Abstract
Medium magnitude debris flow phenomena are widespread in the Kola Peninsula Mountains. Most frequently observed types are snowmelt period slushflows and rainfall-induced debris flows. Similar sets of hazardous events are reported for mountainous areas of Scandinavia, Japan, and Northern America.
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References
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Acknowledgements
This work was supported by RFBR project №17-05-00630 “Spatial and temporal characteristics of interaction of debris flows and fluvial processes in river valleys of the Kola Peninsula low mountains” and GM AAAA-A16-11632810089-5.
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Garankina, E.V. et al. (2019). Integration of Landforms, Deposits and Paleosols Analysis for Reconstructing Holocene Debris Flow Activity in the Low Mountains of Kola Peninsula. In: Chalov, S., Golosov, V., Li, R., Tsyplenkov, A. (eds) Climate Change Impacts on Hydrological Processes and Sediment Dynamics: Measurement, Modelling and Management. Springer Proceedings in Earth and Environmental Sciences. Springer, Cham. https://doi.org/10.1007/978-3-030-03646-1_9
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DOI: https://doi.org/10.1007/978-3-030-03646-1_9
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