Glacial geomorphology of the Shaluli Shan area, southeastern Tibetan Plateau
We present a glacial geomorphological map covering 1.04 x 10(5) km(2) of the Shaluli Shan (Shan Mountain), southeastern Tibetan Plateau. Using a 90 m digital elevation model from the Shuttle Radar Topography Mission and 15/30 m Landsat Enhanced Thematic Mapper Plus satellite imagery, we have mapped...
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Stockholms universitet, Institutionen för naturgeografi och kvartärgeologi (INK)
2012
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ftstockholmuniv:oai:DiVA.org:su-80120 2023-10-29T02:37:01+01:00 Glacial geomorphology of the Shaluli Shan area, southeastern Tibetan Plateau Fu, Ping Heyman, Jakob Hättestrand, Clas Stroeven, Arjen Harbor, Jonathan M. 2012 application/pdf http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-80120 https://doi.org/10.1080/17445647.2012.668762 eng eng Stockholms universitet, Institutionen för naturgeografi och kvartärgeologi (INK) Purdue University Journal of Maps, 2012, 8:1, s. 48-55 orcid:0000-0001-8812-2253 http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-80120 doi:10.1080/17445647.2012.668762 ISI:000305899100006 info:eu-repo/semantics/openAccess glacial geomorphology glaciation landform ice cap Tibetan Plateau Shaluli Shan glacial valley moraine lineations ice-scoured terrain Physical Geography Naturgeografi Article in journal info:eu-repo/semantics/article text 2012 ftstockholmuniv https://doi.org/10.1080/17445647.2012.668762 2023-10-04T22:31:41Z We present a glacial geomorphological map covering 1.04 x 10(5) km(2) of the Shaluli Shan (Shan Mountain), southeastern Tibetan Plateau. Using a 90 m digital elevation model from the Shuttle Radar Topography Mission and 15/30 m Landsat Enhanced Thematic Mapper Plus satellite imagery, we have mapped glacial valleys, marginal moraines, hummocky terrain, glacial lineations and ice-scoured terrain. Lineations and scoured areas largely overlap on the low relief granite plateau of the Shaluli Shan and relate to former ice cap glaciation. These landscape features indicate that past ice cap glaciation included basal sliding conditions, and thus warm-based ice. Glacial valleys and marginal moraines are dominant landforms in the high mountain ranges of Shaluli Shan and occur on and fringing the plateau. This glacial geomorphological map forms the basis for paleoglaciological reconstructions of this southeastern Tibetan Plateau region and indicates the former presence of multiple glaciations involving valley glaciers and ice caps. The map is presented at a scale of 1:630,000. AuthorCount:5; Article in Journal/Newspaper Ice cap Stockholm University: Publications (DiVA) Journal of Maps 8 1 48 55 |
institution |
Open Polar |
collection |
Stockholm University: Publications (DiVA) |
op_collection_id |
ftstockholmuniv |
language |
English |
topic |
glacial geomorphology glaciation landform ice cap Tibetan Plateau Shaluli Shan glacial valley moraine lineations ice-scoured terrain Physical Geography Naturgeografi |
spellingShingle |
glacial geomorphology glaciation landform ice cap Tibetan Plateau Shaluli Shan glacial valley moraine lineations ice-scoured terrain Physical Geography Naturgeografi Fu, Ping Heyman, Jakob Hättestrand, Clas Stroeven, Arjen Harbor, Jonathan M. Glacial geomorphology of the Shaluli Shan area, southeastern Tibetan Plateau |
topic_facet |
glacial geomorphology glaciation landform ice cap Tibetan Plateau Shaluli Shan glacial valley moraine lineations ice-scoured terrain Physical Geography Naturgeografi |
description |
We present a glacial geomorphological map covering 1.04 x 10(5) km(2) of the Shaluli Shan (Shan Mountain), southeastern Tibetan Plateau. Using a 90 m digital elevation model from the Shuttle Radar Topography Mission and 15/30 m Landsat Enhanced Thematic Mapper Plus satellite imagery, we have mapped glacial valleys, marginal moraines, hummocky terrain, glacial lineations and ice-scoured terrain. Lineations and scoured areas largely overlap on the low relief granite plateau of the Shaluli Shan and relate to former ice cap glaciation. These landscape features indicate that past ice cap glaciation included basal sliding conditions, and thus warm-based ice. Glacial valleys and marginal moraines are dominant landforms in the high mountain ranges of Shaluli Shan and occur on and fringing the plateau. This glacial geomorphological map forms the basis for paleoglaciological reconstructions of this southeastern Tibetan Plateau region and indicates the former presence of multiple glaciations involving valley glaciers and ice caps. The map is presented at a scale of 1:630,000. AuthorCount:5; |
format |
Article in Journal/Newspaper |
author |
Fu, Ping Heyman, Jakob Hättestrand, Clas Stroeven, Arjen Harbor, Jonathan M. |
author_facet |
Fu, Ping Heyman, Jakob Hättestrand, Clas Stroeven, Arjen Harbor, Jonathan M. |
author_sort |
Fu, Ping |
title |
Glacial geomorphology of the Shaluli Shan area, southeastern Tibetan Plateau |
title_short |
Glacial geomorphology of the Shaluli Shan area, southeastern Tibetan Plateau |
title_full |
Glacial geomorphology of the Shaluli Shan area, southeastern Tibetan Plateau |
title_fullStr |
Glacial geomorphology of the Shaluli Shan area, southeastern Tibetan Plateau |
title_full_unstemmed |
Glacial geomorphology of the Shaluli Shan area, southeastern Tibetan Plateau |
title_sort |
glacial geomorphology of the shaluli shan area, southeastern tibetan plateau |
publisher |
Stockholms universitet, Institutionen för naturgeografi och kvartärgeologi (INK) |
publishDate |
2012 |
url |
http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-80120 https://doi.org/10.1080/17445647.2012.668762 |
genre |
Ice cap |
genre_facet |
Ice cap |
op_relation |
Journal of Maps, 2012, 8:1, s. 48-55 orcid:0000-0001-8812-2253 http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-80120 doi:10.1080/17445647.2012.668762 ISI:000305899100006 |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1080/17445647.2012.668762 |
container_title |
Journal of Maps |
container_volume |
8 |
container_issue |
1 |
container_start_page |
48 |
op_container_end_page |
55 |
_version_ |
1781061325895499776 |