description Snake River Plain Overview
The Snake River Plain is an arcuate volcanic lowland across southern Idaho. Its eastern part records the movement of the North American Plate over the Yellowstone hotspot, leaving a chain of progressively older volcanic centers, while the western part has a different structural history. The plain contains lava fields, aquifers, major Idaho cities, and extensive irrigated farmland supported by the Snake River and groundwater, so it is both a geological record and a heavily used agricultural and settlement region.
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