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With sub-fossil remains of trees killed by snow avalanches and found in a peat bog, the so-called Schwarzensteinmoor, we could establish a record of Holocene snow avalanche events. The peat bog is located at 2150 m a.s.l. in the timberline ecotone of the Zillertal Alps in the Central Eastern Alps....

Nicolussi, K.; Pindur, P.; Schiessling, P.; Kaufmann, M.; Thurner, A.; Luzian, R.
Bundesamt und Forschungszentrum für Wald (BFW), Institut für Forstschutz, Wien, Austria
BFW Berichte, 2007, No.141, pp 157-176