Snake River Plain
The Snake River Plain is a valley in the U.S. state of Idaho. It covers most of the southern part of the state and is transected by the Snake River. The Snake River Plain was formed by magma rising up below the North American Plate. As the plate moved westward, the magma melted rock under the plate. This melting caused the surface to drop and form the Snake River Plain. Underneath the plain is the Snake River Aquifer. The aquifer is fed by the Snake River and its tributaries. Much of the soil in the Snake River Plain is fertile. As a result, today the primary human purpose of the plain is for agriculture.
Snake River Plain Media
- Snake River view near Twin Falls, Idaho.jpg
The Snake River cutting through the plain leaves many canyons and gorges, such as this one near Twin Falls, Idaho
- Snake River Plain.png
Snake River Plain across southern Idaho
The eastern Snake River Plain, image from NASA's Aqua satellite, 2008
- HotspotsSRP update2013.JPG
Location of Yellowstone Hotspot in Millions of Years Ago
- MoistureChannel.jpg
- MoistureChannel
- 2013-07-07 18 42 21 Natural vegetation on the Snake River Plain near Shoshone Falls in Idaho.jpg
Natural vegetation on the Snake River Plain near Twin Falls
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