The Vatn landslide, Skagafjördur, northern Iceland: evidence of an early Holocene paraglacial crisis and impact on further slope development
International audience The Vatn landslide is of modest size (estimated to 830,000 m3), and the deposit exhibits poor spatial dispersion and longitudinal runout. Its location in the Skagafjördur fjord, Northern Iceland (65 57,337'N, 19 23,900'W), evidences slope post-glacial development in...
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ftunivbrest:oai:HAL:hal-00815642v1 2024-05-19T07:42:39+00:00 The Vatn landslide, Skagafjördur, northern Iceland: evidence of an early Holocene paraglacial crisis and impact on further slope development Decaulne, Armelle Mercier, Denis Cossart, Etienne Thierry, Feuillet Jónsson, Helgi Páll Sæmundsson, Þorsteinn Littoral, Environnement, Télédétection, Géomatique (LETG - Nantes) Université de Caen Normandie (UNICAEN) Normandie Université (NU)-Normandie Université (NU)-École Pratique des Hautes Études (EPHE) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Brest (UBO)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-Institut de Géographie et d'Aménagement Régional de l'Université de Nantes (IGARUN) Université de Nantes (UN)-Université de Nantes (UN) Pôle de recherche pour l'organisation et la diffusion de l'information géographique (PRODIG) Université Paris 1 Panthéon-Sorbonne (UP1)-Institut de Recherche pour le Développement (IRD)-École Pratique des Hautes Études (EPHE) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université Paris-Sorbonne (UP4)-Université Paris Diderot - Paris 7 (UPD7)-Centre National de la Recherche Scientifique (CNRS) Náttúrustofa Norðurlands vestra (NNv) Ríkisins, Sveitafélag Skagafjarðar Vienne, Austria 2013-04-07 https://hal.science/hal-00815642 en eng HAL CCSD hal-00815642 https://hal.science/hal-00815642 EGU General Assembly 2013 https://hal.science/hal-00815642 EGU General Assembly 2013, Apr 2013, Vienne, Austria. p.4169 Mass movement paraglacial geomorphology Iceland déglaciation [SDU.STU.GM]Sciences of the Universe [physics]/Earth Sciences/Geomorphology [SHS.GEO]Humanities and Social Sciences/Geography info:eu-repo/semantics/conferenceObject Conference papers 2013 ftunivbrest 2024-04-25T16:51:15Z International audience The Vatn landslide is of modest size (estimated to 830,000 m3), and the deposit exhibits poor spatial dispersion and longitudinal runout. Its location in the Skagafjördur fjord, Northern Iceland (65 57,337'N, 19 23,900'W), evidences slope post-glacial development in the area. The interest of this landslide is found lower contact: the downslope part of the landslide deposit bumps on a stripe of raised beach, trapping a flat area at its northernmost boundary. The contact between the slide and the beach is open by a deep anthropogenic ditch. Analysis of (i) stratigraphic sections along the ditch, (ii) log section openings in the flat area at the slide contact and (iii) onto the slide deposit, offer numerous dating elements. Lower pits are rich in organic material and tephra layers (the oldest one, H4, is dated to 4,260 cal. BP), while the upper pit revealed little accumulation over the slide deposit surface, exhibiting only tephra layers separated by poor organic units. The combination of radiometric method and geochemical analysis of the tephra layers results in a good time constrain for the landslide occurrence, before 9070 86 cal. BP and 8677 181 cal. BP (oldest tree remnants). Such results reinforce the hypothesis of a major paraglacial geomorphologic crisis at the early Holocene time, leading to numerous slope failures following the last glacial maximum retreat (Mercier et al., in press, The Holocene). The presence of the raised beach at the lower contact with the landslide seems to indicate an occurrence later than 11,000-11,400 cal. BP (intrapolated age of the raised beaches located at 22-31 m a.s.l.), and suggests that isostatic rebound is a relevant triggering factor (Cossart et al, in press, Earth Surface Processes and Landforms). The lower pit section encompasses the full Holocene period, exhibiting a succession of organic layers and a very poor accumulation in minerogenic material. Those 2 m (i) document the palaeoenvironmental settings throughout the Holocene with ... Conference Object Iceland Université de Bretagne Occidentale: HAL |
institution |
Open Polar |
collection |
Université de Bretagne Occidentale: HAL |
op_collection_id |
ftunivbrest |
language |
English |
topic |
Mass movement paraglacial geomorphology Iceland déglaciation [SDU.STU.GM]Sciences of the Universe [physics]/Earth Sciences/Geomorphology [SHS.GEO]Humanities and Social Sciences/Geography |
spellingShingle |
Mass movement paraglacial geomorphology Iceland déglaciation [SDU.STU.GM]Sciences of the Universe [physics]/Earth Sciences/Geomorphology [SHS.GEO]Humanities and Social Sciences/Geography Decaulne, Armelle Mercier, Denis Cossart, Etienne Thierry, Feuillet Jónsson, Helgi Páll Sæmundsson, Þorsteinn The Vatn landslide, Skagafjördur, northern Iceland: evidence of an early Holocene paraglacial crisis and impact on further slope development |
topic_facet |
Mass movement paraglacial geomorphology Iceland déglaciation [SDU.STU.GM]Sciences of the Universe [physics]/Earth Sciences/Geomorphology [SHS.GEO]Humanities and Social Sciences/Geography |
description |
International audience The Vatn landslide is of modest size (estimated to 830,000 m3), and the deposit exhibits poor spatial dispersion and longitudinal runout. Its location in the Skagafjördur fjord, Northern Iceland (65 57,337'N, 19 23,900'W), evidences slope post-glacial development in the area. The interest of this landslide is found lower contact: the downslope part of the landslide deposit bumps on a stripe of raised beach, trapping a flat area at its northernmost boundary. The contact between the slide and the beach is open by a deep anthropogenic ditch. Analysis of (i) stratigraphic sections along the ditch, (ii) log section openings in the flat area at the slide contact and (iii) onto the slide deposit, offer numerous dating elements. Lower pits are rich in organic material and tephra layers (the oldest one, H4, is dated to 4,260 cal. BP), while the upper pit revealed little accumulation over the slide deposit surface, exhibiting only tephra layers separated by poor organic units. The combination of radiometric method and geochemical analysis of the tephra layers results in a good time constrain for the landslide occurrence, before 9070 86 cal. BP and 8677 181 cal. BP (oldest tree remnants). Such results reinforce the hypothesis of a major paraglacial geomorphologic crisis at the early Holocene time, leading to numerous slope failures following the last glacial maximum retreat (Mercier et al., in press, The Holocene). The presence of the raised beach at the lower contact with the landslide seems to indicate an occurrence later than 11,000-11,400 cal. BP (intrapolated age of the raised beaches located at 22-31 m a.s.l.), and suggests that isostatic rebound is a relevant triggering factor (Cossart et al, in press, Earth Surface Processes and Landforms). The lower pit section encompasses the full Holocene period, exhibiting a succession of organic layers and a very poor accumulation in minerogenic material. Those 2 m (i) document the palaeoenvironmental settings throughout the Holocene with ... |
author2 |
Littoral, Environnement, Télédétection, Géomatique (LETG - Nantes) Université de Caen Normandie (UNICAEN) Normandie Université (NU)-Normandie Université (NU)-École Pratique des Hautes Études (EPHE) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Brest (UBO)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-Institut de Géographie et d'Aménagement Régional de l'Université de Nantes (IGARUN) Université de Nantes (UN)-Université de Nantes (UN) Pôle de recherche pour l'organisation et la diffusion de l'information géographique (PRODIG) Université Paris 1 Panthéon-Sorbonne (UP1)-Institut de Recherche pour le Développement (IRD)-École Pratique des Hautes Études (EPHE) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université Paris-Sorbonne (UP4)-Université Paris Diderot - Paris 7 (UPD7)-Centre National de la Recherche Scientifique (CNRS) Náttúrustofa Norðurlands vestra (NNv) Ríkisins, Sveitafélag Skagafjarðar |
format |
Conference Object |
author |
Decaulne, Armelle Mercier, Denis Cossart, Etienne Thierry, Feuillet Jónsson, Helgi Páll Sæmundsson, Þorsteinn |
author_facet |
Decaulne, Armelle Mercier, Denis Cossart, Etienne Thierry, Feuillet Jónsson, Helgi Páll Sæmundsson, Þorsteinn |
author_sort |
Decaulne, Armelle |
title |
The Vatn landslide, Skagafjördur, northern Iceland: evidence of an early Holocene paraglacial crisis and impact on further slope development |
title_short |
The Vatn landslide, Skagafjördur, northern Iceland: evidence of an early Holocene paraglacial crisis and impact on further slope development |
title_full |
The Vatn landslide, Skagafjördur, northern Iceland: evidence of an early Holocene paraglacial crisis and impact on further slope development |
title_fullStr |
The Vatn landslide, Skagafjördur, northern Iceland: evidence of an early Holocene paraglacial crisis and impact on further slope development |
title_full_unstemmed |
The Vatn landslide, Skagafjördur, northern Iceland: evidence of an early Holocene paraglacial crisis and impact on further slope development |
title_sort |
vatn landslide, skagafjördur, northern iceland: evidence of an early holocene paraglacial crisis and impact on further slope development |
publisher |
HAL CCSD |
publishDate |
2013 |
url |
https://hal.science/hal-00815642 |
op_coverage |
Vienne, Austria |
genre |
Iceland |
genre_facet |
Iceland |
op_source |
EGU General Assembly 2013 https://hal.science/hal-00815642 EGU General Assembly 2013, Apr 2013, Vienne, Austria. p.4169 |
op_relation |
hal-00815642 https://hal.science/hal-00815642 |
_version_ |
1799482355849625600 |