Shutter ridge

From Wikipedia, the free encyclopedia
Jump to: navigation, search

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. Shutter ridges occur exclusively at strike-slip faults. Though shutter ridges do not necessarily have to occur near rivers or streams, the presence of the stream makes the name easier to comprehend.

[edit] Example Locations

  • Oakland, California[1]

[edit] References

  1. ^ Easterbrook, Don J. (1999). Surface processes and landforms (2. ed. ed.). Upper Saddle River, NJ: Prentice Hall. ISBN 0138609586. 


Personal tools
Namespaces
Variants
Actions
Navigation
Interaction
Toolbox
Print/export