Kern Canyon Fault
The Kern Canyon Fault is a geological fault which runs the length of Kern Canyon in the southern Sierra Nevada mountains in California.
The fault was once considered inactive, but recent studies show the contrary.[1][2]
The fault is a break in the southern section of the Sierra Nevada-Great Valley Block, manifesting differences in the stresses in this region over a period of over 100 million years. The fault was formerly right lateral-moving (horizontal sliding), but has changed to a normal (vertical lifting) mode of motion over the past several thousands of years.[2]
See also
References
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- Seismic faults of California
- Sierra Nevada (U.S.)
- Geology of Kern County, California
- Geology of Tulare County, California
- Kern River
- Kern River Valley
- Natural history of Kern County, California
- Natural history of Tulare County, California
- Sequoia National Park
- Tectonics stubs
- Kern County, California geography stubs
- Tulare County, California geography stubs