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GEOMORPHOLOGY OF THE MIDDLE KERN RIVER BASIN, SOUTHERN SIERRA NEVADA, CALIFORNIA

1946; Geological Society of America; Volume: 57; Issue: 4 Linguagem: Inglês

10.1130/0016-7606(1946)57[355

1943-2674

Robert W. Webb,

Botany, Ecology, and Taxonomy Studies

Research Article| April 01, 1946 GEOMORPHOLOGY OF THE MIDDLE KERN RIVER BASIN, SOUTHERN SIERRA NEVADA, CALIFORNIA ROBERT W WEBB ROBERT W WEBB UNIVERSITY OF CALIFORNIA, LOS ANGELES. Search for other works by this author on: GSW Google Scholar GSA Bulletin (1946) 57 (4): 355–382. https://doi.org/10.1130/0016-7606(1946)57[355:GOTMKR]2.0.CO;2 Article history received: 21 Mar 1944 first online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation ROBERT W WEBB; GEOMORPHOLOGY OF THE MIDDLE KERN RIVER BASIN, SOUTHERN SIERRA NEVADA, CALIFORNIA. GSA Bulletin 1946;; 57 (4): 355–382. doi: https://doi.org/10.1130/0016-7606(1946)57[355:GOTMKR]2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGSA Bulletin Search Advanced Search Abstract Evidence from study and mapping of erosional levels, from reconstruction of dissected drainage divides, and from geological relations of a volcanic series proves that the Kern River has always followed a southerly course in its cutting in the Kern River Basin, refuting the deductions of Lawson (1904) that the Kern flowed eastward from the upper Kern Basin across Toowa Valley. Structural control of the Kern River by the Kern Canyon fault is shown to have been effected at the beginning of the older of two cycles; principal evidence is found in the plotted erosional surfaces preserved throughout the basin. The Great Western Divide is established as the primary division of drainage in the southern Sierra prior to the development of the Sierra Nevada fault. A hitherto unrecognized period of canyon cutting is recorded by channels cut in the Chagoopa level, now buried by flows, but visible in the walls of Little Kern gorge. Volcanism, in two stages, and periodic movement on the Sierra Nevada fault stagnated and diverted drainage in both tributary and master streams. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.