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

Result code in IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F16%3A10324125" target="_blank" >RIV/00216208:11310/16:10324125 - isvavai.cz</a>

Alternative codes found

RIV/67985891:_____/16:00487921

Result on the web

<a href="http://www.earthquakegeology.com/materials/proceedings/2016_Crestone.pdf" target="_blank" >http://www.earthquakegeology.com/materials/proceedings/2016_Crestone.pdf</a>

DOI - Digital Object Identifier

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Result language

angličtina

Original language name

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

Original language description

Biala Lądecka (Biala Kłodzka) river is located in Lower Silesia (Poland) and its valley separates Góry Złote Mts. (Rychlebské hory Mts.) on the northeast from Góry Bialskie Mts. on the southwest. We investigated geomorphology research of the Biala Lądecka river basin, in order to determine if Quarternary tectonic activity at the Sudetic Marginal Fault is contributing to the river's assymetry. Previous research provided in adajcent area by L. Finckh and G. Götzinger (1931), W. Walczak (1954) and A. Ivan (1966), Biala Lądecka river used to flow across the Góry Złote Mts. directly to Oderská nížina Lowland during Pliocene; currently it flows to Nysa Kłodzka Basin. Our research was focused on analysis of all available cartographic materials (geological and topographic maps), available literature and own detail geomorphological mapping of selected landforms. Spatial distribution of these landforms such as gullies, erosion trenches, dellens, alluvial plains, alluvial fans, springs, swamps, river terraces, could potentially indicate recent tectonic activity in the studied area. Moreover, stream network parameters (measured using DEM data) such as changes in erosion intensity indicated in longitudinal and cross-section profiles, slope gradient and morphometric indexes, e.g. Stream Length (SL) index (Hack 1973), for Biala Ladecka river basin were analyzed. In selected places geophysical measures were used was also performed to discover locations of sediments of the Biala Lądecka paleoriver.

Czech name

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Czech description

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Type

D - Article in proceedings

CEP classification

DC - Seismology, volcanology and Earth structure

OECD FORD branch

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Project

<a href="/en/project/LH12078" target="_blank" >LH12078: Assessment of Tectonic Movements on Active Faults</a><br>

Continuities

S - Specificky vyzkum na vysokych skolach<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Publication year

2016

Confidentiality

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

Article name in the collection

Proceedings of the 7th International INQUA Workshop on Paleoseismology, Active Tectonics and Archaeoseismology

ISBN

978-0-9974355-2-8

ISSN

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e-ISSN

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Number of pages

4

Pages from-to

234-237

Publisher name

INQUA Focus Group 'Earthquake Geology and Seismic Hazards - EGSHaz'

Place of publication

Crestone

Event location

Creston, Colorado, USA

Event date

May 30, 2016

Type of event by nationality

WRD - Celosvětová akce

UT code for WoS article

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