Coffeepot Crater (left center) was the source of voluminous basaltic lava flows in the Jordan Craters volcanic field of SE Oregon.
|Elevation||4,833 ft (1,473 m) |
|Location||Malheur County, Oregon, U.S.|
|Age of rock||less than 30,000 years |
|Mountain type||Volcanic field|
|Last eruption||1250 BCE|
The flows of Jordan Craters volcanic field are the youngest of a large Quaternary basalt fields in the eastern part of the U.S. state of Oregon. The most recent flows come from Coffeepot Crater, a large breached cinder cone. These flows show excellent examples of inflated lava.
The craters are free and open to the public all year.
This article incorporates public domain material from the United States Forest Service document "Deschutes & Ochoco National Forests – Crooked River National Grassland". (archived)
- "Jordan Craters". Global Volcanism Program. Smithsonian Institution. Retrieved 2008-05-16.
- Wood, Charles A.; Jurgen Kienle (1993). Volcanoes of North America. Cambridge University Press. pp. 210–211. ISBN 0-521-43811-X.
- "Jordan Craters". Geographic Names Information System. United States Geological Survey. Retrieved 2008-11-14.
- "Oregon Volcanoes - Jordan Craters Flows". Deschutes & Ochoco National Forests - Crooked River National Grassland. United States Forest Service. 2003-11-26. Archived from the original on 2011-05-12. Retrieved 2008-05-16.
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