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.[1] Shutter ridges occur exclusively at strike-slip faults.

Example Locations[edit]


  1. ^ Glossary, Earthquake Hazards Program, USGS
  2. ^ Easterbrook, Don J. (1999). Surface processes and landforms (2. ed.). Upper Saddle River, NJ: Prentice Hall. ISBN 0-13-860958-6.