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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Bibliographic Details
Published in:Journal of Maps
Main Authors: Fu, Ping, Heyman, Jakob, Hättestrand, Clas, Stroeven, Arjen, Harbor, Jonathan M.
Format: Article in Journal/Newspaper
Language:English
Published: Stockholms universitet, Institutionen för naturgeografi och kvartärgeologi (INK) 2012
Subjects:
glacial geomorphology
glaciation
landform
ice cap
Tibetan Plateau
Shaluli Shan
glacial valley
moraine
lineations
ice-scoured terrain
Physical Geography
Naturgeografi
Ice cap
Online Access:http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-80120
https://doi.org/10.1080/17445647.2012.668762
Description
Summary: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;

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