Titlebook: Cave and Karst Systems of Hungary; Márton Veress,Szabolcs Leél-Őssy Book 2022 Springer Nature Switzerland AG 2022 Hungarian karst areas.Ka

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Klassifizierung optischer Netzwerke,n, the Vértes Plateau, the Gerecse Region, the Buda Hills, the Pilis Mountains, and the Western Mecsek Karst. Their description involves their research history, the general description of their karstification, the morphometric study of the karst features belonging to their area, the morphology, morp

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,Erweiterter Kohärenzmatrizen-Kalkül,ases and visualizations, but the analytical capabilities of GIS were also increasingly applied in karst research. Data collection has been revolutionized by continuously evolving remote sensing methods (e.g. LiDAR). GIS became crucial in doline morphometry, thus in this chapter, we present a detaile

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Klassifizierung optischer Netzwerke,e of well-developed plateau karsts in the humid temperate climate zone. Numerous surface and subsurface landforms (285 caves) were created by the intense karstification of Triassic limestones. The compound multi-phase evolution of karst from the Late Cretaceous to the present is recorded in the morp

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Klassifizierung optischer Netzwerke,ed for completeness (since the Bükk Mountains is the richest in caves in Hungary). By the selection, we aimed to include the most significant caves based on the most representative cave types and sizes, speleothem or archaeological values of the mountains. We review the genetic types of the caves in

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Klassifizierung optischer Netzwerke,d marl, during the Middle and Late Pleistocene. Recently we have 60 km of known cave passages mapped, chiefly in the Rózsadomb (Rose Hill) part of the city. Every cave was discovered by accident (stone quarrying, digging basements, trenching for gas and water pipes, canalization, etc.). These caves

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https://doi.org/10.1007/978-3-8348-9437-3one area. This karst area is similar to the Aggtelek karst and Bükk Mountains (see earlier), basically it is formed by infiltrating cold water and allogenic streams. Besides the rich surface karst forms there are several swallow holes, spring caves and chimneys up to 70 m. This chapter shows the mos

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