Supraglacial Debris of G2 Glacier in Hidden Valley, Mukut Himal, Nepal

Abstract Field investigations of supraglacial debris were carried out during the monsoon season in 1974 on G2 glacier near Tukche Peak in Hidden Valley, Mukut Himal, Nepal. The thickness of the debris layer was observed to increase down-glacier. Laboratory analysis, however, showed a decrease in par...

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Published in:Journal of Glaciology
Main Author: Nakawo, M.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1979
Subjects:
Online Access:http://dx.doi.org/10.1017/s002214300001426x
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214300001426X
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spelling crcambridgeupr:10.1017/s002214300001426x 2024-03-03T08:45:58+00:00 Supraglacial Debris of G2 Glacier in Hidden Valley, Mukut Himal, Nepal Nakawo, M. 1979 http://dx.doi.org/10.1017/s002214300001426x https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214300001426X en eng Cambridge University Press (CUP) Journal of Glaciology volume 22, issue 87, page 273-283 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1979 crcambridgeupr https://doi.org/10.1017/s002214300001426x 2024-02-08T08:36:10Z Abstract Field investigations of supraglacial debris were carried out during the monsoon season in 1974 on G2 glacier near Tukche Peak in Hidden Valley, Mukut Himal, Nepal. The thickness of the debris layer was observed to increase down-glacier. Laboratory analysis, however, showed a decrease in particle size in the same direction. This decrease is explained in terms of mixing of particles contained in glacier ice with the original debris as melting proceeds. A simple relation between debris mass and glacier flow is introduced to explain the observed results. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Hidden Valley ENVELOPE(78.451,78.451,-68.615,-68.615) Journal of Glaciology 22 87 273 283
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Nakawo, M.
Supraglacial Debris of G2 Glacier in Hidden Valley, Mukut Himal, Nepal
topic_facet Earth-Surface Processes
description Abstract Field investigations of supraglacial debris were carried out during the monsoon season in 1974 on G2 glacier near Tukche Peak in Hidden Valley, Mukut Himal, Nepal. The thickness of the debris layer was observed to increase down-glacier. Laboratory analysis, however, showed a decrease in particle size in the same direction. This decrease is explained in terms of mixing of particles contained in glacier ice with the original debris as melting proceeds. A simple relation between debris mass and glacier flow is introduced to explain the observed results.
format Article in Journal/Newspaper
author Nakawo, M.
author_facet Nakawo, M.
author_sort Nakawo, M.
title Supraglacial Debris of G2 Glacier in Hidden Valley, Mukut Himal, Nepal
title_short Supraglacial Debris of G2 Glacier in Hidden Valley, Mukut Himal, Nepal
title_full Supraglacial Debris of G2 Glacier in Hidden Valley, Mukut Himal, Nepal
title_fullStr Supraglacial Debris of G2 Glacier in Hidden Valley, Mukut Himal, Nepal
title_full_unstemmed Supraglacial Debris of G2 Glacier in Hidden Valley, Mukut Himal, Nepal
title_sort supraglacial debris of g2 glacier in hidden valley, mukut himal, nepal
publisher Cambridge University Press (CUP)
publishDate 1979
url http://dx.doi.org/10.1017/s002214300001426x
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214300001426X
long_lat ENVELOPE(78.451,78.451,-68.615,-68.615)
geographic Hidden Valley
geographic_facet Hidden Valley
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 22, issue 87, page 273-283
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s002214300001426x
container_title Journal of Glaciology
container_volume 22
container_issue 87
container_start_page 273
op_container_end_page 283
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