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Subsidence crater
From Wikipedia, the free encyclopedia
A subsidence crater is a hole or depression left on the surface of an area which has had an underground (usually nuclear) explosion. Many such craters are present at the Nevada Test Site, which is no longer in use for nuclear testing.
Subsidence craters are created as the "roof" of the cavity caused by the explosion collapses. This causes the surface to depress into a "sink" (which subsidence craters are sometimes called). It is possible for further collapse to occur from the sink into the explosion chamber. When this collapse reaches the surface, and the chamber is exposed atmospherically to the surface, it is referred to as a chimney.
It is at the point that a chimney is formed through which radioactive fallout may reach the surface.
At the Nevada Test Site, depths of 100 to 500 meters were used for tests.
- See also: Underground nuclear testing
- When a drilling oil well encounters high-pressured gas which cannot be contained either by the weight of the drilling mud or by blow-out preventers, the resulting violent eruption can create a large crater which literally can swallow up a drilling rig. This phenomenon is called "cratering" and in oil field slang and by extension it came to mean physical exhaustion ("I went home and cratered")or the failure of an endeavor ("I tried to do it but the whole idea cratered"). The first President Bush, being an ex-oil man, used the term many times in interviews in the latter sense.