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Landforms in a Pacific fjord system: Douglas Channel, British Columbia, Canada

J. Shaw and D. G. Lintern
Geological Society, London, Memoirs, 46, 81-82, 30 November 2016, https://doi.org/10.1144/M46.105
J. Shaw
1Geological Survey of Canada, Natural Resources Canada, PO Box 1006, Dartmouth, Nova Scotia B2Y 4A2, Canada
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  • For correspondence: John.Shaw@canada.ca
D. G. Lintern
2Geological Survey of Canada, Institute of Ocean Sciences, 9860 West Saanich Road, Sidney, British Columbia V8L 4B2, Canada
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Douglas Channel is part of a complex network of fjords on the Pacific north coast of British Columbia, Canada, an area in which fjords formed under the influence of westward-moving ice of the Cordilleran Ice Sheet (Barrie et al. 2014). The Douglas Channel fjord system (Fig. 1a) extends from the Pacific coast to the town of Kitimat located 150 km inland, and has a maximum depth of 690 m. The fjords are developed within the Coast Range, which has peaks extending up to 1500 m in the study area. The fjord system is located on the North American Plate, east of its boundary with the Pacific Plate. The region is subject to heavy precipitation (>2700 mm a−1 at Kitimat) and melt from snow pack in the interior.

Fig. 1.

Sun-illuminated multibeam bathymetry and seismic data from the Douglas Channel area, British Columbia. Multibeam acquisition system Kongsberg EM120. Frequency 12 kHz. Grid-cell size 5 m. (a) The entire fjord system. (b) Moraine and submarine slide complex at Caamano Sound, showing bank of postglacial mud (A) and residual of unfailed sediment (B). Headwall scar, dashed line. Transport direction …

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Geological Society, London, Memoirs: 46 (1)
Geological Society, London, Memoirs
Volume 46
2016
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Landforms in a Pacific fjord system: Douglas Channel, British Columbia, Canada

J. Shaw and D. G. Lintern
Geological Society, London, Memoirs, 46, 81-82, 30 November 2016, https://doi.org/10.1144/M46.105
J. Shaw
1Geological Survey of Canada, Natural Resources Canada, PO Box 1006, Dartmouth, Nova Scotia B2Y 4A2, Canada
  • Find this author on Google Scholar
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  • For correspondence: John.Shaw@canada.ca
D. G. Lintern
2Geological Survey of Canada, Institute of Ocean Sciences, 9860 West Saanich Road, Sidney, British Columbia V8L 4B2, Canada
  • Find this author on Google Scholar
  • Find this author on PubMed
  • Search for this author on this site

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Landforms in a Pacific fjord system: Douglas Channel, British Columbia, Canada

J. Shaw and D. G. Lintern
Geological Society, London, Memoirs, 46, 81-82, 30 November 2016, https://doi.org/10.1144/M46.105
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