Artigo Revisado por pares

SUBMARINE TOPOGRAPHY IN THE GULF OF ALASKA

1960; Geological Society of America; Volume: 71; Issue: 7 Linguagem: Inglês

10.1130/0016-7606(1960)71[1087

ISSN

1943-2674

Autores

WILLIAM M. GIBSON,

Tópico(s)

Methane Hydrates and Related Phenomena

Resumo

Research Article| July 01, 1960 SUBMARINE TOPOGRAPHY IN THE GULF OF ALASKA WILLIAM M GIBSON WILLIAM M GIBSON 101 WILDWOOD AVE., PIEDMONT 10, CALIF. Search for other works by this author on: GSW Google Scholar GSA Bulletin (1960) 71 (7): 1087–1108. https://doi.org/10.1130/0016-7606(1960)71[1087:STITGO]2.0.CO;2 Article history 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 WILLIAM M GIBSON; SUBMARINE TOPOGRAPHY IN THE GULF OF ALASKA. GSA Bulletin 1960;; 71 (7): 1087–1108. doi: https://doi.org/10.1130/0016-7606(1960)71[1087:STITGO]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 A bathymetric chart of the Gulf of Alaska and approaches covering an area of about 800,000 square nautical miles has been prepared from Coast and Geodetic Survey hydrography, 1925–1957, with a view to defining regional physiographic provinces.The basic data comprise 90 sounding lines across the gulf, 42,000 miles of graphically recorded profiles obtained during the last 5 years, and detailed surveys of 60 seamounts, seaknolls, and ridges. Tentative names are assigned principal features of the sea floor to facilitate discussion.The bathymetry and illustrated profiles reveal clearly the form of the Aleutian Trench, two submarine mountains, several seamount chains and groups, a ridge and trough province, a 200-mile trench west of Vancouver Island, a great trough paralleling the West Coast, and an inferred fracture zone extending in several wide echelon bands across the gulf.The submarine topography is discussed in relation to existing theories of earth science and correlated with features previously mapped on the mainland and in the Central Pacific Ocean. 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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