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Crack in the Ground

Coordinates: 43°19′30″N 120°39′55″W / 43.32508°N 120.66520°W / 43.32508; -120.66520
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This is an old revision of this page, as edited by Leitmotiv (talk | contribs) at 16:50, 15 August 2019 (That article doesn't specifically say it's in the Deschutes Natiotional Forest. It's just an aricle on the on geology. All maps of Deschutes National Forest show Crack in the Ground and Four Craters as being 11 miles away from the boundary). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.
Crack in the Ground

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 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

  1. ^ "Crack In The Ground". Fort Rock Museum. Retrieved 2007-10-16.
  2. ^ 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)

43°19′30″N 120°39′55″W / 43.32508°N 120.66520°W / 43.32508; -120.66520