Fazy rozwoju form skalnych w Magurze Wątkowskiej
View/ Open
Author:
Lach, Jan
xmlui.dri2xhtml.METS-1.0.item-citation: Rocznik Naukowo-Dydaktyczny. 1971, Z. 40, Prace Geograficzne 5, s. [27]-33
xmlui.dri2xhtml.METS-1.0.item-iso: pl
Date: 1971
Metadata
Show full item recordAbstract
In the range of the Wątków Magurian within the Low Beskid Mts., there occur rock measures known as Kornuts. They
can be found both on the summit and on the slopes. In the paper the author describes the measures and tries to
determine their origin. Their occurrence is associated with the presence of thick-banked Magurian sands, their
development being due to the formation of a large slide upon the south-western slopes of the Wątków Magurian. All
observed rock measures are evolving simultaneously, as testified to by the thick layer at the foot of the
mountains.