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Wojciech Wysota
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Formation of subglacial till under transient bed conditions: deposition, deformation, and basal decoupling under a Weichselian ice sheet lobe, central Poland
JA Piotrowski, NK Larsen, J Menzies, W Wysota
Sedimentology 53 (1), 83-106, 2006
1622006
Record of the Vistula ice lobe advances in the Late Weichselian glacial sequence in north-central Poland
W Wysota, P Molewski, RJ Sokołowski
Quaternary International 207 (1-2), 26-41, 2009
1202009
Ice stream motion facilitated by a shallow-deforming and accreting bed
M Spagnolo, E Phillips, JA Piotrowski, BR Rea, CD Clark, CR Stokes, ...
Nature Communications 7 (1), 10723, 2016
722016
Stratygrafia i środowiska sedymentacji zlodowacenia wisły w południowej części dolnego Powiśla
W Wysota
Wydaw. UMK, 2002
632002
Late Weichselian glacier outburst floods in North-Eastern Poland: Landform evidence and palaeohydraulic significance
P Weckwerth, W Wysota, JA Piotrowski, A Adamczyk, A Krawiec, ...
Earth-Science Reviews 194, 216-233, 2019
522019
The signature of strain magnitude in tills associated with the Vistula Ice Stream of the Scandinavian Ice Sheet, central Poland
W Narloch, JA Piotrowski, W Wysota, NK Larsen, J Menzies
Quaternary Science Reviews 57, 105-120, 2012
502012
Sedimentological record of subglacial conditions and ice sheet dynamics of the Vistula Ice Stream (north-central Poland) during the Last Glaciation
W Narloch, W Wysota, JA Piotrowski
Sedimentary Geology 293, 30-44, 2013
462013
“Glacial curvilineations”: New glacial landforms produced by longitudinal vortices in subglacial meltwater flows
JE Lesemann, JA Piotrowski, W Wysota
Geomorphology 120 (3-4), 153-161, 2010
412010
The ice/bed interface mosaic: deforming spots intervening with stable areas under the fringe of the S candinavian I ce S heet at S ampława, P oland
K Tylmann, JA Piotrowski, W Wysota
Boreas 42 (2), 428-441, 2013
392013
Chronology of the Vistulian (Weichselian) glacial events in the lower Vistula region, middle-north Poland
W Wysota, KR Lankauf, J Szmanda, A Chruscinska, HL Oczkowski, ...
Geochronometria 21, 137-142, 2002
352002
Morphology, internal composition and origin of drumlins in the southeastern part of the Chelmno-Dobrzyń Lakeland, North Poland
W Wysota
Sedimentary Geology 91 (1-4), 345-364, 1994
351994
Successive subglacial depositional processes as interpreted from basal tills in the Lower Vistula valley (N Poland)
W Wysota
Sedimentary Geology 193 (1-4), 21-31, 2007
342007
The role of subglacial features in glacialmorpho genesis of the Kujawy Dobrzyń subphase area in the southern and eastern part of the Chełmno-Dobrzyń Lakeland
W Niewiarowski, A Olszewski, W Wysota
Quaternary Studies in Poland 13, 65-76, 1995
281995
Chronologia i zasięgi nasunięć lądolodu na obszarze lobu Wisły podczas stadiału głównego ostatniego zlodowacenia
W Wysota, P Molewski
Przegląd Geologiczny 59 (3), 214-214, 2011
252011
Genesis of the ‘glacial curvilineation’landscape by meltwater processes under the former Scandinavian Ice Sheet, Poland
JE Lesemann, JA Piotrowski, W Wysota
Sedimentary Geology 312, 1-18, 2014
232014
Ice sheet maximum limit of the Vistulian Glaciation in the mid-eastern Chełmno-Dobrzyń Lakeland, northern Poland
W Wysota
Geological Quarterly 43 (2), 189-202, 1999
221999
Stratigraphy and sedimentary environments of the Weichselian Glaciation in the southern part of the Lower Vistula region
W Wysota
Rozprawa habilitacyjna, Uniwersytetu Mikołaja Kopernika w Toruniu, 1-144, 2002
182002
Till formation under a soft-bedded palaeo-ice stream of the Scandinavian Ice Sheet, constrained using qualitative and quantitative microstructural analyses
W Narloch, JA Piotrowski, W Wysota, K Tylmann
Sedimentary geology 326, 64-78, 2015
172015
Sedymentologia interstadialnej serii rzecznej (Rzęczkowo) zlodowacenia wisły (vistulian) odsłoniętej w SW krawędzi Wysoczyzny Chełmińskiej
W Wysota, KR Lankauf, P Molewski, J Szmańda
Acta Universitatis Nicolai Copernici, Geographia 28, 39-63, 1996
151996
Poziomy wysoczyznowe Wysoczyzny Brodnickiej, AUNC
W Niewiarowski, W Wysota
Geografia 19 (60), 39-46, 1986
131986
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