Glacial geomorphology of the terrestrial margins of the tidewater glacier, Nordenskiöldbreen, Svalbard.
A 1:4000 scale map of the terrestrial margins of the foreland of Nordenskiöldbreen depicts a polythermal glacial landsystem containing a record of the landform signatures of individual ice flow units that operate within the glacier snout. A 1:700 map provides a detailed overview of fluted terrain, b...
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Taylor & Francis
2016
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Online Access: | http://dro.dur.ac.uk/19071/ http://dro.dur.ac.uk/19071/1/19071.pdf https://doi.org/10.1080/17445647.2016.1192329 |
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ftunivdurham:oai:dro.dur.ac.uk.OAI2:19071 2023-05-15T16:22:14+02:00 Glacial geomorphology of the terrestrial margins of the tidewater glacier, Nordenskiöldbreen, Svalbard. Ewertowski, M. Evans, D.J.A. Roberts, D.H. Tomczyk, A.M. 2016-11-04 application/pdf http://dro.dur.ac.uk/19071/ http://dro.dur.ac.uk/19071/1/19071.pdf https://doi.org/10.1080/17445647.2016.1192329 unknown Taylor & Francis dro:19071 issn:1744-5647 doi:10.1080/17445647.2016.1192329 http://dro.dur.ac.uk/19071/ http://dx.doi.org/10.1080/17445647.2016.1192329 http://dro.dur.ac.uk/19071/1/19071.pdf This is an Accepted Manuscript of an article published by Taylor & Francis Group in Journal of Maps on 16/06/2016, available online at: http://www.tandfonline.com/[10.1080/17445647.2016.1192329. Journal of maps, 2016, Vol.12(sup1), pp.476-487 [Peer Reviewed Journal] Article PeerReviewed 2016 ftunivdurham https://doi.org/10.1080/17445647.2016.1192329 2020-06-04T22:23:09Z A 1:4000 scale map of the terrestrial margins of the foreland of Nordenskiöldbreen depicts a polythermal glacial landsystem containing a record of the landform signatures of individual ice flow units that operate within the glacier snout. A 1:700 map provides a detailed overview of fluted terrain, based on unmanned aerial vehicle images captured in 2014. The pattern of landforms lying inside the Little Ice Age (LIA) latero-frontal moraine on the northern side of the fjord comprises a fluted till surface, which in turn grades into ice-moulded bedrock. This signature records the recession of a single, wide ice flow unit, which was characterised by limited incorporation of subglacial material and restricted delivery of supraglacial debris. Inside the latero-frontal moraine on the south side of the fjord, a fluted surface is subordinate to a pronounced and large ice-cored moraine complex related to the confluence of five narrower ice flow units, each of which transported significant quantities of englacial and supraglacial debris at their suture zones as a series of longitudinal debris stripes. The suite of foreland landforms is diagnostic of both temperate subglacial and frozen-snout conditions, indicating the operation of a warm polythermal glacier fed by multiple flow units during the LIA. Article in Journal/Newspaper glacier Svalbard Tidewater Durham University: Durham Research Online Nordenskiöldbreen ENVELOPE(17.166,17.166,78.676,78.676) Svalbard Journal of Maps 12 sup1 476 487 |
institution |
Open Polar |
collection |
Durham University: Durham Research Online |
op_collection_id |
ftunivdurham |
language |
unknown |
description |
A 1:4000 scale map of the terrestrial margins of the foreland of Nordenskiöldbreen depicts a polythermal glacial landsystem containing a record of the landform signatures of individual ice flow units that operate within the glacier snout. A 1:700 map provides a detailed overview of fluted terrain, based on unmanned aerial vehicle images captured in 2014. The pattern of landforms lying inside the Little Ice Age (LIA) latero-frontal moraine on the northern side of the fjord comprises a fluted till surface, which in turn grades into ice-moulded bedrock. This signature records the recession of a single, wide ice flow unit, which was characterised by limited incorporation of subglacial material and restricted delivery of supraglacial debris. Inside the latero-frontal moraine on the south side of the fjord, a fluted surface is subordinate to a pronounced and large ice-cored moraine complex related to the confluence of five narrower ice flow units, each of which transported significant quantities of englacial and supraglacial debris at their suture zones as a series of longitudinal debris stripes. The suite of foreland landforms is diagnostic of both temperate subglacial and frozen-snout conditions, indicating the operation of a warm polythermal glacier fed by multiple flow units during the LIA. |
format |
Article in Journal/Newspaper |
author |
Ewertowski, M. Evans, D.J.A. Roberts, D.H. Tomczyk, A.M. |
spellingShingle |
Ewertowski, M. Evans, D.J.A. Roberts, D.H. Tomczyk, A.M. Glacial geomorphology of the terrestrial margins of the tidewater glacier, Nordenskiöldbreen, Svalbard. |
author_facet |
Ewertowski, M. Evans, D.J.A. Roberts, D.H. Tomczyk, A.M. |
author_sort |
Ewertowski, M. |
title |
Glacial geomorphology of the terrestrial margins of the tidewater glacier, Nordenskiöldbreen, Svalbard. |
title_short |
Glacial geomorphology of the terrestrial margins of the tidewater glacier, Nordenskiöldbreen, Svalbard. |
title_full |
Glacial geomorphology of the terrestrial margins of the tidewater glacier, Nordenskiöldbreen, Svalbard. |
title_fullStr |
Glacial geomorphology of the terrestrial margins of the tidewater glacier, Nordenskiöldbreen, Svalbard. |
title_full_unstemmed |
Glacial geomorphology of the terrestrial margins of the tidewater glacier, Nordenskiöldbreen, Svalbard. |
title_sort |
glacial geomorphology of the terrestrial margins of the tidewater glacier, nordenskiöldbreen, svalbard. |
publisher |
Taylor & Francis |
publishDate |
2016 |
url |
http://dro.dur.ac.uk/19071/ http://dro.dur.ac.uk/19071/1/19071.pdf https://doi.org/10.1080/17445647.2016.1192329 |
long_lat |
ENVELOPE(17.166,17.166,78.676,78.676) |
geographic |
Nordenskiöldbreen Svalbard |
geographic_facet |
Nordenskiöldbreen Svalbard |
genre |
glacier Svalbard Tidewater |
genre_facet |
glacier Svalbard Tidewater |
op_source |
Journal of maps, 2016, Vol.12(sup1), pp.476-487 [Peer Reviewed Journal] |
op_relation |
dro:19071 issn:1744-5647 doi:10.1080/17445647.2016.1192329 http://dro.dur.ac.uk/19071/ http://dx.doi.org/10.1080/17445647.2016.1192329 http://dro.dur.ac.uk/19071/1/19071.pdf |
op_rights |
This is an Accepted Manuscript of an article published by Taylor & Francis Group in Journal of Maps on 16/06/2016, available online at: http://www.tandfonline.com/[10.1080/17445647.2016.1192329. |
op_doi |
https://doi.org/10.1080/17445647.2016.1192329 |
container_title |
Journal of Maps |
container_volume |
12 |
container_issue |
sup1 |
container_start_page |
476 |
op_container_end_page |
487 |
_version_ |
1766010202379780096 |