DENUDATION PROCESSES IN THE ARGEŞ SUBCARPATHIANS

Abstract

 Investigations carried out in the small catchments of the Argeş Subcarpathian Hills have shown very high erosion values in the conditions of a facies consisting largely of marl-clay with sand intercalations and slope declivity over 25.0%. Gravitation processes unleashing deep slides and mudflows, enhance denudation on the slopes of torrential basins.

Authors and Affiliations

Valentin TEODORESCU

Keywords

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  • EP ID EP111909
  • DOI -
  • Views 61
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How To Cite

Valentin TEODORESCU (2006).  DENUDATION PROCESSES IN THE ARGEŞ SUBCARPATHIANS. The Annals of Valahia University of Târgoviste, Geographical Series, 6(2), 63-66. https://europub.co.uk/articles/-A-111909