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Statements

Subject Item
n2:RIV%2F61988987%3A17310%2F12%3AA13014K5%21RIV13-MSM-17310___
rdf:type
n8:Vysledek skos:Concept
dcterms:description
The abrupt change in valley floor development occurs throughout the Last Glacial - Interglacial cycle. The presented study is a part of wider research of the Holocene development of the Satina river incision in the Lysá hora mountain group. Detailed sedimentological analysis of a bank outcrop on the Satina river upper reach left bank reveals the presence of colluvial layers formed by debris flows with fluvial intercalations. The river channel is vertically cut into sediments of a relative depth of c. 19m and further into another 4m of the bedrock formed by thinly laminated claystones. We used grain-size, fabric, clast orientation and particle shape analyses in order to determine the genesis of the particular layers. 14 separate fluvial and colluvial layers of sediments have been distinguished in the vertical profile of the total depth of 22m. The abrupt change in valley floor development occurs throughout the Last Glacial - Interglacial cycle. The presented study is a part of wider research of the Holocene development of the Satina river incision in the Lysá hora mountain group. Detailed sedimentological analysis of a bank outcrop on the Satina river upper reach left bank reveals the presence of colluvial layers formed by debris flows with fluvial intercalations. The river channel is vertically cut into sediments of a relative depth of c. 19m and further into another 4m of the bedrock formed by thinly laminated claystones. We used grain-size, fabric, clast orientation and particle shape analyses in order to determine the genesis of the particular layers. 14 separate fluvial and colluvial layers of sediments have been distinguished in the vertical profile of the total depth of 22m.
dcterms:title
Geomorphology of the Satina river valley (Lysá hora mountain group, Moravskoslezské Beskydy Mts) Geomorphology of the Satina river valley (Lysá hora mountain group, Moravskoslezské Beskydy Mts)
skos:prefLabel
Geomorphology of the Satina river valley (Lysá hora mountain group, Moravskoslezské Beskydy Mts) Geomorphology of the Satina river valley (Lysá hora mountain group, Moravskoslezské Beskydy Mts)
skos:notation
RIV/61988987:17310/12:A13014K5!RIV13-MSM-17310___
n8:predkladatel
n9:orjk%3A17310
n3:aktivita
n19:I
n3:aktivity
I
n3:dodaniDat
n5:2013
n3:domaciTvurceVysledku
n10:8228205 n10:6169880
n3:druhVysledku
n17:D
n3:duvernostUdaju
n7:S
n3:entitaPredkladatele
n21:predkladatel
n3:idSjednocenehoVysledku
138092
n3:idVysledku
RIV/61988987:17310/12:A13014K5
n3:jazykVysledku
n15:eng
n3:klicovaSlova
sedimentology; granulometry; valley development; ERT
n3:klicoveSlovo
n4:sedimentology n4:ERT n4:valley%20development n4:granulometry
n3:kontrolniKodProRIV
[EA6FFDAF345C]
n3:mistoKonaniAkce
Sokolov
n3:nazevZdroje
Geomorfologický sborník 10
n3:obor
n12:DE
n3:pocetDomacichTvurcuVysledku
2
n3:pocetTvurcuVysledku
2
n3:rokUplatneniVysledku
n5:2012
n3:tvurceVysledku
STACKE, Václav Tábořík, Petr
n3:typAkce
n18:EUR
n3:zahajeniAkce
2012-04-18+02:00
s:numberOfPages
54
n14:hasPublisher
Ústav struktury a mechaniky hornin AV ČR, v.v.i.
n13:isbn
978-80-260-1823-0
n16:organizacniJednotka
17310