iliiif ■ ' ■ml ' %'^'aJ'' 'MS'- ^°<. fW; ^H^^ "^is'.-< .■«^- V^ ' V ts iJ ". ■• .«.' 'd- •'^"^^T-ff- •/- •-■.< ,^' V -^-a<>' ,. -V ... 'p_ ^y c^^^ ':^'6<:' ,^^' I.r"> ^■:^^<-,\j ^ '^ ■I o. ■?S^->' V'^?:"V X'^';!?^-'/ %^^^--^ X':-!»-Y ..^ \ > 'i' ^ \^ \r 'P^ , ^ • ■■/ \ -o-;-/ %■...:.■■/ %•-#■•/ %'^fS^-/ %■-;•; GEOGRAPHY OF NEW YORK By Ai.bkrt Pkrry Brigham and Charlks T. McFariane Early History. —\\ hen tlie white man first visited the region which is now the state of New York, he found it covered nearly everywhere with forest. In the forest dwelt Indians, among whom the Iroquois were the most important. They consisted of the Mo- hawk, Oneida, Onondaga, Cayuga, and Seneca tribes. Their home was along the plains south of Lake Ontario and extending east- ward past Oneida Lake into the Mohawk \ al- ley ; but their hunters and warriors roamed over a wide area. At their villages they had small clearings where they raised corn, pump- kins, apples, and other products. Nearly 5000 Indians are now livmg on small reserva- tions in New York state. Henry Hudson's explorations for the Dutch in 1609 led to permanent settlements by the Dutch people, extending from New Amster- dam (later the city of New York) up the Hudson River to Albany, which they called E-P 12 Copyright. 1916, 1921. by American Book Company Fort Orange, and up the lower Mohawk River. In 1664, a British fleet took posses- sion of the colony ; and thenceforth, except for a short time in 1673-1674, New York remained under English rule, until the thir- teen Colonies declared their independence in 1776. In the year of Hudson's voyage, a great French explorer, Champlain, coming from the St. Lawrence Valley, sailed up the lake which bears his name. He and other French explorers also visited the regions along the St. Lawrence River and Lake Ontario. They built a fort at the mouth of the Niagara River, and sought to control northern and western New "^'ork. Thus the F^nglish came into conflict with the French along the lakes and the St. Lawrence. In the wars that followed the English were finally victorious, so that France ceded its American possessions to Great Britain. Some Germans, persecuted in their native land, settled in the Mohawk Valley, and as the names Catskill and Yonkers were brought by the Dutch, so Herkimer and Frankfort came from the German settlers. English settlers also poured into the state, both from England and from New England. Many of the geographic names in New York are of English origin, — such as Binghamton, Plattsburg, and Rochester The state also preserves many Indian names, of which Seneca, Oneida, Mohawk, Chenango, Chemung, Genesee, and Niagara are examples. Other names have been given to towns and counties in honor of American statesmen and men in high official station, — such as Washington, Jefferson, Monroe, Madison, Clinton, Hamilton, and Schuyler. Thus the history of New York is in part recorded in its geographic names. g)CI.A608581 -5 1921 .J-Aa^' Map Study, i. in what jiait state of New ^ ork is tlicrc a Dio; jilaiii ? 2. W hat two river valleys form a natural liiake line ? 5. What iiij;hland re<;ion is north of the ?.Iohawk Ri\er and west of Lake Champlain ? 6. In what part of the state is there another iar<;e highland ? 7. What great river valleys reach into the highland of southern New York from Pennsylvania ? 8. W hat river crosses the state and flows into Lake Ontario ? 9. Through how many of these valleys have railroads been con- structed r 10. What city is near the mouth of the Genesee River ? At the mouth of the Oswego Ri\cr r 11. Name two cities near the junction of the Hudson and Mohawk rivers. 12. In what river val- ey is Bmghamton "'. burg? Watertown .' 13. Name four cities in the valley of the Mohaw^k River. 14. Using the scale of miles, measure the greatest length of Long Island. 15. Measure the distance between Syra- cuse and Rochester. In a railroad time table find tiie distance on the railroad between these two cities. Why the difference : GEOGRAPHY OF NEW YORK Position. — New York is in the northeast- ern part of the United States. What states border it on the east .^ On the south.'' Canada is on the north and west ; what rivers and lakes are on the boundary ? The state extends from the Atlantic Ocean at the southeast to the Great Lakes at the northwest. This position between great waterways has promoted the growth of population and com- merce, from early colonial days to the present time. New York is between 40° 30' and 45° north lati- tude. The city of New York is in nearly the same latitude as Madrid, Naples, Constantinople, and Peking. In what longitude is it .'' Size. — The total area of New York (not count- ing any part of the Great Lakes) is 49,204 square miles, of which 1550 miles are water surface. The state is nearly si.x times as large as Massa- chusetts, but less than one fifth the size of Texas. It is slightly larger than Pennsyl- vania. From north to south the state ex- tends 312 miles, covering about 4^ degrees of latitude. A railroad journey from the city of New York to Rouses Point takes about 95^ hours. From east to west, exclusive of Long Island, the distance is slightly greater, — 326 miles. Review. — I. Name the several Iroquois tribes. 2. Describe the coming of the Dutch and the English. 3. What was the early name of Albany .' 4. What parts of New York did the French hold ? 5. What classes of geographic names are found in New York ? 6. What are the boundaries of New York ? 7. What large foreign cities are in about the same latitude as the city of New York .'' 8. What is the area of the state ? 9. How does its area com- pare with that of Massachusetts ? Of Texas ? • ^.^.'^■'^-'^ 1 \i^ y Comparative areas of Texas, New York, and Massachusetts PHYSICAL FEATURES Most of Long Island and Staten Island are low, flat, and sandy, like the Atlantic coastal plain farther to the south ; but some parts are hilly with glacial moraines. Eastern New York belongs to the Appalachian Mountains, although the mountains there have been worn down in places almost to sea level. Man- hattan Island and the Hudson region below the Highlands belong to a hilly lowland, often called the Piedmont region. Southern New York from the Catskills westward is part of the Appalachian Plateau. Finally, the Lake Plains in New York are extensive, especially about Lake Ontario. The state has therefore a great variety of surface and soil. This causes great differences in climate, and in the crops that can be grown, in the different parts of the state. Atlantic Coast Region. — Long Island, the largest island on either coast of the United States, is a part of New York. As its name suggests, its length, 118 miles, is much greater than its extreme width, about 23 miles. The highest point is but little more than 400 feet in altitude. Most of the island is covered with clay, gravel, and sand deposited by glacial ice and by streams flowing from the ice. Through the middle of the island, from west to east, extends a belt of hills, a terminal moraine of the ice sheet. On the north border is another belt of such hills. Among the hills are many ponds and lakes, such as are commonly found in moraine belts. The south parts of the island are nearly flat, slop- ing gently toward the shore. At the eastern end of the island the waters of Gardiners Bav and Peconic Bay reach GKOCiRAPll^' UF NEW ^URK il ;^ ^ / ft »■ . \ i « ^ f I » I I nit nil W^AtLZ^'lUkuh Beach at Coney Island into the land about 30 miles. Along the northwest shore deep bays penetrate the hilly region to a distance of several miles. On the south shore there are long stretches of quiet water, inclosed between the main island and long bordering barrier beaches. Of these Ja- maica and Great South bays are the largest. The longest of the beaches is Fire Island Beach, on which Fire Island light has been erected. Others, famous as summer resorts, are Coney Island and Rockaway Beach, visited daily during warm weather by many thousands from the great cities. On the western end of Long Island are Brooklyn and Queens, two of the boroughs of Greater New York. Many people who carry on business in the great city live in the smaller villages and cities of Long Island, and along the north and the south shores there are many beautiful summer homes. Much of the land is cultivated as truck farms or market gardens, and Long Island thus furnishes a large supply of vegetables and fruits for the metropolis. Staten Island is much like Long Island in character, and constitutes the borough of Richmond. It is separated from Long Island by a strait called the Narrows. At the time Manhattan Island was first settled by white men, its surface was rather irregular. It consisted largely of hard rocks, most of which were but thinly covered with soil. .'\s the great city has spread over the island the smaller irregularities have disap- peared. Minor elevations have been blasted away and minor depressions have been filled. Some larger hills, however, still remain in the northern part of the island, as at Morning- side Heights. Most of the waters which surround .Man- hattan are deep enough to permit large ships to approach the numerous wharves along the water fronts. On the New Jersey side of the Hud.son River are other great wharves, some of them lying under the Palisades, a lofty ridge of lava rock running many miles up the ri\er. The steep cliff adjoining the river is exceedingly picturesque. GEOGRAPHY OF NEW YORK Looking down the Hudson, in the Highlands Mountain and Valley Region of Eastern New York. — Along the eastern border of the state, from Long Island Sound to the head North of the Highlands, the Hudson oc- cupies part of a broad valley that reaches from Glens Falls along the Hudson to Kings- ton and Newburgh and along the Wallkill River to the southwest, into northwestern New Jersey. If is a northern continuation of the Great Appalachian Valley which ex- tends from Alabama to Pennsylvania. This valley is bordered on the northwesi by a mountain range which enters the statf on the south at Port Jervis. It is a north- eastward continuation of the Appalachian ridges of central Pennsylvania. In southern New York the range is called the Shawan- gunk (pronounced shon'gum) Mountains. Adirondack Mountains. — The Adirondack Mountains, like the Highlands of the Hudson. of Lake Champlain, is a belt of hills and low are very old. They occupy the greater part mountains, which may be called the foothills of northern New York, in a circular area of the Berkshires and of the Green Mountains about lOO miles in diameter. The highest of New England. They lie mostly east of the mountain in this region, and m the state, is Hudson, and are the result of the folding of .Mount Marcy ; its altitude is 5344 feet. The ancient rock beds, followed by the wearing ridges and valleys of the Adirondacks have away of the rocks by weathering, glaciers, a northeast and southwest direction. The and streams. main valleys lie below 2000 feet, and where Between Beacon and Peekskill, the Hudson they were obstructed by deposits of glacial flows through a gorge cut across an older waste they contain many beautiful lakes and mountain belt which crosses the state in a ponds. Among such bodies of water are the northeast and southwest direction. This is Saranac Lakes, Lake Placid, Long Lake, the the Hudson Highlands, which have an alti- Tupper Lakes, Schroon Lake, the Ausable tude of 1500 to 1800 feet. Lakes, and the Fulton chain of lakes. (JEU(JRAl'in Ol- NhW YORK Owing to the altitude, the climate of the •\dirondacks is severe ; the winters are long and the snowfall is heavy. Even the summer days are of modtran- heat, and the summer nights are cool. The rocks of the Adirundacks are hard, the soils are thin, and the mountains and valleys alike are covered with forest, chiefly of evergreen trees, such as pine, spruce, and hemlock. Little agriculture can be carried on, and the chief use of the region is for recrea- tion and health. There are thousands of hotels, summer homes, and camps, and the excellent boating, fishing, and hunting attract many visitors in season. There is much lumbering in the Adiron- dacks, and there are many sawmills and paper mills in and near this region. In order to preserve the forests from destruction, the state has bought large tracts of Adirondack lands and holds them as a forest reservation. The object is not only to preserve the lumber, but to prevent floods along the Mohawk, Hudson, and other streams. So long as the forests stand, the mosses, leaves, and forest soil absorb the falling rain, and keep it from pouring at once down the streams to overwhelm fields and homes in the lower valleys. Plateau Region. West of the Hudson River and north of the Wallkill is the upland known as the Catskill Mountains. It faces the broad Hudson \ alley by a steep slope or escarpniLiu, which in its middle and southern parts ranges from 2500 to 4000 feet in altitude. It is a region of many lofty hills and deep valleys and is a part of the highland which extends from eastern New York to Alabama and IS called the Appalachian Plateau. North of the Catskills and west of Alban\ . the plateau rises from the Hudson lowland by the Helderberg Escarpment, a bold clitt often called the Helderberg Mountains. The plateau is bordered on the north by hills slop- ing down to the Mohawk and to the plains farther west. In central and western New York the highland averages from 1800 to 2000 feet in altitude, with broad, open val- leys several hundred feet deep. In the plateau region west of the Catskills, the valleys usually extend in a north and .south direction, and have influenced in a marked way the laying out of roads and railroads. In this region there are manv such well-known lakes as Otsego Lake, and the Lin- ger Lakes, which include .Skaneateles, Owasco, Cayuga, Seneca, Keuka, and Canandaigua. Winds from these bodies of water help to moderate the climate of the bordering lands; they are cool on warm spring days, and warm on cold autumn days. This effect on the weather favors the raising of grapes and other fruits. The pleasures of boating and fishing and the cool breezes from the lakes attract many summer residents to the villages and camps along their shores. GEOGRAPHY OF NEW YORK Lake Plains. — At the eastern end of Lake Ontario, along its southern border, and about the east end of Lake Erie is a region of lowlands known as Lake Plains. From Lake Ontario they extend eastward to include the Oneida Lake region, and continue with a breadth of several miles as far east as the city of Rome. Syracuse is on the south edge of the plains. The lowlands reach north in the western parts of Oswego and Jeffer- son counties, and continue along the St. Lawrence River in northern New York. At one time the waters of the Ontario basin covered these lowlands from the Niagara region to the neighborhood of Water- town. The St. Lawrence Valley was blocked The " Ridge Road," Orleans Count\ by glacial ice and the outlet of the lake was at Rome, down the Mohawk Valley. This ancient lake is known as the glacial Lake Iroquois. Beginning at the Niagara River, at Lewis- ton, New York, a broad, low, gravel ridge runs along the plains to a point east of Rochester. .\s this ridge was above the swampy surface of the adjoining forests, it was used by early settlers as a roadway, and this highway, thickly dotted with farmhouses, is still known as the Ridge Road, in Niagara, Orleans, Monroe, and Wayne counties. This ridge was a barriei beach built in the shallow waters along the south shore of Lake Iroquois. The belt of low- land to the north of it is still covered in many places by the fine silt brought in by streams and deposited on the bottom of the lake. A higher plain stretches northward and eastward from Buffalo, and is called the Erie lake plain. Before the time of Lake Iro- quois, it also was covered by lake waters. The Erie plain descends to the Ontario plain by a steep slope known as the Niagara Escarpment. This is the northern edge of hard limestone rocks over which the Niagara River tumbles to make the great falls. Glacial Invasion. — In times long ago, called the Glacial Period, all of the mainland of New York, except small areas in Allegany and Cattaraugus counties, was covered with a slowly-moving sheet of ice. The ice flowed across the Adirondacks, the Catskills, and the plateau region farther west, and covered most of northern Pennsylvania. This immense glacier pushed along in front of it and under it a vast amount of soil and broken rock. More material of the same sort was carried along with the ice and accumu- lated at the melting margins of the ice sheet. Hills of sandy soil, gravel, and stones, formed GEUURAIMI^ Ol NKW ^()RK III this way, are called moraines. Such hills are found near Rochester, Ithaca, and Cort- land, and at Oriskany Palls and in many other parts of the state. Stones frozen m the ice were rubbed over the bed rocks and gradually worn away, forming; a Hne clay in which some worn stones were also mixed. Some of this material, called bowlder clay or till, was packed into valleys over which the ice passed, thus block- ing the channels through which pre- glacial streams had flowed. Some of the bowlder clay gathered in hills called drumlins, shaped by the ice pushing over them. In the region between Syracuse and lulton on the east and Rochester on the west, and from Auburn and Geneva to Lake Ontario, there are hundreds of drumlins running north and south and rising from 50 to 1 50 feet above the surrounding plain. When the ice finally melted from the sur- face of the state, it left a sheet of stony clay, or till, on most slopes and tops of hills and mountains. But much of the finer muds and sands had been .sorted and spread out on lower lands by the streams that flowed from the melting ice. Many of the cobblestones and bowlders re- mained where they were dropped as the ice melted. Almost everywhere the fields of New York show bowlders and cobblestones which are unlike the bed rocks that lie be- neath the soil. Bowlders in western New ^()rk may ha\e come troiii Canada (ji 1 10111 jiarts of the state north of the locality where they are found. Bowlders on the plateau in central New ^'ork may have come from St. Lawrence County, or from the .Adirondacks or from the Mohawk \'alley. Gorges and Waterfalls. — No other state in the east has .so many splendid waterfalls and gorges as New York. At the close of the Glacial Period, the Niagara River plunged over the Niagara Escarpment at Lewiston. Since that time the gorge, now seven miles long, has been cut, the falls retreating slowly to their present position. So wonderful are the falls and the gorge that the adjoining ground has been made a state reservation, under the control of the Niagara Commis- sion. The other great gorges and falls of the state are also more or less due to the glacial inva- sion. Deposits of glacial waste clogged old valleys and caused the streams to take new courses over rock ledges, and the deep, narro\\ channels then made are not yet old enough to have been broadened by the stream and bv the wasting of the valley sides. Fine examples of such gorges are found along the Genesee from Portage to Mount Morris, and along the same stream at Rochester. Letchworth Park, belonging to the state, is at the upper and middle Portage Falls. GEOGRAPHY OF NEW YORK There are many gorges and waterfalls in the Finger Lake region. Of the gorges Watkins Glen — another state park, at Watkins — is the best known, and is of great beauty. The gorge is in places 300 feet deep, and the small stream that flows through it forms a constant succession of fine cascades and rapids. Near Cayuga Lake is Taghanic Falls, whose height is the greatest in the state, over 200 feet. On West Canada Creek is the Trenton gorge, in which are several beautiful falls. The Cohoes Falls are on the lower Mohawk. The Ausable Chasm is a narrow gorge near Lake Champlain. Review. — i. What physical regions of the eastern United States are represented in New York t 2. Describe the surface of Long Island. 3. Name some of the beaches on the south shore. 4. Describe the surface of Manhattan Island. 5. Locate and describe the gorge of the Hudson. 6. Describe a valley which joins the Hudson Valley at Kingston. 7. Where are the Shawan- gunk Mountains ? 8. Name the highest moun- tain m New York, and give its altitude. 9. What are the chief occupations in the Adirondack region .' 10. Why should the Adirondack forests be pre- served ? II. Of what great region are the Catskili Mountains a part.? 12. What is the Helderberg Escarpment.' 13. Describe the plateau in central and western New York. 14. What purposes are served by the lakes of the plateau f 15. Describe the glacial Lake Iroquois. 16. Ex- plain the origin of the " Ridge Road." 17. What is the Niagara Escarpment? 18. What is till.? 19. What part of New York has many drum- lins .? How were they shaped ? 20. What gorges and waterfalls are owned bv the state ? Lakes. — New York has an exceptional number of large lakes, and most of them are due to the glacial invasion Besides Lake Ontario and Lake Erie, there are such large bodies of water as Chautau- qua, Seneca, Cayuga, and Oneida lakes. Lake Champlain. and Lake George. The Finger Lakes are in old valleys which were deepened and blocked by the ice and its deposits. The same is true of the Adiron- dack Lakes. In all parts of the state are small lakes and ponds, many of which lie or. the uneven surface of the glacial drift. especially where thick morainic accumula- tions are found. Drainage. — The student should review the account of rivers and valleys in the early part of the geography. The drainage of the main- land of New York is remarkable for the fact that its waters belong to so many river sys- tems, reaching the ocean by way of the Gulf of St. Lawrence, New York Bay, Delaware Bay, Chesapeake Bay, and the Gulf of Mexico. Let us study the different river sys- tems of the state in this order. The St. Lawrence Drainage. — A study of the map on page xi shows that more of New York state drains into the St. Lawrence than into any other river system. Several small streams flow into Lake Erie or into Niagara River. The Genesee, the chief river of west- ern New York (p. ii), flows northward across the state to Lake Ontario. The waters of all the Finger Lakes and of Oneida Lake reach Lake Ontario through the Oswego River. The Black River drains a large section of the west- ern Adirondacks and is the most important stream in that part of the state. Like the streams already mentioned, it discharges into Lake Ontario, and as the St. Lawrence River is the outlet of Lake Ontario, the waters from all these streams finally reach the Atlantic through the Gulf of St. Lawrence. The same geo(;raimiy of new york Mohawk (liaiii large areas of tin soutli- ern Adirondacks. On one of the branches, West Canada Creek, at Trenton Falls, is large water power. Power is developed on many other branches, as well as on the Mohawk itself at Little Falls and Cohoes. The Mohawk was navigated by small barges in the early days of the colony, and 'by means of dams and locks it is now used as a section of the Barge Canal. The Delazvare Drain- age. — The Delaware River drains a large IS true of the drauiage of the northern and part of the rugged and picturesque country northeastern .Adirondacks. The Oswe- of southeastern New York into Delaware gatchie. Grass, Racket, St. Regis, and Bay. Some of its tributaries reach far into Salmon rivers flow into the St. Lawrence, the Catskill Mountains, where their falls and while the Saranac and Ausable rivers and the rapids add greatly to the attractiveness of waters of Lake George reach the main stream summer resorts. through Lake Champlain. The Susquehanna Drainage. — The Susque- The Hudson Drainage. — The Hudson River hanna River drains a larger area within the Drainage basins of New York IS the great stream of the southeastern Adiron- dack region. It leaves the mountains a little above Glens Falls and occupies a broad low- state than does the Delaware. It rises in Otsego Lake, and leaves the state near the village of Waverly, reaching the sea at the land valley to a point below Newburgh, head of Chesapeake Bay. Among its trib- thence following the Highland gorge and the utaries are Unadilla Creek and Chenango foot of the Palisades. In its upper course River in central New York, and the Chemung there are numerous falls and rapids, but River flowing from the west, below Fort Edward there are dams and locks The Allegheny Drainage.— 'Vh^- .Allegheny making it part of the Barge Canal, and from River drains parts of Allegany, Cattaraugus, Troy to the ocean it is a tidal stream, much and Chautauqua counties in the southwestern used as a waterwav. The falls are used for part of the state. Its waters finally reach the the development of w^ater power especially Atlantic through the Ohio and Mississippi at Corinth, Spier Falls, Glens Falls, and rivers and the GuH of Mexico. Even Chau- Mechanicville. Scarcely less important than tauijua Lake and its inlet streams, within a the main stream is its great western tributary, few miles of Lake Erie, belong to this drainage the Mohawk. The northern branches of the system. GEOGRAPHY OF NEW YORK Average temperature in Jariuary Average temperature in July Climate. — New York is in the track of the great cyclonic movements which cross the country from west to east. The prevaiHng winds are from the west, and the interior of the state has the continental type of climate, with hot summers and cold winters. The usual maximum temperatures in July or August are from 80° to 90°, and these, owing to the moisture in the air, or its humidity, give sultry and oppressive weather. More rarely 95° or above marks the summer maximum. Throughout the interior of the state, the ground usually has a cover of snow during the winter months. Along the Atlantic coast snows are less frequent, but are occa- sionally very heavy. In the higher plateau regions, temperatures of 20° or 30° below zero may occur once or more during the winter. In the Adi- rondacks, records of 40° or 50° below zero are to be expected. In western New York along the Great Lakes, and in south- em New York by the sea, the extremes are Average annual rainfall more moderate, but the temperatures ranging from 20° down to the zero point are severe on account of the winds on the lakes and on account of the greater humidity by the seashore. The annual rainfall varies from about 30 to about 55 inches annually according to local- ity. There is thus, in ordinary years, every- where ample rainfall for crops, although in some summers there may be several weeks of serious drouth. The heaviest rains occur on the highest mountains, — the Adirondacks and Catskills. Eastern and southeastern New York have more rain than western New York, because of nearness to the sea ; for the southeast and south winds of the cyclonic storms bring moisture from the ocean. The length of the growing period — be- tween the last frost in spring and the first frost in fall — varies from about 130 to about 190 days in different parts of the state. The distribu- tion of crops is much affected by the way different regions vary in temperature. GEOGRAPin' OK NEW YORK The length of the growing season, tlie aver- age temperature, and the average annual rainfall combine to make Long Island, the lower Hudson Valley, and the lake country of western New ^ Ork regions favorable for fruits, wheat, and corn, while the plateau is better suited to grass and oats, and the higher lands of the Catskills and Adirondacks are suitable for little besides forest. Soils. — The soils of New York are ncarl\ everywhere of glacial origin. In most of the Adirondack region the soil is thin, and is not of great fertility, and this combined with an unfavorable climate makes that region un- productive. The rocks under the Lake Plains, and under much of the Hudson and Mohawk valleys, are such that the soils which they form are naturally fertile. Ihe plains were also enriched by the fine mud or silt de- posited in the glacial lakes as already described. The soils of the Catskill-Alle- gheny Plateau are largely formed from the underlying sandstone, which produces rather poor soil. This soil, however, especially in the northern parts of the upland, was un- proved by the waste from the more fertile region to the north when tins waste was transported southward by the ue and mingled with the poorer native sod. Along the flood plains of the Genesee, .Mohawk, Hudson, Black, and Susquehanna rivers, and many lesser streams, the finer glacial material has been moved, worked over, and deposited by the rivers. When these low flat grounds are properly drained and cultivated they produce abundant crops. rile glacial till (p. i\) also usualK gives a fairly good soil. Natural Vegetation and Forest Products. In the /\ilir()iulacks the forest consists mainly i)f white pine, spruce, hemlock, and birch. As white pine is very easily worked, it has been for many years a favorite building material, and most of the mature pine has been cut. The rest of the state has a pre- dominance of hardwood trees, mingled with a lesser number of conifer- ous trees. The chief hardwoods are maple, beech, ash, oak, chest- imt, cherry, and hickory. \mong the softer woods, basswood is widely dis- tributed. The state owns about 2,000,000 acres of forest in the Adirondacks and the Catskills. In botli of these regions there are large estates or private parks, amounting in all to several hundred thousand acres. Other tracts are held by lumber companies. In the less densely settled parts of the state many of the farms still have wood lots, from which the owners get material for fences, firewood, and some coarse lumber. From the sap of the hard maples the farmers make a considerable amount ot maple sirup and maple sugar. Much spruce timber is cur in the Adiron- dacks, whence it is carried to the convenient centers of water power on the outskirts of the region and made into wood pulp. In this industry New York has a high rank, but the total amount of lumber cut each year is much smaller than it was fifty years ago. Through schools of forestry and by private enterprise efl^orts are being made to reforest some of the less valuable lands of the state. ^. Adii GEOGRAPHY OF NEW YORK Animal Life. — Wild life is found in its most conspicuous development in the Adirondacks. Moose and deer are protected by law. Deer may be hunted during a brief season. A single hunter is not permitted to take more than two deer. The law prohibits trapping beaver, which, notwithstanding their abundance in the days of the early fur trader, were for a time in danger of extinction. Black bears are occasionally seen, and a bounty is offered for killing wolves and panthers. Hares, rabbits, and squirrels are common m all parts of the state, as are also muskrats and woodchucks. Foxes are not uncommon, and waterfowl and other game birds still oc- cupy the marshes, lakes, and forests. There is important oyster fishing off the shores of Long Island. Bluefish and clams are also taken, and shad are caught in the Hudson. In the Great Lakes and other fresh waters of the state, the trout, black bass, pickerel, whitefish, and muskellunge are among the important species. F"ish hatcheries are maintained for restocking the lakes and streams with valuable kinds ot fish. All these forms of wild life, and the song birds as well, are under the care of the State Conservation Commission, and game wardens have been appointed to prevent violations of the game laws. Review. — i. What river systems are represented in New York ? 2. Where do the waters of each river system enter the ocean .^ 3. What are the principal rivers of western New York .? 4. What are the main streams in the western Adirondacks .? In the northern Adirondacks.? 5. For what reasons is the Mohawk Valley important ? 6. What are the minimum temperatures of the plateau region ? Of the Adirondack region ? 7. Compare the rainfall of the coast region and of the Great Lake border. 8. How was the soil of the Lake Plains en- riched ? 9. How was the soil of the plateau improved ? 10. Where are flood-plains ? II. What are the leading kinds of hardwood trees in New York ? 12. Describe the regulations for game protection. 13. What commission has charge of these interests ? INDUSTRIES Agriculture. — When the 13th census was taken in 1910, New York stood eighth among the states of the United States in the value of all farm products. Illinois stood first, followed in order by Iowa, Texas, Ohio. Georgia, Missouri, and Kansas. The most valuable single crop in New York was hay and forage, its value being a little less than two fifths of the total value of the farm products of the state. Cereals were second in value with about one fifth of the total. Vegetables, fruits, and forest products followed in order of importance. We have already seen that New York shows great variety in soil, altitude, tempera- ture, and rainfall. Such differences have naturally led to great differences in the kind and character of the crops raised. Wheat is confined almost entirely to western New York. Corn is well distributed over the state except in the Adirondack region, but the crop does not compare with that of the states in the corn belt, from Ohio to Kansas. Oats, being hardy, are grown more generally than corn. Of the lesser cereals, some barley and rye are raised ; and New York ranks with Pennsylvania as one of the leading states in the growing of buckwheat. CJEOCJRAl'HV OF NKW YORK ^ ,.y^§^^^ir^0^^$S! One dot equals :;,000 tons. The solid bl^iclc areas are formed by Oie closeness of the dots In rccioDS ui create' Hay and forage production Hav and forage are not only the largest crop, but in this product New York is surpassed by no state but Iowa. This large product makes possible a great dairying in- dustry. At the census of lyio New ^ ork had more dairy cows than any other state, being slightly in advance of Wisconsin and Iowa. The success of this industry depends upon conditions of soil and chmare, aiui upon nearness to market. The cool uplands of the plateau region are well suited to grass. While the climate is not so favorable for ripen- ing grain, corn can almost everywhere be brought to a state of maturity suitable for silage. In this form it serves as a nourishing food for great numbers of cattle throughout the winter months when other green food is not available. .\s nearly three fourths of the ten millions of people in New York state live in cities and large villages (census of 191 S), they require enormous supplies of dairy products. Rail- roads whose trains carry fresh milk and cream to the city of New York extend through all central New York to Lake Ontario, and far into western and northern New York. Throughout these dairying regions the farm- ers may be seen early in the morning carrying the milk to some near-by milk station, where it is cooled and then shipped in refrigerator cars to New 'V'ork or some other city. One (lot equals ^i#?^ /■^^^-l.^ Number of dairy cows In nearly every dairy district, but more especially in regions at some distance from the larger cities, creameries and cheese fac- tories abound. This is true of the high plateau region of southwestern New York, and of the belt of lowland between the Adirondacks and the Canadian boundary. Various factories are devoted to the manu- facture of condensed milk, milk powder, and other dairy products. In recent years much attention has been given to rearing the best breeds of stock, and both state and federal authorities prevent as far as possible the spread of tuberculosis among cattle. Animals affected by the foot and mouth disease are slaughtered and buried to prevent the spread of that dreaded plague. In the rearing of sheep and swine New York does not take high rank. In the value of poultry, however, the census figures show that New York was exceeded by only five states. Here, as in dairying, however, the trade is chiefly local, as the cities make large demands. In the production of fruits New- York is second only to California. Small fruits are grown in all parts of the state except the Adirondacks, the Catskills, and the plateau of southwestern New York. Orchard fruits are raised everywhere in the state except in the central Adirondacks. They are especially GEOGRAPHY OF NEW YORK Production of orchard fruits abundant on the Lake Plains of western New- York and in the Hudson Valley. South of Lake Ontario is a belt of apple, pear, and peach orchards, unequaled m any other part of our country. New York has regions well fitted in climate and soil for the raising of grapes. Chief of these is the Chautauqua " grape belt," bordering Lake Erie in the southwest corner of the state and extending into Pennsylvania. In this region many grapes are used in the manufacture of unfer- mented grape juice. Ne.xt is the Finger Lake region, particularly about Lake Keuka, andcenteringin the region around Hammonds- port. In this district there Is a large grape juice industry. Some grapes are raised also in the Hudson Valley. New York is the leading state in the produc- tion of potatoes. Western New York and Long Island are the regions of the largest potato production. Miscellaneous vegetables are also important, especially in Long Island, where large quantities are grown for the New ^'ork market, and in Monroe and Erie counties, for the supply of Rochester and Buffalo. Large crops of onions are raised in Orange, Wayne, and Madison counties. Fhe canning of fruits and vegetables has also become an important industry. Among special crops may be named the hops grown in central New ^'ork, mainly in One dot equals l.OOO.OOO pounds. The solid black termed by the Production of grapes Otsego, Schoharie, Oneida, Madison, and Montgomery counties. Peas and beans are raised mainly in northern and western New York, and in the counties bordering Lake Ontario and the f inger Lakes. Some tobacco is raised in central and southern New York ; Onondaga and Chemung are the leading counties in that crop. Hothouse and nursery products are grown in and near the greater cities, and the nursery farms about Roches- ter, Geneva, and Dansville are among the most extensive in the United States. Review. — i. What is the rank of New York in farm products ? 2. What state rivals New York in producing hay and forage? 3. How are dairy supplies furnished to the city of New York : Potato production GE(x;RAnl^ of nkw ^ork 4. Where are creameries and cheese factories numerous ? v What regions in the state raise much orchard fruit ? 6. What regions of New ^'ork arc favorable for grapes? 7. In what parts of the state are hops grown ? Peas and beans? Tobacco? Nursery products ? Water Resources. — When the population of a country increases, well waters are in danger of pollu- tion, and the wells are gradually abandoned. As a result all the large cities and villages of the state, and many smaller ones, now have public water supply. In order to suppl\ water for the city of New ^'ork immense dams and reservoirs were constructed in Westchester and Ulster counties, many miles from the great city. Some cities and villages draw their water supply from large streams, but many rivers have become impure through sewage and the waste from manu- facturing plants. City water supplies, there- fore, are generally drawn from lakes, or from reservoirs fed by small streams in forests or farming districts, where all possible safeguards against pollution have been taken. Thus the city of Utica receives water from reservoirs in the neighboring hills, and from the West Canada Creek, an Adirondack stream; Syra- cuse derives its supply from Skaneateles Lake, Rochester from Hemlock Lake, and Buffalo from Lake Erie at the head of the Niagara River. Few^ states are so well provided with water power as New York. The greatest single water power in the state is at Niagara Falls, where several plants are situ- ated. Here electric power is developed on a large scale. Dvnamos in a Ni and transmitted to Buffalo and to other cities and villages. Ihe waters of the Genesee River at Rochester have long been used foi power. Throughout the plateau and Fingei Lake region many waterfalls are suited to this purpose, and many streams flowing from the Adirondack region provide power foi large mills and factories. Mineral Resources. — Of the mineral re- sources of the state, the most widely distrib- uted are the building stones. Granite is quarried in the Highlands of the Hudson, in some parts of the Adirondacks, and on Grindstone Island in the St. Lawrence River. Limestone is found in the Hudson and Mohawk val- le\s, near Trenton Falls, at ( )riskany Falls, in the hills south of Syracuse, and in the vicinity of Lockport, Niagara Falls, and Buffalo. Several public buildings in Syracuse are constructed of Onondaga limestone. Mar- ble, which is a changed linu-stone, is quarried at (>ou\erneur in St. Lawrence C()unr\, and at Tiickahoe, near the city of New ^'ork. Much ordinary limestone is " burned,"' that is, it is highK powrr pl.'iin GEOGRAPHY OF NEW YORK heated and changed into quicklime. A cer- tain kind of limestone is called hydraulic limestone because when burned and ground it becomes a cement that " sets " under water. Limestone of this kind is quarried near Kings- ton and near Syracuse. Sandstone occurs in many parts ot the state. The Potsdam sandstone of northern New York is a very hard, reddish rock, and a valuable building stone. The Medina the place of the natural limestone cement, and plants for its manufacture are found at several points, as on Cayuga Lake near Ithaca, at Jamesville near Syracuse, at Howe Cave in Schoharie County, and at Hudson and Catskill. Clay is used in many parts of the state for making brick, drain tile, and sewer pipe The largest beds are along the Hudson, and in this valley there has grown up one of the greatest brick-making industries in the world. The bricks are readily transported in scows to New York and other cities. Gypsum occurs in Cayuga County and m some other parts of central and western New York. It is used for fertilizer and for making wall plaster. New York is one of the most important states in the production of salt. Before the coming of the white man, the Iroquois Indians found salt springs where Syracuse now is, and they made salt by evaporating the brine. In 1880, a boring in western New York revealed the fact that there are beds of rock salt far below the surface. These beds are now reached by wells, into which water is poured to dissolve the salt. The brine is then sandstone, quarried in Orleans County, is a brownstone used as a building stone and pumped out and the water is evaporated to for paving blocks. Another sandstone used in building is the bluestone of western New York and of Chenango and neighbor- ing counties. The flagstone of Ulster, Delaware, and Greene counties is quarried in large, thin slabs for various uses. A coarser rock of the same nature, called conglomerate or grit, is quarried in Ulster Count}'. In Washington County, as in the neighbor- ing part of Vermont, slate is quarried and is used for roofing and ornamental work, and for school blackboards. Portland cement is made of limestone and secure the salt. Shafts have also been sunk, clay. The clay may be taken from uncon- so that the salt may be mmed m blocks, solidated clay beds of glacial origin, or from Silver Springs, Warsaw, Retsof, CuylerviUe. more ancient clay rocks, known as shales. Watkins, and Ithaca are localities known for This manufactured cement has largely taken the salt industry. CKOtJRAl'in OF NLW ^()RK The city of Olean is in the mulsr ot a petroleum region whicli extends into New ^Ork from the larger oil fields of western Pennsyl- vania, riiousantls of petro- leum wells ha\e heen bored in Cattaraugus and Allegany counties, and this region still continues to furnish a con- siderable amount of oil. Re- lated to petroleum is natural gas, which occurs in paying quantities in the oil region, also in several other counties of western and central New York. Graphite is mined near Lake George, and much talc, used with pulp in making paper, is found in St. Lawrence County. There are important deposits ot magnetite, a pure kind of iron ore, in the eastern Adiron- dacks on the borders of Lake Champlain. Red hematite, another imn ore, is found in Oneida and Wa\ne couinus : some of it is ground for making a coarse kiiul of led paint. Review. — i. Why do cities seek \v;irer supply from ink.es and the headwaters of rivers ? 2. Describe the largest water power in the state. S. What other regions have much water power? 4. Where is granite found ? Sandstone ? Marble.? Slate? 5. Where are the largest clay deposits in the state ? 6. What use is made of this clay ? 7. By what methods is salt obtained ? 8. What part of the state produces petroleum ? Natural gas ? 9. Where are deposits of iron ore found ? Manufacture. — The total value of all manu- factures in the state of New York, at the census of 1914, was nearly four billion dollars. No other state reached this figure. In like manner the city of New York led all other cities, producing a value of more than two billion dollars. New York has been the first state in the value of its manufactures since 1S25, the date of the opening of the Erie Canal. Through the completion of this great transportation route, the popuiarion of the state grew rapidly, the farm produce was increased, the cities were enlarged, and business and com- merce centered more and more in the Lmpire State, and in its greatest city. Of 265 kinds of manufactures on which the United States census makes reports, 243 are represented in this state, and 217 in the city of New York. New York stands first not only in total value but also in a number of special kinds ot manufactured goods. Among these is men's clothing, in which the product is more than twice that of any other state ; also women's clothing, with about nine times the value of that of any other state. The state also leads in printing and book making, baking products, sugar refining, tobacco manufactures, milli- nery goods, fur goods, pianos and organs, confectionery, copper, tin, and sheet iron products, paint and varnish, patent medicines, and man}- other manufactures. In all the in- dustries named in this paragraph, the city of New York is far in the lead among the cities of the state and of the country. Among the other important manufactures in which the state leads, are hosiery and knit goods, paper, chemicals, electrical machinery and supplies, and carpets and rugs. GEOGRAPHY OF NEW YORK Packing room of a Buffalo flour mill slaughtering and meat packing. No one of these industries falls below $100,000,000 in the state, and the two clothing industries taken together produce an annual value of nearly $600,000,000. The only industry of these five for which the state affords much raw material is printing and publishing. The material is largely paper, and a very large share of the newspaper stock is manufactured in the pulp and paper mills of the Adirondack region. For the other four industries the state provides little material. The clothing indus- tries use cotton, wool, flax, and silk goods as well as furs, feathers, and a variety of metallic and other substances for buttons, buckles, New York state is second to Minnesota in and various ornaments. Practically all of flour and gristmill products. Although it is these materials come from other states or far from the great grain fields of the west, the other countries. In like manner, most of the railways and the ships on the Great Lakes bring enough grain to the New York mills to make this possible. As the greater num- ber of people live in the east, the largest markets are in the east, and there is some- times economy in bringing the grain near to the market where flour is in demand, before it is manufactured. In like manner. New ^'ork ranks next to Illinois and Kansas in meat packing, although the state produces but few of the cattle and swine that supply its meat-packing establish- ments. In this industry, the city ot New York ranks next after Chicago and Kansas City. New York state also ranks high in the production of butter, cheese, and condensed animals which are the raw material of meat milk, reaching more than half the product of packing are brought from states farther west. Wisconsin, the leading state. In foundry and Most of the iron and steel also, for foundry machine shop products the state of New York and machine-shop work, is made in Penn- is second to Pennsylvania and Ohio, and the sylvania and other states, the principal excep- city is next to Chicago. The state takes third tion being the product of furnaces near place in the manufacture of automobiles, and Buffalo and in the region about Lake Cham- second in that of boots and shoes. plain. Thus it is not the presence of raw The five leading industries of New "S'ork, materials, but facilities for transportation and both state and city, are: women's cloth- for marketing the products, that have de- ing, men's clothing, printing and publishing, veloped the largest of New York's manufac- foundrv and machine-shop products, and turing industries. CKOCiRAPin OK NKW YORK The clotliin^ product of New ^'ork is nearly one half of the total for the United States. This means that the state not only clothes most of Its own people, iiut its marketing facilities enable it to supply the people of many other stares. In the same manner, the machine shops rake the steel from other states, make agricultural imiilements, t\ pe- writers, gas machines, gas and water meters, hardware, iron pipe, plumbers' supplies, heat- ing apparatus, structural iron, and many other things, and sell them in all the markets of the world. Another example of raw material hioiight to New ^ oik tor manufacture is lumber. New York toiiiuiU cut much lumber from its forests, but the supply has decreased, and at the present rime about twenty states draw a larger product from their forests than does New York. But this state, nevertheless, supplies three fifths as much as Washington, the leading state in this industry, in tin value of the things made out of lumber. A further case of this kind is found m the grinding of corn, buckwheat, and oats. Of these three grains. New \'ork leads only in the production of buckwheat, and is eleventh in the raising of oats, and twenty-fifth in the throwing of corn. Yet she holds first place HI milling all three. Se\eral manutactuiing industries of New York are localized or concentrated in a single city, or a group of neighboring cities. Nearlj' one third of the hosiery and knit goods, in- cluding knit undergarments, hose, sweaters, knit gloNes and mittens, hoods, and scarfs, produced in this countrx', are made in the state of New ^ oi k. C'ohoes is the center of this industry, where it began in 1832, with the invention by a local manufacturer of a power knitting machine. The falls of the Mohawk at that place lia\e furnished the necessary power. Otiier large mills are found at Am- sterdam, Little Kails, Utica, and other cities and villages in the Mohawk Valley. The making of collars, cuffs, and shirts is localized in the city of Troy, which now makes about nine tenths of all the goods of this kind made in our country. Glens Falls is also a center for this industry. As in the case of knir goods, the raw materials must all be imported, and there is no geographic reason wh\ these special industries should have developed in these particular localities. A favorable start was made many years ago, skilled labor developed, markets were estab- lished, such places as Cohoes and Troy gained a reputation for their products, and the busi- ness has thus centered itself more and more in these cities. GEOGRAPHY OF NEW YORK The same influences led to the location and development of the leather glove and mitten industry. New York makes about 60 per cent of the product in the country. Fulton County has about two fifths of the glove fac- tories of the United States and makes more than half the gloves and mittens, on the basis of value. The industry is cen- tered mainly in the two neighboring cities of Gloversville and Johnstown, in which the making of gloves and mittens is the chief industry. The skins must all be brought from remote regions, and the coal for power is brought from Pennsylvania. Much of the labor, however, is hand labor, and these cities are known everywhere for the quality of the work. Many industries are concentrated in the city of New York. For example, this city produces about 60 per cent of the country's millinery and lace goods, and 70 per cent of the country's fur goods and women's clothing. The refining of sugar is a large industry in the borough of Brooklyn, as is also the roasting and grinding of spices and coffee. Among manufacturing industries which are based on raw materials produced in the state. 1 M^m ml [^^^ Amip' 'i^.^ s Vl^cl^^ rall^. JBIbi iln'^t^fl^ wB pps HHp^ I'^-iM--^ Sewing room in a glove factory, Glovcrsv.lk the making of butter and cheese has been studied under the head of Agriculture. Another kind of manufacture which uses home products is can- ning and preserving. There are nearly 800 establishments of this kind in New York, canning fresh vege- tables and fruits, and making pickles, pre- serves, and sauces Beans, corn, peas, pumpkins, squashes, and tomatoes are tht chief vegetables used. and the fruits consist of apples, pears. peaches, plums, cherries, and berries. Review. — I. Give the value of manufactures in the state, according to the last census. 2. Name several kinds of manufactures in which the state stood first ; several in which the city of New York stood first. 3. What five manufac- turing industries each put out products exceeding in value $100,000,000 ? 4. How does New York rank in the production of lumber, and in the manufacture of lumber.'' 5. Give an account of the concentration of the knit-goods in- dustry. 6. What are the centers of glove mak- ing .'' 7. What industry is concentrated in Troy .' What industries in the city of New York ? Transportation Routes. — The most impor- tant route in the state leads from the city of New York up the Hudson River to Albany, westward to Schenectady on the Mohawk River, through the Mohawk Valley to Utica and Rome, and across the Lake Plains to Niagara and Buffalo. In this distance of about 450 miles from the ocean to the lakes, the only considerable railroad grade is found for a short distance west of Albany. The divide between the Mohawk and Ontario basins is passed at Rome, at an altitude of about 450 feet. This route is followed by the New York Central lines, by the Erie branch of the New York State Barge Canal, and bv a series of state roads. CKOCRAIMH' Ol- NKW \()\iK In the early days people and goods were transported up tin- Hudson by boats. 1 he goods wen then carried across the divitli between Albany and Schenectad\ on the Mohawk River. Thence the passage was by boat up the river to the Oneida Carrying Place, where Rome now is. More than i hundred years ago, settlers passed into central and western New York by this route. From the carrying place at Rome, boats were again used down Wood Creek, and through the Oneida and Oswego rivers to Oswego. From the junc- tion of the Oneida and Seneca rivers the route by the Seneca River led westward n> \uburn, Geneva, and Canandaigua. Very early in the history of the state a small canal, equipped with locks, was dug to avoid the rapids at Little Falls. A canal was also Jug at the Oneida Carrying Place, and a high- way beginning by the Mohawk Ri\er at Utica, known as the Genesee Road, was built through the forest, westward to Auburn and Geneva. Over this road a multitude of settlers went into western New \'ork and on to Ohio. The long journey by boat on the rivers, or by w'agon on new roads, made traffic between western New York and the Hudson Valley tedious and expensive. Farmers could not afford to send their grain and fruit to Albany and New York, where it was needed, and there arose an agitation in favor of a canal to join Lake Erie and the Hudson River. The project was taken up by De Witt Clinton, governor of New York, and in 1S17 the work began near Rome. The canal was completed in 1825. Navigation was begun with an elaborate celebration, and the event was for that time quite as important as the opening of a transcontinental railway to-day. As a consequence, the produce of western New"h'ork could be profitably marketed in the east, and settlers rushed westward to take advantage of rich and cheap lands, and to build new homes in western New York, in Ohio, and on the western prairies. Later, a railway was built from Albany to Schenectady, — the first in the state, — and still later sections were completed between Schenectady and Utica, between Syracuse and Auburn, between Utica and Syracuse, and finally, by the addition of other links, a series of roads joined the city of New York and Buffalo. These roads were made into one system — the New York Central — in 1869. Some years afterward the West Shore Rail- road was built, and as it was finally leased by the New York Central Lines, the last- named system now has four tracks leading from New York to Albany, and six from Albany to Buffalo. Other trunk railways, running for long distances through our state, extend from the city of New York westward. One of the first railroads of New York was the New York Lake Erie and \\ estern, passing through Port Jervis, Binghamton, Elmira, and Hornell, to Dunkirk and the west, and from Hornell ovei the Poitage Gorge of the Genesee River to Buffalo. The Delaware Lackawanna and Western Railroad, entering the state from Pennsylvania, extends from Binghamton to Utica, from Binghamtf)n to Syracuse and GEOGRAPHY OF NEW YORK Oswego, and from Binghamton to Buffalo. The New York Ontario and Western Railway crosses mountain and plateau from New York, by way of the cities of Middletown, Norwich, and Oneida, connecting at Oswego with the Rome Water- town and Ogdensburg division of the New York Central Lines, for the west and north. The Lehigh Valley and Pennsyl- vania railroads run across cen- tral and western New York to ports on Lake Erie and Lake Ontario. All the railroads above described, except the New York Central Lines, carry immense amounts of coal into New York and to lake ports for Canada. The Erie and the Delaware Lackawanna and Western railroads take advantage of the Susquehanna and Chemung valleys, which offer a great east and west route in south- ern New York. Between this route and that of the New York Central Lines, many valleys cut through the plateau in a north and south direction. Many of these valleys are uti- lized by railroads, including the Unadilla, Chenango, Cayuga, Seneca, and Genesee valleys. Another great natural route extends up the Hudson Valley, across the divide near Fort Edward and through the Champlain Valley to Montreal. This route from Albany, Troy, and Schenectady northward is followed by the Delaware and Hudson Railroad, which also reaches from Albany to Binghamton, and to the coal district of northeastern Pennsyl- vania. Several branches of the New York Central Lines serve the region west and north of the Adirondacks, and several rail- roads penetrate the Adirondack region. After the Erie Canal was finished, several other canals were constructed, but some of them were later abandoned. A canal that is still maintained connects Rome with the Canals of New York Black River Valley, by way of Boonville. The other canals still maintained by the state have been enlarged or reconstructed as parts of the Barge Canal system. The New York State Barge Canal is by far the largest and most important piece of canal construction ever undertaken by any state. The navigable waterways thus provided are approximately 540 miles in length, and large and deep enough for barges of 1000 tons each. Several lakes, and several canalized rivers, are included in the system, as shown by the map above. On the map, trace routes from Troy to Buffalo, and to Whitehall ; from Oswego to Syracuse, to Ithaca, and to Watkins. During recent years the state has built many good roads, joining the larger cities and villages, and furnishing outlets for the produce of the farmers. The need of good roads for rural delivery of mails, and for automobile traffic, has been influential in developing this form of transportation facilities. Electric railways have also been extensively built in recent years, not only for the con- venience of cities and their suburbs, but as interurban roads which join many of the larger cities and towns of the state. These roads are most largely developed between Albany and Buffalo, as parallels to sections of the New York Central Lines. CKOCRAlMh Ol NKW ^ORK 1 he city of New \ oik staiitls as tlu wisniii terminus ot the most traveled ot all oeiaii routes between the United States and hurope. It is also one of the principal ports tor the extensive coastinn traffic which follows our shores from Maine to the (lulf ol Mexico. Buffalo is the eastern terminus of much ot the Great Lake trafHc, and there is local traffic on Lake Ontario from Oswego, Roches- ter, and other New' ^'ork ports, to Toronto and K.iii<;sron m Canada. Review. — i. What is the leading transporta- tion route in the state? 2. What large cities are on this route? 3. How was Mohawk naviga- tion first improved ? 4. \\ here was the (ieiiesee Road ? 5. (live an account of the making of the Erie Canal. 6. When was the tirst railway built in the state ? What points did it join ? 7. (live the names and routes of the trunk railroads lead- ing westward through the state. S. What canals are included in the Barge Canal system ? 9. (nve an account of the extension of good roads. 10. What is the importance of HufFalo. in drear Lake traffic ? POPUL.XriON Distribution of Population. At the time of the United States Census of 1920 the popu- lation of New York averaged 211 persons for each square mile. Only four other states have a greater density of population than this; namely, Rhode Island, Massachusetts, New |erse\', and Connecticut. Density of population in New York by counties. iy.;ij I he ma|) nil I his page gives the tleiisity ot jiopulation hy counties. The regions having a ilensity of 100 or more include all the coun- ties from Orange to the eastern end ol Long Island. Kach of the other counties of this density, such as Onondaga, .Monroe, aiul I'.rie, contains one or more large cities and villages. rhe only county that averages less than 3 people per square nnle is Hamilton, which is whollv in the Adirondack region of mountains and torest. In ndirlurn New \ ork, adjoining or near Hamilton County, several counties, Warren, Essex, Clinton, Franklin, St. Lawrence, Lewis, and Herki- mer, have each a density between 17 and 44. Kvery one of these counties has some rich lands and flourishing villages, but each also extends over large areas ot Adirondack forest. Similar densities are found in Allegany, Schuyler. Chenango, Delaware. Schoharie, and Sullivan counties, which have few large villages and whose uplands are largely de- voted to the dairying industry. Interme- diate m density, 50 to lOO, are counties having rich farms, with some large villages and small cities. Examples in this group are Jefferson, Wayne, Orleans. Genesee, Steuben, Madison, Ontario, and I Ister counties. On the whole, the densest populations ot New York are on Long Island, in the Hud- son and Mohawk valleys, on the Lake Plains, and on the flood plains of the Susquehanna and Chemung rivers. In other words, the regions ot lower altitude and milder chmate, of rich soils and good transportation facilities, support the most people. The cities and large villages are growing in pnpulation faster than the country districts. \i rhe time of the 1920 census 82.7 per cent of all the people of the state lived in cities or in \ illages having a population of 2500 or more. Ihe state, in 1910, had about 2.750,000 in- habitants who were born in foreign lands, or somewhat more than one fourth of the whole population. Most of the foreign-born li\e in the cities. The metropolitan district including northeastexn New Jersey and southeastern New York GE(X;RAl'li^' ()| NKW \i)\t popiiLiruin ill New ^'ork. ? 2. What is thi- ilinsity of pop- ulation in your own county : 3. Where are rhe densest populations in the state? 4. How ni;in\ cities are there in Xew \ ork ? 5. W'hat are the horoughs of Cireater New ^'ork .' 6. Ciive iength, width, and altitude of the island of Manhattan. 7. What geographic conditions have favored the growth of the cit\ of New \'ork ? 8. In what parr of the city is thi' wholesale track- centered ? rhe retail trade ? <>• Name sonu- of its public institutions. 10. Name its chief methods of transportation. 11. Under wli.it waters have subways been bmlt ? 12. Ciive location and nidusrries of ^Onkers; ofNewburgh; of Hudson. 13. What institution is at West Point? .'^t Poughkeepsie ? 14. W'hat are the two principal buildings ot .-Xlbaiiy r 15. What are the main industries of iroy ? Of Cohoes ? Of Cdens Falls ? 16. What cities are on the Mohawk River? 17. What are the mam in- dustries of each ? Cities and Villages of the Lake Plains. On the lowlands near the (ireat Lakes are many cities, includinji three which, after New- "N'ork, are rhe largest in the state. These are Biitt'alo, Rochester, and Syracuse. The two chief reasons for their growth are, — first, they are on one of the great natural transportation routes leading from the sea- board to the west, and .second, they are sur- rounded h\ wide areas of productive soil. Oneida is on the south edge of the plain, at the opening of a valley which leads through the plateau to Ringhamton. It is a thriving city, with several manufacturing industries. Near it, on the southeast, is Sherrill, the smallest city in the state. Syracuse also is on the south edge of the plain, and its streets and buildings extend up rhe northern slopes ot the plateau. lor- merly its main industr\' was the making of salt from brines obtained b\- boring. Now its growth IS due to other causes. It is on a spur of the I?arge Canal, and has railway connections in all directions. Among its more important manufactures are automo- biles, iron and steel products, food stuffs, typewriters, and men's clothing. The city is the seat of Syracuse University. Near Syracuse is the large village of Solvay, where great quantities of soda ash, sodium bicar- bonate, and other chemical products are made. Fulton, on the Oswego River, has excellent water power and manufactures woolen goods, firearms, and paper. Oswego, situated where the Oswego River enters Lake Ontario, is on the site of what was an important fort in colonial days. The leading industries are the making of matches, starch, and woolen goods, and the manufacture of boilers. It has a good harbor, and ships large amounts of coal. GEOGRAPHY OF NEW YORK Making cameras, Rochester Auburn, on the outlet of Owasco Lake, is one of the older cities of western New York. Its manufactures are chiefly agricultural im- plements, shoes, cordage, and twine. Seneca Falls is a large village on the outlet of Seneca Lake; it has manufactures of hydraulic ma- chinery. The city of Geneva is at the foot of Seneca Lake. It has nurseries and various manufactures, and is the seat of Hobart College and of the State Agricultural Experi- ment Station. Penn Yan is at the foot of Keuka Lake, and Canandaigua is at the foot ')f the lake bearing the same name. Newark and Lyons are on the main line of railroad between Syracuse and Rochester. Rochester lies on both sides of the Genesee River a few miles from its mouth, and in- cludes the lake port formerh' known as the village of Charlotte. Through this port, much trade is carried on with Toronto and other places in Canada. Rochester is on a branch of the Barge Canal and has several lines of railway. It is in the midst of a most fertile region. Ever since tlie early days, when western New York was the wheat cen- ter of the United States, there have been large rtouring mills at Rochester, where the falls of the Genesee River furnish much water power. The leading manufactures at the present time are men's clothing, shoes, and photographic apparatus, in which industry Rochester leads the world. There are, how ever, many other industries, and the city has more than 1200 industrial plants. About Rochester are some of the largest nursery establishments in the United States, for ornamental trees, fruit trees, vegetable and flower seeds, and bulbs. The city has attractive streets and homes and is the seat of the Mechanics' Insti- tute and the University of Rochester Batavia is midway between Roch- ester and Buffalo. Its main industry is the making of agricultural imple- ments. Medina and Albion are large villages in Orleans County, in the midst ot a rich farming and fruit-raising region. At Albion are extensive quarries. Lockport is a manufacturing city, whose largest industry is flour and grist milling. Buffalo, in 1910, ranked tenth in population among the cities of the United States, but ninth in the value of its manufactured prod- ucts. It is very natural that a great city should grow up at the foot of Lake Erie Between Lake Erie and Lake Ontario naviga- tion is interrupted by the rapids and falls of Niagara. Buffalo is therefore the eastern terminus of most of the Great Lakes traffic from Chicago, Milwaukee, Duluth, Detroit, and many other lake ports. It is the point where the products of the west are transferred from lake ships to the railways or canal. Trunk lines of railways reach out in all direc- tions. Buffalo handles immense quantities of flour and wheat as well as other grains. A lake steamer at Buffalo (;K()c;R.\i»in- of nkw ^ork Many largf elevators liave been Iniilr on the lake front to take care of the transfer of grain from ship to car or barge. liesiik-s grain, there IS a vast trartic in won, coal, and oil. Coal is reaclil\' ac- cessible from PennsN Kama, and is brought to Buffalo for local use and for shipment up the lakes. The city is near extensive oil and Adjoining Buffalo, but under a charter of natural gas regions, and has the advantage of its own, is the city of Lackawanna, which electrical power transmitted from Niagara has grown up in recent years as a steel Falls. This power is used for lighting the making city, using coal from Pennsylvania. city, for street railways, and for manufacturing purposes. Buffalo is an important mar- ket for lumlier, live stock, and fish. Buffalo has more than 1750 manufacturing estab- lishments. The chief indus- tries are slaughtering and meat packing, foundry and machine shop products, and rtour and gristmill products. Copper smelting and refin- ing, and the making of auto- mobiles, linseed oil, candles, and wax, form other large industries. In Buffalo are and iron ore from the Lake Superior region. Several thousand men are employed 111 this industry. Between Buffalo and Niagara Falls are the cities of Tonawanda and North Tonawanda. The latter is an important lum- ber market. Niagara Falls has become an important center, not only because of the attraction of the great falls and the fact that several trunk lines of railway cross the river at this point, but because of the electrical power developed here. It the University of Buffalo, a state normal has become a great center for the manufac- school, and other educational institutions, ture of chemicals, prepared foods, wood pulp, paper, and abrasive materials. Near Niagara Falls is Niagara University. F,ast of Buffalo are the villages of Depew and Lancaster, with shops and factories. On the narrow lake plain southwest ot Buffalo, in Chautauqua County, are Fredonia and Dunkirk. In the former is one of the state normal schools and in the latter there are railroad shops and locomotive works. Cities and Villages of the Plateau. — In the western part of the plateau is Jamestown, a citv on the outlet of Chautauqua Fake. It has manufactures of worsteds and of wooden GEOGRAPHY OF NEW YORK and metal furniture. On the shores of the lake are the Chautauqua Assembly grounds, the headquarters of a widely known move- ment for popular education. Salamanca is a railroad center, with car shops and manufac- tures of lumber. Olean is in the oil region, and its leading industry is the refining of petroleum. Perry has manufactures of knit goods, and Wellsville is the principal village of Allegany County. Homell has large car shops, and Coming has railroad shops and glass factories. Elmira is a large city and important railway center on the Chemung River. Am.ong its leading industries are the making of fire engines and of automobile parts. This city is the seat of Elmira College and also the State Reformatory. East of Elmira are Waverly and Owego, with shops and factories. The largest city in the plateau is Binghamton, situated at the junction of the Susquehanna and Chenango rivers. It has ample railroad facilities, and a large retail and wholesale trade. Binghamton has large manufactures of tobacco. Near the city, on the Susquehanna River, are Johnson City and Endi- cott. At both these places are large shoe factories. Ithaca is magnificently situated at the head of Cayuga Lake, and is the seat of Cornell University Cortland has manufactures of iron and steel, including wire and rolling mill products, and is the seat of a state normal school. Norwich is a trading center for a large dairying region between Utica and Bing- hamton. Oneonta has large rail- road shops and is the seat of a state normal school. Port Jervis on the Delaware River, is in the Appalachian valley southeast of the plateau. It has several kinds of manufactures. Cities and Villages of Northern New York. — Watertown is the largest city in the northern part of the state. Important water power is here supplied by the Black River, and foundry and machine shop work and pulp and paper making are the leading industries. Ogdensburg, in St. Lawrence County, is next to Watertown in population. Its chiel interests are in grain, lumber, and manufac- tures of lumber. Gouverneur, Potsdam, and Massena are important villages in St. Lawrence County. Potsdam is the seat of a state normal school. Massena has water power, and here are located the largest alu- minum works in the LInited States. H^ n '^f^^ \:^\ ^ 1 Rolling cigars, Binghamton (;E0GRAP1I^■ OF NEW YORK Lowville is rhc county seat and leaclinj; \ illage of Lewis County, and Malone is the county seat and chief center of business in Franklin County. Plattsburg is on Lake Cliainphiin. It is the seat of a state normal school, and has lumber interests. A little south of this cit}' is the meeting place of the Catholic Summer School of .America. Whitehall is at the head of Lake Champlain, and is the northern terminus of the Champlain branch of the Barge Canal. The largest village m the midst of the Adirondacks is Saranac Lake, a health resort. Review. — I. What advantage of location ha.s iyracuse What are the leachns; industrit-.s of Syracuse .'' 3. What three cities are each on or near the foot of one of the Finger Lakes ? 4. What transportation facilities has Oswego ? 5. Where is the- State Agricultural Experi- ment Station .? 6. What are the chief industries of Rochester .'' 7. What cities are in Niagara County ? 8. What rank among .American cities has Buffalo in population ? In manu- factures ? 9. What condi- tions promote the commerce of Buffalo .' ID. What are the leading interests of Niagara Falls ? Of North Tonavvanda ? Of Lockport .' II. What are the industries of Jamestown .^ Of Olean .'' Of Corning.'' 12. State the location of Elmira ; of Binghamton. 13. What university is at Ithaca? 14. Locate Cortland; Norwich; Oneonta. 15. What are the leading industries of Watertown ? Of Ogdensburg ? Government. — The chief executive of the consists of two houses,- the Senate, with 51 members elected for two years, and the As- sembly, with 1 50 members elected for one year. There are depart- ments of Public Works. Hanking, Insurance, Fac- tory Inspection, and E.x- cisc. Iwo Public Service Commissions, one for Cireater New York, the other for the rest of the state, have supervision of railways and of such utili- ties as the telegraph and telephone service. Vari- ous commissions care foi public reservations in the Adirondacks, at Saratoga Springs, Niagara Falls, and elsewhere. The Court of Appeals is the highest state court. Below it are man}- divisions and parts of the Supreme Court, with more than lOC judges. Lower courts are provided for coun- ties, cities, and towns. The state is divided into 62 counties. Each countv, except those in Greater New state is the Governor, who holds office for York, is divided into towns, or townships, two years. Other state officers are: the Many of the cities, however, do not form Lieutenant Governor, the Secretary of State, part of any town. Each county, town, city, the Attorney-General, and the State Engi- and village has a government of its own, neer. The legislature, or lawmaking body, with powers fixed by the state government. GEOGRAPHY OF NEW YORK The chief officers of the county are the )udge, the district attorney, the county clerk, the sheriflF, and the coroners. Each county has a capital called the county seat. Here are the county court, the sheriff's office, and the jail, and the office of the county clerk. The chief officer of each town is a supervisor ; and the town supervisors, with others chosen by cities, make up the Board of Supervisors which is the legislative body of the county. The chief officers of a city are the mayor and the council or board of aldermen. Each voter must have been a citizen of the United States for ninety days, and must have resided one year in the state, four months in the county, and 30 days in the election district. Charities and Penal Institutions. — Twelve commissioners constitute the State Board of Charities. They are appointed by the Gover- nor, with the confirmation of the Senate, and hold office for eight years. A large number of charitable and reformatory institutions are supported partly or wholly by the state and its various subdivisions. The Board of Chari- ties has oversight of these institutions and carries on regular visitations. Among the kinds of people thus cared for are juvenile delinquents, the feeble-minded, orphans, the blind, the deaf and dumb, crippled and de- formed children, and the aged. Among the institutions under the care of this board are industrial schools, soldiers' and sailors' homes, county almshouses, and hospitals for tu- berculosis patients. Several state prisons and re- formatories receive convicts whose sentence is for a period of more than one year. Various peniten- tiaries in the state receive those convicted of minor offenses and sentenced for short periods. Hos- pitals for the insane are in the care of the Board of Lunacy. Education. — The educational work of the state is in the charge of the University of the State of New York. This is not a university in the sense of being a localized school. Its powers are committed to twelve persons called Regents who meet in Albany. They are elected by the legislature. Their presiding officer is styled the Chancellor of the University, and they appoint the Commissioner of Educa- tion, who has under his special charge the rural schools, the elementary and high schools of the villages and cities, and the state normal schools. The state is divided into a large number of districts, in each of which an officer called the district superintendent is responsible for the rural schools. In the larger villages and cities, a superintendent of schools is the chief execu- tive officer. Education is compulsory for all children between the ages of eight and sixteen The State College for Teachers is at Albany, and there are also state normal schools located at Brockport, Buffalo, Cortland, Fredonia. Geneseo, New Paltz, Oneonta, Oswego, Plattsburg, and Potsdam. Some of the large cities maintain similar institutions; thus in Greater New York are Hunter College, and the New York, Brooklyn, and Jamaica Train- ing Schools for Teachers. The higher schools are the universities, colleges, and technical schools. Many of GE(X^RAPII^' Ol \K\V >()RK J] > Uiiii ^iiv « College * Technical schoo • NoriiMl scliool The higher educational institutions of New York these have grown up under the patronage ot rehgious denominations, but are now classed as non-sectarian because no rehgious con- ditions are enforced and faculty and students are representative of many chuichcs. ( )n rhi other hand, there are many institutions under Cathohc control, including Fordham University in the city of New York, Niagara Univer- sity near Niagara Falls, and colleges at New Rochelle, in New York (Mt. St. Vin- cent, Manhattan, Brooklyn, St. Francis, and St. John's), in Buffalo (Canisius and D'Youville), and at Allegany in Cattaraugus County (St. Bonaventure's). The oldest of the higher educational institutions of the state is Columbia Uni- versity, in the city of New York, founded in 1754. It has the largest enrollment of all American universities. Af- filiated with Columbia are Barnard College for women, and Teachers College. Other large universities, each with thousands of students, are New York University in the city of New York ; Cornell University at Ithaca, on a splendid site overlooking Cayuga Lake; ami Svracuse I nixersiry 111 S\racuse. Smaller universities are those of Buffalo, of Rochester, of .'\lfred in Allegany Countv, Colgate Unisersity at Hamilton in Madison County, St. Lawrence University- at Canton in St. Lawrence County, and I nion Univer- sity, including I nion College at Schenectady, and professional colleges at Albany. The New York State College of Agriculture is at Cornell University, and the State College of Forestry is at Syracuse University. Besides the many other schools and colleges which belong to the universities, there are some in- dependent colleges, as Adelphi in Brooklyn, Hamilton at Clinton in Oneida County, and Hobart at Geneva ; and some independent technical schools, as Pratt Institute and the Polytechnic Institute in Brooklyn, the Mili- tary Academy at West Point, the Rensselaer Polytechnic Institute at Iroy, the Clark- son Memorial School of Tech- nology at Potsdam, and the Mechanics' Institute at Roch- ester. The College of the City of New York, in Man- hattan borough, is a large college supported by the city. Colleges for women include Klmira College at Elmira, Wells College at Aurora on Cayuga Lake, and Vassar College — one of the oldest and most widely known in the country — at Pough- keepsie. Review. — I. What are tht priiuipal state officers ? 2. What is the duty of the Public Service Commissions? 3. How many counties in New York ? 4. What institutions are found in each county seat ? 5. What are the conditions which qualify voters in this state.'' 6. What are the (luries of the State Board of Charities ? 7. What is the University of the State of New 'V'ork ? S. What normal school is nearest your home.'' 9. Locate four colleges for women; two large universities; two technical schools. COUNTIES OF NEW YORK — AREA AND POPULATION, 1920 Sq. Albany . . . Allegany. - Bronx .... Broome. . . Cattaraugus Cayuga. . . Chautauqua Chemung . Chenango. Clinton. . . Columbia . Cortland. . Delaware . Dutchess. . Erie Essex Miles 527 1,047 42 705 1.343 703 1,069 407 894 1,049 644 503 1,449 806 1,034 1,836 POPULMION- 186,106 36,842 732,016 113,610 71.323 65,221 115,348 65,872 34,969 43,898 38,930 29,625 42,774 91.747 634,588 31,871 Sq. Miles Franklin.. 1,678 Fulton. . . . 516 Genesee . . 496 Greene . . . 643 Hamilton . 1,700 Herkimer . 1,459 Jefterson. . 1,274 Kings .... 70 Lewis .... 1,270 Livingston 631 Madison. . 650 Monroe. . . 663 Montgomery 398 Nassau . . . 274 New York 21 Niagara . . 522 43.541 44.927 37.976 25.796 3.970 64,962 82,250 2,022,262 23,704 36,830 39,535 352,034 57.928 125.727 2,284,103 118,705 Oneida Onondaga Ontario. Orange Orleans. Oswego , Otsego . Putnam Queens Rensselaer Richmond Rockland . 183 St. Lawrence 2,701 Saratoga. . 823 Schenectady 206 Schoharie 642 Sq. Miles Population I 1,250 649 834 396 966 1,009 233 105 663 182,485 241.465 52,652 119,844 28,619 71.045 46,200 10,802 466,811 113,129 115.959 45.548 88,121 60,029 109,363 21,303 Schuyler . Seneca. . . . Steuben. . . Suffolk... Sullivan . . Tioga... . . Tompkins. Ulster. . . . Warren, . . Washington Wayne . . . Westchester Wyoming Yates 336 336 1,401 924 1,002 520 476 1,140 879 837 599 44S 601 343 Population 13,098 24.735 80,627 110,241 33.163 24,212 35.285 74.979 31.673 44,888 48,827 344,086 30,077 16,641 Total... 47,654 10,384,829 CITIES OF NEW YORK— POPULATION, 1920 .Mbany .Amsterdam . . .'\uburn Batavia Beacon Binghamton Buffalo. .. . . Canandaigua. Cohoes Corning Cortland Dunkirk. . Elmira. . , . . Fulton Geneva 113.344 33.524 36,192 13.541 10,996 66,Soo 506,775 7.356 22,987 15,820 13.294 19,336 45.393 13.043 14.648 Glen Cove Glens Falls Ghtversville. . . , Hornell Hudson Ithaca Jamestown. . . . Johnstown Kingston Lackawanna. . . Little Falls Lockport Mechanicville. . Middletown . . . Mount Vernon. 8,664 16,638 22,075 15.025 11.745 17.004 38,917 10,908 26,688 17.918 13,029 21,308 8,i66 18,420 42.726 Newburgh .... New Rochelle. New York 5 Niagara Falls. . . . North Tonawanda Norwich Ogdensburg Olean Oneida Oneonta Oswego Plattsburg Port Jervis Poughkeepsie. . . . Rensselaer 30,366 36,213 ,620,048 50,760 15,482 8,268 14,609 20,506 10,541 11,582 23,626 10,909 10,171 35,000 10,82? Rochester Rome Saratoga Springs Salamanca Schenectady. . . . Sherrill Syracuse Tonawanda Troy Utica Watertown Watervliet White Plains... Yonkers 295.750 26,341 13.181 9,276 88,723 1,761 171,717 10,068 72,013 94,156 31.285 16,073 21,031 100,176 VILLAGES OF 2500 OR MORE — POPULATION, 1920 Village Albion Amityville .... Avon Babylon Baldwinsville . Ballston Spa. . . Bath Brockport Bronxville . . . Canastota Canton Carthage Catskill Cedarhurst . . . . Clyde Cooperstown , . . Chatham Corinth Dansville Depew Dobbs Ferry. . . Dolgeville East .'\urora. . . East Rochester. East Syracuse . EUenville Elmira Heights Endicott Fairport Falconer Fort Edward . . Fort Plain Frankfort Fredonia Freeport Goshen Gouverneur. . . . County Orleans Suffolk Livingston Suffolk Onondaga Saratoga Steuben Monroe Westchester Madison St. Lawrence Jefferson Greene Nassau Wayne Otsego Columbia Saratoga Livingston Erie Westchester Population 4,683 3,265 2,585 2,523 3,685 4,103 4.795 2,930 3.055 3.995 2,631 4.320 4.728 2,838 2,528 2,725 2,710 2,576 4,681 5,850 4,401 Fulton & Herk. 3,448 Erie Monroe Onondaga Ulster Chemung Broome Monroe Chautauqua Washington Montgomery Herkimer Chautauqua Nassau Orange St. Lawrence 3.703 3,901 4,106 3.116 4,188 9,500 4,626 2,742 3.871 2,747 4,198 6,051 8,599 2,843 4.143 Gowanda Granville Green Island. . . Greenport Hamburg Hastings-on- Hudson Haverstraw. . . . Hempstead ... Herkimer Highland Falls. Hoosick Falls. . Hudson Falls. . Ilion Irvington Johnson City. . Kenmore Lancaster La Salle Lawrence LeRoy Lowville Lynbrook Lyons Malone Mamaroneck . . Massena Medina Mineola Mohawk Mt. Kisco Mt. Morris. . . . Newark North Tarrytown Nyack Ossining Owego County Cat. & Erie Washington Albany Suffolk Erie Population 2,673 3.024 4.411 3,122 3.185 W^estchester Rockland Nassau Herkimer Orange Rensselaer Washington Herkimer Westchester Broome Erie Erie Niagara Nassau Genesee Lewis Nassau Wayne Franklin Westchester St. Lawrence Orleans Nassau Herkimer Westchester Livingston Wayne Westchester Rockland Westchester Tioga 5.526 5.226 6,382 io,4S3 2,588 4,896 5.761 10,169 2,701 8,587 3,160 6,059 3,813 2,861 4,203 3,127 4.367 4.253 7.556 6,276 5,993 6,011 3,016 2,919 3,901 3.312 6,964 5.927 4.444 10,739 4.147 Village Patchogue Peekskill Penn Yan Perry Pleasantville . Port Chester Potsdam Rockville Center Rye Sag Harbor. Saranac Lake. Saugerties Scarsdale Scotia Seneca Falls . . . Sidney Silver Creek. . . Solvay Southampton . . Spring Valley. . Suffern Tarrytown .... Tuckahoe Tupper Lake . . Union Walden Walton Wappingers Falls Warsaw Waterford Waterloo Watkins Waverly Wellsville Westfield Whitehall Whitesboro. . . County Population Suffolk 4,031 Westchester 15,868 Yates 5,215 Wyoming 4,717 Westchester 3,590 Westchester 16,573 St. Lawrence 4,039 Nassau 6,262 Westchester 5,308 Suffolk 2,993 Essex & Frank. 5,174 Ulster 4.013 Westchester 3,506 Schenectady 4,358 Seneca 6,389 Delaware 2,670 Chautauqua 3,260 Onondaga 7.352 Suffolk 2,635 Rockland 4,428 Rockland 3,154 Westchester 5,807 Westchester 3,509 Franklin 2,508 Broome 3,303 Orange 5,493 Delaware 3,598 Dutchess 3,235 Wyoming 3,622 Saratoga 2,637 Seneca 3,8o9' Schuyler 2,785 Tioga 5.270 Allegany 5,046 Chautauqua 3,413 Washington 5,258 Oneida 3,038 t^^^v u^ i 'i»^\ ^% w^ /% w /% w •^^0^ .•^°* -^•^^ o^^^r. 0" .'y^V. 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