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Statements

Subject Item
n2:RIV%2F00216208%3A11310%2F07%3A10118646%21RIV12-MSM-11310___
rdf:type
n10:Vysledek skos:Concept
dcterms:description
The first set of U-series ages of the hot-spring travertine from the world-famous Karlovy Vary Spa indicates repeated growth of the travertine accumulation followed by its erosion by the Tepla River. The obtained data are important as an estimate of minimum duration of thermal water circulation in Karlovy Vary and in understanding of the river valley evolution during the youngest geological history. The oldest Th-230/U-234 age data (230 +/- 14 ka BP and 155 +/- 7 ka BP) have been obtained for travertine relicts located 22 in above the present-day bottom of the valley. The extensive travertine accumulation located directly on the valley bottom was formed by gradual growth, particularly during the first half of the Weichselian period, between 100 and 50 ka BP. These data show that the valley bottom was at approximately the same elevation as it is today already during the Eemian interglacial. At the end of the Weichselian the central part of the travertine accumulation was downcut by river erosion. During Holocene the new deposition of travertine was concentrated in this wide trench, being likely repeatedly modified by river activity. The travertine accumulation started to be strongly influenced by humans since the Middle Ages. A significant part of it was quarried out for lime production. The accumulation was later covered by buildings, streets and the reinforced course of the Tepla River. The first set of U-series ages of the hot-spring travertine from the world-famous Karlovy Vary Spa indicates repeated growth of the travertine accumulation followed by its erosion by the Tepla River. The obtained data are important as an estimate of minimum duration of thermal water circulation in Karlovy Vary and in understanding of the river valley evolution during the youngest geological history. The oldest Th-230/U-234 age data (230 +/- 14 ka BP and 155 +/- 7 ka BP) have been obtained for travertine relicts located 22 in above the present-day bottom of the valley. The extensive travertine accumulation located directly on the valley bottom was formed by gradual growth, particularly during the first half of the Weichselian period, between 100 and 50 ka BP. These data show that the valley bottom was at approximately the same elevation as it is today already during the Eemian interglacial. At the end of the Weichselian the central part of the travertine accumulation was downcut by river erosion. During Holocene the new deposition of travertine was concentrated in this wide trench, being likely repeatedly modified by river activity. The travertine accumulation started to be strongly influenced by humans since the Middle Ages. A significant part of it was quarried out for lime production. The accumulation was later covered by buildings, streets and the reinforced course of the Tepla River.
dcterms:title
Evolution of hot-spring travertine accumulation in Karlovy Vary/Carlsbad (Czech Republic) and its significance for the evolution of Tepla valley and Ohre/Eger rift Evolution of hot-spring travertine accumulation in Karlovy Vary/Carlsbad (Czech Republic) and its significance for the evolution of Tepla valley and Ohre/Eger rift
skos:prefLabel
Evolution of hot-spring travertine accumulation in Karlovy Vary/Carlsbad (Czech Republic) and its significance for the evolution of Tepla valley and Ohre/Eger rift Evolution of hot-spring travertine accumulation in Karlovy Vary/Carlsbad (Czech Republic) and its significance for the evolution of Tepla valley and Ohre/Eger rift
skos:notation
RIV/00216208:11310/07:10118646!RIV12-MSM-11310___
n3:aktivita
n4:Z n4:I
n3:aktivity
I, Z(AV0Z30130516)
n3:cisloPeriodika
4
n3:dodaniDat
n19:2012
n3:domaciTvurceVysledku
n15:1265075
n3:druhVysledku
n17:J
n3:duvernostUdaju
n6:S
n3:entitaPredkladatele
n9:predkladatel
n3:idSjednocenehoVysledku
420867
n3:idVysledku
RIV/00216208:11310/07:10118646
n3:jazykVysledku
n18:eng
n3:klicovaSlova
tufas; history; Czechoslovakia; system; series; Bohemian Massif
n3:klicoveSlovo
n5:system n5:history n5:tufas n5:Czechoslovakia n5:Bohemian%20Massif n5:series
n3:kodStatuVydavatele
DE - Spolková republika Německo
n3:kontrolniKodProRIV
[2A88CB4B7C5F]
n3:nazevZdroje
Zeitschrift für Geomorphologie
n3:obor
n12:DB
n3:pocetDomacichTvurcuVysledku
1
n3:pocetTvurcuVysledku
5
n3:rokUplatneniVysledku
n19:2007
n3:svazekPeriodika
51
n3:tvurceVysledku
Žák, Karel Cílek, Václav Vylita, Tomáš Hercman, Helena Mikšíková, Lucie
n3:wos
000251949900002
n3:zamer
n16:AV0Z30130516
s:issn
0372-8854
s:numberOfPages
16
n8:doi
10.1127/0372-8854/2007/0051-0427
n13:organizacniJednotka
11310