair-like crystals, is found in the limestone at St. Louis, occupjdng drusy cavities, resting on calcite or fluor spar. MANGANESE. The peroxide of manganese has been found in several locali- ties in Ste. Genevieve and other counties. 34 HISTORY OF MISSOURI. SILVER AND GOLD. Silver occurs to a limited extent in nearly all the lead mines in the State. Gold, though found in small quantities, has never been profitably worked in any part of Missouri. MARBLE. Missouri has numerous and extensive beds of marble of vari- ous shades and qualities. Some of them are very valuable, and are an important item in the resources of the State. Fort Scott marble is a hard, black, fine-grained marble, with veins of yellow, buff and brown. It receives a fine polish, and is very beautiful. It belongs to the coal measures, and is common in the western part of Vernon County. There are several beds of fine marbles in the St. Louis lime- stone, of St. Louis County. The fourth division of encrinital limestone is a white, coarse- grained crystalline marble of great durability. It crops out in several places in Marion County. The lithographic limestone furnishes a fine, hard-grained, bluish-drab marble, that contrasts finely with white varieties in tessellated pavements. The Cooper marble of the devonian limestone has numerous pellucid crystals of calcareous spar disseminated through a drab or bluish-drab, fine compact base. It exists in great quantities in some localities of Cooper and Mai'ion Counties, and is admira- bly adapted to many ornamental uses. There are extensive beds of fine, variegated marbles in the upper silurian limestones of Cape Girardeau County. Cape Girardeau marble is also a part of the Trenton limestone, located near Cape Girardeau. It is nearly white, strong and durable. This bed is also found near Glencoe, St. Louis County. In the magnesian limestone series there are several beds of very excellent marble. Near Ironton there are beds of semi- crystalline, light-colored marbles, beautifully clouded with buff and flesh colors. In the third magnesian limestone, on the Niangua, is a fine-grained, crystalline, silico-magnesian limestone, light drab, slightly tinged with peach blossom, and beautifully clouded with deep flesh-colored shades. It is twenty feet thick, and crops out in the bluffs of the Niangua for a long distance. HISTORY OF MISSOTJBI. 35 There are numerous other beds in the magnesian limestones, some of which are white and others so clouded as to present the appearance of breccias. The Ozark marbles are well known, some of them having been used to ornament the Capitol at Washington. Wherever the magnesian limestones come near the igneous rocks, we may expect to find them so changed as to present beds of the beautifiil variegated marbles. SULPHATE or BARYTA. In its pure white form, this mineral is very abundant in Mis- souri. It occurs in large beds in the mining regions, as the gangue of our lead veins, and as large masses, especially in the magnesian limestone of the lower silurian rocks. It is utilized as a pigment in connection with lead, and may be made valuable for the same purpose in connection with some of our ferruginous and argillaceous paints. CLAYS. Fire clays, possessing refractory qualities, suitable for making fire brick, occur beneath most of the thicker coal seams. Potter's clay is abundant, especially among the coal measure clays. It is also sometimes found associated with the lowei-* car- boniferous rocks. Kaolin is only found in Southeast Missouri, where porphyries or granites prevail. Brick clays have been found and worked in nearly all the counties where there has been a demand for them. The argilla- ceous portions of the bluflf formation make good brick, as shown in the brick yards all along our large rivers. Some of the ter- tiary clays will make the very best brick. CAVES, ETC. There are several very interesting and quite remarkable caves in the State. Hannibal Cave, situated one mile below the city of Hannibal, and aboiit a quarter of a mile from the Mississippi River, is approached through a broad ravine, hemmed in by lofty ridges, which are at right angles with the river. The ante- chamber is about eight feet high and fifteen feet long. This 36 HISTORY OF MISSOURI. descends into the Narrows, thence through Grand Avenue to Washington Avenue, and througli the latter to Altar Chamber. This is a ferruginous limestone formation, and crystal quartz, carbonate of lime and sulphate of magnesia abound. Stalactites and stalagmites are continually forming by limestone percola- tions. In Bat Avenue Chamber the bats may be seen hanging from the ceiling in clusters, like swarms of bees, some of them fifteen inches from tip to tip. Washington Avenue, over sixteen feet high, with long corridoi's of stalactites and stalagmites, is the largest division of the cave. It contains a spring, and a deep pool, in which are found the wonderful eyeless fish. The Devil's Hall, Alligator Rock, Elephant's Head, two natural wells filled with limpid water. Table Rock, and numbers of other curiosities, will amply repay the tourist for his exploration. Cliff Cave, thirteen miles below St. Louis, has been utilized by the Cliff Cave Wine Company as a wine cellar. There are several caves in Miller County, the largest of which is on Big Tavern Creek, in the bluff near its confluence with the Osage River. The entrance is about twenty-five feet square, and is situated thirty or forty feet above the river, in a solid lime- stone bluff. During the civil war it was used as a retreat by the bandit, Crabtree. The stalactite formations are of strange and fantastic appearance, some of them looking like colossal images of marble, and the whole effect by torchlight is weird and solemn. Phelps County contains several interesting caves, the most accessible of which is Freide's Cave, about nine miles northwest of RoUa. Its mouth is 60 feet in width and 35 feet in height. It has been penetrated to a distance of three miles without find- ing any outlet. The Stalactite Chamber is a beautiful apartment 200 yards in length, varying from 15 to 30 feet in width, and from 5 to 30 feet in height. The Bat Chamber contains thou- sands of wagon loads of guano, which is extensively used by the farmers of the neighborhood. The cave also contains quantities of saltpetre, and during the war large amounts of powder were manufactured there. There are also caves in Christian County. The principal one is two and a half miles northeast of Ozark. Its entrance is HISTOKY OF MISSOUKI. 37 through a rock arch 50 feet across and 80 feet high. About 400 feet from the entrance, the passage is so contracted that the ex- plorer must crawl through on his hands and knees. A fine stream of water, clear and cold, gurgles down through the cave. About twelve miles south of Ozark, near the Forsyth road, on the top of a very high hill, is a small opening, which, about 100 feet from the surface, exjjands into a hall 30 feet wide and about 400 feet long, the sides and top of which are of rock lined with beautiful stalactites. In Stone County at least twenty-five caves have been explored and many more discovered. One mile from Galena is an exten- sive cave from which the early settlers procured saltpetre in large quantities. About two and a half miles above this is a smaller one of great beauty. From the ceiling depend glittering stalac- tites, while the floor sparkles with fragments of gem-like luster. A pearly wall, of about half an inch in thickness and 15 inches high encloses a miniature lake, through whose pellucid waters the wavy stalagmite bottom of this natural basin can be plainly seen. The sacred stillness of the vaulted chamber render.s its name, "The Baptismal Font," a peculiarly fitting one. A cave about twelve miles from Galena is well known among curiosity seekers in the adjacent country. The entrance cham- ber is a large dome-shaped room, whose ceiling is very high ; a glittering mound of stalagmites rises in the center of the room, nearly one-third the height of the ceiling; stretching out at right angles from this are long shining halls leading to other grand arched chambers, gorgeous enough for the revels of the gnome king, and all the genii of the subterranean world. One can not but think of the Inferno, as, wandering down a labyrinth- ian passage, he reaches the verge of an abyss, striking perpen- dicularly to unknown and echoless depths. The name, " Bot- tomless Pit," is well bestowed on this yawning gulf. Knox Cave, in Green County, about seven miles northwest of Springfield, is of large dimensions, and hung in some parts with the most beautiful stalactites. Fisher's Cave, six miles southeast of Springfield, is of simi- lar dimensions, and has a beautiful stream of water flowing out of it. 38 HISTORY OF MISSOURI. There are a number of saltpetre caves along the banks of the Gasconade, which were once profitably worked. Some of these caves are large and interesting, consisting frequently of a succession of rooms joined to each other by arched halls of a considerable height, with walls of white limestone, upon which, as well as upon the floors, the saltpetre is deposited, and is gen- erally so pure as to need but one washing to prepare it for use or export. When these caves were first discovered, it was not uniisual to find in them stone-axes and hammers which led to the belief that they had formerly been worked for some un- known purpose by the savages. It is doubtful whether these tools were left there by the Indians or by another and more civil- ized race which preceded them. There are numerous caves in Perry County, two of which penetrate beneath Perryville. Connor's Cave, seven miles southeast of Columbia, has an en- trance twenty feet wide and eight feet high, and has been ex- plored for several miles. There are extensive and beautiful caves in Texas, Webster, La^vi'ence, Laclede, Oregon and several other counties. MINERAL SPRINGS. Salt springs are exceedingly abundant in the central part of the State. They discharge vast quantities of brine in Cooper, Saline, Howard and the adjoining counties. These brines are near the navigable waters of the Missouri, in the midst of an abundance of wood and coal, and might furnish salt enough to supply all the markets of the continent. Sulphur Springs are also numerous throughout the State. The Chouteau Springs in Cooper, the Monagaw Springs in St. Clair, the Elk Springs in Pike, and the Cheltenham Springs in St. Louis County, have acquired considerable reputation as me- dicinal waters, and have become popular places, of resort. There are similar sulphur springs in other parts of the State. Chalybcaie Springs. — There are a great many springs in the State which are impregnated with some of the salts of iron. Those containing carbonates and sulphates are most common, and several of these are quite celebrated for their medicinal properties. HISTORY OF MISSOURI. 39 Sweet Springs on the Blackwater, and the Chalybeate Spring in the University campus, are perhaps the most noted of the kind in the State. The Sweet Springs flow from cavities in the upper beds of the Burlington limestone. The hill is here forty- seven feet high above water in the Blackwater, spreading out at the back in a flat table-land. The spring itself is about twenty- feet above the river, and has a sweetish alkaline taste. It is use- ful as a promoter of general good health, and is much resorted to at the proper season. The water is used for ordinary cooking and drinking purposes, except for making tea. Petroleum Springs. — These are found in Carroll, Ray, Ran- dolph, Cass, Lafayette, Bates, Vernon and other counties. Many of these springs discharge considerable quantities of oil. The variety called lubricating oil is the most common. It is impossi- ble to tell whether petroleum will be found in paying quantities in these localities, but there is scarcely a doubt that there are reservoirs of considerable quantities. MANUFACTURING. The state of Missouri presents every facility for extensive and successful manufacturing ; abundant timber of the best quality, exhaustless deposits of coal, iron, lead, zinc, marble and granite, unmeasured water power, distributed over the State, a home mar- ket among an industrious and wealth-accumulating people, and a system of navigable rivers and railway trunk line and branches, that permeate, not only the State, but reach out in direct lines fi'om giilf to lake, and from ocean to ocean. Of the manufacturing in Missouri over three-quarters of the whole is done in St. Louis, which produced in 1880, $114,333,375 worth of manufactured articles, thus placing her as the sixth manufacturing city in the Union, being surpassed only by New York, Philadelphia, Chicago, Brooklyn and Boston. The leading manufacturing counties of the State are St. Louis, Jackson, Buchanan, St. Charles, Marion, Franklin, Greene, Cape Girardeau, Platte, Boone, Lafayette, followed by Macon, Clay, Phelps, St. Francois, Washington and Lewis. The subjoined table, arranged from the tenth United States census, will give the reader a comprehensive view of the pres- 40 HISTORY OF MISSOURI. ent state of manufacturing in Missouri, and its variation during^ recent years. No.Es- tabUsb- ments. Average Number of Hands Employed. Total Amount Paid in Wages During the Year. Value of Materials. Year. Capital. Males Above 16 Years. 928 1,053 3,884 6,474 a © 2 Value of Products. 1860 1860 1870 1880 2,923 3,157 11,871 8,592 $ 8,576,607 j 14,880 20,034,220 18,628 80,267,244 66,904 72,607,844 64,200 6,566 4,321 $ 4,692,648 6,669,916 31,055,445 24,309,716 S 12,798,351 23,849,941 115,533,269 110,798,392 S 24,324,418 41,782,731 206,213,429 165,386,205 The products of the principal lines of manufacturing inter- ests, for the year 1880, are as follows: flouring and grist mills, $32,438,831; slaughtering and meat packing, §14,628,630; tobac- co, 16,810,719; iron, steel, etc., $5,154,090; liquors, distilled and malt, $5,575,607; clothing, $4,409,376; lumber, $6,533,253; bag- ging and bags, $2,597,395; saddlery and harness, $3,976,175; oil, $851,000; foundry and machine shop products, $6,798,832: printing and publishing, $4,452,962; sugar and molasses, $4,475,- 740; boots and shoes, $1,982,993; furniture, $2,380,562; paints, $2,825,860; carriages and wagons, $2,483,738; marble and stone works, $1,003,544; bakery products, $3,250,192; brick and tile, $1,602,522; tinware, copper ware and sheet-iron ware, $1,687,- 320; sash, doors and blinds, $1,232,670; cooperage, $1,904,822; agricultural implements, $1,141,822; patent medicines, $1,197,- 090; soap and candles, $1,704,194; confectionery, $1,247,235; drugs and chemicals, $1,220,211; gold and silver reduced and re- fined, $4,158,606. These, together with all other mechanical industries, aggre- gate $165,386,205. RAILROADS. Since 1852, when railroad building began in Missouri, be- tween 4,000 and 5,000 miles of track have been laid. Addi- tional roads are now in process of construction, and many others in contemplation. The State is well supplied with railroads which tread her surface in all directions, bringing her remotest districts into close connection with St. Louis, that great center of western commerce. These roads have a capital stock aggre- gating more than $100,000,000, and a funded debt of about the same amount. HISTOEY OF MISSOURI. 41 The lines of roads which are in operation in the State are as follows : The Missouri Pacific, chartered May 10, 1850; the St. Louis, Iron Mountain & Southern Railroad, which is a consolidation of the Arkansas branch ; the Cairo, Arkansas & Texas Railroad ; the Cairo & Fulton Railroad; the Wabash Western Railway; the St. Louis & San Francisco Railway; the Chicago, Alton & St. Louis Railroad; the Hannibal & St. Joseph Railroad; the Mis- souri, Kansas & Texas Railroad; the Kansas City, St. Joseph & Council Bluffs Railroad; the Keokuk & Kansas City Railway Company ; the St. Louis, Salem & Little Rock Railroad Company^ the Missouri & Western; the St. Louis, Keokuk & Northwest- ern Railroad; the St. Louis, Hannibal & Keokuk Railroad; the Missouri, Iowa & Nebraska Railway; the Quincy, Missouri & Pacific Railroad; the Chicago, Rock Island