Number of the records: 1  

Valley evolution of the Biala Lądecka drainage network during late Cenozoic, Lower Silesia, Poland

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    SYSNO ASEP0486348
    Document TypeC - Proceedings Paper (int. conf.)
    R&D Document TypeConference Paper
    TitleValley evolution of the Biala Lądecka drainage network during late Cenozoic, Lower Silesia, Poland
    Author(s) Stemberk, Jakub (USMH-B) ORCID, RID, SAI
    Štěpančíková, Petra (USMH-B) RID, ORCID, SAI
    Tábořík, Petr (USMH-B) RID, ORCID
    Coubal, Miroslav (USMH-B)
    Source TitleProceedings of the 8th International INQUA Meeting on Paleoseismology, Active Tectonics and Archeoseismology. Handbook and Programme. 13-16 November 2017. - Lower Hutt : GNS Science, 2017 - ISSN 1177-2441 - ISBN 978-1-98-853036-9
    Pagess. 374-377
    Number of pages4 s.
    Publication formOnline - E
    ActionInternational INQUA Meeting on Paleoseismology, Active Tectonics and Archeoseismology /8./
    Event date13.11.2017 - 16.11.2017
    VEvent locationBlenheim
    CountryNZ - New Zealand
    Event typeWRD
    Languageeng - English
    CountryNZ - New Zealand
    KeywordsPoland - Czech border ; NE Europe ; stable continental areas ; Biala Lądecka river ; Bělský fault ; morphometric indexes ; DEM analysis
    Subject RIVDB - Geology ; Mineralogy
    OECD categoryGeology
    R&D ProjectsLH12078 GA MŠMT - Ministry of Education, Youth and Sports (MEYS)
    Institutional supportUSMH-B - RVO:67985891
    AnnotationBiala Lądecka (Biala Kłodzka) river is located in Lower Silesia (Poland) and its valley separates Góry Złote Mts. (Rychlebské hory Mts.) on the NE from Góry Bialskie Mts. on the SW. We conducted geomorphic investigations on the Biala Lądecka river basin, in order to determine if Quarternary tectonic activity at the Bělský fault (or near Marginal Sudetic fault) is contributing to the river’s asymmetry. Our research was focused on analysis of selected landforms, DEM parameters, morphometric indexes and their spatial distribution which could potentially indicate recent tectonic activity in the area. At selected places geophysical measures were used to discover proper location and structure of Bělský fault or presence of suggested morpholineaments. Preliminary results suggest a Quaternary tectonic activity for the Bělský fault. Moreover we tried to clarify nowadays stress regime in study area based striae measurement on fault planes and precise monitoring of selected faults using TM-71 device.
    WorkplaceInstitute of Rock Structure and Mechanics
    ContactIva Švihálková, svihalkova@irsm.cas.cz, Tel.: 266 009 216
    Year of Publishing2018
Number of the records: 1  

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