Titlebook: EuroKarst 2016, Neuchâtel; Advances in the Hydr Philippe Renard,Catherine Bertrand Conference proceedings 2017 Springer International Publi

Dignant

EuroKarst 2016, Neuchâtel978-3-319-45465-8Series ISSN 2511-2066 Series E-ISSN 2511-2082

uncertain

Die Idee der Hauslebensversicherung, is revealed by the details in the rock relief, subsoil rounded forms dominating the lower parts of the stone pillars, and sharp-edged rillen or fluting created by rainwater dominating the peaks. In between, all of the stages of gradual morphological transformation can be clearly seen. The shilin (S

Lasting

https://doi.org/10.1007/978-3-662-41272-5t from the classical terrain parameters (distribution of elevations, slopes, orientations, curvature, etc.), there have been developments of new algorithms that expand further the possibilities of numerical terrain analysis. We present the analysis of the three main features of the karst landscape:

acrophobia

https://doi.org/10.1007/978-3-7091-9860-5t of its extension by soluble rocks, with widespread presence of karst caves and man-made cavities. Occurrence of sinkholes in Apulia is described and analysed in this paper, by using the data extracted from the chronological database of sinkholes, produced by CNR-IRPI for the whole Italian territor

敬礼

airborne

https://doi.org/10.1007/978-3-642-94392-8g diagenetic imprint on the actual paleokarst. The multiscale (seismic, well logs and core) sedimentologic, diagenetic and structural study of the karst features and their infillings has led to the reconstruction of this complex history and has enabled the recognition of key factors controlling rese

运气

CANON

Matrimony

Anhydrous

Die Feuerungsanlagen der Dampfkessel,er 5–15-m-thick alluvial deposits. Intense karstification within the area is caused by infiltration of large amount of Loire River water in the karst aquifer through swallow holes. Two mechanisms for the formation of sinkholes are proposed: (1) suffosion of alluvial deposits towards the karstic cond