Morphostratigraphical correlation of river terraces in the central part of the Bohemian Massif with the European stratigraphical classification of the Quaternary

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F15%3A10312753" target="_blank" >RIV/00216208:11310/15:10312753 - isvavai.cz</a>

Výsledek na webu

<a href="http://dx.doi.org/10.14712/23361980.2015.87" target="_blank" >http://dx.doi.org/10.14712/23361980.2015.87</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.14712/23361980.2015.87" target="_blank" >10.14712/23361980.2015.87</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Morphostratigraphical correlation of river terraces in the central part of the Bohemian Massif with the European stratigraphical classification of the Quaternary

Popis výsledku v původním jazyce

The results of geomorphological research, focused on identification of larger remains of fluvial terrace sedimentary sequences in the Želivka, Sázava, Berounka, Vltava and Labe river-drainage basins in the Bohemian Massif, are presented. The terrace flights are characterised by a variable structure which is conditioned by the bedrock and drainage-network configuration created prior to the Pleistocene. They are formed by the specific hydrodynamic processes during the Quaternary. A series of transverse-valley profiles and longitudinal profiles have been constructed. This has enabled the differentiation of seven main terrace surfaces underlain by Quaternary fluvial sediments. However, the uppermost levels are underlain by Neogene-age deposits that comprise both fluvial and fluvio-lacustrine sediments at altitudes up to 135 m above the present valley floor. The Quaternary incision of the Sázava and Vltava valleys reaches an average depth of over 100 m. This was induced by neotectonic uplif

Název v anglickém jazyce

Morphostratigraphical correlation of river terraces in the central part of the Bohemian Massif with the European stratigraphical classification of the Quaternary

Popis výsledku anglicky

The results of geomorphological research, focused on identification of larger remains of fluvial terrace sedimentary sequences in the Želivka, Sázava, Berounka, Vltava and Labe river-drainage basins in the Bohemian Massif, are presented. The terrace flights are characterised by a variable structure which is conditioned by the bedrock and drainage-network configuration created prior to the Pleistocene. They are formed by the specific hydrodynamic processes during the Quaternary. A series of transverse-valley profiles and longitudinal profiles have been constructed. This has enabled the differentiation of seven main terrace surfaces underlain by Quaternary fluvial sediments. However, the uppermost levels are underlain by Neogene-age deposits that comprise both fluvial and fluvio-lacustrine sediments at altitudes up to 135 m above the present valley floor. The Quaternary incision of the Sázava and Vltava valleys reaches an average depth of over 100 m. This was induced by neotectonic uplif

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DE - Zemský magnetismus, geodesie, geografie

OECD FORD obor

—

Projekt

—

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2015

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Acta Universitatis Carolinae, Geographica

ISSN

0300-5402

e-ISSN

—

Svazek periodika

50

Číslo periodika v rámci svazku

1

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

11

Strana od-do

63-73

Kód UT WoS článku

—

EID výsledku v databázi Scopus

2-s2.0-84934278955