The Montana-Yellowstone Geologic Field Guide Database
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The Yellowstone Plateau-Island Park Region

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Route

Start point

Jackson Hole, Wyoming

End point

Ashton, Idaho

Roads

U.S. 89/287/191, roads through Yellowstone National Park

Total distance

152.8 miles

Geology

Summary

The Yellowstone Plateau, at the center of one of the Earth's largest volcanic fields, spans the continental divide between the Northern and Middle Rocky Mountains at an average elevation of about 2,400 m. The eruptions of the Yellowstone Plateau volcanic field, entirely postdating 2.5 Ma, were exceedingly voluminous but are only the surficial expression of the emplacement of a batholithic volume of rhyolitic magma to high crustal levels. Although the latest eruptions were about 70,000 years ago, an immense hydrothermal system and a variety of geophysical characteristics indicate the continued presence of an active shallow magma chamber.

Key Lithologic Features

Structures

Landforms

Other Features


Reference

Christiansen, R.L., 1989, The Yellowstone Plateau-Island Park Region, in Ruebelmann, K.L., ed., Snake River Plain-Yellowstone Volcanic Province : 28th International Geological Congress, Field Trip Guidebook T305: Washington, D.C., American Geophysical Union, p.14-37.

Availability

Order from the American Geophysical Union Bookstore. Go to the AGU On Line Book Catalog for ordering information.

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