GEOLOGY AND GEOMORPHOLOGY OF THE “ROSANDRA” VALLEY FOR A CULTURAL ENHANCEMENT
Article Sidebar
Main Article Content
Abstract
F. Cucchi et al., Geology and Geomorphology of the “Rosandra” Valley for a Cultural Enhancement. (IT ISSN 0394-3356,
2005).
The Rosandra Valley is located near Trieste (Italy), on the border of Classical Karst, and is a canyon-like depression excavated in tertiary limestone. The origin of the valley is mainly due to presence of faults and overthrusts and different attitude to erosion between
limestone and marls, which makes it a beautiful example of lithological and structural control on morphogenesis. Furthermore, its slopes are interested by extended and mature underground karst phenomena that contribute to making the whole hydro-structure more interesting. The valley is also remarkable for its local vegetation, due to its particular climatic conditions, and to its prehistoric and historical value, stemming from its geographic location.
Article Details
Section
This work is licensed under a Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License.
The Author grants usage rights to others using an open license (Creative Commons or equivalent) allowing for immediate free access to the work and permitting any user to read, download, copy, distribute, print, search, or link to the full texts of articles, crawl them for indexing, pass them as data to software, or use them for any other lawful purpose.