@ARTICLE{Nitychoruk_Jerzy_Morphogenetic_1988, author={Nitychoruk, Jerzy and Dzierżek, Jan}, volume={vol. 9}, number={No 1}, journal={Polish Polar Research}, pages={73-85}, howpublished={online}, year={1988}, publisher={Polish Academy of Sciences}, publisher={Committee on Polar Research}, abstract={Studies over talus cones in nothwestern Wedel Jarlsberg Land enable to define main parameters of these forms, their morphogenetic features and longitudinal profiles. Three zones of occurrence of talus cones have been distinguished, dependent on microlimatic influence of glaciers. Zone A (below 150 m a.s.l.) is not influenced by glaciers. Zone В (from 150 to 350 m a.s.l.) is influenced by glacier snouts. Zone С (over 350 m a.s.l.) is under influence of firn fields. Most intensive development of talus cones in the studied area occurred during the Little Ice Age.}, type={Article}, title={Morphogenetic features of talus cones in northwestern Wedel Jarlsberg Land, Spitsbergen}, URL={http://journals.pan.pl/Content/111250/PDF/1988_1_073-085.pdf}, keywords={Arctic, Spitsbergen, geomorphology, talus cones}, }