Titlebook: Covered Karsts; Márton Veress Book 2016 Springer Science+Business Media Dordrecht 2016 Covered Karst Types.Morphology of the Features.Func

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无动于衷

条街道往前推

Zusammenfassung und Schlussfolgerungen,, to the origin of cover deposits (locally deposited or transported there) and to the age of karstification (syngenetic if the depression in the cover and the form in the bedrock are of the same age and postgenetic if not). Covered karsts may develop in structural landforms (synclines, tectonic grab

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inclusive

re demonstrated. The reasons for activity are taken into account. Activities are typified by character and modes of water inflow. The phenomena related to activity (flood lake, overflow, throughflow, intermittent springs, onfilling) and types of activity (surface inflow, seepage, latent activity, co

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esented. For the above landforms and their varieties, the influencing geological, morphological and hydrological conditions are presented, and the origin, evolution and transformation of landforms are demonstrated. In the presentation of the development of karren, the role of the cover (mainly its g

摘要

asing or decreasing extension of the covered karst) depends on the ratio between the inward transport of cover upon the karst and outward transport (removal of material). Here two-phase landform evolution takes place as on recent allogenic covered karst and renewed allogenic covered karst. On other

Chauvinistic

Study Areas,elek Karst, Asiago Plateau, Bakony Mountains, Bükk Mountains, Durmitor, Northern Limestone Alps, Madagascar, Mecsek Mountains and Pádis plateau. The areas from where observations derive are the Atacama Desert, Biokovo mountains, Cerkniško polje, Crimean Peninsula, Dolomites Iceland, Middle Lena, the Lunan area and Parajd.

痛恨

魔鬼在游行

Zusammenfassung und Schlussfolgerungen,elek Karst, Asiago Plateau, Bakony Mountains, Bükk Mountains, Durmitor, Northern Limestone Alps, Madagascar, Mecsek Mountains and Pádis plateau. The areas from where observations derive are the Atacama Desert, Biokovo mountains, Cerkniško polje, Crimean Peninsula, Dolomites Iceland, Middle Lena, the Lunan area and Parajd.