Titlebook: Interaction between the Epikarst and Surface Karstification (Case Studies); Márton Veress Book 2024 The Editor(s) (if applicable) and The

N斯巴達(dá)人

PANIC

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精致

Truncated Epikarst on Glaciokarst,rements and the characteristics of suffosion dolines. It can be established the averages of bedrock resistivity are mostly large both by profiles and areas, but the largest resistivity differences are also large by profiles and areas too. Taking into consideration resistivity values on glaciokarsts,

河潭

,Karstification of Plate-Shaped Dolines (R?chite, Padis, Romania),ckening out and caprock thinning out, the morphology and elevation conditions of the bedrock and the structure of superficial deposit were investigated. The high resistivity values of the studied area refer to thick epikarst and a piezometric surface of low position. In the area the bedrock is plain

束以馬具

,Denuding Epikarst on Dolomite (Environs of Veszprém, the Bakony Region),ity of dolomite, the characteristics of fractures, the calcareous content and textural characteristics of dolomite samples, the mines of the area, the structure of rubble beds, the angular distribution of the features of dolomite and the altitude differences of Stream Séd, the karstwater level and r

sinoatrial-node

cardiac-arrest

Book 2024lopment of the epikarst of different karst types and the genetics between the epikarst and landscape features. Chapter 1 gives a general description on the epikarst. Chapter 2 describes the sediment structure of subsidence dolines and interprets their development. It illustrates the interaction betw

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osculate