Atraktivita Moravskoslezských Beskyd ve vztahu ke skalnímu lezení

Abstract

The thesis deals with the atractivity of the Moravian-Silesian part of Beskydy Mountains in case of rock climbing. The purpose of the thesis is to define convenient rock climbing locations in the Moravian-Silesian part of Beskydy Mountains in aspect of geological characteristics and climbing convenience. The thesis is oriented to these chosen locations – Štramberk, Godula, Mazák, Medvědí skála, Gírová, Sůlov, Příslop. Severka, Javořinka, rocks under the Muřínkův vrch and the Velký Polom. Most of the climbing locations were formed in the Cretaceous Period (turon and senon) during the Silesian Godula evolution. Flysh character is typical for all the locations except the locations Mazák and Medvědí Skála, which consist of Ostravice sandstone. The Štramberk location was formed in Jurassic Period (tithon) during the Silesian Baška evolution. Štramberk consists of Štramberk limestone. The Gírová location was formed in Paleocene Period during the Magura evolution. Gírová consists of flysh. The most convenient locations are Štramberk, Godula, and Horní and Dolní Mazák because of their amount of the climbing routes and easy access. The rest of the locations are visited only rarely. The reason is a long access to the rocks, unsatisfying climbing resort size, and lack of climbing routes which are not difficult enough and are often not even marked.