Jordan Craters
| Jordan Craters | |
|---|---|
 Coffeepot Crater (left center) was the source of voluminous basaltic lava flows in the Jordan Craters volcanic field of SE Oregon. | |
| Highest point | |
| Elevation | 4,833 ft (1,473 m)[1] |
| Geography | |
| Location | Malheur County, Oregon, U.S. |
| Geology | |
| Age of rock | less than 30,000 years [3] |
| Mountain type | Volcanic field |
| Last eruption | 1250 BCE[1] |
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.[4]
Jordan Craters is approximately 200 kilometres (120 mi) southwest of Boise, Idaho.[3]
The craters are free and open to the public all year.
See also
ha ha tashelle rocks succker
References
This article incorporates public domain material from Deschutes & Ochoco National Forests – Crooked River National Grassland. United States Forest Service.
(archived)
- ^ a b "Jordan Craters". Global Volcanism Program. Smithsonian Institution. Retrieved 2008-05-16.
- ^ "Jordan Craters". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2008-11-14.
- ^ a b Wood, Charles A.; Jurgen Kienle (1993). Volcanoes of North America. Cambridge University Press. pp. 210–211. ISBN 0-521-43811-X.
- ^ "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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