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Tsunamis and tectonic deformation at the northern Cascadia margin: a 3000-year record from Deserted Lake, Vancouver Island, British Columbia, Canada

Department of Geography and Institute for Quaternary Research, Simon Fraser University, Burnaby, BC, V5A 1S6, Canada

J. -P. Guilbault

BRAQ-Stratigraphie, 10555 Meilleur, Montréal, Qc, H3L 3K4, Canada

J. J. Clague

Earth Sciences and Institute for Quaternary Research, Simon Fraser University, Burnaby, BC, V5A 1S6, Canada

P. T. Bobrowsky

Geological Survey Branch, Ministry of Energy, Mines and Resources, 1810 Blanshard St, Victoria, BC, V8V 1X4, Canada

Three layers of sand occur within a sequence of muddy gyttja in a 3 m core recovered from Deserted Lake, which lies at the head of a fjord on the central west coast of Vancouver Island, British Columbia, Canada. The sedimentology and microfossil assemblages of these layers are consistent with deposition by tsunamis. Radiocarbon ages suggest that the tsunamis were generated by plate-boundary earthquakes at the Cascadia subduction zone about 2600, 1600 and 300 years ago. Diatom and protozoan contents of the gyttja layers indicate that relative sea level fell in the periods between tsunamis. The sea-level changes are probably a product of interseismic uplift of the North America plate margin. Post-tsunami diatom and protozoan assemblages are generally more marine than their pre-tsunami counterparts, suggesting that the study site subsided during earth quakes. Estimates of interseismic and coseismic deformation during one earthquake cycle indicate that less than half of the interseismic uplift was recovered during the earthquake, leading to cumulative, or permanent, uplift of the area.

Key Words: Cascadia subduction zone • diatoms • foraminifers • relative sea level • tectonics • tsunamis • British • Columbia • late Holocene

The Holocene, Vol. 10, No. 4, 429-439 (2000)
DOI: 10.1191/095968300666654539


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