Kellen Gunderson on Death Valley. Kellen (website) is a PhD Candidate at Lehigh University in Bethlehem, PA, United States. He is a tectonic geomorphologist currently working on spatial and temporal scales of fault slip rate variability in the Northern Apennines, Italy.
Death Valley (part 1)
To most people Death valley seems desolate. Its true that this inhospitable area is a difficult place for any life form to eke out a living, but geologists see anything but desolation. To a geologist, Death Valley is a place of incredible energy. It is a place where active natural processes are laid to bare and impossible to miss.
Death Valley is an extensional basin formed at the western edge of the Basin and Range province in California. The amount of extension that has occurred here is immense and it is visible by the over 9000′ of relief present between the valley floor and the adjacent mountain ranges.
Badwater Basin is the lowest place on North America. Its also a nice place to enjoy an apple.
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If you are lucky, you find a place where the hanging wall and footwall of the core complex are both still present.
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Beautiful desolation. These badlands are made up of Miocene deposits that filled Death Valley during the early stages of extension.
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Thanks to Kellen for this post. As Death Valley is an incredibly geologically diverse area, I am sure we will return to this place.
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