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Geomorphosites Assessments of the Glacial and Periglacial Landforms from Southern Carpathians

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Landform Dynamics and Evolution in Romania

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Abstract

Geomorphosites are landforms that in time have received a certain value due to human perception. This value can be scientific, ecological, aesthetic, cultural-historical and economic. The Southern Carpathians present numerous and various glacial and periglacial geomorphosites. In order to obtain an overall image of this area, the authors calculated indexes for glacial, periglacial and global geomorphic diversity. Geomorphic diversity is a dimensionless parameter that shows the number and diversity of geomorphosites within the study area. Global geomorphic diversity (glacial and periglacial) has a medium value of 0.365, with differences between glacial and periglacial. The values for glacial geomorphic diversity varied between 0 and 0.90 with a medium value of 0.30. The periglacial geomorphic diversity had higher values, ranging between 0.10 and 0.95 with a medium value of 0.43. In the Southern Carpathians, The Viștea basin (Făgăraș Mts.) was chosen as study area for an evaluation of geomorphosites. Several methods amongst the most widely used in the literature (Pralong in Géomorphol Relief Processus Environ 3:189–196, 2005; Coratza and Giusti in Il Quaternario 18(1):307–313, 2005; Bruschi and Cendrero in Il Quaternario 18(1):293–306, 2005; Serrano and Gonzalez-Trueba in Géomorphol Relief Processus Environ 3:197–208, 2005; Reynard et al. in Geogr Helv 62 3:148–158, 2007; Pereira et al. in Geogr Helv 62(3):159–169, 2007; Zouros  in Geogr Helv 62 3: 169–180, 2007; Comănescu et al. in Forum Geografic. Studii şi cercetări de geografie şi protecţia mediului XI:54–61, 2012) were applied and their results were subsequently compared. Each of the above-mentioned methods has their strong and weak points and the resulted global values vary on a large scale. The hierarchy obtained for each method in particular shows much smaller differences. By adding all the resulted ranks, the authors can conclude that the Viștea Valley glacial geomorphosite is the most important one from the Viștea basin.

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Correspondence to Laura Comănescu .

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Comănescu, L., Nedelea, A. (2017). Geomorphosites Assessments of the Glacial and Periglacial Landforms from Southern Carpathians. In: Radoane, M., Vespremeanu-Stroe, A. (eds) Landform Dynamics and Evolution in Romania. Springer Geography. Springer, Cham. https://doi.org/10.1007/978-3-319-32589-7_10

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