The geological record of paleotsunamis striking Shikotan island, in the lesser Kurils, during holocene time View Full Text


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

2008-08

AUTHORS

N. G. Razzhigaeva, L. A. Ganzei, T. A. Grebennikova, A. A. Kharlamov, A. Ya. Ilyev, V. M. Kaistrenko

ABSTRACT

Paleotsunami remains have been studied in Middle/Late Holocene peat bogs and lacustrine deposits on Shikotan I. We determined the age of the events, the inundation areas, and the distance the tsunami waves traveled on shores of varying structures. The frequency of tsunami occurrence was nonuniform; these events were the most frequent in the middle of the Late Holocene. Data are provided for specific areas of the island’s coast, sequences have been identified containing numerous interbeds of tsunamigenic sand, which can be used as markers. The composition of the tsunamigenic sand has been analyzed to reveal its similarities with and differences to other coastal marine facies and to determine the sources of the material. These data could serve as a basis for compiling a highly detailed geological record of these events for the southern Kuril region during the last 6000 years. More... »

PAGES

262-277

References to SciGraph publications

Identifiers

URI

http://scigraph.springernature.com/pub.10.1134/s0742046308040040

DOI

http://dx.doi.org/10.1134/s0742046308040040

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1037163802


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136 Shirshov Institute of Oceanology, Russian Academy of Sciences, 117997, Moscow, Russia
137 rdf:type schema:Organization
138 https://www.grid.ac/institutes/grid.494538.7 schema:alternateName Institute of Marine Geology and Geophysics
139 schema:name Institute of Marine Geology and Geophysics, Far East Division, Russian Academy of Sciences, 693000, Yuzhno-Sakhalinsk, Russia
140 rdf:type schema:Organization
 




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