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VERMONT , a See also:North See also:Atlantic See also:state of the See also:United States of See also:America, and one of the New ,See also:England See also:group, lying between See also:latitude 42° 44 and 45° 0' 43" N., and between longitudes 3° 35' and 5° 29' E. from See also:Washington . It is bounded N. by the See also:Canadian See also:province of See also:Quebec, E. by the See also:Connecticut See also:river, which separates it from New See also:Hampshire, S. by See also:Massachusetts, and W. by New See also:York and See also:Lake See also:Champlain, which separates it in See also:part from New York . Its See also:total See also:area is 9564 sq. m., and of this 440 sq. m. is See also:water See also:surface . Surface.—Vermont is a portion of the See also:plateau-like New England upland, broken by See also:mountain ranges, individual mountains and high hills, rising above the See also:general upland surface, and by deep narro,v valleys, cut below that surface . The mean See also:elevation of the ssvir . 33state above the See also:sea is about moo ft . Extremes range from Io6 ft. at Maquam on the N.E. See also:shore of Lake Champlain (96 ft.) to 4364 ft. at the See also:summit of See also:Mount See also:Mansfield, about 25 M . E. of that lake . The most prominent feature of the surface is the See also:Green Mountains, which extend nearly N. and S. through the state a little W. of the See also:middle . From the Massachusetts border N. for two-thirds the length of the state the range is only slightly broken, but farther N. it is cut deep by the valleys of the Winooski and Lamoille See also:rivers . The See also:crest See also:line is generally more than 2000 ft. high, considerable areas are above 2500 ft., and the following summits exceed 4000 ft.: Mount Mansfield, 4364 ft.; Killington See also:Peak, 4241 ft.; See also:Camel's Hump, 4088 ft.; Mount See also:Lincoln, 4078 ft.; and See also:Jay Peak, 4018 ft . See also:West of the Green Mountains the Taconic Mountains See also:form a nearly parallel (but distinct) range, extending from New York and Massachusetts N. nearly to the centre of Vermont; and a See also:series of broken uplifts, known as the Red Sandrock Mountains, extend farther N. along the shore of Lake Champlain .
The Taconic Mountains rise in very irregular masses to 1500-2000 ft., and reach their maximum elevation in Mount See also:Equinox at 3816 ft
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The Red Sandrock Mountains are similar to one another in form and structure, generally rounded on the N. and E., but with some rugged escarpments facing the lake; their highest point is Snake Mountain (1271 ft.) in See also:Addison See also:county
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There are no mountain ranges in the state E. of the Green Mountains, but distributed along the entire E. border are a number of tall and See also:oval or conical shaped masses known as the Granitic Mountains, and between these and the Green Mountains the See also:country is largely occupied by high hills and deeply carved valleys
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Mount Ascutney, one of the Granitic Mountains, rises abruptly from the See also:floor of the Connecticut Valley to a height of 3320 ft
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The least broken See also:section of Vermont is on the somewhat See also:gentle slope of the Green Mountains in the N.W. and on See also:Grand Isle, North See also:Hero See also:Island, and Isle La Motte in Lake Champlain
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The forms of Vermont's mountains, even to the highest summits, were to a See also:great extent rounded by glaciation, but as the rocks vary much in texture and are often steeply inclined, stream erosion has cut valleys deep and narrow, often See also:mere See also:gorges
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Where the Green Mountain range is unbroken, in the S. two-thirds of the state, it forms a water-parting between the streams which flow W. or N.W. into Lake Champlain or the See also:Hudson river and those flowing S.E. into the Connecticut river; but farther N. the line separating the Hudson-Champlain See also:basin - from the Connecticut basin runs among the Granitic Mountains; and extending 25 m
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S. from the Canadian border is a small area that is drained N. into Lake Memphremagog, the See also:waters of which, like those of Lake Champlain, are tributary to the St See also:Lawrence river
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North of Massachusetts the Connecticut river is wholly within New Hampshire—Vermont's eastern boundary is See also:low-water See also:mark on the W. See also:bank of the Connecticut river
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The largest and only navigable rivers of Vermont are among those flowing into Lake Champlain: the Missisquoi, the Lamoille, the Winooski and See also:Otter See also:Creek
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The See also:Batten Kill is the See also:principal river flowing into the Hudson
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The See also:Deerfield, West, See also:Williams, See also:
The See also:Black, See also:Barton and See also:Clyde rivers flow into Lake Memphremagog
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Vermont's rivers are generally See also:swift, and in many places they are made very picturesque by their clear and sparkling waters, rapids, falls, gorges and wooded See also:banks
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Lake Champlain, which lies beautifully in the valley between the Green and Adirondack mountains, belongs mostly to Vermont
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The state has a shore line upon it of 15o m. or more, and in its N. portion are numerous islands which are attractive resorts during the summer See also:season
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On the N. border of the state is Lake Memphremagog with islands, a rugged prominence known as See also:Owl's See also:Head on its W. border, Jay Peak, farther back, and a beautiful farming country to the eastward
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There are also a large number of small lakes and ponds lying wholly within the state
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Of these Lake Bomoseen in See also:Rutland county and See also:Willoughby Lake in See also:
Prominent among a great variety of See also:song-birds and insectivorous birds are the See also:robin, See also:blue See also:bird, See also:cat bird, sparrows, meadow-See also:lark, bobolink, thrushes, chickadee, wrens, See also:
The state's See also:lumber See also:trade was important until 189o, when the white pine was nearly exhausted, although there were still spruce and hemlock
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See also:Climate.—The state usually has long and severe winters and cool summers, but sudden changes of temperature are common at all seasons
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The mean temperature for See also:January, the coldest See also:month, is only 17° F.; for the three See also:winter months it is 19° F., and for the five months from See also:November to See also: The best soils are in the west section, where See also:limestone See also:clays or See also:shell marls are common . Forests.--Vermont was heavily forested with white pine, spruce and hemlock, and, in the southern part of the state and along the shore of Lake Champlain, with some hard See also:woods . The white pine had been much cut off by 1890 and it is no longer commercially important . The woodland area of the state in 1900 was estimated to be 3900 sq. m., about 43 % of the land area of the state . See also:Fisheries.—Lake Champlain furnishes the only commerical fishing grounds in Vermont, with the exceptions of small catches of white fish in Lake Bomoseen, Lake St See also:Catherine in Rutland county and Lake Memphremagog . The total catch in 1895 was 208,139 lb, valued at $716o, and in 1902 was 528,682 lb, valued at $37,669 . The See also:capital invested in fisheries in 1902 was $9417, and the number of men employed, 145 . The most valuable fish taken was See also:wall-eyed pike, and the catch of this fish and of pickerel from Lake Champlain in 1902 exceeded in value that from any other See also:body of fresh water in the United States excepting Lake See also:Huron and Lake See also:Erie . The wall-eyed pike taken in 1902 were valued at $16,915 (210,936 lb) ; white fish, $5777 (80,191 lb) ; pickerel, $4144 (51,711 lb) ; yellow perch, $2575 (43,917 lb) ; sturgeon, $2051 (15,590 ib), and suckers, $1854 (37,375 lb) ; other varieties taken in smaller quantities included See also:smelt, See also:sun-fish and eels . See also:Agriculture.—Vermont is largely an agricultural state: in 1900, out of a total of 134,933 perscns engaged in gainful occupations, 49,82o were engaged in agriculture, 36,18o in manufacturing and See also:mechanical pursuits, 23,028 in domestic and See also:personal service, 18,889 in trade and transportation, and 7016 in professional service; and of a total land area of 9124 sq. m., 7382 sq. m . (4,724,400 acres) were included in farms . The percentage of improved farm land; as in See also:Maine, New York and See also:Pennsylvania, increased from 1850 until 1890 and decreased after 189o; and in 1900 out of a total acreage of 4,724,400 acres only 2,126,624 acres (45%) were improved .
Of the 33,104 farms in the state in 1900, 25,982 were farmed by their owners, 1373 by part owners, 314 by owners and tenants, 2424 by See also:cash tenants, '396 by See also:share tenants, and 615 by managers; 637 farms had mor. than 500 acres, 3431 were between 26o and 500 acres, 5512 between 175 and 26o acres, 10,215 between See also:ion and 175 acres, 6513 between 5o and too acres, 3511between 20 and 50 acres, and 3285 less than 20 acres; and See also:dairy produce was the principal source of income of more than one-See also:half of these (16,700), live stock the principal source of income of 7323 farms, and See also:hay and See also:grain of 2519 farms
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The general sterility of the soil except along rivers and the bases of hills has made intensive cultivation always necessary, and the competition of new and See also:rich western farm lands has made the agriculture of Vermont develop further toward specialization in dairying and raising live stock
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In 1910 there were 495,000 neat See also:cattle (285,000 milch cows), 94,000 horses (average value, $106), 229,000 See also:sheep and 95,000 See also:swine
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The horses of Vermont have been famous in the development of See also:American racing See also:stocks; the See also:Morgan stock is best known, and other famous Vermont strains are Messenger and Black See also:Hawk
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Hay and See also:forage are the most important crops, and Vermont See also:grasses for grazing have been favourably known since the See also:close of the 18th See also:century
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In 1909 on 879,000 acres a See also:crop of hay (excluding forage) was raised' valued at $16,155,000
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The cereals are relatively unimportant
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The largest cereal crop is oats, of which, in 1909, 2,608,000 bushels (valued at $1,304,000) were produced on 81,000 acres
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Mines and Quarries.—The principal See also:mineral resource of Vermont is its See also:building and monumental See also: It is found generally throughout the western part of the state . The principal See also:supply is in West Rutland, See also:Proctor and Pittsford; this, the " Rutland marble," is a duller, less lustrous white, and of a greater durability than the See also:Carrara marble, and is used largely for monuments and statuary . There are other large quarries at Dorset and See also:East Dorset, See also:Bennington county; the finest See also:marbles from this region are the white, slightly marked with See also:pale brown and with greenish lines; they are commonly used for building, the Harvard Medical School and the See also:office of the U.S . See also:Senate being examples . At Rutland, Proctor and Dorset many darker shades are found, including " See also:moss vein, " See also:olive green and various shades of blue, green, yellow and See also:pink, which are used for ornamental purposes . There are important quarries in See also:Franklin county (at Swanton), the stone being a dark Chazy limestone, in which pink and red (" See also:jasper," " 1 onnaise " and ` royal red ") marbles of See also:Cambrian See also:age are found . At Monkton, Addison county, there is a See also:quarry from which other red marbles are taken; and at Roxbury, Washington county, a See also:fine See also:serpentine, called " green marble," or verde See also:antique, is quarried . On Isle La Motte, Grand Isle county, there are marble quarries, the characteristic See also:colours of the marble being " See also:Fisk black " and " Fisk See also:grey." The output of marble in 1908 was valued at $4,679,960 (out of a total of $7,733,920 for the entire See also:production of, marble in the United States) . Only less important and only less See also:early to be established in Vermont was the See also:quarrying of granite, which began in 1812, but which has been See also:developed chiefly since 188o, largely by means of the building of " granite railroads " which connect each quarry with a See also:main railway line—a means of transportation as important as the logging See also:rail-ways of the Western states and of See also:Canada . The largest granite quarries are near See also:Barre, Washington county, a See also:city which owes its importance to the quarries . The Barre granites, like those of See also:Woodbury and See also:Calais (also in Washington county) and part of those of South Ryegate, See also:Kirby and See also:Newark (See also:Caledonia county), are of the See also:biotite type ; they are grey, except the stone from Newark, which is pinkish . Of the See also:quartz-See also:monzonite type are the whitish granites of See also:Bethel and See also:Rochester (Windsor county) and See also:Randolph See also:Orange county), the See also:light grey of Dummerston (See also:Windham county), and the darker greys of See also:Cabot (Washington county), See also:Derby (Orleans county), Hardwick and Groton (Caledonia county). and Topsham (Orange county) . The olive green See also:syenite found on Mount Ascutney, near the Connecticut river, in Windsor county, is a hornblendeaugite . Other important granite quarries are near See also:Williamstown, Dummerston, See also:Berlin and Woodbury . The total value of the output of granite in the state in 1908 was $2,451,933 . In 1908 the output of limestone was valued at $20,731 ; there are limestone quarries in Washington and Orange counties and on Isle La Motte . See also:Slate-quarrying and cutting is carried on in the south-western part of the state, in Rutland county; there are important quarries at See also:Fair Haven, Poultney, See also:Castleton, See also:Wells and Pawlet . In Washing-ton county there are quarries near Northfield . The See also:industry began about 184o, though one quarry had been opened as early as 1805 . There are two green varieties, called in the trade " sea-green " and " unfading green, " the former being used for a cheap roofing slate; and there are purplish varieties . In 1908,the value of slate produced was $1,710,491 (out of a total production for the United States of $6,316,817) . Manufactures.—The first important industry of the state was " rafting " lumber from Vermont through Lake Champlain and the See also:Richelieu and St Lawrence rivers to Quebec . Burlington became a great lumber See also:market for a trade moving in the direction of See also:Boston after the Richelieu river was blocked to See also:navigation and railway transportation began, and in 1882 Burlington was the third lumber centre in the United States . Mountain streams furnish important water-See also:power, and the typical factory of Vermont has long been a sawmill run by a water-See also:wheel .
The value of sawmill products in 1905 was $5,888,441, and of planing-See also: |