Impact of multiple glacial surges - a geomorphological map from Brúarjökull, East Iceland
Udgivelsesdato: 2008 Simultaneously with geological field investigations at the surge-type glacier Bruarjokull in August 2003, aerial photographs covering the central part of the glacier including the Kringilsarrani area were recorded with the purpose of mapping glacial landforms. A glacial geomorph...
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ftcopenhagenunip:oai:pure.atira.dk:publications/a41cf590-0411-11de-b05e-000ea68e967b 2024-04-14T08:12:01+00:00 Impact of multiple glacial surges - a geomorphological map from Brúarjökull, East Iceland Kjær, Kurt H. Korsgaard, Niels Jákup Schomacker, Anders 2008 https://curis.ku.dk/portal/da/publications/impact-of-multiple-glacial-surges--a-geomorphological-map-from-bruarjoekull-east-iceland(a41cf590-0411-11de-b05e-000ea68e967b).html eng eng info:eu-repo/semantics/restrictedAccess Kjær , K H , Korsgaard , N J & Schomacker , A 2008 , ' Impact of multiple glacial surges - a geomorphological map from Brúarjökull, East Iceland ' , Journal of Maps , vol. 4 , no. 1 , pp. 5-20 . article 2008 ftcopenhagenunip 2024-03-21T17:28:06Z Udgivelsesdato: 2008 Simultaneously with geological field investigations at the surge-type glacier Bruarjokull in August 2003, aerial photographs covering the central part of the glacier including the Kringilsarrani area were recorded with the purpose of mapping glacial landforms. A glacial geomorphological map has been completed at a scale 1: 16,000 including more than 20,000 landforms from an area of c. 8 km(2). Manual classification of landforms was carried out directly in stereoscopic view using a digital photogrammetric workstation taking full advantage of the texture, topography and spatial context of individual landforms. We mapped subglacial lineations such as flutes and drumlins on till plains, pitted outwash, eskers, minor meandering ridges, crevasse fill ridges, ice-free dead-ice moraine and concertina ridges, outwash fans and lake sediment plains. In addition, erosional drainage channels, ice-marginal ridges, overridden end-moraines, and extra-marginal ice wedge polygons and collapsed palsas were mapped. The mapped glacial landforms originate from at least four surges: pre-1810, 1810, 1890 and 1964. The distribution of landforms on the Bruarjokull fore field has close resemblance to landform assemblages of palaeo-ice streams. The present terrain surface at Bruarjokull is the cumulated result of multiple landform generations because each surge has superimposed a new association of landforms on older surfaces. Article in Journal/Newspaper glacier Iceland palsas University of Copenhagen: Research Brúarjökull ENVELOPE(-16.157,-16.157,64.682,64.682) |
institution |
Open Polar |
collection |
University of Copenhagen: Research |
op_collection_id |
ftcopenhagenunip |
language |
English |
description |
Udgivelsesdato: 2008 Simultaneously with geological field investigations at the surge-type glacier Bruarjokull in August 2003, aerial photographs covering the central part of the glacier including the Kringilsarrani area were recorded with the purpose of mapping glacial landforms. A glacial geomorphological map has been completed at a scale 1: 16,000 including more than 20,000 landforms from an area of c. 8 km(2). Manual classification of landforms was carried out directly in stereoscopic view using a digital photogrammetric workstation taking full advantage of the texture, topography and spatial context of individual landforms. We mapped subglacial lineations such as flutes and drumlins on till plains, pitted outwash, eskers, minor meandering ridges, crevasse fill ridges, ice-free dead-ice moraine and concertina ridges, outwash fans and lake sediment plains. In addition, erosional drainage channels, ice-marginal ridges, overridden end-moraines, and extra-marginal ice wedge polygons and collapsed palsas were mapped. The mapped glacial landforms originate from at least four surges: pre-1810, 1810, 1890 and 1964. The distribution of landforms on the Bruarjokull fore field has close resemblance to landform assemblages of palaeo-ice streams. The present terrain surface at Bruarjokull is the cumulated result of multiple landform generations because each surge has superimposed a new association of landforms on older surfaces. |
format |
Article in Journal/Newspaper |
author |
Kjær, Kurt H. Korsgaard, Niels Jákup Schomacker, Anders |
spellingShingle |
Kjær, Kurt H. Korsgaard, Niels Jákup Schomacker, Anders Impact of multiple glacial surges - a geomorphological map from Brúarjökull, East Iceland |
author_facet |
Kjær, Kurt H. Korsgaard, Niels Jákup Schomacker, Anders |
author_sort |
Kjær, Kurt H. |
title |
Impact of multiple glacial surges - a geomorphological map from Brúarjökull, East Iceland |
title_short |
Impact of multiple glacial surges - a geomorphological map from Brúarjökull, East Iceland |
title_full |
Impact of multiple glacial surges - a geomorphological map from Brúarjökull, East Iceland |
title_fullStr |
Impact of multiple glacial surges - a geomorphological map from Brúarjökull, East Iceland |
title_full_unstemmed |
Impact of multiple glacial surges - a geomorphological map from Brúarjökull, East Iceland |
title_sort |
impact of multiple glacial surges - a geomorphological map from brúarjökull, east iceland |
publishDate |
2008 |
url |
https://curis.ku.dk/portal/da/publications/impact-of-multiple-glacial-surges--a-geomorphological-map-from-bruarjoekull-east-iceland(a41cf590-0411-11de-b05e-000ea68e967b).html |
long_lat |
ENVELOPE(-16.157,-16.157,64.682,64.682) |
geographic |
Brúarjökull |
geographic_facet |
Brúarjökull |
genre |
glacier Iceland palsas |
genre_facet |
glacier Iceland palsas |
op_source |
Kjær , K H , Korsgaard , N J & Schomacker , A 2008 , ' Impact of multiple glacial surges - a geomorphological map from Brúarjökull, East Iceland ' , Journal of Maps , vol. 4 , no. 1 , pp. 5-20 . |
op_rights |
info:eu-repo/semantics/restrictedAccess |
_version_ |
1796309754139639808 |