Identification and analysis of large paleo-landslides at Mount Burnaby, British Columbia
2017; Geological Society of America; Linguagem: Inglês
10.2113/eeg-1955
ISSN1558-9161
AutoresMirko Francioni, Doug Stead, John J. Clague, Allison May Westin,
Tópico(s)Geotechnical Engineering and Analysis
ResumoResearch Article| May 23, 2018 Identification and Analysis of Large Paleo-landslides At Mount Burnaby, British Columbia Mirko Francioni; Mirko Francioni 1 Camborne School of Mines, University of Exeter, Penryn Campus, Penryn, Cornwall, TR10 9FE, UK 1Corresponding author email: M.Francioni@exeter.ac.uk Search for other works by this author on: GSW Google Scholar Doug Stead; Doug Stead Department of Earth Sciences, Simon Fraser University, 8888 University Dr, Burnaby, BC V5A 1S6, Canada Search for other works by this author on: GSW Google Scholar John J. Clague; John J. Clague Department of Earth Sciences, Simon Fraser University, 8888 University Dr, Burnaby, BC V5A 1S6, Canada Search for other works by this author on: GSW Google Scholar Allison Westin Allison Westin Department of Earth Sciences, Simon Fraser University, 8888 University Dr, Burnaby, BC V5A 1S6, Canada Search for other works by this author on: GSW Google Scholar Author and Article Information Mirko Francioni 1 Camborne School of Mines, University of Exeter, Penryn Campus, Penryn, Cornwall, TR10 9FE, UK Doug Stead Department of Earth Sciences, Simon Fraser University, 8888 University Dr, Burnaby, BC V5A 1S6, Canada John J. Clague Department of Earth Sciences, Simon Fraser University, 8888 University Dr, Burnaby, BC V5A 1S6, Canada Allison Westin Department of Earth Sciences, Simon Fraser University, 8888 University Dr, Burnaby, BC V5A 1S6, Canada 1Corresponding author email: M.Francioni@exeter.ac.uk Publisher: Association of Environmental & Engineering Geologists First Online: 12 Feb 2018 Online Issn: 1558-9161 Print Issn: 1078-7275 © 2018 Association of Environmental & Engineering Geologists Environmental & Engineering Geoscience (2018) 24 (2): 221–235. https://doi.org/10.2113/EEG-1955 Article history First Online: 12 Feb 2018 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Mirko Francioni, Doug Stead, John J. Clague, Allison Westin; Identification and Analysis of Large Paleo-landslides At Mount Burnaby, British Columbia. Environmental & Engineering Geoscience 2018;; 24 (2): 221–235. doi: https://doi.org/10.2113/EEG-1955 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 This article presents a multi-scale and multi-disciplinary study of large, late Pleistocene or early Holocene slumps in Eocene sedimentary rocks at Mount Burnaby, just east of Vancouver, British Columbia (BC). Airborne Light Detection and Ranging (LiDAR) and field data were integrated into a Geographic Information System to understand the origin, kinematics, and subsequent history of the landslides. Products derived from the bare-earth LiDAR data include an engineering geomorphology map, shaded relief maps, and several LiDAR slope profiles. To understand the landslides better, we analyzed discontinuities and structural lineaments. The structure of the Eocene rocks underlying Mount Burnaby was compared with trends of local lineaments and the shape of the coastline of Burrard Inlet and Indian Arm as well as trends of regional faults and lineaments identified by previous researchers working in southwest BC. Two main joint systems likely played a key role in conditioning the north slope of Mount Bur-naby for failure. The landslides likely happened during or soon after deglaciation of the area at the end of the Pleistocene on the steep north face of Mount Burnaby after a 200-m fall in relative sea level caused by glacio-isostatic uplift of the crust. 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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