Dynamics of rock glaciers of the Northern Tien Shan and the Djungar Ala Tau, Kazakhstan
Abstract Over 1500 active rock glaciers have been identified in the Northern Tien Shan and the Djungar Ala Tau, Kazakhstan. Studies of the dynamics of six near‐glacier rock glaciers for 15–60 years show rates of movement in the main body of the rock glacier of 0.16–14.0 m/y. These also vary with tim...
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crwiley:10.1002/ppp.3430030105 2024-06-02T08:13:10+00:00 Dynamics of rock glaciers of the Northern Tien Shan and the Djungar Ala Tau, Kazakhstan Gorbunov, Aldar P. Titkov, Sergei N. Polyakov, Victor G. 1992 http://dx.doi.org/10.1002/ppp.3430030105 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.3430030105 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.3430030105 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Permafrost and Periglacial Processes volume 3, issue 1, page 29-39 ISSN 1045-6740 1099-1530 journal-article 1992 crwiley https://doi.org/10.1002/ppp.3430030105 2024-05-03T12:05:28Z Abstract Over 1500 active rock glaciers have been identified in the Northern Tien Shan and the Djungar Ala Tau, Kazakhstan. Studies of the dynamics of six near‐glacier rock glaciers for 15–60 years show rates of movement in the main body of the rock glacier of 0.16–14.0 m/y. These also vary with time. Factors involved include climatic change, changes in ice content in the source area, flow of glacial meltwater through the rock glacier, changes in gradient of the underlying surface and changes in width of the valley through which it moves. Article in Journal/Newspaper Permafrost and Periglacial Processes Wiley Online Library Permafrost and Periglacial Processes 3 1 29 39 |
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Open Polar |
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Wiley Online Library |
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crwiley |
language |
English |
description |
Abstract Over 1500 active rock glaciers have been identified in the Northern Tien Shan and the Djungar Ala Tau, Kazakhstan. Studies of the dynamics of six near‐glacier rock glaciers for 15–60 years show rates of movement in the main body of the rock glacier of 0.16–14.0 m/y. These also vary with time. Factors involved include climatic change, changes in ice content in the source area, flow of glacial meltwater through the rock glacier, changes in gradient of the underlying surface and changes in width of the valley through which it moves. |
format |
Article in Journal/Newspaper |
author |
Gorbunov, Aldar P. Titkov, Sergei N. Polyakov, Victor G. |
spellingShingle |
Gorbunov, Aldar P. Titkov, Sergei N. Polyakov, Victor G. Dynamics of rock glaciers of the Northern Tien Shan and the Djungar Ala Tau, Kazakhstan |
author_facet |
Gorbunov, Aldar P. Titkov, Sergei N. Polyakov, Victor G. |
author_sort |
Gorbunov, Aldar P. |
title |
Dynamics of rock glaciers of the Northern Tien Shan and the Djungar Ala Tau, Kazakhstan |
title_short |
Dynamics of rock glaciers of the Northern Tien Shan and the Djungar Ala Tau, Kazakhstan |
title_full |
Dynamics of rock glaciers of the Northern Tien Shan and the Djungar Ala Tau, Kazakhstan |
title_fullStr |
Dynamics of rock glaciers of the Northern Tien Shan and the Djungar Ala Tau, Kazakhstan |
title_full_unstemmed |
Dynamics of rock glaciers of the Northern Tien Shan and the Djungar Ala Tau, Kazakhstan |
title_sort |
dynamics of rock glaciers of the northern tien shan and the djungar ala tau, kazakhstan |
publisher |
Wiley |
publishDate |
1992 |
url |
http://dx.doi.org/10.1002/ppp.3430030105 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.3430030105 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.3430030105 |
genre |
Permafrost and Periglacial Processes |
genre_facet |
Permafrost and Periglacial Processes |
op_source |
Permafrost and Periglacial Processes volume 3, issue 1, page 29-39 ISSN 1045-6740 1099-1530 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/ppp.3430030105 |
container_title |
Permafrost and Periglacial Processes |
container_volume |
3 |
container_issue |
1 |
container_start_page |
29 |
op_container_end_page |
39 |
_version_ |
1800736567996710912 |