Veselský M., Lačný A. & Hók J., 2014: Závrty na Dlhom vrchu: modelová štúdia ich vzniku na lineárnych diskontinuitách (Malé Karpaty). Acta Geologica Slovaca, 6, 2, 159–168.


Závrty na Dlhom vrchu: modelová štúdia ich vzniku na lineárnych diskontinuitách (Malé Karpaty)

Dolines on the Dlhý vrch hill: case study of doline evolution on linear discontinuity (Malé Karpaty Mts.)


Michal Veselský1, Alexander Lačný2 & Jozef Hók2

1Katedra fyzickej geografie a geoekológie, Prírodovedecká fakulta, Univerzita Komenského v Bratislave, Mlynská dolina G, 842 15 Bratislava, Slovensko, michal.veselsky@uniba.sk
2Katedra geológie a paleontológie, Prírodovedecká fakulta, Univerzita Komenského v Bratislave, Mlynská dolina G, 842 15 Bratislava, Slovensko

Abstract

Dolines as specific surface form can be considered to be the indicator of karst landscape. The main hypothesis of this study is lithological and tectonic discontinuity, which influenced formation of doline line. Doline line in Dlhý vrch hill is built up by border deposits of the Carpathian Keuper and carbonates rock of the Vysoká Formation and is oriented in the NW–SE directions with rauhwackes as a consequence of tectonic processe. 12 parameters from DTM were measured which has been created by using theodolite Topcon GTS-105N and GPS TRIMBLE PATHFINDER PRO-XRS (DGPS signal). According to exact geological and geomorphological survey and the study of morphometric parameters of dolines in study area, the main hypotheses of doline evolution in lithological and tectonic discontinuity were discussed and it is possible to approve relation between geology and geomorphology. The dolines can be considered to be indicator of karst landscape, but also indicator of lithological and tectonics discontinuity.


Key words: Western Carpathians, Malé Karpaty Mts., dolines, Dlhý vrch hill, linear discontinuity, paleoflow


Manuskript doručený: 2014-03-03

Manuskript revidovaný: 2014-09-12


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