Large-scale sedimentary bedforms and sediment dynamics on a glaciated tectonic continental shelf: Examples from the Pacific margin of Canada

• Published in: Continental shelf research Vol. 29; no. 5; pp. 796 - 806
• Main Authors: Barrie, J. Vaughn, Conway, Kim W., Picard, Kim, Greene, H. Gary
• Format: Journal Article
• Language: English
• Published: Elsevier Ltd 30-03-2009
• Subjects: Brackish; British Columbia; Marine; Multibeam bathymetry; Sediment dynamics; Subaqueous dunes; Wave-cut terraces; INE, North America, Georgia Strait; INE, Canada, British Columbia, Hecate Strait; Wave-cut terraces; Sediment dynamics; British Columbia; Subaqueous dunes; Multibeam bathymetry
• ISSN: 0278-4343; 1873-6955
• DOI: 10.1016/j.csr.2008.12.007

The Pacific margin of Canada has been subjected to tectonism, dramatic sea level change and vigorous storm and tidal energy since glacial times resulting in a complex seafloor. Extensive multibeam mapping of this shelf has provided an opportunity to understand how these processes have impacted sedimentology and morphology. Bathymetric restriction of the tidally dominated flow between the inland seas and the open Pacific has resulted in the development of very large subaqueous dune fields and terrace moats. For example, in the southern Strait of Georgia nearly symmetrical dunes with wavelengths between 100 and 300
m, dune heights up to 28
m, cover the seafloor in 170–210
m water depth. In northern Hecate Strait a 72
km
2 area of large 2D dunes occurs at the transition with Dixon Entrance which opens to the Pacific Ocean and steep (>10°) wave-cut terraces and drowned spits, a result of sea level changes during the Holocene, are now being undercut to generate moats 7
m deep, in a narrowing shelf trough. Currents, with velocities ranging between 0.2 and 2.2
m
s
−1, are dominated by semi-diurnal tidal streams that are continually modified by wind and estuarine circulation. There appears to be a clear association of grain size, water depth and flow velocity controlling the size of the subaqueous dunes.