| Four Craters Lava Field | |
|---|---|
 Craters of the aptly named Four Craters Lava Field are seen here from the NW on Green Mountain. | |
| Highest point | |
| Elevation | 4,924 ft (1,501 m)[1] |
| Coordinates | 43°21′36″N120°39′46″W / 43.360009°N 120.66267°W /43.360009; -120.66267[2] |
| Geography | |
 | |
| Location | Lake County,Oregon, U.S. |
| Geology | |
| Rock age | Holocene[3] |
| Mountain type | volcanic field |
| Last eruption | < 50,000 years ago[4] |
Four Craters Lava Field is abasalticvolcanic field located south east ofNewberry Caldera in the U.S. state ofOregon.[1] The volcanic field covers about 30 square kilometers and post-datesMount Mazama's eruption.[3] FourHolocenecinder cones are the source of the flows in the field and are aligned along a fissure trending N 30° W. The cones rise 75 to 120 meters above the flows and the distance between the northernmost and southernmost cones is about 3.5 kilometers.[4]
Closely related to the Four Craters lava field isCrack-in-the-Ground located at the southwest corner of the field. The eruptions from the field were accompanied by a slight sinking of the older rock surface. This shallow,graben-like sink is about 3 kilometers wide and extends to the south into an old lake basin. Crack-in-the-Ground marks the western edge of this small, volcano-tectonic depression and is nearly 9 meters deep and over a meter wide. The crack is the result of a tension fracture along a hingeline produced by the draping of Green Mountain lava flows over the edge of upthrown side of the concealedfault zone.[4]
This article incorporatespublic domain material fromDeschutes & Ochoco National Forests - Crooked River National Grassland.United States Forest Service. (archived)