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Andrzej Traczyk
Researcher at University of Wrocław
Publications - 20
Citations - 228
Andrzej Traczyk is an academic researcher from University of Wrocław. The author has contributed to research in topics: Glacier & Glacial period. The author has an hindex of 7, co-authored 20 publications receiving 183 citations.
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10Be exposure age chronology of the last glaciation in the Krkonoše Mountains, Central Europe
TL;DR: In this paper, a new chronology of the last glaciation is established for the Krkonose (Giant) Mountains, Central Europe, based on in-situ produced 10Be in moraine boulders.
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On the potential for a bottom active layer below coastal permafrost: the impact of seawater on permafrost degradation imaged by electrical resistivity tomography (Hornsund, SW Spitsbergen)
Marek Kasprzak,Mateusz C. Strzelecki,Andrzej Traczyk,Marta Kondracka,Michael Lim,Krzysztof Migała +5 more
TL;DR: In this paper, the results of two-dimensional electrical resistivity tomography (ERT) of permafrost developed in coastal zone of Hornsund, SW Spitsbergen were presented.
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How high - resolution DEM based on airborne LiDAR helped to reinterpret landforms : examples from the Sudetes, SW Poland
TL;DR: In this paper, the authors review recent advances in landform mapping and interpretation in the mountainous terrain of the Sudetes (SW Poland), possible due to the availability of high-resolution airborne LiDAR data.
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Use of 10 Be exposure ages and Schmidt hammer data for correlation of moraines in the Krkonoše Mountains, Poland/Czech Republic
TL;DR: In this article, exposure ages and relative-age data are presented from eight sites in the Łomnica andŁomniczka valleys to provide essential information for reconstructing local glaciation chronology.
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LiDAR and 2D Electrical Resistivity Tomography as a Supplement of Geomorphological Investigations in Urban Areas: a Case Study from the City of Wrocław (SW Poland)
Marek Kasprzak,Andrzej Traczyk +1 more
TL;DR: In this article, the authors presented a method of using and linking these sources of spatial information about landforms in such areas, which can be used in such a specific environment to reconstruct natural, buried terrain morphology.