Mapping and dating Late Holocene advances of Nansenbreen on Erdmannflya, Svalbard
Arctic temperatures are rising twice as fast as global temperatures. Consequently, understanding theeffect of this change on glacial dynamics and sea-level variations is of critical importance. The high-Arcticarchipelago of Svalbard is a unique site to study ice marginal landforms and their paleo-en...
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Stockholms universitet, Institutionen för naturgeografi
2021
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ftstockholmuniv:oai:DiVA.org:su-201077 2023-05-15T15:11:10+02:00 Mapping and dating Late Holocene advances of Nansenbreen on Erdmannflya, Svalbard Missana, Amandine F. J. M. 2021 application/pdf http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-201077 eng eng Stockholms universitet, Institutionen för naturgeografi http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-201077 info:eu-repo/semantics/openAccess Glacial geology sedimentology geomorphology sea-level radiocarbon dating Natural Sciences Naturvetenskap Earth and Related Environmental Sciences Geovetenskap och miljövetenskap Geology Geologi Physical Geography Naturgeografi Student thesis info:eu-repo/semantics/bachelorThesis text 2021 ftstockholmuniv 2023-02-23T21:43:41Z Arctic temperatures are rising twice as fast as global temperatures. Consequently, understanding theeffect of this change on glacial dynamics and sea-level variations is of critical importance. The high-Arcticarchipelago of Svalbard is a unique site to study ice marginal landforms and their paleo-environmentalimplications and to link Holocene climate and glacial variations. This study maps and age dates themoraine complex of Nansenbreen, a glacier terminating in the fjord of Isfjorden, in Borebukta north ofErdmannflya lowland. This reconstruction aims to determine the processes of formation of the morainecomplex and its implications for sea-level, glacial activity and Late Holocene climate reconstruction andmodelling. A sedimentological and landform map is therefore produced, using aerial images and fieldobservations. The map is coupled with radiocarbon dating of moraine deposits. Thereby, two moraines are differentiated. The most ice-distal moraine is interpreted as marking themaximum extent of Nansenbreen. Both moraines present features suggesting that they were glaciotectonisedthrough englacial-thrusting during surge events. Radiocarbon dates allow to establish a maximumconstraining age of 750 +/- 50 years BP for the maximum extent of Nansenbreen. This age correspondsto the Medieval Warm Period, an epoch marked by warm climate conditions. Hence, it is thoughtthat Nansenbreen underwent a surge triggered by influxes of warm Atlantic ocean currents into Isfjorden.Finally, the mapping shows that the moraines formed after a regression undergone by the wholeErdmannflya lowland. Erdmannflya therefore represents a suitable study site for sea-level studies. Svalbard Holocene Elucidation of Raised Beach Emergence and Timing (SHERBET) Bachelor Thesis Arctic glacier Isfjord* Isfjorden Svalbard Stockholm University: Publications (DiVA) Arctic Borebukta ENVELOPE(14.323,14.323,78.354,78.354) Erdmannflya ENVELOPE(14.187,14.187,78.312,78.312) Nansenbreen ENVELOPE(14.011,14.011,78.357,78.357) Raised Beach ENVELOPE(163.783,163.783,-74.983,-74.983) Svalbard |
institution |
Open Polar |
collection |
Stockholm University: Publications (DiVA) |
op_collection_id |
ftstockholmuniv |
language |
English |
topic |
Glacial geology sedimentology geomorphology sea-level radiocarbon dating Natural Sciences Naturvetenskap Earth and Related Environmental Sciences Geovetenskap och miljövetenskap Geology Geologi Physical Geography Naturgeografi |
spellingShingle |
Glacial geology sedimentology geomorphology sea-level radiocarbon dating Natural Sciences Naturvetenskap Earth and Related Environmental Sciences Geovetenskap och miljövetenskap Geology Geologi Physical Geography Naturgeografi Missana, Amandine F. J. M. Mapping and dating Late Holocene advances of Nansenbreen on Erdmannflya, Svalbard |
topic_facet |
Glacial geology sedimentology geomorphology sea-level radiocarbon dating Natural Sciences Naturvetenskap Earth and Related Environmental Sciences Geovetenskap och miljövetenskap Geology Geologi Physical Geography Naturgeografi |
description |
Arctic temperatures are rising twice as fast as global temperatures. Consequently, understanding theeffect of this change on glacial dynamics and sea-level variations is of critical importance. The high-Arcticarchipelago of Svalbard is a unique site to study ice marginal landforms and their paleo-environmentalimplications and to link Holocene climate and glacial variations. This study maps and age dates themoraine complex of Nansenbreen, a glacier terminating in the fjord of Isfjorden, in Borebukta north ofErdmannflya lowland. This reconstruction aims to determine the processes of formation of the morainecomplex and its implications for sea-level, glacial activity and Late Holocene climate reconstruction andmodelling. A sedimentological and landform map is therefore produced, using aerial images and fieldobservations. The map is coupled with radiocarbon dating of moraine deposits. Thereby, two moraines are differentiated. The most ice-distal moraine is interpreted as marking themaximum extent of Nansenbreen. Both moraines present features suggesting that they were glaciotectonisedthrough englacial-thrusting during surge events. Radiocarbon dates allow to establish a maximumconstraining age of 750 +/- 50 years BP for the maximum extent of Nansenbreen. This age correspondsto the Medieval Warm Period, an epoch marked by warm climate conditions. Hence, it is thoughtthat Nansenbreen underwent a surge triggered by influxes of warm Atlantic ocean currents into Isfjorden.Finally, the mapping shows that the moraines formed after a regression undergone by the wholeErdmannflya lowland. Erdmannflya therefore represents a suitable study site for sea-level studies. Svalbard Holocene Elucidation of Raised Beach Emergence and Timing (SHERBET) |
format |
Bachelor Thesis |
author |
Missana, Amandine F. J. M. |
author_facet |
Missana, Amandine F. J. M. |
author_sort |
Missana, Amandine F. J. M. |
title |
Mapping and dating Late Holocene advances of Nansenbreen on Erdmannflya, Svalbard |
title_short |
Mapping and dating Late Holocene advances of Nansenbreen on Erdmannflya, Svalbard |
title_full |
Mapping and dating Late Holocene advances of Nansenbreen on Erdmannflya, Svalbard |
title_fullStr |
Mapping and dating Late Holocene advances of Nansenbreen on Erdmannflya, Svalbard |
title_full_unstemmed |
Mapping and dating Late Holocene advances of Nansenbreen on Erdmannflya, Svalbard |
title_sort |
mapping and dating late holocene advances of nansenbreen on erdmannflya, svalbard |
publisher |
Stockholms universitet, Institutionen för naturgeografi |
publishDate |
2021 |
url |
http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-201077 |
long_lat |
ENVELOPE(14.323,14.323,78.354,78.354) ENVELOPE(14.187,14.187,78.312,78.312) ENVELOPE(14.011,14.011,78.357,78.357) ENVELOPE(163.783,163.783,-74.983,-74.983) |
geographic |
Arctic Borebukta Erdmannflya Nansenbreen Raised Beach Svalbard |
geographic_facet |
Arctic Borebukta Erdmannflya Nansenbreen Raised Beach Svalbard |
genre |
Arctic glacier Isfjord* Isfjorden Svalbard |
genre_facet |
Arctic glacier Isfjord* Isfjorden Svalbard |
op_relation |
http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-201077 |
op_rights |
info:eu-repo/semantics/openAccess |
_version_ |
1766342072927780864 |