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• W2316595132 abstract "Research Article| February 01, 2015 Complex Landslide Triggered in an Eocene Volcanic-Volcaniclastic Succession along Sutherland River, British Columbia, Canada ANDRÉE BLAIS-STEVENS; ANDRÉE BLAIS-STEVENS 1 Geological Survey of Canada, 601 Booth Street, Ottawa, Ontario, K1A 0E8 1Corresponding author email: ablais@nrcan.gc.ca. Search for other works by this author on: GSW Google Scholar MARTEN GEERTSEMA; MARTEN GEERTSEMA BC Ministry of Forests, Lands, and Natural Resource Operations, 1044 5th Avenue, Prince George, British Columbia V2L 5G4 Search for other works by this author on: GSW Google Scholar JAMES W. SCHWAB; JAMES W. SCHWAB P.O. Box 2525, Smithers, British Columbia V0J 2N0 Search for other works by this author on: GSW Google Scholar THEO W. J. VAN ASCH THEO W. J. VAN ASCH Department of Physical Geography, Utrecht University, P.O. Box 80115, 3508 TC Utrecht, The Netherlands Search for other works by this author on: GSW Google Scholar Author and Article Information ANDRÉE BLAIS-STEVENS 1 Geological Survey of Canada, 601 Booth Street, Ottawa, Ontario, K1A 0E8 MARTEN GEERTSEMA BC Ministry of Forests, Lands, and Natural Resource Operations, 1044 5th Avenue, Prince George, British Columbia V2L 5G4 JAMES W. SCHWAB P.O. Box 2525, Smithers, British Columbia V0J 2N0 THEO W. J. VAN ASCH Department of Physical Geography, Utrecht University, P.O. Box 80115, 3508 TC Utrecht, The Netherlands 1Corresponding author email: ablais@nrcan.gc.ca. Publisher: Association of Environmental & Engineering Geologists First Online: 02 Mar 2017 Online ISSN: 1558-9161 Print ISSN: 1078-7275 © 2015 Association of Environmental & Engineering Geologists Environmental & Engineering Geoscience (2015) 21 (1): 35–45. https://doi.org/10.2113/gseegeosci.21.1.35 Article history First Online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation ANDRÉE BLAIS-STEVENS, MARTEN GEERTSEMA, JAMES W. SCHWAB, THEO W. J. VAN ASCH; Complex Landslide Triggered in an Eocene Volcanic-Volcaniclastic Succession along Sutherland River, British Columbia, Canada. Environmental & Engineering Geoscience 2015;; 21 (1): 35–45. doi: https://doi.org/10.2113/gseegeosci.21.1.35 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 SocietyEnvironmental & Engineering Geoscience Search Advanced Search Abstract On July 13, 2005 a complex 3 Mm3 and 1.5 km long rock slide-debris avalanche occurred near Sutherland River, 40 km west of Fort St. James, British Columbia, Canada. The landslide was initiated in a succession of sub-horizontal competent mafic basalts (Endako Formation) capping weaker felsic volcanic and volcaniclastic rocks (Ootsa Lake Group) of Eocene age. Several landslides have been observed in similar volcanic successions worldwide including in southern British Columbia. Some common characteristics of these landslides are: structurally undisturbed; horizontal to sub-horizontal bedding; curved head scarp; steep joints; debris consists of intact blocks; volcaniclastics containing smectite (expandable clay mineral); fossils and lignite within the volcaniclastics. The Sutherland landslide is one of many large landslides that have occurred in recent years in northern British Columbia. At least eight other large landslides have been triggered in volcanic rocks within the Nechako plateau. 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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• W2316595132 title "Complex Landslide Triggered in an Eocene Volcanic-Volcaniclastic Succession along Sutherland River, British Columbia, Canada" @default.
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