fg

Subscribe2


 

Volume XI |

The Evaluation of Geomorphosites from the Ponoare Protected Area

Abstract: In the present paper we present a new method of evaluating the geomorphosite. The method is presented by us/ our team and it was tested in the protected area Ponoare. In the first part of the article, we will apply, for the geomorphosites inventorized here, the other methods of evaluation known worldwide, and after that we will evaluate geomorphosites by following the new method proposed by us, a method which is adapted to geomorphological reality and to the reality of touristic exploitation of the analysed area. There were taken into account the methods developed up to now in the specialized literature, namely: the method of evaluating the touristic value of geomorphosites for the evaluation of the touristic value conceived by J. P. Pralong in 2005, the method developed in 2007 by E. Reynard et al.; the method developed at the University of Modena and Reggio Emilia by P. Coratza and C. Giusti in 2005; and the method proposed at the University of Cantabria by V. M. Bruschi and A. Cendrero in 2005; the method developed by the University from Valladolid by E. Serrano and J. J. Gonzales Trueba in 2005; the method proposed by the University of Minho in 2007 by P. Pereira, the Greek method developed by N. Zourous in 2005 and the Slavonian method proposed in 2012 by B. Erhatic. The results obtained show different quantitative values compared to previous methods, but comparing the rank obtained by each geomorphosite during the evaluation, the rank stays the same. The values are situated in a different deviation compared to other methods, having in view that for additional values firstly the cultural value is reduced in the analysed area.

Volume X |

The Landforms of the Făgărăș Mountains (The Argeș Mountain Catchment): Analysis of the Related Dynamic Processes

Abstract: The present configuration of the Făgăraş Mountains is a snapshot of the long-term evolution that brought about significant alterations of the landscape, and especially of the relief, which has acquired different features depending on the intensity of the relationship between the exogenous and endogenous agents. Relief shaping in the study area is controlled by the orographic and climatic features. However, the climate of the high and middle-height mountains is the main cause that determines the mechanism, the intensity and the spatial distribution of the shaping processes. The massiveness and the considerable height of the Făgăraş Mountains, which exceed 2500 m altitude (Moldoveanu peak 2544 m, Negoiu peak 2535 m, Lespezi peak 2522 m, Vanatoarea lui Buteanu peak 2507 m, etc.), are responsible for the vertical zonation of climate and vegetation. The study area lies in the middle of the Southern Carpathians range, on the southern slope of the Făgăraş Mountains (the Arges mountain catchment). The scale of investigated phenomena and the frequency of their occurrence allow us to distinguish two types of different phenomena on the basis of their geological or geomorphological origin. Each slope section was analyzed by using a series of parameters considered as being stable from the morphodynamic point of view.

Volume VIII |

Inventoring and Evaluation of Geomorphosites in the Bucegi Mountains

Abstract: Geomorphosites stand for relief forms or geomorphologic processes that in time have gained an aesthetic, scientific, cultural, historical or economic value, as a result of human perception. Taking into consideration the above mentioned definition, the present paper aims at inventorying and evaluating part of the geomorphosites in the Bucegi Mountains. The final purpose is to propose some measures for a better protection and tourist promotion. The presence of numerous geomorphosites in the Bucegi Mountains is the direct result of the presence of limestones and conglomerates, as well as the succession of different modelling systems in time (glacial, periglacial, fluvial). We analysed this area since there are many and varied geomorphosites, and at the same time, it is one of the major tourist destinations (the largest number of tourists and the best tourist infrastructure within the Romanian Carpathian Mountains).