Abstract
Research Article| January 01, 1966 TIN MOUNTAIN LANDSLIDE, SOUTHEASTERN CALIFORNIA, AND THE ORIGIN OF MEGABRECCIA B. C BURCHFIEL B. C BURCHFIEL DEPT. GEOLOGY, RICE UNIVERSITY, HOUSTON, TEXAS Search for other works by this author on: GSW Google Scholar GSA Bulletin (1966) 77 (1): 95–100. https://doi.org/10.1130/0016-7606(1966)77[95:TMLSCA]2.0.CO;2 Article history received: 07 May 1965 first online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share MailTo Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation B. C BURCHFIEL; TIN MOUNTAIN LANDSLIDE, SOUTHEASTERN CALIFORNIA, AND THE ORIGIN OF MEGABRECCIA. GSA Bulletin 1966;; 77 (1): 95–100. doi: https://doi.org/10.1130/0016-7606(1966)77[95:TMLSCA]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 The Tin Mountain landslide deposit in southeastern California consists of approximately 2.35 billion cubic yards of megabreccia. The megabreccia is due to landsliding from steep slopes produced by a fault. Thus, the Tin Mountain landslide deposit confirms the landslide interpretation proposed by many workers for numerous megabreccia occurrences in the Basin and Range province. 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.
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