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    See Article History Alternative Titles: Besides the 48 conterminous states that occupy the middle latitudes of the continent, the United States includes the state of Alaskaat the northwestern extreme of North America, and the island state of Hawaiiin the mid-Pacific Ocean. The conterminous states are bounded on the north by Canadaon the east by the Atlantic Oceanon the south by the Gulf of Mexico and Mexicoand on the west by the Pacific Ocean.

    The United States is the fourth largest country in the world in area after RussiaCanada, and China. The national capital is Washingtonwhich is coextensive with the District of Columbiathe federal capital region created in Fishing boat at the harbour at Portsmouth, New Hampshire. Its physical environment ranges from the Arctic to the subtropical, from the moist rain forest to the arid desert, from the rugged mountain peak to the flat prairie.

    Although the total population of the United States is large by world standards, its overall population density is relatively low. United StatesThe United States. The United States contains a highly diverse population. Unlike a country such as China that largely incorporated indigenous peoples, the United States has a diversity that to a great degree has come from an immense and sustained global immigration. Probably no other country has a wider range of racial, ethnic, and cultural types than does the United States.

    In addition to the presence of surviving Native Americans including American Indians, Aleutsand Eskimos and the descendants of Africans taken as slaves to the New World, the national character has been enriched, tested, and constantly redefined by the tens of millions of immigrants who by and large have come to America hoping for greater social, political, and economic opportunities than they had in the places they left.

    Despite its relative economic self-sufficiency in many areas, the United States is the most important single factor in world trade by virtue of the sheer size of its economy. Its exports and imports represent major proportions of the world total.

    The United States also impinges on the global economy as a source of and as a destination for investment capital. The United States is relatively young by world standards, being less than years old; it achieved its current size only in the midth century.

    America was the first of the European colonies to separate successfully from its motherland, and it was the first nation to be established on the premise that sovereignty rests with its citizens and not with the government. In its first century and a half, the country was mainly preoccupied with its own territorial expansion and economic growth and with social debates that ultimately led to civil war and a healing period that is still not complete.

    In the 20th century the United States emerged as a world power, and since World War II it has been one of the preeminent powers.

    It has not accepted this mantle easily nor always carried it willingly; the principles and ideals of its founders have been tested by the pressures and exigencies of its dominant status. The United States still offers its residents opportunities for unparalleled personal advancement and wealth. However, the depletion of its resources, the contamination of its environment, and the continuing social and economic inequality that perpetuates areas of poverty and blight all threaten the fabric of the country.

    The Editors of Encyclopaedia Britannica Land The two great sets of elements that mold the physical environment of the United States are, first, the geologic, which determines the main patterns of landforms, drainage, and mineral resources and influences soils to a lesser degree, and, second, the atmospheric, which dictates not only climate and weather but also in large part the distribution of soils, plants, and animals.

    Although these elements are not entirely independent of one another, each produces on a map patterns that are so profoundly different that essentially they remain two separate geographies. Since this article covers only the conterminous United States, see also the articles Alaska and Hawaii. To east and west this lowland rises, first gradually and then abruptly, to mountain ranges that divide it from the sea on both sides.

    The two mountain systems differ drastically. The Appalachian Mountains on the east are low, almost unbroken, and in the main set well back from the Atlantic. From New York to the Mexican border stretches the low Coastal Plain, which faces the ocean along a swampy, convoluted coast.

    The gently sloping surface of the plain extends out beneath the sea, where it forms the continental shelfwhich, although submerged beneath shallow ocean water, is geologically identical to the Coastal Plain.

    Southward the plain grows wider, swinging westward in Georgia and Alabama to truncate the Appalachians along their southern extremity and separate the interior lowland from the Gulf. West of the Central Lowland is the mighty Cordillera, part of a global mountain system that rings the Pacific basin.

    The Cordillera encompasses fully one-third of the United States, with an internal variety commensurate with its size. At its eastern margin lie the Rocky Mountains, a high, diverse, and discontinuous chain that stretches all the way from New Mexico to the Canadian border. Pent between the Rockies and the Pacific chain is a vast intermontane complex of basins, plateaus, and isolated ranges so large and remarkable that they merit recognition as a region separate from the Cordillera itself.

    These regions—the Interior Lowlands and their upland fringes, the Appalachian Mountain system, the Atlantic Plain, the Western Cordillera, and the Western Intermontane Region—are so various that they require further division into 24 major subregions, or provinces. The Interior Lowlands and their upland fringes Andrew Jackson is supposed to have remarked that the United States begins at the Allegheniesimplying that only west of the mountains, in the isolation and freedom of the great Interior Lowlands, could people finally escape Old World influences.

    GeographyLearn about the different physcial landscapes that make up the American Midwest.

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    This enormous region rests upon an ancient, much-eroded platform of complex crystalline rocks that have for the most part lain undisturbed by major orogenic mountain-building activity for more thanyears. In the United States most of the crystalline platform is concealed under a deep blanket of sedimentary rocks. In the far north, however, the naked Canadian Shield extends into the United States far enough to form two small but distinctive landform regions: As in the rest of the shield, glaciers have stripped soils away, strewn the surface with boulders and other debris, and obliterated preglacial drainage systems.

    Most attempts at farming in these areas have been abandoned, but the combination of a comparative wilderness in a northern climate, clear lakes, and white-water streams has fostered the development of both regions as year-round outdoor recreation areas.

    Mineral wealth in the Superior Upland is legendary. Iron lies near the surface and close to the deepwater ports of the upper Great Lakes. South of the Adirondack Mountains and the Superior Upland lies the boundary between crystalline and sedimentary rocks; abruptly, everything is different. The core of this sedimentary region—the heartland of the United States—is the great Central Lowland, which stretches for 1, miles 2, kilometres from New York to central Texas and north another 1, miles to the Canadian province of Saskatchewan.

    To some, the landscape may seem dull, for heights of more than 2, feet metres are unusual, and truly rough terrain is almost lacking. Landscapes are varied, however, largely as the result of glaciation that directly or indirectly affected most of the subregion. North of the Missouri — Ohio river line, the advance and readvance of continental ice left an intricate mosaic of boulders, sand, gravel, silt, and clay and a complex pattern of lakes and drainage channels, some abandoned, some still in use.

    The southern part of the Central Lowland is quite different, covered mostly with loess wind-deposited silt that further subdued the already low relief surface. Elsewhere, especially near major rivers, postglacial streams carved the loess into rounded hills, and visitors have aptly compared their billowing shapes to the waves of the sea.

    Above all, the loess produces soil of extraordinary fertility. The Central Lowland resembles a vast saucer, rising gradually to higher lands on all sides.

    Southward and eastward, the land rises gradually to three major plateaus. Beyond the reach of glaciation to the south, the sedimentary rocks have been raised into two broad upwarps, separated from one another by the great valley of the Mississippi River. The Ozark Plateau lies west of the river and occupies most of southern Missouri and northern Arkansas ; on the east the Interior Low Plateaus dominate central Kentucky and Tennessee.

    Except for two nearly circular patches of rich limestone country—the Nashville Basin of Tennessee and the Kentucky Bluegrass region —most of both plateau regions consists of sandstone uplands, intricately dissected by streams.

    Local relief runs to several hundreds of feet in most places, and visitors to the region must travel winding roads along narrow stream valleys. The soils there are poor, and mineral resources are scanty. Eastward from the Central Lowland the Appalachian Plateau —a narrow band of dissected uplands that strongly resembles the Ozark Plateau and Interior Low Plateaus in steep slopes, wretched soils, and endemic poverty—forms a transition between the interior plains and the Appalachian Mountains.

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    Usually, however, the Appalachian Plateau is considered a subregion of the Appalachian Mountains, partly on grounds of location, partly because of geologic structure. Unlike the other plateaus, where rocks are warped upward, the rocks there form an elongated basin, wherein bituminous coal has been preserved from erosion. This Appalachian coallike the Mesabi iron that it complements in U. Extensive, thick, and close to the surface, it has stoked the furnaces of northeastern steel mills for decades and helps explain the huge concentration of heavy industry along the lower Great Lakes.

    The western flanks of the Interior Lowlands are the Great Plainsa territory of awesome bulk that spans the full distance between Canada and Mexico in a swath nearly miles km wide. The Great Plains were built by successive layers of poorly cemented sand, silt, and gravel—debris laid down by parallel east-flowing streams from the Rocky Mountains.

    Seen from the east, the surface of the Great Plains rises inexorably from about 2, feet metres near OmahaNebraskato more than 6, feet 1, metres at CheyenneWyomingbut the climb is so gradual that popular legend holds the Great Plains to be flat. True flatness is rare, although the High Plains of western TexasOklahomaKansasand eastern Colorado come close.

    More commonly, the land is broadly rolling, and parts of the northern plains are sharply dissected into badlands. Epimethius The main mineral wealth of the Interior Lowlands derives from fossil fuels. Coal occurs in structural basins protected from erosion—high-quality bituminous in the Appalachian, Illinoisand western Kentucky basins; and subbituminous and lignite in the eastern and northwestern Great Plains. Petroleum and natural gas have been found in nearly every state between the Appalachians and the Rockies, but the Midcontinent Fields of western Texas and the Texas Panhandle, Oklahoma, and Kansas surpass all others.

    Aside from small deposits of lead and zincmetallic minerals are of little importance. The Appalachian Mountain system The Appalachians dominate the eastern United States and separate the Eastern Seaboard from the interior with a belt of subdued uplands that extends nearly 1, miles 2, km from northeastern Alabama to the Canadian border. They are old, complex mountains, the eroded stumps of much greater ranges. Present topography results from erosion that has carved weak rocks away, leaving a skeleton of resistant rocks behind as highlands.

    Geologic differences are thus faithfully reflected in topography. In the Appalachians these differences are sharply demarcated and neatly arranged, so that all the major subdivisions except New England lie in strips parallel to the Atlantic and to one another. The western side of this belt forms the long slender rampart of the Blue Ridge Mountains, containing the highest elevations in the Appalachians Mount MitchellNorth Carolina6, feet [2, metres] and some of its most handsome mountain scenery.

    On its eastern, or seaward, side the Blue Ridge descends in an abrupt and sometimes spectacular escarpment to the Piedmonta well-drained, rolling land—never quite hills, but never quite a plain. Before the settlement of the Midwest the Piedmont was the most productive agricultural region in the United States, and several Pennsylvania counties still consistently report some of the highest farm yields per acre in the entire country.

    West of the crystalline zone, away from the axis of primary geologic deformation, sedimentary rocks have escaped metamorphism but are compressed into tight folds.

    Erosion has carved the upturned edges of these folded rocks into the remarkable Ridge and Valley country of the western Appalachians. Long linear ridges characteristically stand about 1, feet metres from base to crest and run for tens of miles, paralleled by broad open valleys of comparable length.

    In Pennsylvania, ridges run unbroken for great distances, occasionally turning abruptly in a zigzag pattern; by contrast, the southern ridges are broken by faults and form short, parallel segments that are lined up like magnetized iron filings. By far the largest valley—and one of the most important routes in North America—is the Great Valleyan extraordinary trench of shale and limestone that runs nearly the entire length of the Appalachians. It provides a lowland passage from the middle Hudson valley to HarrisburgPennsylvania, and on southward, where it forms the Shenandoah and Cumberland valleys, and has been one of the main paths through the Appalachians since pioneer times.

    In New England it is floored with slates and marbles and forms the Valley of Vermontone of the few fertile areas in an otherwise mountainous region. Bantosh Topography much like that of the Ridge and Valley is found in the Ouachita Mountains of western Arkansas and eastern Oklahoma, an area generally thought to be a detached continuation of Appalachian geologic structure, the intervening section buried beneath the sediments of the lower Mississippi valley.

    The once-glaciated New England section of the Appalachians is divided from the rest of the chain by an indentation of the Atlantic. Although almost completely underlain by crystalline rocks, New England is laid out in north—south bands, reminiscent of the southern Appalachians.

    The rolling, rocky hills of southeastern New England are not dissimilar to the Piedmont, while, farther northwest, the rugged and lofty White Mountains are a New England analogue to the Blue Ridge. Mount WashingtonNew Hampshire, at 6, feet [1, metres], is the highest peak in the northeastern United States. The westernmost ranges—the TaconicsBerkshiresand Green Mountains —show a strong north—south lineation like the Ridge and Valley.

    Unlike the rest of the Appalachians, however, glaciation has scoured the crystalline rocks much like those of the Canadian Shield, so that New England is best known for its picturesque landscape, not for its fertile soil.

    The Atlantic Plain The eastern and southeastern fringes of the United States are part of the outermost margins of the continental platform, repeatedly invaded by the sea and veneered with layer after layer of young, poorly consolidated sediments. Part of this platform now lies slightly above sea level and forms a nearly flat and often swampy coastal plain, which stretches from Cape CodMassachusettsto beyond the Mexican border.

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