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Marek Kasprzak

Biographic Data

ID237229
NAMEMarek Kasprzak
GIVEN NAMESMarek
FAMILY NAMEKasprzak
SIGNATUREKASPRZAK M
AFFILIATIONSUniversity of Wrocław
ORCID0000-0002-8265-8441
VERIFIEDYes
TOTAL WORKS8
TOTAL CITATIONS14
WORKS AS AUTHOR8
WORKS AS EDITOR0
FIRST PUBLICATION YEAR2019
LATEST PUBLICATION YEAR2026
H-INDEX2
  • Long-term effects of mining activities in the karst area

    Open Access•Marta Sadkiewicz, Marek Kasprzak•ARTICLE•Anthropocene•2026

  • Ice jams and spring flooding across Ostrobothnia

    Open Access•Marek Kasprzak, Alun Hubbard•ARTICLE•Nordia Geographical Publications•2025

    Seasonal snow and ice play a key role in the hydrological regimes of Arctic and sub-Arctic river catchments that differentiate them from their lower latitude counterparts. Against a backdrop of assumed reduced spring flooding due to ongoing Arctic warming resulting in shorter winters with less snowfall, we examine the prevailing conditions that led to spring-melt flooding, its impact and mitigation management strategies across Northern Ostrobothn…

  • Geomorphic evidence of extreme events in the High Arctic (Wedel Jarlsberg Land, Svalbard)

    Open Access•Marek Kasprzak•ARTICLE•Nordia Geographical Publications•2025

    Among the geomorphological processes determined by meteorological conditions, topography, and geological factors, floods and various mass movements have an extreme origin. In the High Arctic, which is the domain of cryogenic processes, extreme events can reach a scale and intensity never before observed, considering the exceptionally rapid environmental changes caused by global warming. It is widely believed that the frequency of extreme events w…

  • Spatial and temporal patterns of near‐surface ground temperature in the Arctic mountain catchment

    Open Access•Marek Kasprzak, Mariusz Szymanowski•ARTICLE•Land Degradation and Development•2023

    We consider the case of a mountain catchment representative of southwest Spitsbergen to investigate the spatial and temporal variation in temperature of the near‐surface ground. We set up 20 thermistor strings distributed in different parts of the catchment, combine the measured data with land surface temperature (LST) retrieved from Landsat imagery, and verify the depth of ground thawing using electrical resistivity tomography. Under current cli…

  • Eurasian Animals and Quaternary Environments

    Open Access•Krzysztof Stefaniak, Thijs Van Kolfschoten et al.•ARTICLE•Quaternary International•2022

  • Middle Palaeolithic, Transitional or Upper Palaeolithic

    Open Access•Andrzej Wiśniewski, Zdzisław Jary et al.•ARTICLE•Quaternary International•2021•Cited by: 1•References: 51

  • Colluvial sediments originating from past land-use activities in the Erzgebirge Mountains, Central Europe

    Open Access•K Kaiser, Johann Friedrich Tolksdorf et al.•ARTICLE•Archaeological and Anthropological…•2021•Cited by: 8•References: 68

    Colluvial sediments originating from soil erosion on slopes have proven to constitute significant evidence for tracing past human impact on mountain landscapes. In the Central European Erzgebirge (Ore) Mountains, colluvial sediments are associated with specific landforms (footslopes, slope flattenings, dells) and cover a share of 11% (11,905 ha) of the regional soil landscape. Thirteen pedosedimentary sections with colluvial layers were investiga…

  • Taphonomic and paleoecological aspects of large mammals from Sudety Mts (Silesia, SW Poland), with particular interest to the carnivores

    Open Access•Adrian Marciszak, Artur Sobczyk et al.•ARTICLE•Quaternary International•2019•Cited by: 5•References: 20

  • Colluvial sediments originating from past land-use activities in the Erzgebirge Mountains, Central Europe

    Open Access•K Kaiser, Johann Friedrich Tolksdorf et al.•ARTICLE•Archaeological and Anthropological…•2021•Cited by: 8•References: 68

    Colluvial sediments originating from soil erosion on slopes have proven to constitute significant evidence for tracing past human impact on mountain landscapes. In the Central European Erzgebirge (Ore) Mountains, colluvial sediments are associated with specific landforms (footslopes, slope flattenings, dells) and cover a share of 11% (11,905 ha) of the regional soil landscape. Thirteen pedosedimentary sections with colluvial layers were investiga…

  • Taphonomic and paleoecological aspects of large mammals from Sudety Mts (Silesia, SW Poland), with particular interest to the carnivores

    Open Access•Adrian Marciszak, Artur Sobczyk et al.•ARTICLE•Quaternary International•2019•Cited by: 5•References: 20

  • Middle Palaeolithic, Transitional or Upper Palaeolithic

    Open Access•Andrzej Wiśniewski, Zdzisław Jary et al.•ARTICLE•Quaternary International•2021•Cited by: 1•References: 51

  • Taphonomic and paleoecological aspects of large mammals from Sudety Mts (Silesia, SW Poland), with particular interest to the carnivores

    Open Access•Adrian Marciszak, Artur Sobczyk et al.•ARTICLE•Quaternary International•2019•Cited by: 5•References: 20

  • Middle Palaeolithic, Transitional or Upper Palaeolithic

    Open Access•Andrzej Wiśniewski, Zdzisław Jary et al.•ARTICLE•Quaternary International•2021•Cited by: 1•References: 51

  • Colluvial sediments originating from past land-use activities in the Erzgebirge Mountains, Central Europe

    Open Access•K Kaiser, Johann Friedrich Tolksdorf et al.•ARTICLE•Archaeological and Anthropological…•2021•Cited by: 8•References: 68

    Colluvial sediments originating from soil erosion on slopes have proven to constitute significant evidence for tracing past human impact on mountain landscapes. In the Central European Erzgebirge (Ore) Mountains, colluvial sediments are associated with specific landforms (footslopes, slope flattenings, dells) and cover a share of 11% (11,905 ha) of the regional soil landscape. Thirteen pedosedimentary sections with colluvial layers were investiga…

  • Eurasian Animals and Quaternary Environments

    Open Access•Krzysztof Stefaniak, Thijs Van Kolfschoten et al.•ARTICLE•Quaternary International•2022

  • Spatial and temporal patterns of near‐surface ground temperature in the Arctic mountain catchment

    Open Access•Marek Kasprzak, Mariusz Szymanowski•ARTICLE•Land Degradation and Development•2023

    We consider the case of a mountain catchment representative of southwest Spitsbergen to investigate the spatial and temporal variation in temperature of the near‐surface ground. We set up 20 thermistor strings distributed in different parts of the catchment, combine the measured data with land surface temperature (LST) retrieved from Landsat imagery, and verify the depth of ground thawing using electrical resistivity tomography. Under current cli…

  • Ice jams and spring flooding across Ostrobothnia

    Open Access•Marek Kasprzak, Alun Hubbard•ARTICLE•Nordia Geographical Publications•2025

    Seasonal snow and ice play a key role in the hydrological regimes of Arctic and sub-Arctic river catchments that differentiate them from their lower latitude counterparts. Against a backdrop of assumed reduced spring flooding due to ongoing Arctic warming resulting in shorter winters with less snowfall, we examine the prevailing conditions that led to spring-melt flooding, its impact and mitigation management strategies across Northern Ostrobothn…

  • Geomorphic evidence of extreme events in the High Arctic (Wedel Jarlsberg Land, Svalbard)

    Open Access•Marek Kasprzak•ARTICLE•Nordia Geographical Publications•2025

    Among the geomorphological processes determined by meteorological conditions, topography, and geological factors, floods and various mass movements have an extreme origin. In the High Arctic, which is the domain of cryogenic processes, extreme events can reach a scale and intensity never before observed, considering the exceptionally rapid environmental changes caused by global warming. It is widely believed that the frequency of extreme events w…

  • Long-term effects of mining activities in the karst area

    Open Access•Marta Sadkiewicz, Marek Kasprzak•ARTICLE•Anthropocene•2026

Geology (7 works) · Geography (6 works) · Paleontology (4 works) · Archaeology (3 works) · Geology and Paleoclimatology Research (3 works) · Physical geography (3 works) · Pleistocene-Era Hominins and Archaeology (3 works) · Alluvium (2 works) · Archaeology and ancient environmental studies (2 works) · Cave (2 works)

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