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Michał Makos

Biographic Data

ID6374270
NAMEMichał Makos
GIVEN NAMESMichał
FAMILY NAMEMakos
SIGNATUREMAKOS M
AFFILIATIONSUniversity of Warsaw
VERIFIEDNo
TOTAL WORKS3
TOTAL CITATIONS0
WORKS AS AUTHOR3
WORKS AS EDITOR0
FIRST PUBLICATION YEAR2013
LATEST PUBLICATION YEAR2019
H-INDEX0
  • Late Pleistocene climate of Poland in the mid-European context

    Open Access•Leszek Marks, Michał Makos et al.•ARTICLE•Quaternary International•2019

  • Timing of glacier advances and climate in the High Tatra Mountains (Western Carpathians) during the Last Glacial Maximum

    Open Access•Michał Makos, Jan Dzierżek et al.•ARTICLE•Quaternary Research•2014

    During the Last Glacial Maximum (LGM), long valley glaciers developed on the northern and southern sides of the High Tatra Mountains, Poland and Slovakia. Chlorine-36 exposure dating of moraine boulders suggests two major phases of moraine stabilization, at 26–21 ka (LGM I — maximum) and at 18 ka (LGM II). The dates suggest a significantly earlier maximum advance on the southern side of the range. Reconstructing the geometry of four glaciers in t…

  • Deglaciation chronology and paleoclimate of the Pięciu Stawów Polskich/Roztoki Valley, high Tatra Mountains, Western Carpathians, since the Last Glacial Maximum, inferred from 36Cl exposure dating and…

    Open Access•Michał Makos, Jerzy Nitychoruk et al.•ARTICLE•Quaternary International•2013

No prominent works on this page.

  • Deglaciation chronology and paleoclimate of the Pięciu Stawów Polskich/Roztoki Valley, high Tatra Mountains, Western Carpathians, since the Last Glacial Maximum, inferred from 36Cl exposure dating and…

    Open Access•Michał Makos, Jerzy Nitychoruk et al.•ARTICLE•Quaternary International•2013

  • Timing of glacier advances and climate in the High Tatra Mountains (Western Carpathians) during the Last Glacial Maximum

    Open Access•Michał Makos, Jan Dzierżek et al.•ARTICLE•Quaternary Research•2014

    During the Last Glacial Maximum (LGM), long valley glaciers developed on the northern and southern sides of the High Tatra Mountains, Poland and Slovakia. Chlorine-36 exposure dating of moraine boulders suggests two major phases of moraine stabilization, at 26–21 ka (LGM I — maximum) and at 18 ka (LGM II). The dates suggest a significantly earlier maximum advance on the southern side of the range. Reconstructing the geometry of four glaciers in t…

  • Late Pleistocene climate of Poland in the mid-European context

    Open Access•Leszek Marks, Michał Makos et al.•ARTICLE•Quaternary International•2019

Climatology (3 works) · Geography (3 works) · Geology and Paleoclimatology Research (3 works) · Glacial period (3 works) · Glacier (3 works) · Physical geography (3 works) · Climate change (2 works) · Geology (2 works) · Geomorphology (2 works) · Last Glacial Maximum (2 works)

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