Glacial lakes in the Horgos river basin and their outbreak risk assessment

The river Khorgos (in Kazakhstan – Korgas) is a boundary river between Kazakhstan and China. Its basin is located in the central part of southern slope of Dzhungarskiy (Zhetysu) Alatau range. According to agreement between Kazakhstan and China at the boundary transition of Khorgos in the floodplain...

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Main Authors: A. P. Medeu, T. G. Tokmagambetov, A. L. Kokarev, P. A. Plekhanov, N. S. Plekhanova
Format: Article
Language:Russian
Published: Nauka 2015-04-01
Series:Лëд и снег
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Online Access:https://ice-snow.igras.ru/jour/article/view/122
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author A. P. Medeu
T. G. Tokmagambetov
A. L. Kokarev
P. A. Plekhanov
N. S. Plekhanova
author_facet A. P. Medeu
T. G. Tokmagambetov
A. L. Kokarev
P. A. Plekhanov
N. S. Plekhanova
author_sort A. P. Medeu
collection DOAJ
description The river Khorgos (in Kazakhstan – Korgas) is a boundary river between Kazakhstan and China. Its basin is located in the central part of southern slope of Dzhungarskiy (Zhetysu) Alatau range. According to agreement between Kazakhstan and China at the boundary transition of Khorgos in the floodplain of the river Khorgos the large Center of Frontier Cooperation is erected. Estimation of safety of the mentioned object including connection with possible glacial lakes outbursts has the importance of political-economical value. Nowadays development of glacial lakes in the overhead part of Khorgos river basin has reached apogee. As a roof we can mention the maximum of total glacial lakes area (1,7 million m² in 41 lakes) and emptied kettles of former glacial lakes. Six lakes reached highly dangerous outburst stage: the volume of lakes reached some million m³, maximum depth up to 30–40 m. Focal ground filtration of the water from lakes takes place. Development of glacial lakes in Khorgos river basin will continue, and these lakes give and will give real danger for the Center of Frontier Cooperation in case of outburst of naturally dammed lake Kazankol with the similar mechanism of Issyk lake outburst, occurred in 1963 in ZailijskiyAlatau (Ile Alatau).
format Article
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institution Kabale University
issn 2076-6734
2412-3765
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publishDate 2015-04-01
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record_format Article
series Лëд и снег
spelling doaj-art-56f8dcffda0d4cbe99c577febff93c0a2025-08-20T04:00:26ZrusNaukaЛëд и снег2076-67342412-37652015-04-015339910610.15356/2076-6734-2013-3-99-106116Glacial lakes in the Horgos river basin and their outbreak risk assessmentA. P. Medeu0T. G. Tokmagambetov1A. L. Kokarev2P. A. Plekhanov3N. S. Plekhanova4Institute of Geography, Kazakhstan Republic, Almaty;Institute of Geography, Kazakhstan Republic, Almaty;Institute of Geography, Kazakhstan Republic, Almaty;Achmedsafin Institute of Hydrogeology and Geoecology, Kazakhstan Republic, AlmatyAchmedsafin Institute of Hydrogeology and Geoecology, Kazakhstan Republic, AlmatyThe river Khorgos (in Kazakhstan – Korgas) is a boundary river between Kazakhstan and China. Its basin is located in the central part of southern slope of Dzhungarskiy (Zhetysu) Alatau range. According to agreement between Kazakhstan and China at the boundary transition of Khorgos in the floodplain of the river Khorgos the large Center of Frontier Cooperation is erected. Estimation of safety of the mentioned object including connection with possible glacial lakes outbursts has the importance of political-economical value. Nowadays development of glacial lakes in the overhead part of Khorgos river basin has reached apogee. As a roof we can mention the maximum of total glacial lakes area (1,7 million m² in 41 lakes) and emptied kettles of former glacial lakes. Six lakes reached highly dangerous outburst stage: the volume of lakes reached some million m³, maximum depth up to 30–40 m. Focal ground filtration of the water from lakes takes place. Development of glacial lakes in Khorgos river basin will continue, and these lakes give and will give real danger for the Center of Frontier Cooperation in case of outburst of naturally dammed lake Kazankol with the similar mechanism of Issyk lake outburst, occurred in 1963 in ZailijskiyAlatau (Ile Alatau).https://ice-snow.igras.ru/jour/article/view/122degradation of glaciationglacial outburstglacier lakesmudflow activity
spellingShingle A. P. Medeu
T. G. Tokmagambetov
A. L. Kokarev
P. A. Plekhanov
N. S. Plekhanova
Glacial lakes in the Horgos river basin and their outbreak risk assessment
Лëд и снег
degradation of glaciation
glacial outburst
glacier lakes
mudflow activity
title Glacial lakes in the Horgos river basin and their outbreak risk assessment
title_full Glacial lakes in the Horgos river basin and their outbreak risk assessment
title_fullStr Glacial lakes in the Horgos river basin and their outbreak risk assessment
title_full_unstemmed Glacial lakes in the Horgos river basin and their outbreak risk assessment
title_short Glacial lakes in the Horgos river basin and their outbreak risk assessment
title_sort glacial lakes in the horgos river basin and their outbreak risk assessment
topic degradation of glaciation
glacial outburst
glacier lakes
mudflow activity
url https://ice-snow.igras.ru/jour/article/view/122
work_keys_str_mv AT apmedeu glaciallakesinthehorgosriverbasinandtheiroutbreakriskassessment
AT tgtokmagambetov glaciallakesinthehorgosriverbasinandtheiroutbreakriskassessment
AT alkokarev glaciallakesinthehorgosriverbasinandtheiroutbreakriskassessment
AT paplekhanov glaciallakesinthehorgosriverbasinandtheiroutbreakriskassessment
AT nsplekhanova glaciallakesinthehorgosriverbasinandtheiroutbreakriskassessment