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dc.contributor.author Michael J. en_US
dc.contributor.author Duncan J. en_US
dc.contributor.author Neil F. en_US
dc.contributor.author John M. en_US
dc.contributor.author Shaun J. en_US
dc.contributor.author Samuel en_US
dc.date.accessioned 2010-12-15T10:52:17Z
dc.date.available 2010-12-15T10:52:17Z
dc.date.issued 2009-06 en_US
dc.identifier http://dx.doi.org/10.1016/j.quascirev.2009.04.009 en_US
dc.identifier.citation Hambrey , M J , Quincey , D J , Glasser , N F , Reynolds , J M , Richardson , S J & Clemmens , S 2009 , ' Sedimentological, geomorphological and dynamic context of debris-mantled glaciers, Mount Everest (Sagarmatha) region, Nepal ' Quaternary Science Reviews , vol 28 , no. 11-12 , pp. 1084-1084 . , 10.1016/j.quascirev.2009.04.009 en_US
dc.identifier.other PURE: 155516 en_US
dc.identifier.other dspace: 2160/6004 en_US
dc.identifier.uri http://hdl.handle.net/2160/6004
dc.description.abstract This paper presents the sediment, landform and dynamic context of four avalanche-fed valley glaciers (Khumbu, Imja, Lhotse and Chukhung) in the Mount Everest (Sagarmatha) region of Nepal. All four glaciers have a mantle of debris dominated by sandy boulder-gravel that suppresses melting to an increasing degree towards the snout, leading to a progressive reduction in the overall slope of their longitudinal profile. Prominent lateral–terminal moraine complexes, also comprising sandy bouldergravel, enclose the glaciers. These terminal moraines originally grew by accretion of multiple sedimentary facies of basal glacial and supraglacial origin, probably by folding and thrusting when the glaciers were more dynamic during the Little Ice Age. The four glaciers are in various stages of recession, and demonstrate a range of scenarios from down-wasting of the glacier tongue, through morainedammed lake development, to post-moraine-dam breaching. Khumbu Glacier is at the earliest stage of supraglacial pond formation and shows no sign yet of developing a major lake, although one is likely to develop behind its >250 m high composite terminal moraine. Imja Glacier terminates in a substantial body of water behind a partially ice-cored moraine dam (as determined from geophysical surveys), but morphologically appears unlikely to be an immediate threat. Chukhung Glacier already has a breached moraine and a connected debris fan, and therefore no longer poses a threat. Lhotse Glacier has an inclined, free-draining tongue that precludes hazardous lake development. From the data assembled, a conceptual model, applicable to other Himalayan glaciers, is proposed to explain the development of large, lateral-terminal moraine complexes and associated potentially hazardous moraine dams. – 2008 Elsevier Ltd. All rights reserved en_US
dc.format.extent 1 en_US
dc.relation.ispartof Quaternary Science Reviews en_US
dc.title Sedimentological, geomorphological and dynamic context of debris-mantled glaciers, Mount Everest (Sagarmatha) region, Nepal en_US
dc.contributor.pbl Institute of Geography & Earth Sciences en_US
dc.contributor.pbl Centre for Glaciology en_US


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