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Death Valley National Park
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This small cinder cone has been cut and offset by a branch of the Death Valley Fault zone. The upper part of the once symmetrical cone has been moved to the right 300 feet (91 meters) relative to the lower part (arrows indicate movement direction). This fault is a right-lateral strike-slip fault.
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| Death Valley geology | Death Valley National Park | Geology field trip | | Death Valley time| Geologist's page | Image gallery | | USGS Geology in the Parks home | NPS Park Geology Tour home |
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http://www.nature.nps.gov/grd/usgsnps/deva/galcin.html
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