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

安心地散步

Infusion

ession is analysed. In the genetic classification of ponors, the distribution of non-karstic rocks and the position of karst water are considered. In the description of the evolution of DSDs, the karstic and non-karstic influences are overviewed, and it is investigated from what landforms (subsidenc

Chromatic

AMPLE

General Description of Karst,tified and described; surface karst features (karren, dolines, poljes, etc.) are defined broken down to their main varieties with their brief characterisation. The main genetic types of caves are presented. Karst types are identified according to their geological conditions (such as covering, struct

隱語

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, Cerkni?ko polje, Crimean Peninsula, Dolomites Iceland, Middle Lena, the

淺灘

Methods,morphometric analyses, study of bedrock structure for karst features, mapping (topographic, karst morphological, denudational), aerial imaging, preparation of cross-sections, oblique views and block diagrams. For the investigation of the cover, engine-driven helical borer, geophysical techniques wer

CANT

Classification of Covered Karsts,, 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

迅速成長

Gustatory

Covered Karst Processes,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

補角

Landform Evolution and Development,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