Holocene moraine chronology, Spitsbergen, Svalbard: lichenometric evidence for multiple Neoglacial advances in the Arctic
Late Holocene (Neoglacial) moraines occurring within 1 or 2 km of present glacier margins are prominent features in the forefields of Spitsbergen glaciers. 'Little Ice Age' moraines are typically the most extensive and best preserved; moraines of older Holocene advances are much less commo...
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Online Access: | http://dx.doi.org/10.1177/095968369300300204 http://journals.sagepub.com/doi/pdf/10.1177/095968369300300204 |
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crsagepubl:10.1177/095968369300300204 2024-06-23T07:50:25+00:00 Holocene moraine chronology, Spitsbergen, Svalbard: lichenometric evidence for multiple Neoglacial advances in the Arctic Werner, A. 1993 http://dx.doi.org/10.1177/095968369300300204 http://journals.sagepub.com/doi/pdf/10.1177/095968369300300204 en eng SAGE Publications http://journals.sagepub.com/page/policies/text-and-data-mining-license The Holocene volume 3, issue 2, page 128-137 ISSN 0959-6836 1477-0911 journal-article 1993 crsagepubl https://doi.org/10.1177/095968369300300204 2024-06-04T06:28:22Z Late Holocene (Neoglacial) moraines occurring within 1 or 2 km of present glacier margins are prominent features in the forefields of Spitsbergen glaciers. 'Little Ice Age' moraines are typically the most extensive and best preserved; moraines of older Holocene advances are much less common. Where observed, older moraines occur as moraine remnants and provide irrefutable evidence of earlier Neoglacial advances. The fragmentary moraine record indicates two 'Little Ice Age' advances and two older Neoglacial advances. Lichenometry provides calibrated ages for periods of moraine stabilization. The oldest moraines stabilized by ca. 1500 years ago, and a second group of moraines stabilized by ca. 1000 years ago. 'Little Ice Age' moraines were deposited during two periods: an early group of moraines stabilized ca. 650 years ago and a later group during the last several centuries. The proposed moraine chronology compares well with other proxy climate records on Spitsbergen and with moraine records from areas bordering the Norwegian-Greenland Sea. Article in Journal/Newspaper Arctic glacier glacier Greenland Greenland Sea Svalbard Spitsbergen SAGE Publications Arctic Greenland Svalbard The Holocene 3 2 128 137 |
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Open Polar |
collection |
SAGE Publications |
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crsagepubl |
language |
English |
description |
Late Holocene (Neoglacial) moraines occurring within 1 or 2 km of present glacier margins are prominent features in the forefields of Spitsbergen glaciers. 'Little Ice Age' moraines are typically the most extensive and best preserved; moraines of older Holocene advances are much less common. Where observed, older moraines occur as moraine remnants and provide irrefutable evidence of earlier Neoglacial advances. The fragmentary moraine record indicates two 'Little Ice Age' advances and two older Neoglacial advances. Lichenometry provides calibrated ages for periods of moraine stabilization. The oldest moraines stabilized by ca. 1500 years ago, and a second group of moraines stabilized by ca. 1000 years ago. 'Little Ice Age' moraines were deposited during two periods: an early group of moraines stabilized ca. 650 years ago and a later group during the last several centuries. The proposed moraine chronology compares well with other proxy climate records on Spitsbergen and with moraine records from areas bordering the Norwegian-Greenland Sea. |
format |
Article in Journal/Newspaper |
author |
Werner, A. |
spellingShingle |
Werner, A. Holocene moraine chronology, Spitsbergen, Svalbard: lichenometric evidence for multiple Neoglacial advances in the Arctic |
author_facet |
Werner, A. |
author_sort |
Werner, A. |
title |
Holocene moraine chronology, Spitsbergen, Svalbard: lichenometric evidence for multiple Neoglacial advances in the Arctic |
title_short |
Holocene moraine chronology, Spitsbergen, Svalbard: lichenometric evidence for multiple Neoglacial advances in the Arctic |
title_full |
Holocene moraine chronology, Spitsbergen, Svalbard: lichenometric evidence for multiple Neoglacial advances in the Arctic |
title_fullStr |
Holocene moraine chronology, Spitsbergen, Svalbard: lichenometric evidence for multiple Neoglacial advances in the Arctic |
title_full_unstemmed |
Holocene moraine chronology, Spitsbergen, Svalbard: lichenometric evidence for multiple Neoglacial advances in the Arctic |
title_sort |
holocene moraine chronology, spitsbergen, svalbard: lichenometric evidence for multiple neoglacial advances in the arctic |
publisher |
SAGE Publications |
publishDate |
1993 |
url |
http://dx.doi.org/10.1177/095968369300300204 http://journals.sagepub.com/doi/pdf/10.1177/095968369300300204 |
geographic |
Arctic Greenland Svalbard |
geographic_facet |
Arctic Greenland Svalbard |
genre |
Arctic glacier glacier Greenland Greenland Sea Svalbard Spitsbergen |
genre_facet |
Arctic glacier glacier Greenland Greenland Sea Svalbard Spitsbergen |
op_source |
The Holocene volume 3, issue 2, page 128-137 ISSN 0959-6836 1477-0911 |
op_rights |
http://journals.sagepub.com/page/policies/text-and-data-mining-license |
op_doi |
https://doi.org/10.1177/095968369300300204 |
container_title |
The Holocene |
container_volume |
3 |
container_issue |
2 |
container_start_page |
128 |
op_container_end_page |
137 |
_version_ |
1802641315441147904 |