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• W1980072019 abstract "Research Article| September 01, 2005 Trail of sand in upper Monterey Canyon: Offshore California Charles K. Paull; Charles K. Paull 1Monterey Bay Aquarium Research Institute, Moss Landing, California 95039, USA Search for other works by this author on: GSW Google Scholar Patrick Mitts; Patrick Mitts 1Monterey Bay Aquarium Research Institute, Moss Landing, California 95039, USA Search for other works by this author on: GSW Google Scholar William Ussler, III; William Ussler, III 1Monterey Bay Aquarium Research Institute, Moss Landing, California 95039, USA Search for other works by this author on: GSW Google Scholar Rendy Keaten; Rendy Keaten 1Monterey Bay Aquarium Research Institute, Moss Landing, California 95039, USA Search for other works by this author on: GSW Google Scholar H. Gary Greene H. Gary Greene 1Monterey Bay Aquarium Research Institute, Moss Landing, California 95039, USA Search for other works by this author on: GSW Google Scholar GSA Bulletin (2005) 117 (9-10): 1134–1145. https://doi.org/10.1130/B25390.1 Article history received: 22 Apr 2003 rev-recd: 13 Apr 2004 accepted: 26 Apr 2004 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 Charles K. Paull, Patrick Mitts, William Ussler, Rendy Keaten, H. Gary Greene; Trail of sand in upper Monterey Canyon: Offshore California. GSA Bulletin 2005;; 117 (9-10): 1134–1145. doi: https://doi.org/10.1130/B25390.1 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 Detailed sampling of the axis and flanks of upper Monterey Canyon (water depths of <1500 m) was undertaken using a remotely operated vehicle (ROV)–deployed vibracoring system. The objective was to document the characteristics and distribution of sediment within the canyon and to elucidate the sources and processes by which materials move into and through the canyon. Detailed multibeam bathymetric surveys guided the sampling. The combination of core data, multi-beam bathymetry, and multi-beam reflectivity reveals for the first time the facies and facies distribution patterns associated with the axial channel of an active submarine canyon. Coarse-grained deposits form a narrow trail of material that is tightly restricted to the axial channel floor, indicating that upper Monterey Canyon is an active submarine system closely coupled to sand transport along the shoreline. Sand from the modern beach and nearshore environment captured by the canyon head is moving down the axial channel of the canyon, while fine-grained sediments are accumulating on the flanks of the canyon. Our observations suggest that other submarine canyons in close proximity to the shoreline are presently active and that a modern supply of sand-sized material is moving down these canyon systems. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W1980072019 title "Trail of sand in upper Monterey Canyon: Offshore California" @default.
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