Crack in the Ground
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Crack in the Ground is a volcanic fissure about 2 miles (3.2 km) long [1] with depths measuring nearly 30 feet (9 m) below ground level[2] in Central Oregon, United States. The formation of the fissure occurred between 700ka and 12ka, approximately 700,000 to 12,000 years ago.[3] The eruptions from the Four Craters Lava Field were accompanied by a slight sinking of the older rock surface, forming a shallow, graben-like structure about 2 miles (3.2 km) wide and extending to the south into an old lake basin. Crack in the Ground marks the western edge of this small, volcano-tectonic depression. 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 concealed fault zone. The fissure is located at the southwest corner of Four Craters Lava Field.[2] Hikers can walk the length of the main crack and explore its tributaries.
See also
References
- ^ "Crack In The Ground". Fort Rock Museum. Retrieved 2007-10-16.
- ^ a b "Four Craters Field". US Forest Service. Archived from the original on 2010-11-09. Retrieved 2017-10-16.
{{cite web}}: Unknown parameter|deadurl=ignored (|url-status=suggested) (help) - ^ "Paleoseismology of Crack-in-the-Ground Fault, Central Oregon". US Forest Service. December 2011. Retrieved 2019-08-15.
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43°19′30″N 120°39′55″W / 43.32508°N 120.66520°W
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