Category: Geography & Travel
- Also called:
- Great American Desert
Top Questions
What are the Great Plains?
The Great Plains is the name of a high plateau of grasslands that is located in parts of the United States and Canada in North America and has an area of approximately 1,125,000 square miles (2,900,000 square km). Also called the Great American Desert,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 Lowlands and the Canadian Shield on the east and the Rocky Mountains on the west. Some sections are extremely flat, while other areas contain tree-covered mountains. Low hills and incised stream valleys are common.
How big are the Great Plains?
The Great Plains, located in North America, have an area of approximately 1,125,000 square miles (2,900,000 square km), roughly equivalent to one-third of the United States. Their length from north to south is some 3,000 miles (4,800 km) and their width from east to west is 300 to 700 miles. 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 Lowlands and the Canadian Shield on the east and the Rocky Mountains on the west.
Where are the Great Plains located?
The Great Plains are located on the North American continent, in the countries of the United States and Canada. In the United States, the Great Plains contain parts of 10 states: Montana, North Dakota, South Dakota, Wyoming , Nebraska, Kansas, Colorado, Oklahoma, Texas, and New Mexico. In Canada, the Great Plains lie in parts of the three Prairie Provinces—Manitoba, Saskatchewan, and Alberta—and portions of the Northwest Territories.
Which states are located within the Great Plains?
Parts of 10 U.S. states lie within the Great Plains. They are Montana, North Dakota, South Dakota, Wyoming, Nebraska, Kansas, Colorado, Oklahoma, Texas, and New Mexico. The Great Plains also extend into Canada, into portions of Manitoba, Saskatchewan, Alberta, and the Northwest Territories.
What is the climate of the Great Plains?
The Great Plains have a continental climate. Much of the plains experience cold winters and warm summers, with low precipitation and humidity, much wind, and sudden changes in temperature. More rainfall occurs in summer than in winter, except in some of the northwestern parts of the Great Plains. 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.
Read more below:Physical features: Soils and climate
Great Plains, 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 km), their width from 300 to 700 miles, and their area approximately 1,125,000 square miles (2,900,000 square km), 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 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 mm) 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.
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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, Alberta, and Winnipeg, Manitoba, 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 gray wolves (timber wolves). The region is not without its share of insect pests, such as the locust and the tiny chigger.
The Great Plains, also known as the Great American Desert, constitute a massive high plateau of grasslands stretching across parts of the United States and Canada. Spanning roughly 1,125,000 square miles (2,900,000 square km), this area lies between the Rio Grande in the south and the Mackenzie River delta at the Arctic Ocean in the north. Bounded by the Interior Lowlands and the Canadian Shield to the east and the Rocky Mountains to the west, the Great Plains encompass landscapes of diverse topography, ranging from extremely flat sections like the Llano Estacado in Texas and New Mexico to tree-covered mountains such as the Black Hills in South Dakota and various ranges in Montana.
Geographically, they cover portions of 10 U.S. states—Montana, North Dakota, South Dakota, Wyoming, Nebraska, Kansas, Colorado, Oklahoma, Texas, and New Mexico—as well as parts of three Canadian Prairie Provinces—Manitoba, Saskatchewan, and Alberta—along with sections of the Northwest Territories.
Climate-wise, the Great Plains experience a continental climate characterized by cold winters and warm summers, with low precipitation and humidity. Rainfall patterns vary across the region, with the southern plains receiving 15 to 25 inches annually, decreasing towards the northern plains with 12 to 15 inches. The eastern margin in Nebraska can see up to 25 inches, while the western margin in Montana receives less than 15 inches. The Gulf of Mexico serves as the primary moisture source for the region.
A defining meteorological phenomenon of the western Great Plains is the chinook, a warm, dry wind that descends from the eastern slope of the Rockies, capable of swiftly raising temperatures by 30 to 40 °F (17 to 22 °C).
The vegetation in the Great Plains predominantly comprises grasslands—tallgrass and medium grass prairies in the east, transitioning to shortgrass and bunchgrass steppes in the west. This natural cover is interspersed with plant species like yucca, prickly pear cactus, mesquite, and sagebrush, while gallery forests border the rivers, featuring drought-resistant trees such as cottonwood and box elder.
Historically, this region was home to vast herds of grazing mammals like buffalo (bison) and pronghorn, with the former nearly eliminated due to human activities. Other wildlife, including prairie dogs, coyotes, prairie chickens, and rattlesnakes, thrive in this environment, alongside various insect pests such as locusts and chiggers.
The Great Plains' intricate topography, climate patterns, and diverse flora and fauna make it a fascinating and ecologically rich region in North America.
