Artigo Revisado por pares

Structural Studies in Southern Nevada and Western Arizona

1926; Geological Society of America; Volume: 37; Issue: 4 Linguagem: Inglês

10.1130/gsab-37-551

ISSN

1943-2674

Autores

Chester R. Longwell,

Tópico(s)

Geology and Paleoclimatology Research

Resumo

Research Article| December 30, 1926 Structural Studies in Southern Nevada and Western Arizona CHESTER R. LONGWELL CHESTER R. LONGWELL Search for other works by this author on: GSW Google Scholar GSA Bulletin (1926) 37 (4): 551–584. https://doi.org/10.1130/GSAB-37-551 Article history received: 29 Jun 1926 first online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation CHESTER R. LONGWELL; Structural Studies in Southern Nevada and Western Arizona. GSA Bulletin 1926;; 37 (4): 551–584. doi: https://doi.org/10.1130/GSAB-37-551 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu nav search search input Search input auto suggest search filter All ContentBy SocietyGSA Bulletin Search Advanced Search Abstract IntroductionGrand Wash, a tributary of Colorado River in northwestern Arizona, lies in a wide valley whose position is determined by a zone of profound faulting. This valley marks throughout its length a sharp and definite boundary between two major physiographic and structural provinces. East of the valley the Grand Wash Cliffs rise precipitously, as a pair of giant steps, to an elevation averaging 4,000 feet above the valley floor. These cliffs form the abrupt western limit of a great tabular mass, the Shiwits division of the Colorado Plateau, in which the stratified rocks are nearly horizontal over a wide area. West of Grand Wash Valley and reaching into southern Nevada lies the Virgin Range, a complexly broken fault block, in which the same formations exposed in the Grand Wash Cliffs are tilted at high angles. Continuing to the west, other ranges structurally similar to the Virgin Range alternate with . . . This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not currently have access to this article.

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