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Description
  • Land forms are a result of geologic and geomorphologic processes that occur on the earth’s surface thus land forms are not chaotic, but have been structured by geologic and geomorphic processes over time. The geomorphology of volcanic formations as a whole seems to be a reflection of the underlying geology with steep-sided land forms occurring at each of the “strong” rock units and long, with gentle slopes and topographic breaks found on „soft“ rocks. To support this theory, we employed and tested new methodology combining information arising from field surveys together with visual interpretation and statistical spatial analysis of morphometric slope-depending classes to define the spatial extent of various volcanic formations and to identify major tectonic phenomena from features derived from the geomorphology in more accurate way.
  • Land forms are a result of geologic and geomorphologic processes that occur on the earth’s surface thus land forms are not chaotic, but have been structured by geologic and geomorphic processes over time. The geomorphology of volcanic formations as a whole seems to be a reflection of the underlying geology with steep-sided land forms occurring at each of the “strong” rock units and long, with gentle slopes and topographic breaks found on „soft“ rocks. To support this theory, we employed and tested new methodology combining information arising from field surveys together with visual interpretation and statistical spatial analysis of morphometric slope-depending classes to define the spatial extent of various volcanic formations and to identify major tectonic phenomena from features derived from the geomorphology in more accurate way. (en)
Title
  • Slope dependent morphometric analysis as a tool contributing to reconstruction of volcano evolution
  • Slope dependent morphometric analysis as a tool contributing to reconstruction of volcano evolution (en)
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  • Slope dependent morphometric analysis as a tool contributing to reconstruction of volcano evolution
  • Slope dependent morphometric analysis as a tool contributing to reconstruction of volcano evolution (en)
skos:notation
  • RIV/00025798:_____/11:00000467!RIV12-MZP-00025798
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • I, P(GA205/09/1989), Z(MZP0002579801)
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
  • 229891
http://linked.open...ai/riv/idVysledku
  • RIV/00025798:_____/11:00000467
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • morphometry,DEM,Conchagua Volcano,Doupovské hory Volcanic Complex,morphology,volcanology (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...ontrolniKodProRIV
  • [62B7560ECB94]
http://linked.open...i/riv/mistoVydani
  • Rijeka
http://linked.open...vEdiceCisloSvazku
  • Neuveden
http://linked.open...i/riv/nazevZdroje
  • Earth and Environmental Sciences
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...v/pocetStranKnihy
http://linked.open...cetTvurcuVysledku
http://linked.open...vavai/riv/projekt
http://linked.open...UplatneniVysledku
http://linked.open...iv/tvurceVysledku
  • Kopačková, Veronika
  • Rapprich, Vladislav
  • Zelenková, Kateřina
  • Šebesta, Jiří
http://linked.open...n/vavai/riv/zamer
number of pages
http://purl.org/ne...btex#hasPublisher
  • InTech
https://schema.org/isbn
  • 978-953-307-468-9
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