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(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)

KOTARBA A. ;

Abstract

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)

Source

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 ;

Language

Polonais

INIST-CNRS, Cote INIST : 17047

Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI), 1994.
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