Jordan Craters | |
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![]() 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] |
Coordinates | 43°06′43″N117°24′58″W / 43.1118219°N 117.4159899°W [2] |
Geography | |
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Location | Malheur County, Oregon, United States |
Geology | |
Rock age | 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 series of large Quaternary basalt fields in the eastern part of the U.S. state of Oregon. The field is thought to be approximately 3200 years old, based on findings of a lake sediment coring experiment in 1986. It was formed by basaltic pahoehoe emanating from vents throughout the area. [4]
The most recent flows come from Coffeepot Crater, a large breached cinder cone. These flows show excellent examples of inflated lava. [5] Historically, it is believed that Coffeepot Crater held a pond of lava that would occasionally breach the sides of the crater to flow freely into the field. [4]
Jordan Craters is approximately 120 miles (200 km) southwest of Boise, Idaho [3] and 18 miles (30 km) northwest of Jordan Valley, Oregon. [4]
The craters are free and open to the public all year.
This article incorporates public domain material from Deschutes & Ochoco National Forests – Crooked River National Grassland. United States Forest Service. (archived)