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  • Karst evolution depends particularly on the time available for process evolution and on the geographical and geological conditions of the exposure of the rock. The longer the time, the higher the hydraulic gradient and the larger the amount of solvent water entering the karst system, the more evolved is the karst. Stratigraphic discontinuities directly influence the intensity and extent of karstification. Unconformities influence the stratigraphy of the karst through the time-span that is available for subaerial processes. The definite end occurs at the moment when the host rock, together with its karst phenomena, has completely been eroded/denuded.
  • Karst evolution depends particularly on the time available for process evolution and on the geographical and geological conditions of the exposure of the rock. The longer the time, the higher the hydraulic gradient and the larger the amount of solvent water entering the karst system, the more evolved is the karst. Stratigraphic discontinuities directly influence the intensity and extent of karstification. Unconformities influence the stratigraphy of the karst through the time-span that is available for subaerial processes. The definite end occurs at the moment when the host rock, together with its karst phenomena, has completely been eroded/denuded. (en)
  • Vývoj krasu zvláště závisí na času, který je k dispozici pro rozvoj procesu a na geplogických a geografických podmínkách obnažení hornin. Čím je delší čas k dispozici, vyšší hydraulický spád a větší množství rozpouštědla může vstoupit do krasového systému, tím vice vyvinutý je kras. Stratigrafické discontinuity přímo ovlivňují intenzitu a rozsah krasovění. Nesouhlasnosti ovlivňují stratigrafii krasu čase, který je k dispozici pro rozvoj subaerických procesů. Úplný konec krasu se vyskytuje v okamžiku, kdy hostitelská hornina spolu s vyvinutým krasem je zcela erodována či denudována. (cs)
Title
  • Karst processes and time
  • Karst processes and time (en)
  • Krasové procesy a čas (cs)
skos:prefLabel
  • Karst processes and time
  • Karst processes and time (en)
  • Krasové procesy a čas (cs)
skos:notation
  • RIV/67985831:_____/08:00312600!RIV09-AV0-67985831
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • Z(AV0Z30130516)
http://linked.open...iv/cisloPeriodika
  • 1
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
http://linked.open.../riv/druhVysledku
http://linked.open...iv/duvernostUdaju
http://linked.open...titaPredkladatele
http://linked.open...dnocenehoVysledku
  • 374590
http://linked.open...ai/riv/idVysledku
  • RIV/67985831:_____/08:00312600
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • karst; speleogenesis; geochronology; unconformites (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • PL - Polská republika
http://linked.open...ontrolniKodProRIV
  • [7566FA7421CB]
http://linked.open...i/riv/nazevZdroje
  • Geologos
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 14
http://linked.open...iv/tvurceVysledku
  • Bosák, Pavel
http://linked.open...n/vavai/riv/zamer
issn
  • 1426-8981
number of pages
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