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Glacier response in the European Alps to Heinrich event 1 cooling: the Gschnitz stadial. Ivy-Ochs, S., Kerschner, H., Maisch, M., Christl, M., Kubik, P. Latest Pleistocene and Holocene glacier variation in the European Alps. Ivy-Ochs, S., Kerschner, H., Reuther, A., Preusser, F., Maisch, M., Kubik, P. Chronology of the last gglacial cycle in the European Alps. The timing of deglaciation on the northern Alpine foreland (Switzerland). Modelled climatic conditions indicate cold and dry climate with 9-10ºC lower temperature and 30-50% lower precipitation. Würm glaciation in the Biała Woda Valley, High Tatra Mountains. Deglaciation in the Sucha Woda and Panszczyca valleys in the Polish High Tatras. The Lateglacial Interstadial 2 is recorded as fast thinning of glaciers in the upper part of the catchments between 15 and 13 ka. Deglaciation in the High Tatra Mountains (Bia1a Woda Valley as example). Studia Geomorphologica Carpatho-Balcanica 31, 57–81. Studia Geomorphologica Carpatho-Balcanica 35, 7–38. The LG3 glacial episode is marked by well-fomed terminal moraines which were formed at around 12.5 ka. High Mountain environment of the Tatras in the period of pleistocene and holocene transition. In: Proceedings of XVII CBGA Congress, Bratislava, 1e4 September 2002.
Both of them can be correlated with the Greenland Stadial 2a (the Oldest Dryas).
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Investigation on the glaciation of the High Tatra Mountains has an over 200 years long history.