Výsledky vyhledávání - "Tomasz Salamon"

Ice-crevasse sedimentation in the eastern part of the Głubczyce Plateau (S Poland) during the final stage of the Drenthian Glaciation

Autor: Tomasz Salamon

Publikováno v: Open Geosciences, Vol 12, Iss 1, Pp 726-736 (2020)

Glacial sediments in the eastern part of the Głubczyce Plateau, at the Krowiarki site, were studied. Two units were distinguished within the sedimentary succession. The lower unit is composed of mainly sandy sediments with diamicton interbeds, the u

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d1725230bc0985ee07efcc4119af38b5
https://doi.org/10.1515/geo-2020-0182

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Response of a mountain‐foreland fluvial system to an advancing ice sheet, southern Poland

Autor: Tomasz Salamon, Tomasz Zieliński

Publikováno v: Boreas. 48:695-712

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::cf0d86b7929c394c56e5c5f036f49630
https://doi.org/10.1111/bor.12389

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Sedimentary and structural record of the Scandinavian Ice Sheet margin dynamics at the SE part of the Głubczyce Plateau, a foreland of the East Sudetes Mountains (S Poland)

Autor: Tomasz Salamon

Publikováno v: Geomorphology. 413:108349

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::ccb53ec8b600f4c6752f3199e4f10150
https://doi.org/10.1016/j.geomorph.2022.108349

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A rare signature of subglacial outburst floods developed along structural ice weaknesses in the southern sector of the Scandinavian Ice Sheet during the Drenthian Glaciation, S Poland

Autor: Maciej J. Mendecki, Tomasz Salamon

Publikováno v: Geomorphology. 378:107593

We present the study of a subglacial drainage system that developed in the base of the Scandinavian Ice Sheet at the border of the Silesian Lowland and Silesian Upland (southern Poland) during the Drenthian Glaciation as a result of large outburst fl

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::febbdb1b0954671e9f9376e51b5b22af
https://doi.org/10.1016/j.geomorph.2021.107593

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Subglacial conditions and Scandinavian Ice Sheet dynamics at the coarse-grained substratum of the fore-mountain area of southern Poland

Autor: Tomasz Salamon

Publikováno v: Quaternary Science Reviews. 151:72-87

The fore-mountain areas of southern Poland are locally composed of the coarse-grained sediments of alluvial fans, which created unusual conditions under the advancing Scandinavian Ice Sheet during the Elsterian glaciation. This highly permeable subst

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::d461164be3e68d167f4bd6fa4fc626f4
https://doi.org/10.1016/j.quascirev.2016.09.002

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Sedimentary record of a Scandinavian Ice Sheet drainage system and till deposition over subglacial obstacles promoting basal sliding (an example from southern Poland)

Autor: Tomasz Salamon

Publikováno v: Sedimentary Geology. 330:108-121

Subglacial obstacles occurring in the path of advancing ice sheets generally generate higher longitudinal compression and higher frictional drag than a flat substrate. However, in the case of a soft sediment substratum, they can have a very different

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::c19129404e4e2cf476e485924b893235
https://doi.org/10.1016/j.sedgeo.2015.10.005

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Development of the topography-controlled Upper Odra ice lobe (Scandinavian Ice Sheet) in the fore-mountain area of southern Poland during the Saalian glaciation

Autor: Tomasz Salamon

Publikováno v: Quaternary Science Reviews. 123:1-15

During the Saalian (Drenthe) glaciation, the Upper Odra ice lobe constituted the most southern part of the Scandinavian Ice Sheet in central Europe. The lobe was situated in an area with varied topography in the foreland of a mountain range. The ice

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::8d1822aa34003037e0cc6035f562a249
https://doi.org/10.1016/j.quascirev.2015.05.033

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Reply to comment by D. Nývlt on 'Development of the topography-controlled Upper Odra ice lobe (Scandinavian Ice Sheet) in the fore-mountain area of southern Poland during the Saalian glaciation'

Autor: Tomasz Salamon

Publikováno v: Quaternary Science Reviews. 133:185-187

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::46a208dbe2a3e1ddf3ee33d77b398ac1
https://doi.org/10.1016/j.quascirev.2015.12.008

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Elsterian ice sheet dynamics in a topographically varied area (southern part of the Racibórz–Oświęcim Basin and its vicinity, southern Poland)

Autor: Tomasz Salamon

Publikováno v: Geological Quarterly. 61

During the Elsterian Glaciation, the Scandinavian Ice Sheet, before reaching its maximum extent, advanced over the mountainous foreland of Southern Poland, which was characterized by a substrate of increasingly varied relief. One such area was the hi

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::cdd97d11345b0c015e1412ead912d760
https://doi.org/10.7306/gq.1350

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The alleged Early Palaeolithic artefacts are in reality geofacts: a revision of the site of Kończyce Wielkie 4 in the Moravian Gate, South Poland

Autor: Tomasz Salamon, Andrzej Wiśniewski, Józef Lewandowski, Janusz Badura

Publikováno v: Journal of Archaeological Science. 52:189-203

In this paper we show that a site Konczyce Wielkie 4 (SW Poland) published in JAS (2010a) by Foltyn et al. can no longer be accepted as a reliable evidence for the oldest presence of humans in the northern part of Carpathians and Sudetes Mountains (M

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::c50314c205973e72bccf225b13e4cc15
https://doi.org/10.1016/j.jas.2014.07.022

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