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Par Collection Par Auteur- CLAGUE, J.J. (2)
- GRIMM, K.A. (1)
- BENSON, B.E. (1)
- HUNTLEY, D.J. (1)
- Analyse isotopique ; British Columbia ; Canada ; Datation C 14 ; Granulométrie ; Ile ; Marais littoral ; Milieu humide ; Sable ; Stratigraphie ; Sédimentologie ; Séisme ; Tsunami ; Vancouver (1)
- British Columbia ; C 14 dating ; Canada ; Dating ; Earthquake ; Humid environment ; Methodology ; Sand ; Stratigraphic correlation ; Stratigraphy ; Tsunami ; United States of America ; Washington State (1)
- British Columbia ; C 14 dating ; Canada ; Earthquake ; Grain size distribution ; Humid environment ; Island ; Isotope analysis ; Sand ; Sedimentology ; Stratigraphy ; Tidal marsh ; Tsunami ; Vancouver (1)
- British Columbia ; Canada ; Corrélation stratigraphique ; Datation ; Datation C 14 ; Etats-Unis ; Milieu humide ; Méthodologie ; Sable ; Stratigraphie ; Séisme ; Tsunami ; Washington State (1)
- Tsunami deposits beneath tidal marshes on northwestern Vancouver Island, British Columbia
- Analyse isotopique ; British Columbia ; Canada ; Datation C 14 ; Granulométrie ; Ile ; Marais littoral ; Milieu humide ; Sable ; Stratigraphie ; Sédimentologie ; Séisme ; Tsunami ; Vancouver
- British Columbia ; C 14 dating ; Canada ; Earthquake ; Grain size distribution ; Humid environment ; Island ; Isotope analysis ; Sand ; Sedimentology ; Stratigraphy ; Tidal marsh ; Tsunami ; Vancouver
- The aim of this paper is to characterize tsunami deposits in Holocene peat at tidal marshes on northwestern Vancouver Island. The AA. studied the architecture, stratigraphy, and sedimentology of 2 sand sheets at Fair Harbour, Neroutsos Inlet
- [b1] Earth and Ocean Sciences, Univ. British Columbia, Vancouver, Canada
- before the tsunami. Historical records and radiocarbon dating show that the sand at each of the 3 sites, near Tofino and Port Alberni on Vancouver Island, is 150 to 400 yr old than the optical ages. These optical ages support the hypothesis
- that the Vancouver Island sands were deposited by a tsunami generated by a large earthquake on the Cascadia subduction zone about 300 yr ago.