Geografie 2001, 106, 148-165
Morphostructural analysis of the Czech part of the Čantoryjská hornatina Hilly Region
The article evaluates the morphostructural construction of the Czech part of the Čantoryjská hornatina Hilly Region with taking full advantage of a detailed geomorphologic mapping and multicriterial morphostructural analysis. As a result of the upper Tertiary and Quaternary neotectonics, there arose a graded internally ranged morphostructure with features of vaulted deformations and faults.
Keywords
Slezské Beskydy Mountains, Čantoryjská hornatina Hilly Region, mapping of morphostructures, flysch rocks.
Funding
Autor děkuje Grantové agentuře Ostravské univerzity za finanční podporu projektu IGS 311056/01.