Great Plains

a semiarid region E of the Rocky Mountains, in the U.S. and Canada.

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Continental slope of central North America.

It stretches from the Rio Grande at the U.S.-Mexico border in the south to the Mackenzie River delta along the Arctic Ocean in the north and from the Interior Lowlands and the Canadian Shield in the east to the Rocky Mountains in the west. The plains embrace parts of 10 U.S. states and 4 Canadian provinces, covering an area of about 1,125,000 sq mi (2,900,000 sq km). A high plateau of semiarid grassland, these prairie regions in both the U.S. and Canada produce the major proportion of wheat grown in each country and are also important cattle-and sheep-herding areas. Parts of the plains have reserves of coal and lignite, petroleum, and natural gas.

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▪ region, North America

Introduction

also called Great American Desert  

 major physiographic province of North America. The Great Plains lie between the Rio Grande in the south and the delta of the Mackenzie River at the Arctic Ocean in the north and between the Interior Lowland and the Canadian Shield on the east and the Rocky Mountains on the west. Their length is some 3,000 miles (4,800 kilometres), their width from 300 to 700 miles, and their area approximately 1,125,000 square miles (2,900,000 square kilometres), roughly equivalent to one-third of the United States. Parts of 10 states of the United States (Montana, North Dakota, South Dakota, Wyoming, Nebraska, Kansas, Colorado, Oklahoma, Texas, and New Mexico) and the three Prairie Provinces of Canada (Manitoba, Saskatchewan, and Alberta) and portions of the Northwest Territories are within the Great Plains proper. Some writers have used the 100th west meridian as the eastern boundary, but a more precise one is the eastward-facing escarpments—the Balcones Escarpment in the far south and the Missouri Escarpment in the north—that run from Texas to North Dakota, generally somewhat east of the 100th meridian. In the Canadian portion the line dividing the Great Plains from the Canadian Shield runs east of the Red River of the North, cuts through Lake Winnipeg, and then curves northwestward, crossing Lake Athabasca, Great Slave Lake, and Great Bear Lake; in the far north, the plains reach the Arctic Ocean in a narrow strip just west of the Mackenzie delta.

Physical features

Relief and drainage

 The Great Plains are a vast high plateau of semiarid grassland. Their altitude at the base of the Rockies in the United States is between 5,000 and 6,000 feet (1,500 and 1,800 metres) above sea level; this decreases to 1,500 feet at their eastern boundary. The altitudes of the Canadian portion are lower, and near the Arctic Ocean the surface is only slightly above sea level. Some sections, such as the Llano Estacado (Staked Plains) in western Texas and eastern New Mexico, are extremely flat; elsewhere, tree-covered mountains—the Black Hills of South Dakota and the Bear Paw, Big Snowy, and Judith mountains of Montana—rise 1,500 to 2,000 feet above the general level of the plains. In general, this landscape is not the flat, featureless plain that most envision it to be; low hills and incised stream valleys are commonplace.

      In the United States the Great Plains are drained by the Missouri River and its tributaries (the Yellowstone, Platte, and Kansas) and the Red, Rio Grande, and Arkansas (Arkansas River) rivers, which flow eastward from the Rockies in broad, steep-sided, shallow valleys. The Red River of the North, which forms the border between North Dakota and Minnesota, drains north into Canada. In Canada the Saskatchewan River and its tributaries constitute the main drainage system.

Soils and climate

      The soil groups of the Great Plains are correlated with rainfall and natural grass cover. In the more humid region with taller, heavier grass cover, deep, black soils (mollisols) with much organic matter developed. Sections with less moisture have lighter, shallower soils with less organic matter, while in the most arid regions the soils are even thinner, lighter in colour, and less organic in composition. Most of the soils have an accumulation of carbonates in their lower horizons, translocated there by infiltrating water. Advancing from east to west across the Great Plains, the climate gets progressively drier and, hence, the depth of carbonates decreases.

      The Great Plains have a continental climate. Over much of their expanse, cold winters and warm summers prevail, with low precipitation and humidity, much wind, and sudden changes in temperature. The major source of moisture is the Gulf of Mexico, and the amount falls off both to the north and west. Thus, the southern plains have 15 to 25 inches (380 to 640 millimetres) of rain annually, the northern plains 12 to 15 inches, the eastern margin in Nebraska 25 inches, and the western margin in Montana less than 15 inches. More rainfall occurs in summer than in winter, except in some of the northwestern parts of the Great Plains. The southern parts of the Canadian Great Plains receive 10 to 20 inches and have a growing season of 70 to 110 days. The growing season averages 240 days in Texas and 120 days at the U.S.-Canadian boundary. A distinctive winter phenomenon of the western Great Plains is the chinook, a warm, dry wind that blows down the eastern slope of the Rocky Mountains and can raise temperatures by as much as 30 to 40 °F (17 to 22 °C) in a short period.

Plant and animal life

      Natural vegetation in the Great Plains is dominated by grasses—tallgrass and medium grass prairie in the east and shortgrass and bunchgrass steppes in the west. These grasslands include forbs and larger plants such as the yucca and the prickly pear cactus in marginal areas, as well as shrubs and some small trees such as the mesquite and the sagebrush. Much of the natural grass cover, however, has been removed to create agricultural land or is heavily overgrazed, allowing for an increase in less-palatable species such as the cactus. Gallery (riparian) forests are found along the rivers and include hardy xerophytic (drought-tolerant) trees such as box elder and cottonwood. Coniferous evergreens (primarily Ponderosa pine) dominate the mountain islands, such as the Black Hills. Between Edmonton, Alta., and Winnipeg, Man., a transition zone trending northwest-southeast and known as the “Parklands” is found, where the grasslands gradually give way to forest; and north of 54° N latitude coniferous forests dominate the vegetation.

 Before European settlement, the Great Plains were the home of immense herds of grazing mammals: the buffalo (bison) and the pronghorn. The buffalo were nearly eliminated, but the pronghorn continued to thrive. Other grassland-adapted animals that thrive together with agriculture include prairie dogs, coyotes, prairie chickens, and rattlesnakes. In the northern coniferous forests are found moose, woodland caribou, Canada lynx, and timber wolves. The region is not without its share of insect pests, such as the locust and the tiny chigger.

The people and economy

      The Great Plains were sparsely populated (human migration) until about 1600. Spanish colonists from Mexico had begun occupying the southern plains in the 16th century and had brought with them horses and cattle. The introduction of the horse subsequently gave rise to a flourishing Plains Indian culture. In the mid-19th century, settlers from the eastern United States began to supplant the Indians, the latter being relegated to marginal agricultural areas set aside as reservations. European immigrants also played an important role in settling the plains; by 1910, foreign-born immigrants and their children constituted nearly half the population of the six northern plains states (Montana, North Dakota, South Dakota, Wyoming, Nebraska, and Kansas), with the British, Germans (many of them from Russia), and Scandinavians the leading ethnic groups. The Prairie Provinces were settled by British, German Russians (many of them Mennonites), Ukrainians, and Scandinavians.

      Many of the immigrants were religious, thrifty, hardworking people who developed a strong attachment to the land. Kinship and nationality ties drew the plainsmen together, and they would travel long distances to visit and exchange work. Class differentiation was less and the status ladder shorter than in Europe or parts of North America that had been settled longer.

      Although there are still few large cities, some three-fifths of the population is urban. The largest cities are Edmonton and Calgary in Alberta and Denver in Colorado; smaller cities include Saskatoon and Regina in Saskatchewan, Amarillo, Lubbock, and Odessa in Texas, and Oklahoma City in Oklahoma. The rural population has remained sparse.

      Ranchers (ranch) traditionally enjoyed their remoteness and looked upon their rangeland as the last remaining trace of the Old West, with its vast expanse of plains and untamed wilderness. Not generally a gregarious kind of people, they were highly individualistic in politics. Farmers, more inclined to social interaction, made economic cooperatives strong on the plains. Since the end of World War II, ranchers and farmers alike have valued horsemanship and rodeos as symbols of a tradition and style of life that evolved from the natural habitat.

      The need for larger farms and ranches to produce viable economic units has led to a heavy migration from the rural areas. This exodus has been demoralizing for the farmers, ranchers, and businessmen who remained, and it has made survival more difficult for churches, schools, and the rural trading centres. The low density of population has concentrated services increasingly in a few centres, necessitating long trips to attend school and church, to do business, and to recreate. To meet these difficulties, some farmers have moved into town to live and commuted back to their land to work, a revival of a centuries-old pattern.

      Indians on horseback exploited the buffalo herds for some two and a half centuries; but in the 1870s cattle replaced the buffalo, and cowboys replaced the Indians. In the 1880s and '90s farmers began to crowd the ranchers, and wheat began to replace cattle. Settlement came in years of good rains, so the Great Plains were overpopulated in the first rush. A heavy emigration followed the twin blows of drought and economic depression in the 1930s. Many grain farmers left because their farms were too small and more vulnerable to drought than the cattle ranches. Those who stayed built up the size of their holdings, saved against hard times, and added livestock to grain farming. These people were aided considerably by the construction after World War II of numerous dams in the Missouri River basin, which provided flood control, hydroelectric power, and irrigation. In addition, an immense source of groundwater, the Ogallala Aquifer, was tapped for irrigation water for an area extending from Nebraska to the Texas Panhandle. Additionally, the region has become a favoured place for cattle feedlots, where range-fed cattle are fattened for market on range-grown corn.

      Thus, the Great Plains have remained basically an agricultural area producing wheat, cotton, corn (maize), sorghum, and hay and raising cattle and sheep. Eight of the leading U.S. wheat states (Kansas, North Dakota, Texas, Montana, Nebraska, Colorado, Oklahoma, and South Dakota) lie within the Great Plains, and the Prairie Provinces are the leading wheat producers in Canada. Of increasing importance are crops of such oilseeds as sunflower and canola. Livestock accounts for a large percentage of farm income in most of the plains states.

 The Great Plains states also produce much mineral wealth, with Texas leading the nation in mineral production and four other plains states (Oklahoma, New Mexico, Wyoming, and Kansas) ranking high. Four of the plains states have the largest coal reserves in the nation (Wyoming, North Dakota, Montana, and Colorado) but, except for Wyoming, rank low in actual production. Texas leads the United States in production of petroleum and natural gas, and several other plains states are substantial producers. Alberta leads Canada in petroleum and natural gas and has huge reserves of tar sands.

Study and exploration

      European knowledge of the Great Plains began with the expedition of the Spanish explorer Francisco Vázquez de Coronado in 1539–41. American interest in the region was sparked by the Louisiana Purchase (1803), which gave rise to the great Lewis and Clark Expedition in 1804–06. Two subsequent expeditions are of note: the first, led by Zebulon Pike (1805–07), explored the Arkansas and Red rivers; and the second, led by Stephen Long (1820), concentrated on the Platte and Arkansas river basins and caused Long to characterize the region as the “Great American Desert.” Fur trappers and then settlers traveling through the region on the Oregon, Mormon, and Santa Fe trails completed the basic knowledge of the plains.

      Study of the Great Plains in the 20th century concentrated on their agricultural and mineral potential, as well as on their natural history. Since World War II more emphasis has been placed on ecological studies of the soils, groundwater, and effects of the use of agricultural chemicals. Research also has been undertaken on the effects of rural depopulation and on the impact the region's natural grass cover—particularly its restoration—may have on global climatic conditions, including the greenhouse effect.

Elwyn B. Robinson John L. Dietz

Additional Reading

The physical environment of the Great Plains is described in Tim Fitzharris, The Wild Prairie: A Natural History of the Western Plains (1983); and Claude A. Barr, Jewels of the Plains: Wild Flowers of the Great Plains Grasslands and Hills (1983). Ian Frazier, Great Plains (1989), combines a discussion of the landscape with a survey of social life and customs. The first important historical account of the Great Plains was Walter Prescott Webb, The Great Plains (1931, reprinted 1981). Webb's brilliant interpretation of cultural adaptation is extended in Carl Frederick Kraenzel, The Great Plains in Transition (1955). The past and present of North American Indian culture are explored in Robert H. Lowie, Indians of the Plains (1954, reprinted 1982); Preston Holder, The Hoe and the Horse on the Plains: A Study of Cultural Development Among North American Indians (1970, reprinted 1991); and Peter Iverson (ed.), The Plains Indians of the Twentieth Century (1985). Mari Sandoz, Old Jules (1935, reprinted 1985), is a classic novel on the frontier and pioneer life of European settlers. John W. Bennett, Northern Plainsmen: Adaptive Strategy and Agrarian Life (1969, reissued 1976), is an anthropologist's analysis of modern trends for the Canadian plains. William Least Heat-Moon, PrairyErth (A Deep Map): An Epic History of the Tallgrass Prairie Country (1991), is a classic narrative of one man's interpretation of the Great Plains landscape.John L. Dietz

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