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Dendrogeomorphic reconstruction of lahar activity and triggers: Shiveluch volcano, Kamchatka Peninsula, Russia

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Abstract

Lahars are highly concentrated, water-saturated volcanic hyperconcentrated flows or debris flows containing pyroclastic material and are a characteristic mass movement process on volcanic slopes. On Kamchatka Peninsula (Russian Federation), lahars are widespread and may affect remote settlements. Historical records of past lahar occurrences are generally sparse and mostly limited to events which damaged infrastructure on the slopes or at the foot of volcanoes. In this study, we present a tree-ring-based reconstruction of spatiotemporal patterns of past lahar activity at Shiveluch volcano. Using increment cores and cross sections from 126 Larix cajanderi trees, we document 34 events covering the period AD 1729–2012. Analyses of the seasonality of damage in trees reveal that 95% of all lahars occurred between October and May and thus point to the predominant role of the sudden melt of the snow cover by volcanic material. These observations suggest that most lahars were likely syn-eruptive and that lahar activity is largely restricted to periods of volcanic activity. By contrast, rainfall events do not seem to play a significant role in lahar triggering.

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Acknowledgements

The authors kindly acknowledge all the Russian and Swiss scientists who were involved in this project for their valuable support and advice during and after fieldwork. Special thanks also go to the editors, James White and Lucia Capra, as well as to the reviewers for insightful comments. This research was supported by the Scientific and Technological Cooperation Program Switzerland-Russia and by the projects 13-05-12061, 14-05-00768, and 15-05-08694 of the Russian Foundation for Basic Research. Satellite images were provided by MSU Geoportal.

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Correspondence to M. Stoffel.

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Salaorni, E., Stoffel, M., Tutubalina, O. et al. Dendrogeomorphic reconstruction of lahar activity and triggers: Shiveluch volcano, Kamchatka Peninsula, Russia. Bull Volcanol 79, 6 (2017). https://doi.org/10.1007/s00445-016-1094-4

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