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Deeply weathered granitic batholith, major and often-discussed physiographic feature in the eastern Mojave Desert. Northwest of Cima, and south of Interstate 15.
Elevation: 5745ft, 1751m.
Articles that refer to this location:
- Eastern Mojave Geology -- A Botanist's View:
about pediments;
- Summaries of Literature About the Mid Hills.:
50100;
Literature Referring To This Location:
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Davis, William Morris. 1933.
Granitic domes of the Mohave Desert, California.
Transactions of the San Diego Society of Natural History.
VII(20):211-258.
San Diego, CA: San Diego Society of Natural History, 1933.
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Sharp, R. P. 1954.
The nature of Cima Dome [Part 8].
pp. 49-52 in Jahns, R. H. (ed.).
Geology of southern California.
68(3):49-52.
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Sharp, Robert P. 1957.
Geomorphology of Cima Dome, Mojave Desert, California.
Bulletin of the Geological Society of America.
68(3):273-290.
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Strudley, Mark W., A. Brad Murray, and P. K. Haff. 2006.
Emergence of pediments, tors, and piedmont junctions from a bedrock weathering-regolith thickness feedback.
Geology.
34(10):805-808.
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Vasek, F. C., and M. G. Barbour. 1988.
Mojave Desert scrub vegetation.
pp. pp. 835-868 in Barbour, Michael G., and Jack Major. 1988.
Terrestrial Vegetation of California, New Expanded Edition.
Special Publication Number 9..
1988.
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Date and time this article was prepared:5:20:18 PM, 4/24/2026.
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