Shutter ridge
Appearance
From Wikipedia, the free encyclopedia
A shutter ridge is a ridge which has moved along a fault line, blocking or diverting drainage. Typically, a shutter ridge creates a valley corresponding to the alignment of the fault that produces it.[1] Shutter ridges occur exclusively at strike-slip faults.
Example Locations
[edit ]- Oakland, California[2]
- Dragon's Back, Carrizo Plain, CA
References
[edit ]- ^ Glossary, Earthquake Hazards Program, USGS Archived 2014年09月29日 at the Wayback Machine
- ^ Easterbrook, Don J. (1999). Surface processes and landforms (2. ed.). Upper Saddle River, NJ: Prentice Hall. ISBN 0-13-860958-6.
Stub icon
This article about structural geology is a stub. You can help Wikipedia by expanding it.