Abstract
The movement of waste rocks dumps together with ice, stored on the glaciers of the high-altitude Kumtor gold mine is reviewed in this paper. This mining site is located in the central part of the Tien Shan (Kyrgyzstan). There are no other cases around the world, when the waste rocks and removed ice were stored on the active mountain glaciers. The landslide has formed in the area of dumps, stored on the Davydov glacier, and the displacement velocity has dramatically increased in spring 2013. Due to the accelerated movement of rock-ice mass, a number of Kumtor mine infrastructural units was destroyed with economic losses of about USD 100 million. This article presents the results of monitoring of the landslide displacements and provides analysis of the causes for its acceleration. The potential environmental impact of further development of the gravitational mass movement and impact on the Kumtor gold mine facilities were assessed.
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References
Barsch D (1996) Rockglaciers: indicators for the present and former geoecology in high mountain environments. Springer, Berlin, 331 p
Gorbunov AP, Titkov SN, Polyakov VG (1992) Dynamics of rock glaciers of the Northern Tien Shan and the Djungar Ala Tau, Kazakhstan. Permafrost Periglac Process 3(1):29–39
Vasilenko EV, Gromyko AN, Dmitriev DN, Macheret YuYA (1988) The structure of the Davydov glacier according to the radio sounding and the thermal drilling data. Data of Glaciological Studies 62: 208–215 (in Russian)
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Torgoev, I., Omorov, B. (2014). Mass Movement in the Waste Dump of High-Altitude Kumtor Goldmine (Kyrgyzstan). In: Sassa, K., Canuti, P., Yin, Y. (eds) Landslide Science for a Safer Geoenvironment. Springer, Cham. https://doi.org/10.1007/978-3-319-04996-0_79
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DOI: https://doi.org/10.1007/978-3-319-04996-0_79
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