Number of the records: 1
Valley evolution of the Biala Lądecka drainage network during late Cenozoic, Lower Silesia, Poland
- 1.
SYSNO ASEP 0486348 Document Type C - Proceedings Paper (int. conf.) R&D Document Type Conference Paper Title Valley 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 Title Proceedings 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 Pages s. 374-377 Number of pages 4 s. Publication form Online - E Action International INQUA Meeting on Paleoseismology, Active Tectonics and Archeoseismology /8./ Event date 13.11.2017 - 16.11.2017 VEvent location Blenheim Country NZ - New Zealand Event type WRD Language eng - English Country NZ - New Zealand Keywords Poland - Czech border ; NE Europe ; stable continental areas ; Biala Lądecka river ; Bělský fault ; morphometric indexes ; DEM analysis Subject RIV DB - Geology ; Mineralogy OECD category Geology R&D Projects LH12078 GA MŠMT - Ministry of Education, Youth and Sports (MEYS) Institutional support USMH-B - RVO:67985891 Annotation Biala 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.
Workplace Institute of Rock Structure and Mechanics Contact Iva Švihálková, svihalkova@irsm.cas.cz, Tel.: 266 009 216 Year of Publishing 2018
Number of the records: 1