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Application of electrical and electromagnetic methods to study sedimentary covers in high mountain areas
Authors:Sylwia Tomecka-Suchoń  Bogdan ?oga?a  Tomis?aw Go??biowski  Gra?yna Dzik  Tomasz Dzik  Krzysztof Jochymczyk
Institution:1.Department of Geophysics, Faculty of Geology, Geophysics and Environmental Protection,AGH University of Science and Technology,Cracow,Poland;2.Department of Applied Geology, Faculty of Earth Sciences,Silesian University,Sosnowiec,Poland;3.Division of Geodesy, Geophysics and Engineering Geology, Department of Geotechnics, Faculty of Environmental Engineering,Cracow University of Technology,Cracow,Poland;4.Institute of Innovative Technologies EMAG,Katowice,Poland;5.Geofizyka Kraków SA,Cracow,Poland
Abstract:The results of geophysical studies conducted with selected electrical and electromagnetic methods in the Kondratowa Valley in the Tatra Mountains (the Carpathian Mountains, Poland) are presented in the article. The surveys were performed with the following methods: electrical resistivity tomography (ERT), georadar (GPR) and conductivity meter (CM). The objective of the noninvasive geophysical measurements was to determine the thickness of the Quaternary postglacial sediments that fill the bottom of the valley and to designate the accumulation of boulders deposited on Quaternary sediments. The results of ERT surveys conducted along the axis of the valley allowed to determine the changeability of the thickness of the postglacial sediments and allowed to designate a few areas of occurrence of boulders. The ERT, GPR and CM surveys conducted across the valley allowed to designate with high accuracy the thickness of the accumulation of boulders sliding down the valley bottom from the couloirs surrounding the valley.
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