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(Article of periodic en Anglais - 1995)

Document title

Quaternary development of Kateřinohorská Vaul relief in the Krušné hory Mountains

Authors(s) and Affiliation(s)

VILÍMEK V. (1) ;
(1) Charles University, Faculty of Science, Department of Physical Geography and Geoecology, Prague, TCHEQUE, REPUBLIQUE

Abstract

The relief development of the region was in the Quaternary period more influenced by tectonic movements than by climatic oscillations. A more intensive erosion due to younger upliftings erased traces of relief. Considering the character of accumulations, it can be supposed that an intensive uplifting of Ore Mountains (Krušné hory) went on in the Middle Pleistocene, beginning in the Riss. Holocene processes seem to be less intensive. - (MS)

Source

Article of periodic

published at : Acta universitatis carolinae. Geographica / ISSN 0300-5402 / CODEN AUCGBZ

Editor : Universita Karlova, Praha - TCHECOSLOVAQUIE (1966)

Millesime : 1995, vol. 30, suppl. [pp. 115-137]

Bibliographic references : 34 ref.

Collation : Illustration ;

Language

Anglais

INIST-CNRS, Cote INIST : 8423 M

Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI), 1997.
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