Are Icelandic rock-slope failures paraglacial? Age evaluation of seventeen rock-slope failures in the Skagafjörður area, based on geomorphological stacking, radiocarbon dating and tephrochronology

Autor: Mercier, Denis, Coquin, Julien, Feuillet, Thierry, Decaulne, Armelle, Cossart, Etienne, Jónsson, Helgi Pall, Sæmundsson, Þorstein

Publikováno v: In Geomorphology 1 November 2017 296:45-58

An Overview of Postglacial Sediment Records from Colluvial Accumulations in Northwestern and North Iceland

Autor: Decaulne, Armelle, Scemundsson, Porsteinn, Jónsson, Helgi Páll

Publikováno v: Arctic, Antarctic, and Alpine Research, 2009 Feb 01. 41(1), 37-47.

Externí odkaz: https://www.jstor.org/stable/40305854

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Impacts of post glacial rebound on landsliding at a regional scale in Northern Iceland (Skagafjörður): spatial distribution and mechanisms involved

Autor: Cossart, Etienne, Mercier, Denis, Decaulne, Armelle, Feuillet, Thierry, Jónsson, Helgi Páll, Sæmundsson, Þorsteinn

Publikováno v: Geomorphology and Sustainability, 8th IAG International Conference on Geomorphology
Geomorphology and Sustainability, 8th IAG International Conference on Geomorphology, Aug 2013, Paris, France. p. 628

International audience; Paraglaciation has often been considered as a main predisposing factor in landslide occurrence; its consequences have been particularly well identified at a fine scale (especially on bedrock jointing). However, the impacts of

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::10907f5b8ffb026bee596b97a8bdbde4
https://hal.archives-ouvertes.fr/hal-00859837

Impacts of post-glacial rebound on landslide spatial distribution at a regional scale in northern Iceland (Skagafjörður)

Autor: Cossart, Etienne, Mercier, Denis, Decaulne, Armelle, Feuillet, Thierry, Jónsson, Helgi Páll, Sæmundsson, Þorsteinn

Publikováno v: Earth Surface Processes and Landforms
Earth Surface Processes and Landforms, Wiley, 2013, 39 (3), p. 336-350. ⟨10.1002/esp.3450⟩

International audience; In de-glaciated areas, para-glaciation (i.e. the conditioning of landscapes by prior glaciation) has often been considered a major predisposing factor in landslide occurrence; its consequences have been particularly well ident

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::b9b1fed7ec69a4b67de0eac87726d200
https://hal.archives-ouvertes.fr/hal-00859798