Evidence for Subglacial Deformation and Deposition during a Complete Advance-Stagnation Cycle of Kötlujökull, Iceland – A Case Study
A geological section, 70 m long and 3–4 m high, cut into dead-ice moraine in front of Kötlujökull, has been described. Five-sediment associations were recognized representing (1) proglacial glacio-fluvial sedimentation, (2) deposition and deformation in ice-marginal environment, (3) subglacial defor...
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ftcopenhagenunip:oai:pure.atira.dk:publications/d378aaec-bdb8-4965-9b5e-d6a32572f0b8 2024-02-27T08:40:45+00:00 Evidence for Subglacial Deformation and Deposition during a Complete Advance-Stagnation Cycle of Kötlujökull, Iceland – A Case Study Klint, K E S Richardt, N Krüger, Johannes Schomacker, A Krüger, Johannes Kjær, Kurt H 2010 https://curis.ku.dk/portal/da/publications/evidence-for-subglacial-deformation-and-deposition-during-a-complete-advancestagnation-cycle-of-koetlujoekull-iceland--a-case-study(d378aaec-bdb8-4965-9b5e-d6a32572f0b8).html https://doi.org/10.1016/S1571-0866(09)01309-8 eng eng Elsevier info:eu-repo/semantics/restrictedAccess Klint , K E S , Richardt , N & Krüger , J 2010 , Evidence for Subglacial Deformation and Deposition during a Complete Advance-Stagnation Cycle of Kötlujökull, Iceland – A Case Study . in A Schomacker , J Krüger & K H Kjær (eds) , The Mýrdalsjökull Ice Cap, Iceland. Glacial Processes, Sediments and Landforms on an Active Volcano . Elsevier , Amsterdam and Oxford , Developments in Quaternary Sciences , vol. 13 , pp. 145-158 . https://doi.org/10.1016/S1571-0866(09)01309-8 /dk/atira/pure/core/keywords/TheFacultyOfScience Faculty of Science Kötlujökull bookPart 2010 ftcopenhagenunip https://doi.org/10.1016/S1571-0866(09)01309-8 2024-02-01T00:00:06Z A geological section, 70 m long and 3–4 m high, cut into dead-ice moraine in front of Kötlujökull, has been described. Five-sediment associations were recognized representing (1) proglacial glacio-fluvial sedimentation, (2) deposition and deformation in ice-marginal environment, (3) subglacial deformation and deposition from dynamically active ice, (4) subglacial deposition from stagnant ice and (5) supraglacial re-deposition in dead-ice environment during de-icing. This complete sedimentary sequence represents a single glacier advance-stagnation cycle. The melt-out till displays moderate consolidation, moderate content of fines and angular clasts, and a very strong clast fabric. The lodgement/deformation till displays strong to very strong consolidation, relatively high content of fines, low content of angular clasts, and a weak to strong clast fabric. The occurrence of water-escape structures below the basal till and complete lack of brittle deformations in the lodgement/deformation till suggest water-saturated subglacial conditions during the advance of Kötlujökull. Book Part glacier Iceland University of Copenhagen: Research 145 158 |
institution |
Open Polar |
collection |
University of Copenhagen: Research |
op_collection_id |
ftcopenhagenunip |
language |
English |
topic |
/dk/atira/pure/core/keywords/TheFacultyOfScience Faculty of Science Kötlujökull |
spellingShingle |
/dk/atira/pure/core/keywords/TheFacultyOfScience Faculty of Science Kötlujökull Klint, K E S Richardt, N Krüger, Johannes Evidence for Subglacial Deformation and Deposition during a Complete Advance-Stagnation Cycle of Kötlujökull, Iceland – A Case Study |
topic_facet |
/dk/atira/pure/core/keywords/TheFacultyOfScience Faculty of Science Kötlujökull |
description |
A geological section, 70 m long and 3–4 m high, cut into dead-ice moraine in front of Kötlujökull, has been described. Five-sediment associations were recognized representing (1) proglacial glacio-fluvial sedimentation, (2) deposition and deformation in ice-marginal environment, (3) subglacial deformation and deposition from dynamically active ice, (4) subglacial deposition from stagnant ice and (5) supraglacial re-deposition in dead-ice environment during de-icing. This complete sedimentary sequence represents a single glacier advance-stagnation cycle. The melt-out till displays moderate consolidation, moderate content of fines and angular clasts, and a very strong clast fabric. The lodgement/deformation till displays strong to very strong consolidation, relatively high content of fines, low content of angular clasts, and a weak to strong clast fabric. The occurrence of water-escape structures below the basal till and complete lack of brittle deformations in the lodgement/deformation till suggest water-saturated subglacial conditions during the advance of Kötlujökull. |
author2 |
Schomacker, A Krüger, Johannes Kjær, Kurt H |
format |
Book Part |
author |
Klint, K E S Richardt, N Krüger, Johannes |
author_facet |
Klint, K E S Richardt, N Krüger, Johannes |
author_sort |
Klint, K E S |
title |
Evidence for Subglacial Deformation and Deposition during a Complete Advance-Stagnation Cycle of Kötlujökull, Iceland – A Case Study |
title_short |
Evidence for Subglacial Deformation and Deposition during a Complete Advance-Stagnation Cycle of Kötlujökull, Iceland – A Case Study |
title_full |
Evidence for Subglacial Deformation and Deposition during a Complete Advance-Stagnation Cycle of Kötlujökull, Iceland – A Case Study |
title_fullStr |
Evidence for Subglacial Deformation and Deposition during a Complete Advance-Stagnation Cycle of Kötlujökull, Iceland – A Case Study |
title_full_unstemmed |
Evidence for Subglacial Deformation and Deposition during a Complete Advance-Stagnation Cycle of Kötlujökull, Iceland – A Case Study |
title_sort |
evidence for subglacial deformation and deposition during a complete advance-stagnation cycle of kötlujökull, iceland – a case study |
publisher |
Elsevier |
publishDate |
2010 |
url |
https://curis.ku.dk/portal/da/publications/evidence-for-subglacial-deformation-and-deposition-during-a-complete-advancestagnation-cycle-of-koetlujoekull-iceland--a-case-study(d378aaec-bdb8-4965-9b5e-d6a32572f0b8).html https://doi.org/10.1016/S1571-0866(09)01309-8 |
genre |
glacier Iceland |
genre_facet |
glacier Iceland |
op_source |
Klint , K E S , Richardt , N & Krüger , J 2010 , Evidence for Subglacial Deformation and Deposition during a Complete Advance-Stagnation Cycle of Kötlujökull, Iceland – A Case Study . in A Schomacker , J Krüger & K H Kjær (eds) , The Mýrdalsjökull Ice Cap, Iceland. Glacial Processes, Sediments and Landforms on an Active Volcano . Elsevier , Amsterdam and Oxford , Developments in Quaternary Sciences , vol. 13 , pp. 145-158 . https://doi.org/10.1016/S1571-0866(09)01309-8 |
op_rights |
info:eu-repo/semantics/restrictedAccess |
op_doi |
https://doi.org/10.1016/S1571-0866(09)01309-8 |
container_start_page |
145 |
op_container_end_page |
158 |
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