Mechanisms of slab avalanche release and impact in the Dyatlov Pass incident in 1959

2019 - 2022

The Dyatlov Pass incident is an intriguing unsolved mystery from the last century. In February 1959, a group of nine experienced Russian mountaineers perished during a difficult expedition in the northern Urals. A snow avalanche hypothesis was proposed, among other theories, but was found to be inconsistent with the evidence of a lower-than-usual slope angle, scarcity of avalanche signs, uncertainties about the trigger mechanism, and abnormal injuries of the victims. The challenge of explaining these observations has led us to a physical mechanism for a slab avalanche caused by progressive wind-blown snow accumulation on the slope above the hikers’ tent. Here we show how a combination of irregular topography, a cut made in the slope to install the tent and the subsequent deposition of snow induced by strong katabatic winds contributed after a suitable time to the slab release, which caused severe non-fatal injuries, in agreement with the autopsy results.

Dyatlov Pass fig.1
Pictures taken at the tent location shortly before and weeks after the incident, and a sketch of the slope before the incident. a, last picture of the Dyatlov group taken before sunset, while making a cut in the slope to install the tent. Photograph courtesy of the Dyatlov Memorial Foundation. b, broken tent covered with snow as it was found during the search 26 days after the event. Photograph courtesy of the Dyatlov Memorial Foundation. c, configuration of the Dyatlov tent installed on a flat surface after making a cut in the slope below a small shoulder. Snow deposition above the tent is due to wind transport of snow.
Dyatlov Pass fig.2
MPM simulation of the dynamics of a snow-slab avalanche and its impact on a human body. Blue snow particles represent regions in which the yield condition has been met. The inset shows a simulated (3D MPM) thorax deflection (normalized by an original thorax height of 20 cm) for a crash test with a 10 kg rigid mass impacting the thorax at a 7 m/s velocity (black curve) and for impacts by 0.125, 0.25, and 0.5 m3 elastoplastic snow blocks of 400 kg/m3 density and velocities of 2 m/s (orange dash-dotted curve, red dashed curve, and red solid curve, respectively). Injury levels correspond to the AIS11.

Funding

Swiss National Science Foundation (grant numbers PCEFP2_181227 and 200021_168998)

Researchers

Prof. Dr. Johan Gaume
Prof. Dr. Alexander M. Puzrin

Publications

Contact

Prof. Dr. Alexander Puzrin
Full Professor at the Department of Civil, Environmental and Geomatic Engineering
Head of Institute for Geotechnical Engineering
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Institut für Geotechnik
Stefano-Franscini-Platz 5
8093 Zürich
Switzerland

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