Ice-cored drumlins at the surge-type glacier Bruarjokull, Iceland: a transitional-state landform
This paper presents data on a glacial landform that, to Our knowledge, has not previously been described in the literature: the ice-cored drumlin. The study area is the forefield of the surge-type glacier Bruarjokull at the northeastern margin of the Vatnajokull ice cap, Fast Iceland. Based on sedim...
Published in: | Journal of Quaternary Science |
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Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
John Wiley & Sons Inc.
2006
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Subjects: | |
Online Access: | https://lup.lub.lu.se/record/419389 https://doi.org/10.1002/jqs.949 |
_version_ | 1828690838545235968 |
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author | Schomacker, Anders Kruger, J Kjaer, Kurt |
author_facet | Schomacker, Anders Kruger, J Kjaer, Kurt |
author_sort | Schomacker, Anders |
collection | Lund University Publications (LUP) |
container_issue | 1 |
container_start_page | 85 |
container_title | Journal of Quaternary Science |
container_volume | 21 |
description | This paper presents data on a glacial landform that, to Our knowledge, has not previously been described in the literature: the ice-cored drumlin. The study area is the forefield of the surge-type glacier Bruarjokull at the northeastern margin of the Vatnajokull ice cap, Fast Iceland. Based on sedimentological field investigations and aerial photograph interpretation, a qualitative model for the formation of ice-cored drumlins is proposed. The drumlin core consists of stagnant glacier ice from a previous advance and bubbly ice formed by snowdrifts, which were incorporated during the most recent advance-the 1963-64 surge. This advance deposited a mantle of basal till and streamlined the ice-cored moraines. Till deformation and deposition on the drumlin ice-core is facilitated by a substratum of low-permeability ice-cored moraines. |
format | Article in Journal/Newspaper |
genre | glacier Ice cap ice core Iceland |
genre_facet | glacier Ice cap ice core Iceland |
geographic | Stagnant Glacier |
geographic_facet | Stagnant Glacier |
id | ftulundlup:oai:lup.lub.lu.se:e9cbdabd-8606-4aa5-b3a3-dd41f270c658 |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(-125.053,-125.053,57.866,57.866) |
op_collection_id | ftulundlup |
op_container_end_page | 93 |
op_doi | https://doi.org/10.1002/jqs.949 |
op_relation | https://lup.lub.lu.se/record/419389 http://dx.doi.org/10.1002/jqs.949 wos:000234864700008 scopus:31344445385 |
op_source | Journal of Quaternary Science; 21(1), pp 85-93 (2006) ISSN: 1099-1417 |
publishDate | 2006 |
publisher | John Wiley & Sons Inc. |
record_format | openpolar |
spelling | ftulundlup:oai:lup.lub.lu.se:e9cbdabd-8606-4aa5-b3a3-dd41f270c658 2025-04-06T14:53:06+00:00 Ice-cored drumlins at the surge-type glacier Bruarjokull, Iceland: a transitional-state landform Schomacker, Anders Kruger, J Kjaer, Kurt 2006 https://lup.lub.lu.se/record/419389 https://doi.org/10.1002/jqs.949 eng eng John Wiley & Sons Inc. https://lup.lub.lu.se/record/419389 http://dx.doi.org/10.1002/jqs.949 wos:000234864700008 scopus:31344445385 Journal of Quaternary Science; 21(1), pp 85-93 (2006) ISSN: 1099-1417 Geology glacier surge ice-cored moraine drumlin Iceland Bruarjokull contributiontojournal/article info:eu-repo/semantics/article text 2006 ftulundlup https://doi.org/10.1002/jqs.949 2025-03-11T14:07:57Z This paper presents data on a glacial landform that, to Our knowledge, has not previously been described in the literature: the ice-cored drumlin. The study area is the forefield of the surge-type glacier Bruarjokull at the northeastern margin of the Vatnajokull ice cap, Fast Iceland. Based on sedimentological field investigations and aerial photograph interpretation, a qualitative model for the formation of ice-cored drumlins is proposed. The drumlin core consists of stagnant glacier ice from a previous advance and bubbly ice formed by snowdrifts, which were incorporated during the most recent advance-the 1963-64 surge. This advance deposited a mantle of basal till and streamlined the ice-cored moraines. Till deformation and deposition on the drumlin ice-core is facilitated by a substratum of low-permeability ice-cored moraines. Article in Journal/Newspaper glacier Ice cap ice core Iceland Lund University Publications (LUP) Stagnant Glacier ENVELOPE(-125.053,-125.053,57.866,57.866) Journal of Quaternary Science 21 1 85 93 |
spellingShingle | Geology glacier surge ice-cored moraine drumlin Iceland Bruarjokull Schomacker, Anders Kruger, J Kjaer, Kurt Ice-cored drumlins at the surge-type glacier Bruarjokull, Iceland: a transitional-state landform |
title | Ice-cored drumlins at the surge-type glacier Bruarjokull, Iceland: a transitional-state landform |
title_full | Ice-cored drumlins at the surge-type glacier Bruarjokull, Iceland: a transitional-state landform |
title_fullStr | Ice-cored drumlins at the surge-type glacier Bruarjokull, Iceland: a transitional-state landform |
title_full_unstemmed | Ice-cored drumlins at the surge-type glacier Bruarjokull, Iceland: a transitional-state landform |
title_short | Ice-cored drumlins at the surge-type glacier Bruarjokull, Iceland: a transitional-state landform |
title_sort | ice-cored drumlins at the surge-type glacier bruarjokull, iceland: a transitional-state landform |
topic | Geology glacier surge ice-cored moraine drumlin Iceland Bruarjokull |
topic_facet | Geology glacier surge ice-cored moraine drumlin Iceland Bruarjokull |
url | https://lup.lub.lu.se/record/419389 https://doi.org/10.1002/jqs.949 |