This HTML5 document contains 51 embedded RDF statements represented using HTML+Microdata notation.

The embedded RDF content will be recognized by any processor of HTML5 Microdata.

Namespace Prefixes

PrefixIRI
dctermshttp://purl.org/dc/terms/
n20http://purl.org/net/nknouf/ns/bibtex#
n12http://linked.opendata.cz/resource/domain/vavai/projekt/
n7http://linked.opendata.cz/resource/domain/vavai/riv/tvurce/
n16http://linked.opendata.cz/resource/domain/vavai/subjekt/
n8http://linked.opendata.cz/ontology/domain/vavai/
n17http://linked.opendata.cz/resource/domain/vavai/zamer/
n13https://schema.org/
shttp://schema.org/
n4http://linked.opendata.cz/ontology/domain/vavai/riv/
skoshttp://www.w3.org/2004/02/skos/core#
rdfshttp://www.w3.org/2000/01/rdf-schema#
n2http://linked.opendata.cz/resource/domain/vavai/vysledek/
n15http://linked.opendata.cz/resource/domain/vavai/vysledek/RIV%2F00025798%3A_____%2F11%3A00000467%21RIV12-MZP-00025798/
rdfhttp://www.w3.org/1999/02/22-rdf-syntax-ns#
n6http://linked.opendata.cz/ontology/domain/vavai/riv/klicoveSlovo/
n14http://linked.opendata.cz/ontology/domain/vavai/riv/duvernostUdaju/
xsdhhttp://www.w3.org/2001/XMLSchema#
n21http://linked.opendata.cz/ontology/domain/vavai/riv/jazykVysledku/
n5http://linked.opendata.cz/ontology/domain/vavai/riv/aktivita/
n22http://linked.opendata.cz/ontology/domain/vavai/riv/druhVysledku/
n19http://linked.opendata.cz/ontology/domain/vavai/riv/obor/
n18http://reference.data.gov.uk/id/gregorian-year/

Statements

Subject Item
n2:RIV%2F00025798%3A_____%2F11%3A00000467%21RIV12-MZP-00025798
rdf:type
n8:Vysledek skos:Concept
rdfs:seeAlso
http://www.intechopen.com/articles/show/title/slope-dependent-morphometric-analysis-as-a-tool-contributing-to-reconstruction-of-volcano-evolution
dcterms: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.
dcterms: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
skos:prefLabel
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
skos:notation
RIV/00025798:_____/11:00000467!RIV12-MZP-00025798
n8:predkladatel
n16:ico%3A00025798
n4:aktivita
n5:P n5:I n5:Z
n4:aktivity
I, P(GA205/09/1989), Z(MZP0002579801)
n4:dodaniDat
n18:2012
n4:domaciTvurceVysledku
n7:2361825 n7:7557744 n7:6279155 n7:1008293
n4:druhVysledku
n22:C
n4:duvernostUdaju
n14:S
n4:entitaPredkladatele
n15:predkladatel
n4:idSjednocenehoVysledku
229891
n4:idVysledku
RIV/00025798:_____/11:00000467
n4:jazykVysledku
n21:eng
n4:klicovaSlova
morphometry,DEM,Conchagua Volcano,Doupovské hory Volcanic Complex,morphology,volcanology
n4:klicoveSlovo
n6:DEM n6:Conchagua%20Volcano n6:volcanology n6:Doupovsk%C3%A9%20hory%20Volcanic%20Complex n6:morphology n6:morphometry
n4:kontrolniKodProRIV
[62B7560ECB94]
n4:mistoVydani
Rijeka
n4:nazevEdiceCisloSvazku
Neuveden
n4:nazevZdroje
Earth and Environmental Sciences
n4:obor
n19:DB
n4:pocetDomacichTvurcuVysledku
4
n4:pocetStranKnihy
630
n4:pocetTvurcuVysledku
4
n4:projekt
n12:GA205%2F09%2F1989
n4:rokUplatneniVysledku
n18:2011
n4:tvurceVysledku
Šebesta, Jiří Zelenková, Kateřina Rapprich, Vladislav Kopačková, Veronika
n4:zamer
n17:MZP0002579801
s:numberOfPages
22
n20:hasPublisher
InTech
n13:isbn
978-953-307-468-9