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ring fault

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ring fault [′riŋ ‚fȯlt]
(geology)
A fault that bounds a rift valley.
A steep-sided fault pattern that is cylindrical in outline and associated with cauldron subsidence. Also known as ring fracture.


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Surface mapping and sampling by Seabridge during 2005 have traced part of an arcuate ring fault along the edge of the basin which may have been the conduit for precious metals in the system.
Geologic and alteration mapping and geophysical surveys have identified a major system of ring faults defining a large domal feature averaging 2,100 meters in diameter that appears to control the emplacement of ore in the existing open pits and present reserve base.
And, since each OmniSwitch port acts as a token ring bridge, beaconing conditions and other ring faults are isolated to a very small number of users.
 
 
 
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