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Snake River Plain

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NameColor on MapEPA Code‡
Treasure Valley12a
Lava Fields12b
Camas Prairie12c
Dissected Plateaus and Teton Basin12d
Upper Snake River Plain12e
Semiarid Foothills12f
Eastern Snake River Basalt Plains12g
Mountain Home Uplands12h
Magic Valley12i
Unwooded Alkaline Foothills12j

† Status: ✓ = Complete ○ = Needs Image … = Incomplete ∅ = Stub Only

This code refers to the US EPA's Level 4 ecoregion codes for the continental U.S., see here.

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About the Snake River Plain

The Snake River Plain is a broad, crescent-shaped valley located mostly within southern Idaho, stretching slightly into Oregon and barely reaching a tiny portion of Wyoming. As the name suggests, it centers around the Snake river, which is fed by streams and rivers flowing in from surrounding mountainous regions, primarily areas to the north and east, with less water arriving from the west and south.

The region has a semi-arid steppe climate with strong seasonality of temperature and precipitation. The bulk of water available here arrives from surrounding regions, with only small amounts falling as precipitation. Summers are warm to hot, with little rainfall, especially in the west, whereas the remainder of the year is slightly wetter, with precipitation peaking in May and, in the west of the region, also in December. Temperatures decrease significantly (by about 10°F / 5.5°C) moving from west to east, owing to a gradual increase in elevation, but there is no appreciable increase in precipitation. The frost-free period varies from 50 to 170 days. There is a large temperature variation from day to night, especially in summer, and there can be significant variation in weather from day to day. Winters are cold and there is usually some persistent snowfall.

The terrain here is flatter than most of the surrounding regions, mostly consisting of flat to gently-sloping plains and alluvial valleys, with some low hills and scattered lava fields. There are, however, some steep escarpmentments along the river valley, and some steep-walled canyons around the edges of this region. Soils here tend to be alkaline and somewhat saline, especially on the drier sites, with a higher concentation of minerals than is ideal for plant growth, however, there are areas of richer soils that formed under grasslands, and the soils are often suitable for agriculture with irrigation.

Naturally this area was covered with sagebrush steppe, with dominant plants being Wyoming sagebrush, bigbasin sagebrush, mountain sagebrush, bluebunch wheatgrass, Idaho fescue, Indian ricegrass, rabbitbrush, and fourwing saltbush. Vegetation on lava fields is sparse.

The areas closest to the Snake river have been heavily developed for agriculture, using the river for irrigation. Canals and reservoirs have altered the natural structure of waterways. The main crops grown here include sugar beets, potatoes, alfalfa, various small grains, and assorted vegetables. There are also cattle feedlots and dairy farming. Farther from the river, rangeland is common. Although Idaho is not the most populous state, this region is the most urbanized portion of it, containing all but one of the state's largest cities: Boise, Meridian, Nampa, Idaho Falls, Pocatello, Caldwell, and Twin Falls are all located here.

This region is bordered to the south and west by the Northern Basin and Range, a slightly region that is drier overall, and has more variable topography; this border is marked by a watershed divide, with the southern region draining into the endorheic Great Basin. In the east, this region is bordered to the east and north by the Middle Rockies, a mountainous region. In the west, it is bordered to the north and east by the Idaho Batholith, another mountainous region that has slightly higher rainfall than the Middle Rockies, and it also shares a small border to the northwest with the Blue Mountains, a region of lower, more open mountains.

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References

1. Wiken, E., Griffith, G. "North American Terrestrial Ecoregions - Level III", Commission for Environmental Cooperation, (2011) Web.