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strike-slip fault

American  
[strahyk lip fawlt] / ˈstraɪk ˌlɪp ˌfɔlt /

noun

  1. Geology. a vertical fracture in Earth's crust, where the masses of fractured rock slide past one another horizontally, a well-known example of which is the San Andreas Fault.


strike-slip fault British  

noun

  1. a geological fault on which the movement is along the strike of the fault

"Collins English Dictionary — Complete & Unabridged" 2012 Digital Edition © William Collins Sons & Co. Ltd. 1979, 1986 © HarperCollins Publishers 1998, 2000, 2003, 2005, 2006, 2007, 2009, 2012

strike-slip fault Scientific  
  1. A geologic fault in which the blocks of rock on either side of the fault slide horizontally, parallel to the strike of the fault.

  2. See Note and illustration at fault


Example Sentences

Examples are provided to illustrate real-world usage of words in context. Any opinions expressed do not reflect the views of Dictionary.com.

This earthquake was triggered by a strike-slip fault, where two large sections of the Earth's crust move horizontally past each other along a vertical fracture.

From Science Daily

The earthquake occurred along the Sagaing Fault, which is a strike-slip fault.

From Science Daily

That’s a strike-slip fault, the seismic action you get is when these plates slide past each other.

From Los Angeles Times

The East Anatolian Fault is a strike-slip fault.

From Reuters

Large strike-slip fault zones on land are not common , Dr. Hough said; the San Andreas Fault in California is another example.

From New York Times