Year: 2021
Pages: 37-51
UDC: 551.444.2 (470.57)
Number: 3
Type: scientific article
DOI: https://doi.org/10.31084/2619-0087/2021-3-5
Topic: ARTICLES AND PUBLICATIONS
Authors: Smirnov, Alexandr I.
The Global Geopark UNESCO “Yangan-Tau” is the first GGN UNESCO in Russia; it is located within the boundaries of Salavat district of the Bashkortostan Republic. Geopark is located at the boundary between Europe and Asia; Geopark’ territory covers two major karst areas — 1) a karst of the East European Plain (karst of plains) and 2) the karst of the Ural mountains (karst of mountains). It is established that on the territory of Geopark, along with the traditional carbonate karst, specific clastic karst is developed. Carbonate karst is widespread in both plain and mountainous parts of the geopark and is associated mainly with the Lower and Upper Paleozoic limestones, dolomites and marls. Clastokarst is developed exclusively in the plain part of the geopark in gypsiferous Lower Permian terrigenous rocks. The forms of karst evidence and the main geological and geomorphological regularities of their distribution are characterized in the paper. When assessing the current activity of karst development and the degree of its impact on the settlements and other economic objects of the local ecionomy, the karst hazard is evaluated as non-hazardous and potentially hazardous. The map of the karst of the Geopark at a scale of 1:500,000 is presented, which reflects the types of karst and its most typical surface and underground forms
“Yangan-Tau” Geopark, Ufa Plateau, Ai River Plain, carbonate karst, clastokarst