Geoscience Reference
In-Depth Information
Sheridan
Powder River Basin
Big Horn
Basin
Cody
Gillette
Worland
Newcastle
Wind River
Basin
Casper
Lander
Great
Divide
Basin
Green
River
Basin
Rawlins
Rock
Springs
Laramie
Cheyenne
0
50
100 km
≥ 9,000 ft
≥ 7,000 ft
5,000 ft
0
50
100 miles
Fig. 3.1. General topographic map of Wyoming with the
names of selected towns and intermountain basins. elevation
is given as number of feet above sea level. See fig. 1.2 for the
names of mountain ranges and other basins. Adapted from
Martner (1986).
elevation in determining plant and animal distribution
patterns.
Based on elevation, topography, geologic charac-
teristics, and location with regard to the continental
Divide, several ecological regions can be identified. the
Great Plains characterize the eastern third of Wyoming,
with elevations ranging from 3,125 to 7,524 feet. Sum-
mer precipitation is more frequent on the plains than
farther west. Grasslands are the most common vegeta-
tion type, and there is evidence to suggest that bison
were more numerous there than in the Great Basin of
Utah and nevada. 3 With more bison, plants on the
Great Plains evolved adaptations to withstand grazing
from large herbivores; hence, they are more tolerant of
livestock grazing than are plants in the Great Basin.
to the west of the Great Plains is a region of moun-
tains and intermountain basins (see figs. 1.2 and 3.1).
the continental Divide passes through the middle
of this region, splitting west of Rawlins to form the
Great Divide Basin, which has no drainage to either
the Pacific or Atlantic oceans. the Divide around this
closed basin is relatively low, about 7,000 feet above sea
level, and is characterized by sagebrush steppe rather
than the coniferous forest or alpine tundra typical to
the north and south. For this reason, the Pony express,
various wagon trails, and the first transcontinental
railroad passed through the area in the 1800s. Most of
the basins range in elevation from about 3,960 to 7,260
feet, with the highest basins in the south (see figs. 1.1
and 3.1).
 
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