Retarded deglaciation of north-Spitsbergen fjords during the last glacial – an example of bathymetric controls on the dynamics of retreating glaciers
North and west Spitsbergen fjords acted as pathways for fast-flowing ice streams during the last glacial (e.g. Ottesen et al., 2005). The deglaciation of west Spitsbergen fjords occurred stepwise and the ice retreat terminated around 11,200 cal. years BP (calendar years before the present; e.g. Forw...
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Geophysical Research Abstracts
2012
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ftawi:oai:epic.awi.de:32136 2023-05-15T15:33:54+02:00 Retarded deglaciation of north-Spitsbergen fjords during the last glacial – an example of bathymetric controls on the dynamics of retreating glaciers Forwick, Matthias Vorren, Tore O. Hass, H. Christian Vogt, Christoph 2012 https://epic.awi.de/id/eprint/32136/ https://hdl.handle.net/10013/epic.40785 unknown Geophysical Research Abstracts Forwick, M. , Vorren, T. O. , Hass, H. C. orcid:0000-0003-2649-6828 and Vogt, C. (2012) Retarded deglaciation of north-Spitsbergen fjords during the last glacial – an example of bathymetric controls on the dynamics of retreating glaciers , American Geophysical Union Fall Meeting, San Francisco, 3 December 2012 - 7 December 2012 . hdl:10013/epic.40785 EPIC3American Geophysical Union Fall Meeting, San Francisco, 2012-12-03-2012-12-07Geophysical Research Abstracts Conference notRev 2012 ftawi 2022-10-02T23:12:31Z North and west Spitsbergen fjords acted as pathways for fast-flowing ice streams during the last glacial (e.g. Ottesen et al., 2005). The deglaciation of west Spitsbergen fjords occurred stepwise and the ice retreat terminated around 11,200 cal. years BP (calendar years before the present; e.g. Forwick & Vorren, 2009, 2011, and references therein; Baeten et al., 2010). However, the deglaciation dynamics and chronology of north Spitsbergen fjords still remain poorly understood. We present swath-bathymetry, high-resolution seismic data and two sediment cores from the approx. 110 km long, N-S oriented Wijdefjorden-Austfjorden fjord system, the largest fjord system on northern Spitsbergen. The data indicate that – as in the fjords on west Spitsbergen – multiple halts and/or readvances interrupted the retreat of the ice front during the final phase of the last glacial. However, even though the study area and several west Spitsbergen fjords are fed by the same glacier source (the ice field Lomonosovfonna), the final deglaciation of Wijdefjorden-Austfjorden took place after 9300 cal. years BP, i.e. at least approx. 2000 years later than in the west. We assume that the retarded deglaciation in the north is mainly related to the fjord bathymetry, i.e. a more than 35 km wide and up to 60 m high area in the central parts of the study area (approx. 45 km beyond the present fjord head) that acted as pinning point for the grounded glacier. Multiple, relatively large and partly stacked moraine ridges and sediment wedges are suggested to reflected that the ice front retreated slowly across this shallow area and that repeated readvances interrupted this retreat. The absence of larger sediment wedges in the deeper parts between the shallow area and the fjord head may indicate that the final retreat occurred relatively rapid. References: Baeten, N.J., Forwick, M., Vogt, C. & Vorren, T.O., 2010. Late Weichselian and Holocene sedimentary environments and glacial activity in Billefjorden, Svalbard. In: Howe, J.A., Austin, ... Conference Object Austfjord* Billefjorden glacier Svalbard Wijdefjord* Spitsbergen Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Svalbard Austin Billefjorden ENVELOPE(16.417,16.417,78.563,78.563) Lomonosovfonna ENVELOPE(17.663,17.663,78.774,78.774) Wijdefjorden ENVELOPE(15.569,15.569,79.543,79.543) Austfjorden ENVELOPE(16.234,16.234,79.010,79.010) |
institution |
Open Polar |
collection |
Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
op_collection_id |
ftawi |
language |
unknown |
description |
North and west Spitsbergen fjords acted as pathways for fast-flowing ice streams during the last glacial (e.g. Ottesen et al., 2005). The deglaciation of west Spitsbergen fjords occurred stepwise and the ice retreat terminated around 11,200 cal. years BP (calendar years before the present; e.g. Forwick & Vorren, 2009, 2011, and references therein; Baeten et al., 2010). However, the deglaciation dynamics and chronology of north Spitsbergen fjords still remain poorly understood. We present swath-bathymetry, high-resolution seismic data and two sediment cores from the approx. 110 km long, N-S oriented Wijdefjorden-Austfjorden fjord system, the largest fjord system on northern Spitsbergen. The data indicate that – as in the fjords on west Spitsbergen – multiple halts and/or readvances interrupted the retreat of the ice front during the final phase of the last glacial. However, even though the study area and several west Spitsbergen fjords are fed by the same glacier source (the ice field Lomonosovfonna), the final deglaciation of Wijdefjorden-Austfjorden took place after 9300 cal. years BP, i.e. at least approx. 2000 years later than in the west. We assume that the retarded deglaciation in the north is mainly related to the fjord bathymetry, i.e. a more than 35 km wide and up to 60 m high area in the central parts of the study area (approx. 45 km beyond the present fjord head) that acted as pinning point for the grounded glacier. Multiple, relatively large and partly stacked moraine ridges and sediment wedges are suggested to reflected that the ice front retreated slowly across this shallow area and that repeated readvances interrupted this retreat. The absence of larger sediment wedges in the deeper parts between the shallow area and the fjord head may indicate that the final retreat occurred relatively rapid. References: Baeten, N.J., Forwick, M., Vogt, C. & Vorren, T.O., 2010. Late Weichselian and Holocene sedimentary environments and glacial activity in Billefjorden, Svalbard. In: Howe, J.A., Austin, ... |
format |
Conference Object |
author |
Forwick, Matthias Vorren, Tore O. Hass, H. Christian Vogt, Christoph |
spellingShingle |
Forwick, Matthias Vorren, Tore O. Hass, H. Christian Vogt, Christoph Retarded deglaciation of north-Spitsbergen fjords during the last glacial – an example of bathymetric controls on the dynamics of retreating glaciers |
author_facet |
Forwick, Matthias Vorren, Tore O. Hass, H. Christian Vogt, Christoph |
author_sort |
Forwick, Matthias |
title |
Retarded deglaciation of north-Spitsbergen fjords during the last glacial – an example of bathymetric controls on the dynamics of retreating glaciers |
title_short |
Retarded deglaciation of north-Spitsbergen fjords during the last glacial – an example of bathymetric controls on the dynamics of retreating glaciers |
title_full |
Retarded deglaciation of north-Spitsbergen fjords during the last glacial – an example of bathymetric controls on the dynamics of retreating glaciers |
title_fullStr |
Retarded deglaciation of north-Spitsbergen fjords during the last glacial – an example of bathymetric controls on the dynamics of retreating glaciers |
title_full_unstemmed |
Retarded deglaciation of north-Spitsbergen fjords during the last glacial – an example of bathymetric controls on the dynamics of retreating glaciers |
title_sort |
retarded deglaciation of north-spitsbergen fjords during the last glacial – an example of bathymetric controls on the dynamics of retreating glaciers |
publisher |
Geophysical Research Abstracts |
publishDate |
2012 |
url |
https://epic.awi.de/id/eprint/32136/ https://hdl.handle.net/10013/epic.40785 |
long_lat |
ENVELOPE(16.417,16.417,78.563,78.563) ENVELOPE(17.663,17.663,78.774,78.774) ENVELOPE(15.569,15.569,79.543,79.543) ENVELOPE(16.234,16.234,79.010,79.010) |
geographic |
Svalbard Austin Billefjorden Lomonosovfonna Wijdefjorden Austfjorden |
geographic_facet |
Svalbard Austin Billefjorden Lomonosovfonna Wijdefjorden Austfjorden |
genre |
Austfjord* Billefjorden glacier Svalbard Wijdefjord* Spitsbergen |
genre_facet |
Austfjord* Billefjorden glacier Svalbard Wijdefjord* Spitsbergen |
op_source |
EPIC3American Geophysical Union Fall Meeting, San Francisco, 2012-12-03-2012-12-07Geophysical Research Abstracts |
op_relation |
Forwick, M. , Vorren, T. O. , Hass, H. C. orcid:0000-0003-2649-6828 and Vogt, C. (2012) Retarded deglaciation of north-Spitsbergen fjords during the last glacial – an example of bathymetric controls on the dynamics of retreating glaciers , American Geophysical Union Fall Meeting, San Francisco, 3 December 2012 - 7 December 2012 . hdl:10013/epic.40785 |
_version_ |
1766364497828642816 |