Electrical Resistivity in Post-glacial Measurements on Western Pomerania, Poland
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Anna Wysowska-Swiebodzinska
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| Transactions of the VSB - Technical University of Ostrava, Civil Engineering Series |
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2008, Volume 8, Issue 2, Pages 335-340
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Doi: Not indexed
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Determining physical properties of postglacial deposits was an aim of examinations and on the basis of disintegrations of value of the resistance examining the spatial lengthiness of these structures. Two measuring profiles were made at applying depicting the resistivity imaging method. This method let the appropriate resistance of layers for determining the thickness and disintegrations in checked structures: layer of deposit kame on average 20 m (sands and graveles) and layer of boulder clays on average 30 m. Outside these two layers on the second profile transitional layer was determined, probably it is weater level about disturbed geological construction, which results around transgressive of character of glaciation of the Pomeranian phase. In the first profile beneath the layer of boulder clays a level of sands was reached, most probably Miocene.
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