Indigenous grassland biomes on the Great Plains include the steppe-like short grass prairie (light green) and mixed grasses between the 100th and 98th parallels. This map of the grasses, crops, and other vegetation suggests that the Great Plains extend farther east than the geologic and most geographic depictions of the Great Plains; the coniferous patch in South Dakota represents the Black Hills. About UsInspired by Ralph Hauenstein’s life of leadership and service, the Hauenstein Center for Presidential Studies is dedicated to raising a community of ethical, effective leaders for the twenty-first century.
The tall grass prairie to the east (dark green) is often used to distinguish the eastern boundary of the Great Plains from the Central Lowlands.

Note that the region’s boundaries, viewed from the perspective of agriculture and land use, extend into Mexico and Canada. Using different criteria, each map locates the region’s boundaries differently, especially its soft eastern margin that merges into the lower Central Plains and tall grass prairie. Geologically, the High Plains, as the term suggests, are composed of numerous layers of relatively horizontal sedimentary rock that slopes gently east from the Rockies toward the Missouri-Mississippi rivers. Our boundaries depend on a combination of climatic, topographical, political, and cartographic criteria, and are ultimately drawn along county borders.

The interior cities include Moose Jaw, Regina, Billings, Minot, Bismarck, Rapid City, Pierre, Lincoln, Wichita, Abilene (Kansas), Topeka, Amarillo, Lubbock, Midland, Odessa, Abilene (Texas), and Roswell.
Among the landforms on the High Plains are plateaus, mesas, buttes, hogbacks, bluffs, badlands, loess formations, moraines left by continental glaciers, and driftless plains that largely escaped glaciation. Depending on where one puts the boundaries of the region, elevations range from 7,000 feet in Colorado (the Black Forest) to under 1,000 feet in North Dakota (along the Red River) and Texas (Edwards Plateau).

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