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

Kód výsledku v 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>

Nalezeny alternativní kódy

RIV/67985891:_____/16:00487921

Výsledek na webu

<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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Jazyk výsledku

angličtina

Název v původním jazyce

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

Popis výsledku v původním jazyce

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.

Název v anglickém jazyce

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

Popis výsledku anglicky

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.

Druh

D - Stať ve sborníku

CEP obor

DC - Seismologie, vulkanologie a struktura Země

OECD FORD obor

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Projekt

<a href="/cs/project/LH12078" target="_blank" >LH12078: Hodnocení tektonických pohybů na aktivních zlomech</a><br>

Návaznosti

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

Rok uplatnění

2016

Kód důvěrnosti údajů

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

Název statě ve sborníku

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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Počet stran výsledku

4

Strana od-do

234-237

Název nakladatele

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

Místo vydání

Crestone

Místo konání akce

Creston, Colorado, USA

Datum konání akce

30. 5. 2016

Typ akce podle státní příslušnosti

WRD - Celosvětová akce

Kód UT WoS článku

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