Snake River Volcanic Plain

Western U.S. - Idaho


SUMMARY

Type: volcanic plain
Activity: dormant
Last Eruption: about 2,000 yrs ago
Rock Type: basalt and rhyolite
Eruptive Volume: ?
Location Map from Xerox PARC
Latitude: 42.7 N
Longitude: 113.5 W


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:

  • None

Recent Activity:

  • None

Data Sources:

  • Volcanoes of the World - Simkin & Siebert
  • Volcanoes of North America - Wood & Kienle

ADDITIONAL INFORMATION


Last Update: 1/8/01