THE INVENTORY AND HIERARCHY OF GEOMORPHOSITES IN THE VLĂDEASA MASSIF

At first glance, the Vlădeasa Massif does not stand out in the Apuseni Mountains in terms of the number of geomorphosites it contains, nor in terms of their diversity. But, if one carefully analyzes the landforms in this area, one would find a surprisingnumber of landmarks that could be classified a...

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Main Author: GABRIELA COCEAN
Format: Article
Language:English
Published: Publishing House of the Romanian Academy 2012-12-01
Series:Revue Roumaine de Géographie
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Online Access:http://www.rjgeo.ro/atasuri/revue%20roumaine%2056_2/G.%20Cocean.pdf
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author GABRIELA COCEAN
author_facet GABRIELA COCEAN
author_sort GABRIELA COCEAN
collection DOAJ
description At first glance, the Vlădeasa Massif does not stand out in the Apuseni Mountains in terms of the number of geomorphosites it contains, nor in terms of their diversity. But, if one carefully analyzes the landforms in this area, one would find a surprisingnumber of landmarks that could be classified as geomorphosites. Karstic landforms are the most numerous among these, surprisingly one may add, for a massif that is mainly build up by volcanic rocks and crystalline schists. The karst geomorphosites are all situated in the limestone area of the massif, the Stanciului Valley. After a diagnosis performed on these potential geomorphosites, using the method already successfully applied for the Trascău Mountains, the list of geomorphosites in the Vlădeasa Massif, containing 20 such sites was generated. Most of them are endokarstic forms: caves, potholes and swallets, but there are also peaks, one waterfall and some valley sectors. Among these, the top three sites could occupy leading positions in a hierarchy of geomorphosites in the Apuseni Mountains due to their unique features, and high values: VârfuraşuCave, Răchiţele Waterfall and Pietrele Albe klippes
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spelling doaj-art-9ed525eedae6494e9e3de1b93d1b9a062025-02-02T02:06:11ZengPublishing House of the Romanian AcademyRevue Roumaine de Géographie1220-53112012-12-01562175181THE INVENTORY AND HIERARCHY OF GEOMORPHOSITES IN THE VLĂDEASA MASSIFGABRIELA COCEANAt first glance, the Vlădeasa Massif does not stand out in the Apuseni Mountains in terms of the number of geomorphosites it contains, nor in terms of their diversity. But, if one carefully analyzes the landforms in this area, one would find a surprisingnumber of landmarks that could be classified as geomorphosites. Karstic landforms are the most numerous among these, surprisingly one may add, for a massif that is mainly build up by volcanic rocks and crystalline schists. The karst geomorphosites are all situated in the limestone area of the massif, the Stanciului Valley. After a diagnosis performed on these potential geomorphosites, using the method already successfully applied for the Trascău Mountains, the list of geomorphosites in the Vlădeasa Massif, containing 20 such sites was generated. Most of them are endokarstic forms: caves, potholes and swallets, but there are also peaks, one waterfall and some valley sectors. Among these, the top three sites could occupy leading positions in a hierarchy of geomorphosites in the Apuseni Mountains due to their unique features, and high values: VârfuraşuCave, Răchiţele Waterfall and Pietrele Albe klippeshttp://www.rjgeo.ro/atasuri/revue%20roumaine%2056_2/G.%20Cocean.pdfgeomorphositesVlădeasa MassifendokarstexokarstRomania
spellingShingle GABRIELA COCEAN
THE INVENTORY AND HIERARCHY OF GEOMORPHOSITES IN THE VLĂDEASA MASSIF
Revue Roumaine de Géographie
geomorphosites
Vlădeasa Massif
endokarst
exokarst
Romania
title THE INVENTORY AND HIERARCHY OF GEOMORPHOSITES IN THE VLĂDEASA MASSIF
title_full THE INVENTORY AND HIERARCHY OF GEOMORPHOSITES IN THE VLĂDEASA MASSIF
title_fullStr THE INVENTORY AND HIERARCHY OF GEOMORPHOSITES IN THE VLĂDEASA MASSIF
title_full_unstemmed THE INVENTORY AND HIERARCHY OF GEOMORPHOSITES IN THE VLĂDEASA MASSIF
title_short THE INVENTORY AND HIERARCHY OF GEOMORPHOSITES IN THE VLĂDEASA MASSIF
title_sort inventory and hierarchy of geomorphosites in the vladeasa massif
topic geomorphosites
Vlădeasa Massif
endokarst
exokarst
Romania
url http://www.rjgeo.ro/atasuri/revue%20roumaine%2056_2/G.%20Cocean.pdf
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