A model for the formation of the Pradol (Pradolino) dry valley in W Slovenia and NE Italy

A model for the formation of the Pradol (Pradolino) dry valley in W Slovenia and NE Italy

In tectonically active mountain ranges, the landscape is shaped by the interplay of erosion/sedimentation and tectonically driven crustal deformation. Characteristic landforms such as moraines, wind gaps, fault scarps, and river terraces can be used to decipher the landscape evolution. However, th...

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Bibliographic Details
Main Authors: Manuel DIERCKS, Christoph GRÜTZNER, Marko VRABEC, Kamil USTASZEWSKI
Format: Article
Language:English
Published: Geological Survey of Slovenia 2021-07-01
Series:Geologija
Subjects:
wind gap
lgm
erosion
bedrock incision
pradol
Online Access:http://www.geologija-revija.si/dokument.aspx?id=1406

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