The Seven Islands, Svalbard: glaciation at the margin
On the Seven Islands, north of Nordaustlandet, Svalbard, decreasing snow cover has made previously inaccessible stratigraphic sections in coastal cliffs possible to investigate. Sections on two of the islands, Phippsøya and Parryøya, reveal mainly raised marine deposits, representing one or more coa...
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ftulundlup:oai:lup.lub.lu.se:b9d8d74e-69ee-412f-89a6-b78b29e05d23 2023-05-15T15:38:58+02:00 The Seven Islands, Svalbard: glaciation at the margin Alexanderson, Helena Schomacker, Anders Farnsworth, Wesley R. Noormets, Riko Kirchner, Nina Ingolfsson, Olafur 2018 https://lup.lub.lu.se/record/b9d8d74e-69ee-412f-89a6-b78b29e05d23 eng eng https://lup.lub.lu.se/record/b9d8d74e-69ee-412f-89a6-b78b29e05d23 Geology contributiontoconference/abstract info:eu-repo/semantics/conferenceObject text 2018 ftulundlup 2023-02-01T23:37:11Z On the Seven Islands, north of Nordaustlandet, Svalbard, decreasing snow cover has made previously inaccessible stratigraphic sections in coastal cliffs possible to investigate. Sections on two of the islands, Phippsøya and Parryøya, reveal mainly raised marine deposits, representing one or more coarsening upward sequences (emergence cycles) at each site, which in turn imply preceding regional glaciations (cf. Alexanderson et al. in press). Optically stimulated luminescence (OSL) ages are pending but radiocarbon (14C) ages and correlation to a previously studied site on Phippsøya (Forman and Ingólfsson 2000) suggest at least two events that occurred during the late Weichselian-early Holocene and prior to 40 14C ka BP, respectively. These results, along with observations of postglacial land uplift and of transport of erratic boulders to the islands, provide information on the glacial history and dynamics of an area close to the margin of the Svalbard-Barents Sea ice sheet.ReferencesAlexanderson, H., Henriksen, M., Ryen. H.T., Landvik, J.Y. and Peterson, G. in press. 200 ka of glacial events in NW Svalbard: An emergence cycle facies model and regional correlations. arktos. Forman, S.L. and Ingólfsson, Ó, 2000. Late Weichselian glacial history and postglacial emergence of Phippsøya, Sjuøyane, northern Svalbard: a comparison of modelled and empirical estimates of a glacial-rebound hinge line. Boreas 29, 16-25. Conference Object Barents Sea Nordaustlandet Parryøya Phippsøya Sea ice Sjuøyane Svalbard Lund University Publications (LUP) Barents Sea Boreas ENVELOPE(-3.933,-3.933,-71.300,-71.300) Nordaustlandet ENVELOPE(22.400,22.400,79.800,79.800) Parryøya ENVELOPE(20.694,20.694,80.650,80.650) Phippsøya ENVELOPE(20.793,20.793,80.709,80.709) Ryen ENVELOPE(15.401,15.401,68.007,68.007) Sjuøyane ENVELOPE(20.503,20.503,80.729,80.729) Svalbard |
institution |
Open Polar |
collection |
Lund University Publications (LUP) |
op_collection_id |
ftulundlup |
language |
English |
topic |
Geology |
spellingShingle |
Geology Alexanderson, Helena Schomacker, Anders Farnsworth, Wesley R. Noormets, Riko Kirchner, Nina Ingolfsson, Olafur The Seven Islands, Svalbard: glaciation at the margin |
topic_facet |
Geology |
description |
On the Seven Islands, north of Nordaustlandet, Svalbard, decreasing snow cover has made previously inaccessible stratigraphic sections in coastal cliffs possible to investigate. Sections on two of the islands, Phippsøya and Parryøya, reveal mainly raised marine deposits, representing one or more coarsening upward sequences (emergence cycles) at each site, which in turn imply preceding regional glaciations (cf. Alexanderson et al. in press). Optically stimulated luminescence (OSL) ages are pending but radiocarbon (14C) ages and correlation to a previously studied site on Phippsøya (Forman and Ingólfsson 2000) suggest at least two events that occurred during the late Weichselian-early Holocene and prior to 40 14C ka BP, respectively. These results, along with observations of postglacial land uplift and of transport of erratic boulders to the islands, provide information on the glacial history and dynamics of an area close to the margin of the Svalbard-Barents Sea ice sheet.ReferencesAlexanderson, H., Henriksen, M., Ryen. H.T., Landvik, J.Y. and Peterson, G. in press. 200 ka of glacial events in NW Svalbard: An emergence cycle facies model and regional correlations. arktos. Forman, S.L. and Ingólfsson, Ó, 2000. Late Weichselian glacial history and postglacial emergence of Phippsøya, Sjuøyane, northern Svalbard: a comparison of modelled and empirical estimates of a glacial-rebound hinge line. Boreas 29, 16-25. |
format |
Conference Object |
author |
Alexanderson, Helena Schomacker, Anders Farnsworth, Wesley R. Noormets, Riko Kirchner, Nina Ingolfsson, Olafur |
author_facet |
Alexanderson, Helena Schomacker, Anders Farnsworth, Wesley R. Noormets, Riko Kirchner, Nina Ingolfsson, Olafur |
author_sort |
Alexanderson, Helena |
title |
The Seven Islands, Svalbard: glaciation at the margin |
title_short |
The Seven Islands, Svalbard: glaciation at the margin |
title_full |
The Seven Islands, Svalbard: glaciation at the margin |
title_fullStr |
The Seven Islands, Svalbard: glaciation at the margin |
title_full_unstemmed |
The Seven Islands, Svalbard: glaciation at the margin |
title_sort |
seven islands, svalbard: glaciation at the margin |
publishDate |
2018 |
url |
https://lup.lub.lu.se/record/b9d8d74e-69ee-412f-89a6-b78b29e05d23 |
long_lat |
ENVELOPE(-3.933,-3.933,-71.300,-71.300) ENVELOPE(22.400,22.400,79.800,79.800) ENVELOPE(20.694,20.694,80.650,80.650) ENVELOPE(20.793,20.793,80.709,80.709) ENVELOPE(15.401,15.401,68.007,68.007) ENVELOPE(20.503,20.503,80.729,80.729) |
geographic |
Barents Sea Boreas Nordaustlandet Parryøya Phippsøya Ryen Sjuøyane Svalbard |
geographic_facet |
Barents Sea Boreas Nordaustlandet Parryøya Phippsøya Ryen Sjuøyane Svalbard |
genre |
Barents Sea Nordaustlandet Parryøya Phippsøya Sea ice Sjuøyane Svalbard |
genre_facet |
Barents Sea Nordaustlandet Parryøya Phippsøya Sea ice Sjuøyane Svalbard |
op_relation |
https://lup.lub.lu.se/record/b9d8d74e-69ee-412f-89a6-b78b29e05d23 |
_version_ |
1766370417311744000 |