Formy lodowcowe i wodnolodowcowe w Dolinie Kościeliskiej (Tatry Zachodnie)

Abstract

Glacial and fluvioglacial forms In the Kościeliska Valley (Western Tatra Mts.).Summary. In the upper part of Kościeliska Valley several erosive (cirque and glacial trimlines) and accumulative (terminal moraines, marginal moraines, interlobate moraines and fossil rock glacier) glacial forms can be easily seen. Basing on their order and extent as well as on correlation other Tatrya valleys the deglaciation process of last mountain glaciations (Würm — Białka Stadial) in the Kościeliska Valley can be tentatively reconstructed.