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Crooked River caldera information


Crooked River caldera
Crooked River caldera is located in Oregon
Crooked River caldera
Crooked River caldera
Highest point
Coordinates44°18′N 120°54′W / 44.3°N 120.9°W / 44.3; -120.9
Geography
LocationDeschutes, Crook, and Jefferson counties, Oregon, U.S.
Geology
Age of rock29.5 Ma
Mountain typeCaldera, supervolcano
Volcanic arcCascade Volcanic Arc, Ochoco Mountains
Last eruption29.5 million years ago

The Crooked River caldera is a large and ancient volcano that straddles three central Oregon counties. The diameter of the caldera is about 41 by 27 kilometres (25 mi × 17 mi) and is notable for the welded tuff present at Gray Butte, Smith Rock, Powell Buttes, Grizzly Mountain and Barnes Butte. The volcano is considered extinct and last erupted about 29.5 Ma.[1]

  1. ^ The Crooked River Caldera is also a supervolcano. "Field trip guide to the Oligocene Crooked River caldera: Central Oregon's Supervolcano, Crook, Deschutes, and Jefferson Counties, Oregon" (PDF). Oregon Geology. Oregon Department of Geology and Mineral Studies. 2009. Retrieved 2014-12-29.

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Crooked River caldera

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The Crooked River caldera is a large and ancient volcano that straddles three central Oregon counties. The diameter of the caldera is about 41 by 27 kilometres...

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United States. It is composed of welded tuff and is a part of the Crooked River caldera. A recreation trail for hiking, horseback riding, and mountain biking...

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