SUMMARYType: volcanic plain |
Geologic Background:The Snake River Plain is a long lived band of volcanic vents extending from near the Oregon border to the Yellowstone Plateau. A sequence of progressively younger silicic calderas have been formed beginning near the Oregon-Idhao border some 16 million years ago and ending at the Yellowstone Plateau about 600,000 years ago. Younger basaltic activity has filled most of the calderas leaving a flat plain of low basaltic shields. Some of the features on the plain include: Historic Activity:
Recent Activity:
Data Sources:
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ADDITIONAL INFORMATION
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Last Update: 1/8/01 |