The Great Plains As a Natural Region: the Basics
Proceedings of the South Dakota Academy of Science,Vol. 80 (2001) 259 THE GREAT PLAINS AS A NATURAL REGION: THE BASICS Richard A. Peterson Wewela, SD 57578 ABSTRACT The need for this paper became apparent during a review of articles in the Prairie Naturalist(1986-1995), where the term, Great Plains, was used to de- scribe many different areas/regions, most of which were outside of established natural boundaries. The Rocky Mountains have long been the agreed upon western boundary of the Great Plains and the primary factor in the develop- ment of the Great Plains; indeed, without the uplift of the Rocky Mountains there would not be a Great Plains region. Consistent natural boundaries for the Great Plains, were in general use after 1931, when Nevin M. Fenneman de- scribed the region in Physiography of the Western United States, and reaffirmed the eastern boundary as originally fixed by John Wesley Powell in 1895. Typ- ical Great Plains landforms (plains and buttes) have resulted from the moun- tain uplift and subsequent sediment deposits that increased the elevation of the Great Plains relative to the Central Lowlands. The Great Plains, in the rain shadow of the Rocky Mountains, have been characterized by a dry subhumid to semiarid climate. The potential natural vegetation of the Great Plains has been, since the last retreat of the continental glaciers 8,000-10,000 years ago, grass/forb vegetation - mostly a mix of mid and short grasses. True Prairie has been limited to the moist side of the dry/moist boundary. These differences between the grasslands of the Great Plains and the grasslands of the Central Lowlands have resulted in differences in occurrence and abundance of grass- land animal species, such as black-tailed prairie dog, black-footed ferret, swift fox, pronghorn, ferruginous hawk, prairie falcon and lark bunting.
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