(Article of periodic en Polonais - 1991 - 1992)

Document title

Reliktowe lodowce gruzowe jako element deglacjacji Tatr Wysokich (Polonais)
Les glaciers rocheux reliques, élément de la déglaciation dans les Hautes Tatras

Authors(s) and Affiliation(s)



Most of relict rock glaciers recognised in the High Tatra Mountains have topography of a stagnant ice landscape. According to field mapping small number of rock glaciers can be classified as relict permafrost features, at altitudes of 1450 m to 1950 m a.s.l. Boundary conditions for periglacial realm existed in this altitudinal belt during the Younger Dryas. Here shift to an altitude of 2200 m a.s.l. - (DG)


Article of periodic

published at : Studia geomorphologica Carpatho-Balcanica / ISSN 0081-6434 / CODEN SGCAAE

Editor : Państwowe Wydawnictwo Naukowe, Warszawa - POLOGNE (1967)

Millesime : 1991-1992, vol. 25-26 [pp. 133-150]

Bibliographic references : 21 réf.

Collation : Illustration ;



INIST-CNRS, Cote INIST : 17047

Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI), 1994.
Refdoc record number (ud4) : 6076372 : Permanent link - XML version
Powered by Pxxo