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MARYLAND

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Originally appearing in Volume V17, Page 833 of the 1911 Encyclopedia Britannica.
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MARYLAND  , a See also:

South See also:Atlantic See also:state of the See also:United States, and one of the See also:original thirteen, situated between latitudes 370 53' and 390 44 N. and longitudes 75° 4' and 790 33' W . (the precise western boundary has not been determined) . It is bounded N. by See also:Pennsylvania and See also:Delaware; E. by Delaware and the Atlantic Ocean; S. and W. by the See also:Potomac See also:river and its See also:north See also:branch, which See also:separate it, except on the extreme W. border, from See also:Virginia and See also:West Virginia; W., also, by West Virginia . It is one of the small states of the See also:Union—only seven are smaller—its See also:total See also:area being 12,327 sq. m. of which 2386 sq. m. are See also:water See also:surface . See also:Physical Features.—Maryland is crossed from north to south by each of the leading topographical regions of the See also:east See also:section of the united States—the Coastal See also:Plain, the See also:Piedmont See also:Plateau, the Appalachian Mountains, and the Appalachian Plateau—hence its See also:great diversity of surface . The portion within the Coastal Plain embraces nearly the whole of the south-east See also:half of the state and is commonly known as See also:tide-water Maryland . It is marked off from the Piedmont Plateau by a " Fall See also:Line " extending from See also:Washington (D.C.) north-east through See also:Baltimore to a point a little south of the north-east corner of the state, and is divided by the Chesapeake See also:Bay into two parts known as the East See also:Shore and the West Shore . The East Shore is a See also:low level plain, the least elevated section of the state . Along its entire Atlantic border extends the narrow sandy Sinepuxent See also:Beach, which encloses a shallow See also:lagoon or bay also called Sinepuxent at the north, where, except in the extreme north, it is very narrow, and Chincoteague at the south, where its width is in most places from 4 to 5 M . Between this and the Chesapeake to the west and north-west there is a slight See also:general rise, a height of about 10o ft. being reached in the extreme north . A water-parting extending from north-east to south-west and See also:close to the Atlantic border separates the East Shore into two drainage systems, though that next to the Atlantic is insignificant . That on the Chesapeake See also:side is drained chiefly by the Pocomoke, See also:Nanticoke, Choptank and See also:Chester See also:rivers, together with their numerous branches, the general direction of all of which is south-west .

The branches as well as the upper parts of the See also:

main streams flow through broad and shallow valleys; the See also:middle courses of the main streams See also:wind their way through See also:reed-covered marshes, the water ebbing and flowing with the tide; in their See also:lower courses they become estuarine and the water flows between low See also:banks . The West Shore is somewhat more undulating than the East and also more elevated . Its general slope is from north-west to south-east; along the west border are points 300 ft. or more in height . The See also:principal riverscrossing this section are the Patuxent, Patapsco and See also:Gunpowder, with which may be grouped the Potomac, forming the state's See also:southern boundary . These rivers, lined in most instances with terraces 30 to 40 ft. high on one or both sides, flow south-east into the Chesapeake Bay through valleys bounded by low hills . The Fall Line, which forms the boundary between the Coastal Plain and the Piedmont Plateau, is a See also:zone in which a descent of about Too ft. or more is made in many places within a few See also:miles and in consequence is marked by waterfalls, cascades and rapids . The See also:part of Maryland within the Piedmont Plateau extends west from the Fall Line to the See also:base of Catoctin See also:Mountain, or the west border of See also:Frederick See also:county, and has an area of about 2500 sq. m . In general it has a broad See also:rolling surface . It is divided into two sections by an elevated See also:strip known as See also:Parr's See also:Ridge, which extends from north-east to south-west a See also:short distance west of the middle . The east section rises from about 450 ft. along the Fall Line to from 85o to 900 ft. along the See also:summit of Parr's Ridge . Its principal streams are those that See also:cross the West Shore of the Coastal Plain and here wind their way from Parr's Ridge rapidly toward the south-east in narrow steep-sided See also:gorges through broad See also:lime-See also:stone valleys . To the west of Parr's Ridge the surface for the most part slopes gently down to the east See also:bank of the Monocacy river (which flows nearly at a right See also:angle with the streams east of the Ridge), and then from the opposite bank rises rapidly toward the Catoctin Mountain; but just above the mouth of the Monocacy on the east side of the valley is See also:Sugar See also:Loaf Mountain, which makes a steep ascent of 1250 ft .

The portion of the state lying within the Appalachian Region is commonly known as Western Maryland . To the eastward it abounds in mountains and valleys; to the westward it is a rolling plateau . West of Catoctin Mountain (1800 ft.) is See also:

Middletown Valley, with Catoctin See also:Creek See also:running through it from north to south, and the See also:Blue Ridge Mountains (2400 ft.), near the Pennsylvania border, forming its west slope . Farther west the serrated crests of the Blue Ridge overlook the Greater Appalachian Valley, here 73 M. in width, the broad gently-rolling slopes of the Great Cumber-See also:land or See also:Hagerstown Valley occupying its eastern and the Appalachian Ridges its western portion . Through the eastern portion See also:Antietam Creek to the east and Conococheague Creek to the west flow rapidly in meandering trenches that in places exceed 75 ft. in See also:depth . The Appalachian Ridges of the western portion begin with North Mountain on the east and end with See also:Wills Mountain on the west . They are See also:long, narrow, uniformly-sloping and level-crested mountains, extending along parallel lines from north-east to south-west, and reaching a maximum height in See also:Martin's Ridge of more than 2000 ft . Overlooking them from the west are the higher ranges of the Alleghenies, among which the See also:Savage, Backbone and See also:Negro Mountains reach elevations of 3000 ft. or more . In the extreme west part of the state these mountains See also:merge, as it were, into a rolling plateau, the Appalachian Plateau, having an See also:average See also:elevation of 2500 ft . All rivers of Western Maryland flow south into the Potomac except in the extreme west, where the See also:waters of theYoughiogheny and its tributaries flow north into the See also:Monongahela . See also:Fauna and See also:Flora . In See also:primitive times See also:deer, ducks, turkeys, See also:fish and oysters were especially numerous, and wolves, squirrels and crows were a source of annoyance to the See also:early settlers .

Deer, See also:

black bears and See also:wild See also:cats (See also:lynx) are still found•in some uncultivated sections . Much more numerous are squirrels, rabbits, ground-hogs " (woodchucks), opossums, skunks, weasels and minks . Many See also:species of ducks are also still found; and the reed-See also:bird (bobolink), " See also:partridge " (elsewhere called See also:quail or " Bob See also:White "), ruffed See also:grouse (elsewhere called partridge), See also:woodcock, See also:snipe, See also:plover and Carolina See also:rail still abound . The waters of the Chesapeake Bay are especially See also:rich in oysters and crabs, and there, also, See also:shad, alewives, " striped " (commonly called " See also:rock ") See also:bass, See also:menhaden, white See also:perch and weak-fish (" See also:sea-See also:trout ") occur in large See also:numbers . Among the more See also:common trees are several species of See also:oak, See also:pine, See also:hickory, gums and See also:maple, and the See also:chestnut, the See also:poplar, the See also:beech, the See also:cypress and the red See also:cedar; the merchantable pine has been cut, but the chestnut and other hard See also:woods of West Maryland are still a product of considerable value . Among wild See also:fruit-trees are the See also:persimmon and See also:Chickasaw See also:plum; See also:grape-vines and a large variety of See also:berry-bushes grow wild and in abundance . See also:Climate.—The climate of Maryland in the south-east is influenced by ocean and bay--perhaps also by the sandy See also:soil—while in the west it is influenced by the mountains . The prevailing winds are See also:westerly; but generally north-west in See also:winter in the west section and south-west in summer in the south section . In the south the normal winter is mild, the normal summer rather hot; in the west the normal winter is See also:cold, the normal summer cool . The normal average See also:annual temperature for the entire state is between 53° and 54° F:, ranging from 48° at Grantsville in the north-west to 53° at See also:Darlington in the north-east, and to 57° at Princess See also:Anne in the south-east . The normal temperature for the state during See also:July (the warmest See also:month) is 75.2° F., and during See also:January (the coldest month) 32.14° F . Although the west section is generally much the cooler in summer, yet both of the greatest extremes' recorded since 1891 were at points not far apart in Western Maryland: 109° F. at Boettcherville and — 26° F. at Sunnyside .

The normal annual precipitation for the state is about 43 in . It is greatest, county producing the second largest quantity of strawberries of about 53 in., on the east slope of Catoctin Mountain, owing to the elevations which obstruct the moisture-bearing winds, and is above the average along the middle of the shores of the Chesapeake . It is least, from 25 to 35 in., in the Greater Appalachian Valley, in the south on the West Shore, and along the Atlantic border . During See also:

spring and summer the precipitation throughout the state is about 2 in. more than during autumn and winter . Soils and See also:Agriculture.—The great variety of soils is one of the more marked features of Maryland . On the East Shore to the north is a marly See also:loam overlying a yellowish-red See also:clay sub-soil, to the south is a soil quite stiff with See also:light coloured clay, while here and there, especially in the middle and south, are considerable areas both of light sandy soils and tidal See also:marsh loains . On the West Shore the soils range from a light sandy loam in the lower levels south from Baltimore to rather heavy barns overlying a yellowish clay on the rolling uplands and on the terraces along the Potomac and Patuxent . See also:Crossing the state along the lower edge of the Fall Line is a See also:belt heavy with clay, but so impervious to water as to be of little value for agricultural purposes . The soils of the Piedmont Plateau east of Parr's Ridge are, like the under-lying rocks, exceptionally variable in See also:composition, texture and See also:colour . For the most part they are considerably heavier with clay than are those of the Coastal Plain, and better adapted to general agricultural purposes . Light loams, however, are found both in the north-east and south-east . A soil of very close texture, the See also:gabbro, is found, most largely in the north-east .

Alluvial barns occupy the narrow river valleys; but the most common soil of the section is that formed from See also:

gneiss with a large per cent. of clay in the subsoil . West of Parr's Ridge in the Piedmont, the principal soils are those the See also:character of which is determined either by decomposed red See also:sandstone or by decomposed See also:limestone . In the east portion of the mountainous region the soil so well adapted to See also:peach culture contains much clay, together with particles of See also:Cambrian sandstone . In Hagerstown Valley are rich red or yellow limestone-clay soils . The See also:Allegheny ridges have only a thin stony soil; but See also:good limestone, sandstone, shale and alluvial soils, occur in the valleys and in some of the plateaus of the extreme west . Of the total land surface of the state 82 % was in 1900 included in farms and 68% of the farmland was improved . There were 46,012 farms, of which 15,833 contained less than 5o acres, 3940 contained 26o acres or more, and 79 contained 1,000 acres or more—the average See also:size being 112.4 acres . In 1890, 69% of the farms were worked by the owners or their managers, in 1900 only 66.4%; but See also:share tenants outnumber See also:cash tenants by almost three to one . Of the total number of farms about seven times as many are operated by white as by negro farmers, though the number of farms operated by white share tenants outnumber those operated by negro share tenants by only about five to one . Of all the inhabitants of the state, at least ten years old, who in 1900 were engaged in gainful occupations, 20.8% were farmers . The leading agricultural pursuits are the growing of See also:Indian See also:corn and See also:wheat and the raising of livestock, yet it is in the See also:production of fruits, vegetables and See also:tobacco, that Maryland ranks highest as an agricultural state, and in no other state except South Carolina is so large a per cent. of the value of the See also:crop expended for fertilizers . In 1907, according to the See also:Year See also:Book of the U.S .

See also:

Department of Agriculture, the Indian corn crop was 22,196,000 bushels, valued at $11,986,000; the wheat crop was 14,763,000 bushels, valued at $14,172,000; the See also:oat crop was 825,000 bushels, valued at $404,000; and the crop of See also:rye was 315,000 bushels, valued at $236,000 . Of the livestock, hogs were the most numerous in 1900, See also:cattle next, See also:sheep third, and horses See also:fourth . The See also:hay and See also:forage crop of 1899 (exclusive of corn-stalks) See also:grew on 374,848 acres . Until after the middle of the 18th See also:century tobacco was the See also:staple crop of Maryland, and the total yield did not reach its maximum until 186o when the crop amounted to 51,000 hhds . ; from this it decreased to 14,000 hhds., or 12,356,838 lb in 1889; in 1899 it See also:rose again to 24,589,480 lb, in 1907 the crop was only 16,962,000 lb, less than that of nine other states . In See also:market-See also:garden products, including small fruits, Maryland ranked in 1899 See also:sixth among the states of the Union, the crop being valued at $4,766,760, an increase of 350'9% over that of 1889 . In the yield both of strawberries and of tomatoes it ranked first; the yield of raspberries and blackberries is also large . In its crop of See also:green-peas Maryland was exceeded (1899) by New See also:York only; in sweet Indian corn it ranked fifth; in kale, second; in See also:spinach, third; in cabbages, ninth . The number of peach-trees, especially in the west part of the state, where the quality is of the best, is rapidly increasing, and in the yield of peaches and nectarines the state ranked thirteenth in 1899; in the yield of See also:pears it ranked fifth; in apples seventeenth . The Indian-corn, wheat and livestock sections of the state, are in the Piedmont Plateau, the Hagerstown Valley and the central portion of the East Shore . See also:Garrett county in the extreme north-west, however, raises the largest number of sheep . Most of the tobacco is grown in the south counties of the West Shore .

The great centre for vegetables and small fruits is in the counties bordering on the north-west shore of the Chesapeake, and in See also:

Howard, Frederick and Washington counties, directly west, Anne See also:Arundel all the counties in the Union in 1899 . Peaches and pears grow in large quantities in See also:Kent and neighbouring counties on the East Shore and in Washington and Frederick counties; apples grow in abundance in all parts of the Piedmont Plateau . The woodland area of the state in 1900 was 4400 sq. m., about 44% (estimated in 1907 to be 3450 sq. m., about 35%) of the total land area, but with the exception of considerable oak and See also:chest-See also:nut, some maple and other hard woods in west Maryland, about all of the merchantable See also:timber has been cut . The See also:lumber See also:industry, nevertheless, has steadily increased in importance, the value of the product in 1860 amounting to only $605,864, that in 1890 to $1,600,472, and that in 1900 to $2,650,082, of which sum $2,495,169 was the value of products under the factory See also:system; in 1905 the value of the factory product was $2,750,339 . See also:Fisheries.—In 1897 the value of the See also:fishery product of Maryland was exceeded only by that of See also:Massachusetts, but by 1901, although it had, increased somewhat during the four years, it was exceeded by the product of New See also:Jersey, of Virginia and of New York . Oysters constitute more than 8o% of the total value, the product in 1901 amounting to 5,685,561 bushels, and being valued at $3,031,518 . The See also:supply on natural beds has been diminishing, but the planting of private beds promises a large increase . Crabs are next in value and are caught chiefly along the East Shore and in Anne Arundel and See also:Calvert counties on the West Shore . Shad, to the number of 3,111,181 and valued at $120,602, were caught during 1901 . In See also:Somerset and See also:Worcester counties clams are a source of considerable value . The terrapin catch decreased in value from $22,333 in 1891. to $1,139 in 1901 . The total value of the fish product of 1901 was $3,767,461 .

The state See also:

laws for the See also:protection of fish and See also:shell-fish were long carelessly enforced because of the fishermen's strong feeling against them, but this sentiment has slowly changed and enforcement has become more vigorous . Minerals and Manufactures.—The See also:coal deposits, which See also:form a part of the well-known See also:Cumberland See also:field, furnish by far the most important See also:mineral product of the state; more than 98% of this, in 1901, was See also:mined in Allegany county from a See also:bed about 20 M. long and 5 m. wide and the See also:remainder in Garrett county, whose deposits, though undeveloped, ar, of great value . The coal is of two varieties: bituminous and semi-bituminous . The bituminous is of excellent quality for the manufacture of See also:coke and See also:gas, but up to 1902 had been mined only in small quantities . Most of the product has been of the semi-bituminous variety and of the best quality in the See also:country for the See also:generation of See also:steam . Nearly all the high grade blacksmithing coal mined in the United States comes from Maryland . The deposits were discovered early in the 19th century (probably first in 1804 near the See also:present See also:Frostburg), but were not exploited until railway transport became available in 1842, and the output was not large until after the close of the See also:Civil See also:War; in 1865 it was 1,025,208 short tons, from which it steadily increased to 5,532,628 short tons in 1907 . From 1722 until the War of See also:Independence the See also:iron-ore product of North and West Maryland was greater than that of any of the other colonies, but since then ores of See also:superior quality have been discovered in other states and the output in Maryland, taken chiefly from the west border of the Coastal Plain in Anne Arundel and See also:Prince See also:George's counties, has become comparatively of little importance—24,367 long tons in 1902 and only 8269 tons in 1905 . See also:Gold, See also:silver and See also:copper ores, have been found in the state, and attempts have been made to mine them, without much success . The Maryland See also:building stone,, of which there is an abundance of good quality, consists chiefly of granites, limestones, See also:slate, See also:marble and sandstones, the greater part of which is quarried in the east section of the Piedmont Plateau especially in See also:Cecil county, though some limestones, including those from which See also:hydraulic See also:cement is manufactured, and some See also:sand-stones are obtained from the western part of the Piedmont Plateau and the east section of the Appalachian region; the value of stone quarried in the state in 1907 was $1,439,355, of which $1,183,753 was the value of See also:granite, $142,825 that of limestone, $98,918 that of marble, and $13,859 that of sandstone . See also:Brick, See also:potter's and See also:tile See also:clays are obtained most largely along the west border of the Coastal Plain, and See also:fire-clay from the coal region of West Maryland; in .1907 the value of clay products was $1,886,362 . Materials for See also:porcelain, including See also:flint, feldspar and See also:kaolin, -abound in the east portion of the Piedmont, the kaolin chiefly in Cecil county, and material for mineral paint in Anne Arundel and Prince George's counties, as well as farther north-west .

Between 185o and 1900, while the See also:

population increased 103.8%, the average number of wage-earners employed in manufacturing establishments increased 2,58'5%, constituting 5.2% of the total population in 185o and 9.1% in 1900 . In 1900 the total value of manufactured goods was $242,552,990, an increase of 41.1% over that of 1890 . Of the total given for 1900, $211,076,143 was the value of products under the factory system; and in 1905 the value of factory products was $243,375,996, being 15.3 % more than in 1900 . The products of greatest value in 1905 were: See also:custom-made men's clothing; fruits and vegetables and oysters, canned and preserved; iron and See also:steel; foundry and See also:machine-See also:shop products, including stoves and furnaces; See also:flour and grist See also:mill products; See also:tin-See also:ware, coppersmithing and See also:sheet iron working; fertilizers; slaughtering and See also:meat-packing; cars and See also:repairs by steam See also:railways; shirts; provided that once in twenty years, beginning with 1887, the wish of the See also:people in regard to calling a See also:convention for altering the constitution shall be ascertained by a See also:poll . Any constitution or constitutional See also:amendment proposed by such constitutional convention comes into effect only if approved by a See also:majority of the votes See also:cast in a popular See also:election . Since 1870 See also:suffrage has been the right of all male citizens (including negroes) twenty-one years of See also:age or over who shall have lived within the state for one year and within the county or the legislative See also:district of the See also:city of Baltimore in which they may offer to See also:vote for six months immediately preceding an election; persons convicted of See also:larceny or other infamous See also:crime and not since pardoned by the See also:governor, as well as lunatics or those who have been convicted of See also:bribery at a previous election are excepted . In 1908 the General See also:Assembly passed a See also:law providing for annual See also:direct See also:primary elections (outside of Baltimore; and making the Baltimore See also:special primary law applicable to state as well as city officials), but, as regards state See also:officers, making only a slight improvement upon previous conditions inasmuch as the county or district is the unit and the vote of county or district merely " instructs " delegates to the party's state nominating convention, See also:representation in which is not strictly in proportion to population, the rural counties having an See also:advantage over Baltimore; no nomination See also:petition is required . In the same year a separate law was passed providing for primary elections for the choice of United States senators; but here also the method is not that of nomination by a See also:plurality throughout the state, but by the vote of counties and legislative districts, so that this measure, like the other primary law, is not sufficiently direct to give Baltimore a vote proportional to its population . The See also:chief executive authority is vested in a governor elected by popular vote for a See also:term of four years . Since becoming a state See also:Mary-land has had no See also:lieutenant-governor except under the constitution of 1864; and the See also:office of governor is to be filled in See also:case of a vacancy by such See also:person as the General Assembly may elect.' Any See also:citizen of Maryland may be elected to the office who is See also:thirty years of age or over, who has been for ten years a citizen of the state, who has lived in the state for five years immediately preceding election, and who is at the See also:time of his election a qualified voter therein . Until 1838 the governor had a rather large appointing See also:power, but since that date most of the more important offices have been filled by popular election . He, however, still appoints, subject to the See also:confirmation of the See also:senate, the secretary of state, the See also:superintendent of public See also:education, the See also:commissioner of the land office, the See also:adjutant-general, justices of the See also: