Holocene relative sea level changes along the Seattle fault at Restoration Point, Washington
In their paleoenvironmental reconstruction for the Restoration Point Marsh, the AA. see no abrupt change in relative sea level (RSL) nearly as large as the uplift during the Seattle fault earthquake 1000 cal yr B.P. However, they do infer environmental changes that could represent smaller earthquakes or, alternatively, the opening and closing of a beach berm
Quaternaire marin ; Holocène ; Niveau marin ; Mouvement vertical ; Séisme ; Diatomée ; Paléo-environnement ; Biostratigraphie ; Datation C 14 ; Faille ; Salinité ; Etats-Unis ; Washington State ; Pacifique Nord
Marine quaternary ; Holocene ; Sea level ; Vertical movement ; Earthquake ; Diatom ; Palaeo-environment ; Biostratigraphy ; C 14 dating ; Fault ; Salinity ; United States of America ; Washington State ; North Pacific Ocean
Article of periodic
published at : Quaternary research / ISSN 0033-5894 / CODEN QRESAV
Editor : Elsevier, San Diego, CA - ETATS-UNIS (1970)
Millesime : 2000, vol. 54, no3 [pp. 384-393]
Bibliographic references : 32 ref.
Collation : Illustration ;
Anglais
INIST-CNRS, Cote INIST : 15739