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VERMONT

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Originally appearing in Volume V27, Page 1029 of the 1911 Encyclopedia Britannica.
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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 . 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 . 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 . Mount Ascutney, one of the Granitic Mountains, rises abruptly from the See also:floor of the Connecticut Valley to a height of 3320 ft . 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 . 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 . 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 . 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 . 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 . 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 . The See also:Batten Kill is the See also:principal river flowing into the Hudson . The See also:Deerfield, West, See also:Williams, See also:White, Passumpsic and Nulhegan rivers are the largest of the many streams which are tributary to the Connecticut .

The See also:

Black, See also:Barton and See also:Clyde rivers flow into Lake Memphremagog . 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 . Lake Champlain, which lies beautifully in the valley between the Green and Adirondack mountains, belongs mostly to Vermont . 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 . 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 . There are also a large number of small lakes and ponds lying wholly within the state . Of these Lake Bomoseen in See also:Rutland county and See also:Willoughby Lake in See also:Orleans county are the largest . Willoughby Lake is about 6 m. See also:long by 1–i 2 m. wide, and its situation between two rugged mountains makes a See also:scene of great natural beauty . All the lakes of the state were formed by glaciation . See also:Fauna.—The most See also:common See also:wild animals are See also:deer, rabbits, squirrels, raccoons, skunks, woodchucks and muskrats . There are some porcupines, red foxes, minks and See also:martens, but the See also:moose, See also:wolf and See also:lynx are practically See also:extinct . The ruffed See also:grouse (or " See also:partridge ") is the most common of See also:game birds, but See also:woodcock, ducks and geese are quite common .

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:brown thrasher, See also:gold See also:finch, See also:cedar See also:wax-wing, flycatchers, nuthatches, flicker (See also:golden-winged See also:woodpecker), downy and hairy woodpeckers, See also:rose-breasted See also:grosbeak, See also:Baltimore See also:oriole, See also:barn-See also:swallow, See also:chimney swift, See also:purple See also:martin, purple finch (See also:linnet), vireos and several See also:species of warblers . Birds of- See also:prey comprise several species of See also:hawks and owls, and a few eagles . A few See also:sturgeon are taken in Lake Champlain . The lakes, ponds and streams afford some of the best See also:trout fishing in the country, and many of them also abound in pickerel, See also:pike, See also:perch, black See also:bass and See also:land-locked See also:salmon . "There is a state See also:fish and game See also:commissioner, and the state has a fish II hatchery at See also:Roxbury and a See also:forest and game See also:farm at See also:Sharon . There are Federal hatcheries at Swanton (for pike perch and yellow perch) and at See also:Holden (for trout) . See also:Flora.—Vermont (vent mont), the Green Mountain State, was so named from the See also:evergreen forests of its mountains, whose principal trees are spruce and See also:fir on the upper slopes and white See also:pine and See also:hemlock on the See also:lower . Among See also:deciduous trees the state is noted for its See also:sugar maples; See also:birch and See also:beech are common on the hills, and oaks, See also:elm, See also:hickory, ash, See also:poplar, basswood, See also:willow, See also:chestnut and butternut on the less elevated areas . Among indigenous See also:fruit-bearing trees, shrubs, vines and See also:plants are the See also:plum, See also:cherry, See also:grape, See also:blackberry, See also:raspberry, See also:cranberry and See also:strawberry . A few of the medicinal plants are See also:ginseng, See also:pleurisy See also:root, snake root, See also:blood root, blue See also:flag and marshmallow . See also:Orchids are very prominent among a great variety of flowering plants . Along the shore of Lake Champlain are a few species of maritime plants that remain from the See also:time when portions of western Vermont were covered by the sea, and on the upper slopes of some of the higher mountains are a few Alpine species; these, however, are much less numerous on the Green Mountains of Vermont than on the White Mountains of New Hampshire .

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 . See also:Climate.—The state usually has long and severe winters and cool summers, but sudden changes of temperature are common at all seasons . 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:March inclusive it is 24.3° F . For See also:July, the warmest month, the mean temperature is 68° F.; for the entire See also:year it is 43° F . Extremes of temperature have ranged from -36° F. at See also:Woodstock, See also:Windsor county, in See also:February 1896 to 97° F. at See also:Cornwall, Addison county, in See also:June 1901 . The eastern section of the state is colder than the western, and the central or most mountainous section is still colder; for example, the mean See also:annual temperature of See also:Burlington, on Lake Champlain, is 46° F., while that of See also:Saint Johnsbury, a little farther S. and near the E. border, is only 42 ° F., and that of See also:Northfield, still farther S. but in the middle section, is only 41° F . The mean annual precipitation for the entire state is about 38.5 in.; more See also:rain falls in summer than in any other season, and more falls in the See also:southern section than in the See also:northern . The See also:average annual fall of See also:snow throughout the state is about 90 in., but at See also:Jacksonville near the S. border it often exceeds See also:Ito in . More snow falls in February than in any other month . In the Connecticut and Hudson-Champlain valleys the winds See also:blow mostly from either the N. or the S., but in several of the smaller valleys the prevailing winds are from the N.W . See also:Soil.—The soil is for the most part glacial See also:drift, composed of See also:clay, See also:sand and See also:gravel, and varying greatly in See also:depth . On the higher elevations it is generally stony and sterile, but in the valleys and on many of the lower hills, where it consists largely of clay and sand, it is quite productive .

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 . 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 . 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 . 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 . 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 . In 1909 on 879,000 acres a See also:crop of hay (excluding forage) was raised' valued at $16,155,000 . The cereals are relatively unimportant . 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 . Mines and Quarries.—The principal See also:mineral resource of Vermont is its See also:building and monumental See also:stone, including See also:marble and See also:granite and a small amount of limestone . The value of the total amount of stone produced in 1908 in Vermont was $7,152,624 . Vermont marble is the best and most plentiful in the United States . It has been quarried since 1785; marble monuments were first manufactured about 1808; and at See also:South See also:Dorset in 1818 marble seems first to have been sawed in blocks, the earlier method having been chiselling .

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:

mill products $3,080,117 . Closely connected with the manufacture of lumber is the making of See also:paper and See also:wood pulp, centralized at See also:Bellows Falls, with water-power on the Connecticut river and with the raw materials near; the product was valued in 1905 at $3,831,448 . Dairy See also:industries have rapidly increased in value: in 1905 the value of See also:butter and See also:cheese was $6,416,44, more than any other single industry under the See also:census See also: