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MAINE
, a See also:North See also:Atlantic See also:state of the See also:United States of See also:America, the most north-easterly state in the See also:Union, and the largest of the New See also:England See also:group
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It lies between 430 4' and 470 27' 33" N., and between 66° 56' 48" and 71° 6' 41" W
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It is bounded N.W. by the See also:Canadian See also:province of See also:Quebec; N. and E. by the Canadian province of New See also:Brunswick, from which it is separated in See also:part by the natural barriers of the See also:Saint See also: The south slope which contains nearly all the mountains and is generally more hilly, has a mean descent toward the sea of about 7 ft. to the mile, the fall being greater in the W., where the mountains are high at the N. and the See also:shore See also:low at the S., and less to the E., where the water-parting is See also:lower and the shore high and rocky . After the uplift which caused the rivers to cut below the See also:general " uplands," and develop well marked valleys for themselves, came the See also:period of the great See also:continental glaciation . The See also:glacier or See also:ice See also:sheet overran all Maine, irregularly scouring out the See also:bed See also:rock to produce rock basins, damming up many river valleys with glacial deposits and completely disarranging the drainage lines . When the ice melted, the rock basins and the dammed-up valleys filled with water to produce lakes . This is the origin of the numerous lakes of Maine, which give it some of its most beautiful scenery, and help to make it a See also:holiday resort in summer . These lakes are about 1600 in number, are scattered in all parts of the state, are especially numerous at high elevations, and have an aggregate area of more than 2000 sq. m . Few other regions have so many large lakes so variously ' This See also:condition results from the fact that Maine and the adjacent region were worn down nearly to sea-level by stream erosion, except certain peaks and ridges inland; then the region was elevated and numerous river valleys were cut down below the general erosion surface formed before . Thus we have a general " upland surface," above which the mountain remnants See also:tower, and below which the rivers have been entrenched.situated, and with such beauty of aspect and surroundings . They contribute largely to a See also:constant See also:supply of water See also:power for which the course of the rivers of S.W . Maine are exceptionally well adapted', many of them abound in See also:trout, salmon, togue, See also:black See also:bass and pickerel; and near them there is still much See also:game . Moosehead Lake (about 120 sq. m.; 35 M. long and from 2 M. to 10 M. wide), on the boundary between Piscataquis and See also:Somerset counties, is the largest in Maine and the largest inland See also:body of water wholly in New England ; the Kennebec River is its See also:principal outlet and Mt Kineo rises abruptly to about 176o ft. above the sea (about 700 ft. above the lake) on its eastern shore . Other lakes, such as the Rangeley Lakes,2 Chesuncook and Twin Lakes on the See also:Penobscot, and the Grand or Schoodic Lakes, in the western boundary at the See also:head See also:waters of the Saint Croix River, equal or surpass Moosehead in picturesqueness . The glacier or ice sheet, above referred to, de-posited till or See also:boulder See also:clay, which was compacted under the enormous pressure of the ice sheet to See also:form the " hard-See also:pan " referred to later . The glaciation is also responsible for the poor See also:soil of most of the state, for, although the rocks are the same crystallines which give good soils further south in unglaciated regions, all the decayed portions of the Maine rocks have been removed by glacial erosion, revealing fresh, barren rock over great areas, or depositing the rather sterile hard-pan as a thin coating in other places . After the uplift came a period of subsidence, during which this region sank one or more thousand feet, allowing the sea to encroach on the See also:land and run far inland into the previously made river valleys . This depression probably occurred during the glacial period, perhaps toward its See also:close, and is responsible for the second most important feature of Maine physiography, the embayed coast . To this subsidence are due the picturesque coastal scenery, the numerous islands and bays, the good harbours and the See also:peculiar coast-line . The shortest distance between the N.E. and the S.W. extremities of the coast is only 225 M.; but, on See also:account of projections and indentations, the coast-line See also:measures not less than 2500 M . The headlands, the deep indentations and the numerous islands in the bays and beyond produce a beautiful mingling of land and sea and give to the whole ocean front the See also:appearance of a fringed and tasselled border; west of the mouth of the Kennebec River are a marshy shore and many low grassy islands; but See also:east of this river the shore becomes more and more bold, rising in the precipitous cliffs and rounded summits of Mt Desert and Quoddy Head, 1527 and moo ft. high respectively . All along the coast-line there are capacious and well-protected harbours, Casco, Penobscot, Frenchman's, Machias and Passamaquoddy bays being especially noteworthy . After the subsidence came another period of uplift, possibly still in progress . This uplift has brought up submarine deposits of sand, &c., to form little coastal plains at some points along the coast, providing good land for See also:settlement and clay for See also:brick and pottery . Further See also:evidence of this uplift is found in old beach lines now well above sea-level . The principal river systems of Maine are the Saint John on the north slope, and the Penobscot, the Kennebec, the Androscoggin, and the See also:Saco on the south slope . The mean height of the See also:basin of the St John is exceeded only by that of the Androscoggin, but the fall of the St John River through the greater part of its course in Maine is only sufficient to give a sluggish or a See also:gentle current . The Penobscot, Kennebec, Androscoggin and Saco have numerous falls and rapids . See also:Fauna.—The See also:animal See also:life of Maine shows a mixture of See also:northern and See also:southern forms, and very little that is peculiar as compared with surrounding regions . The state has moose, caribou and See also:deer, especially in the northern part . The black See also:bear, See also:wolf, catamount, See also:wolverine, See also:wild See also:cat, See also:fox, See also:beaver, racoon, See also:marten, See also:sable, See also:woodchuck, See also:skunk, See also:otter, See also:mink, See also:rabbit and See also:squirrel are also found . Geese, ducks and other water See also:fowl frequent the lakes and bays in the migratory See also:season, and eagles, gulls, See also:hawks, kingfishers, owls, .See also:plover, See also:woodcock, " See also:partridge " (ruffed See also:grouse), See also:robins, orioles, bobolinks, blue birds, swallows, sparrows, and many other insectivorous birds are See also:common . In the inland waters salmon, trout, togue (Salvelinus namaycush), pickerel and bass abound; along the shore there are lobsters, clams and scallops (See also:Peden irradians) ; and off the shore are See also:herring, alewives, See also:mackerel, See also:cod, See also:halibut, See also:haddock, smelts, See also:hake, See also:menhaden, porgies and porpoises . The game in the North See also:Woods attracts large See also:numbers of sportsmen during the autumn season . See also:Flora.—Maine was formerly covered with forests, principally of white See also:pine and spruce, but mixed with these were some See also:hemlock, tamarack, See also:cedar, and, on the south slope, See also:birch, See also:poplar, See also:oak, See also:maple and See also:beech . See also:Chestnut and See also:walnut are rare and are found only near 2 This name is applied to a See also:chain of lakes (the Rangeley, or Oquossoc, the Cupsuptic, the Mooselookmeguntic, the Molechunkamunk or Upper See also:Richardson, the Welokenebacook or Lower Richardson, and the Umbagog) in Franklin and See also:Oxford counties, in the western part of the state; the Umbagog extends into New Hampshire and its outlet See also:helps to form the Androscoggin River . These lakes are connected by straits, have a See also:total area of between 8o and 90 sq. m., and are from 1200 to 1500 ft. above the sea . They are sometimes called the Androscoggin Lakes . the south-west border . In 1900 about 21 % of the state's area was cleared, and much besides had once been cleared, but not being suited to agriculture had become reforested . Of See also:fruit trees the See also:chief is the See also:apple . The See also:plum, See also:cherry and See also:pear also thrive . The See also:peach grows well only in the south-west near the border . See also:Species of See also:grape, See also:gooseberry and See also:currant are native, and others are cultivated with See also:advantage . The See also:blackberry, See also:raspberry, blueberry and See also:strawberry grow wild in profusion throughout the state . Climate.—The climate of the state is moist and, for its See also:latitude, See also:cold . Extremes of temperature are not so great as farther inland in the same latitude; for the summer heats are tempered by the sea and the cool north winds, and the See also:winter cold is so constant as to be less severely See also:felt than the changing temperature of more southern districts . The summers are See also:short, there being only about 41 months between frosts even in the southern sections, and the mean summer temperature is about 62° F . The mean winter temperature is approximately 2o° F., and the mean See also:annual temperature for the entire state is 42° F., that for the north slope being about 5° F. less than that for the south slope . Although the temperature remains See also:pretty steadily below the freezing point for at least three months of the See also:year, many of the harbours remain unobstructed; for the tides and the prevailing off-shore winds break up and drive off the ice . The precipitation is about 42 in. annually, and is distributed very evenly throughout the year, io–I! in. of See also:rain or its See also:equivalent in See also:snow falling each season . During 41 months about 44% of the precipitation is in the form of snow; but the snow-fall varies from about 60 in. on the coast to more than 100 in. on the north slope . The winds are variable; at no season of the year is it usual for them to See also:blow from the same direction for many days in See also:succession . But, with the exception of those from the west, they are maritime and consequently moisture-bearing . In summer, especially in the latter part of it, the cool and moist N. or N.E. winds often cause a considerable part of the state to be enveloped in See also:fog for several days in succession . Agriculture.—The soil is for the most part glacial See also:drift, containing a large mixture of clay with sand or See also:gravel, and the sub-soil is mostly " hard-pan," i.e. mingled clay and boulders which have been so much compressed by glacial See also:action as to make the mixture hard and ledge-like . Except in the valley of the Aroostook and along the Kennebec, the Penobscot, and some other rivers, the soil is generally unfit for cultivation, there being too little See also:alluvium mixed with it to make it fertile . In the Arroostook valley, however, is the largest undivided area of good arable land in all New England, the soil being a deep, porous, yellow See also:loam well adapted to the growth of cereals and to See also:market gardening . The most sterile regions are on the mountains and along the coast . Because of, the cold climate, the large areas in which there is little or no good arable land, the growing demand for See also:timber land, and the large and constant supply of water-power afforded by the principal rivers, agriculture in Maine, as in all the other New England states except See also:Vermont, is a smaller See also:industry than manufacturing; in 1900 there were 87,932 See also:people engaged in manufacturing and only 76,932 engaged in agriculture . Only 32.9% of the state's land area was in that year included in farms, only 37.9% of this See also:farm land was improved, and only 16.3% of the improved land was in crops other than See also:hay and See also:forage . Nevertheless, as indicated by the unusually large proportion of farmers who either own their farms or pay See also:cash See also:rent for them, farming usually is profitable . The number of farms in 1900 was 59,299; of these 18,644 contained between 50 and See also:loo acres and 17,191 contained between See also:ioo and 175 acres, the See also:average See also:size being Io6.2 acres; 54,263 (or 91.5 %) were operated by their owners, 775 were operated by part owners, 2030 by cash tenants, and only 745 by See also:share tenants . Beginning with the middle of the 19th See also:century, the increasing competition of the more productive soils of the West, the growth of See also:urban population in the state, and the number of summer visitors effected the reforesting of much poor land and the more intensive cultivation of the better arable land . The cultivation of cereals, for example, has given way to a marked extent in nearly all the farming districts except in Aroostook county to market gardening, dairying, and See also:egg and poultry See also:production . The number of See also:dairy cows increased from 157,240 in 1890 to 183,000 in 1908, and the annual production of See also:milk increased from 57,969,791 gallons in 1890 to 99,586,188 gallons in 1900 . The number of other neat See also:cattle (180,878 in 1900; 151,000 in 1908) decreased during every See also:decade from 1860 to 1900; the number of See also:sheep in 1900 was 427,209 (31.9% less than in 1890), and in 1908 it was 267,000; but the number of horses in 1890 and 1900 was about the same (140,310 in 1900, but only 116,000 in 1908) . Hay is still by far the largest See also:crop, the acreage of it and of forage in 1899 being 1,270,254 acres, or 76.5% of that of all crops, and the yield was 1,133,932 tons; in 1907 the acreage was 1,400,000 acres, and the crop was 2,100,000 tons . The acreage of cereals decreased from 187,013 in 188o, when agriculture in Aroostook county was little See also:developed, to 166,896 in 1899, when the cereal acreage in Aroostook county alone was 82,069 . Maine potatoes are of a See also:superior quality, and the acreage of this crop increased from 49,617 in 1889 to 1i8,000 in 1907 . Sweet See also:Indian See also:corn, cabbages, turnips, cucumbers and tomatoes are grown in large quantities . The fruit crop consists very largely of apples and strawberries (1,421,773 bushels of apples and 1,066,86oquarts of strawberries in 1899) . The output of eggs increased from 9,369,534 dozen in 1889 to 13,304,150 dozen in 1899 . The most productive dairy See also:section of the state is a See also:belt extending from the south-west corner N.E. entirely across the state and embracing the whole or parts of the counties of See also:York, Oxford, See also:Cumberland, Androscoggin, Kennebec, Penobscot and Aroostook . See also:Lumber Industry.—Except in the remote parts, the valuable white pine, for which Maine was long noted, has been cut; but the See also:wood-land of the state was estimated in 1900 at 23,700 sq. m. or 79% of its area . The tendency is for this area to increase, for the See also:establishment between 1890 and 1900 of large See also:paper and pulp See also:mills on some of the principal rivers of the south slope greatly increased the value of forests, especially those of spruce and poplar . The state makes large appropriations for preventing and extinguishing See also:forest fires, and in 1903 established a See also:department of forestry in the university of Maine . Good spruce, which is by far the most valuable timber in the state and is used most largely for the manufacture of paper and pulp, stands in large quantities in the St John, Venobscot, Androscoggin and Kennebec basins . Poplar, also used for the manufacture of paper, abounds in several sections of the south slope, but is most abundant in the basin of the Kennebec . White birch, used largely for the manufacture of spools, is found throughout a wide belt extending across the middle of the state . There is much cedar on the north slope . Oak, maple and beech are rather scarce . A new growth of white pine and other timber is gradually becoming valuable . The value of the timber product increased from $11,849,654 in 1890 to $13,489,401 in 1900, and to $17,937,683 in 1905 . See also:Fisheries.—Fishing has always been an important industry in Maine . From 1901 to 1904 inclusive, the average annual catch amounted to 195,335,646 lb, and its average value was $5,557,083• In 1908, according to state reports, the catch was 185,476,343 lti, valued at $3,849,900 .
See also:Herrings are caught in largest quantities (in 1908, according to state reports, 68,210,800 lb, valued at $450,665), and Maine is noted for the See also:canning of the smaller her-rings under the name of " sardines." In 1908, according to state reports, the take of lobsters was 17,635,980 ib, valued at $I,558,252
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Maine markets more clams than any other state in the Union, and the catches of cod, hake, haddock, See also:smelt, mackerel, See also:swordfish, See also:shad, See also:pollock, cusk, salmon, alewives, eels and halibut are of importance
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The scallop See also:fishery is becoming more and more valuable
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For the See also:protection and promotion of the See also:lobster fishery the United States See also:government has established a lobster hatchery at Boothbay Harbor; and the state legislature enacted a See also:law in 1895 prohibiting the taking of lobsters less than See also:io2 in. in length (one effect of this law being to drive the lobster-canning industry from the state) and another law in 1903 for the protection of lobsters with eggs attached
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This latter law directs the state See also:fish See also:commissioner to See also:purchase such lobsters whenever caught and either to liberate them or to sell them to the United States for keeping in a fish hatchery
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Minerals.—The principal See also:mineral products are See also:granite, See also:limestone, See also:slate, clay products and mineral waters
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In 1905 Maine held first See also:rank among the states of the Union as a producer of granite, the value of the output being $2,713,795
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In 1907 Maine's granite was valued at $2,146,420, that of See also:Massachusetts at $2,328,777, and that of Vermont at $2,693,889
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The See also: Black granite was quarried in 1907 at 12 quarries, in York, See also:Lincoln, See also:Waldo, Penobscot and See also:Washington counties . Limestone abounds, especially in the south-east part of the state, but it is quarried chiefly in See also:Knox county . As its See also:colour —blue and blue-black streaked with white=-renders it undesirable for building purposes, nearly all of it is burned into See also:lime, which has become a very important See also:article of manufacture in the city of See also:Rockland; the industry See also:dates back to 1733 in Knox county . In 1907 the quantity of lime burned in Maine was 159,494 tons and its value was $747,947 . Slate is quarried chiefly in Piscataquis county, most of it being used for roofing, but some for blackboards; in 1907 the amount quarried in Maine was valued at $236,106 . About 1896 some remarkably white and pure feldspar began to be quarried in Androscoggin, Oxford and Sagadahoc counties, but afterwards the spar See also:mined in Maine was of less excellent quality; in 1907 the production in Maine was valued at $157,3334, the total for the entire country being $499,069 . Clay is obtaine in various places, and in 1905 the total value of the clay products was $619,294 . In Oxford county See also:tourmaline, See also:spodumene (or See also:kunzite) and See also:beryl occur, the tourmaline crystals being notably large and beautiful . Mineral water occurs in many localities, particularly in Androscoggin, York, Cumberland and Oxford counties; the most famous springs are the Poland Springs in Androscoggin county . Most of the mineral waters bottled in the state are chalybeate and slightly alkaline—saline; their average temperature is about 43° . In 1908 27 springs were reported, their aggregate sales amounting to 1,182,322 gallons . See also:Copper, See also:gold alloyed with See also:platinum, See also:iron ore, See also:barytes, See also:graphite and See also:lead occur in small quantities in the state .
In 1908 the total mineral product of the state was valued at $7,044,678
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Manufactures.—Although Maine has no See also:coal and only a very small amount of iron ore within her See also:borders for the encouragement of manufacturing, yet the abundance of See also:fine timber and the numerous coves, bays and navigable streams along or near the coast promoted See also:ship-building from the first, and this was the leading industry of the state until about the middle of the 19th century, when wooden See also:ships began to be supplanted by those of iron and See also:steel
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Until about the same See also:time, when the Maine liquor law was passed, the manufacture of See also:rum from See also:molasses, received in See also:exchange for lumber and fish in the West Indies, was also an important industry
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It was not until See also:early in the 19th century that the large and constant supply of water power afforded by the rivers began to be used to any considerable extent
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The first See also:cotton See also: It ranked ninth in 1900 and tenth in 1905 in the value of its cotton goods . Portland, See also:Lewiston, See also:Biddeford, and See also:Auburn are the leading manufacturing cities, and in 1905 the total value of their manufactures was 21.5% of those of the entire state . But from 1900 to 1905 the value of manufactures See also:grew most rapidly in Rock-land (especially noted for lime), the increase being from $1,243,881 to $1,822,591 (46.5%), and in See also:Waterville, where the increase was from $2,283,536 to $3,069,309 (34.4%) . Among the largest paper mills are those a |