Mária Bizubová
Neobyčajné kamenné útvary Slovenska
Číslo: 3/2017
Periodikum: Biologie-Chemie-Zeměpis
DOI: 10.14712/25337556.2017.3.3
Klíčová slova: pasivní morfostruktura, kamenný útvar, skalní město, skalní okno, skalní jehla, skalní hřib, morphostrukture, passive morphostructure, rock arch, rock needle, mushroom rock
Pro získání musíte mít účet v Citace PRO.
are relief features created by the interaction of endogenous and exogenous processes, with the dominant role of
tectonic movements. Passive forms of morphostructures are significantly influenced by structural-lithological characteristics
of the rocks the structures are formed of. Their current appearance reflects the transformation of geological structures that
have lost mobility. Geomorphological characteristics of rocks are important in forming passive morphostructures. Passive
morphostructures form a structural type of relief or structural georelief. Structural georelief is characterized by frequent occurrence
of many rocks forms of georelief of various shapes, such as nappe wrecks, cliffs, rock walls, rock parade, rock towers,
rock needles, quest, dissected supply channels of volcano (necks) lava flows in the inverse position and others. Many of these
objects may be suitable not only for the educational process in the school, but especially for experiential learning in nature
associated with a variety of outdoor activities.