Sharp, Robert P. (1954) The Nature of Cima Dome. In: Geology of Southern California. California Division of Mines and Geology Bulletin. Vol.1. No.170. California Division of Mines and Geology , Sacramento, CA, pp. 49-52. https://resolver.caltech.edu/CaltechAUTHORS:20200221-151117104
![]() |
PDF
- Published Version
See Usage Policy. 5MB |
Use this Persistent URL to link to this item: https://resolver.caltech.edu/CaltechAUTHORS:20200221-151117104
Abstract
In the Mojave Desert of southeasternmost California is a remarkably smooth, symmetrical rock-alluvial dome which takes its name from Cima on the Union Pacific Railroad. Lawson (1915, pp. 26, 33) cited Cima Dome as a prime example of a panfan, but Thompson (1929, p. 550) later showed that its upper part is bare rock. Davis (1933, pp. 240-243) considered it a fine example of a convex desert dome evolved from back-wearing of a fault block, but this concept is contradicted by the geological relations (Hewett, 1954), which throw more light on the nature and origin of Cima Dome than do geomorphological theories.
Item Type: | Book Section | ||||||
---|---|---|---|---|---|---|---|
Related URLs: |
| ||||||
Additional Information: | © 1954 State of California, Dept. of Natural Resources, Division of Mines. Contribution No. 645, Division of the Geological Sciences, California Institute of Technology. | ||||||
Other Numbering System: |
| ||||||
Series Name: | California Division of Mines and Geology Bulletin | ||||||
Issue or Number: | 170 | ||||||
Record Number: | CaltechAUTHORS:20200221-151117104 | ||||||
Persistent URL: | https://resolver.caltech.edu/CaltechAUTHORS:20200221-151117104 | ||||||
Usage Policy: | No commercial reproduction, distribution, display or performance rights in this work are provided. | ||||||
ID Code: | 101471 | ||||||
Collection: | CaltechAUTHORS | ||||||
Deposited By: | Tony Diaz | ||||||
Deposited On: | 22 Feb 2020 19:29 | ||||||
Last Modified: | 22 Feb 2020 19:29 |
Repository Staff Only: item control page