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Max Maisch

Biographic Data

ID3751380
NAMEMax Maisch
GIVEN NAMESMax
FAMILY NAMEMaisch
SIGNATUREMAISCH M
AFFILIATIONSUniversity of Zurich
VERIFIEDNo
TOTAL WORKS9
TOTAL CITATIONS1
AUTHOR COUNT9
EDITOR COUNT0
FIRST PUBLICATION YEAR1982
LATEST PUBLICATION YEAR2018
H-INDEX1
  • Piecing together the Lateglacial advance phases of the Reussgletscher (central Swiss Alps)

    Open Access•Max Boxleitner, Ivy-Och et al.•ARTICLE•Geographica Helvetica•2018

    Exposure dating has substantially improved our knowledge about glacier advances during the Younger Dryas (YD) and the early Holocene. The glacier development after the Last Glacial Maximum (LGM) and the timing of morphologically evidenced, earlier Lateglacial re-advances is, however, still widely unknown. In this study we used 10Be surface exposure and radiocarbon dating to address these phases and corresponding landforms in the catchment of the …

  • Multi-methodological reconstruction of the lake level at Morgarten in the context of the history of the Swiss Confederation

    Open Access•M Egli, Max Maisch et al.•ARTICLE•The Holocene•2015•References: 1

    In AD 1315, the Habsburgs fought against the Swiss Confederation at Morgarten. Since historical records are very limited, the battle has been the subject of very controversial discussions. Its location and outcome seem likely to have been influenced by the landscape and the size of the Aegeri lake, but only sparse and contradictory information are available. Numerical, semi-quantitative and relative dating techniques were applied to reconstruct t…

  • Combination of Numerical Dating Techniques Using 10 Be in Rock Boulders and 14 C of Resilient Soil Organic Matter for Reconstructing the Chronology of Glacial and Periglacial Processes in a High Alpin…

    Open Access•Filippo Favilli, M Egli et al.•ARTICLE•Radiocarbon•2009•Cited by: 1•References: 49

    Glacier fluctuations and paleoclimatic oscillations during the Late Quaternary in Val di Rabbi (Trentino, northern Italy) were reconstructed using a combination of absolute dating techniques ( 14 C and 10 Be) and soil chemical characterization. Extraction and dating of the stable fraction of soil organic matter (SOM) gave valuable information about the minimum age of soil formation and contributed to the deciphering of geomorphic surface dynamics…

  • Mensch - Umwelt - Klima

    Open Access•Max Maisch, Frank Preusser•ARTICLE•Geographica Helvetica•2008

    No abstract available

  • Klimaänderung und Gletscherskitourismus

    Open Access•Bruno Abegg, U König et al.•ARTICLE•Geographica Helvetica•1994

    No abstract available

  • Zum neuzeitlichen, gegenwärtigen und zukünftigen Gletscherschwund in Graubünden

    Open Access•Max Maisch•ARTICLE•Geographica Helvetica•1991

    No abstract available

  • Die Gletscher um "1850" und "Heute" im Bünderland und in den angrenzenden Gebieten

    Open Access•Max Maisch•ARTICLE•Geographica Helvetica•1987

    An inventory of data for the extent of ice in 1850 is presented and compared to the extent of alpine glaciers in 1973 as recorded by the Swiss glacier inventory. Special attention is given to the position and spatial Variation of snowline altitudes based on data for the general ice retreat between 1850 and 1973. The ränge of snowline altitudes (as given by the 2 :1 -equilibrium line calculation) reflects the topography and the related change from…

  • Zur Gletscher-, Vegetations- und Klimageschichte der Schweiz seit der Späteiszeit

    Open Access•Gerhard Furrer, C Burga et al.•ARTICLE•Geographica Helvetica•1987

    A Statistical analysis of published and compilated snowline data for the late-glacial Stades of Gschnitz, Clavadel, Daun and Egesen is presented. The calculation of snowline and snowline-depression (compared to the extent of 1850) is based on the 2: 1 -equilibrium line method. The Interpretation does not show significant differences in snowline-depression between the Lower Engadin (Eastern Alps) and the Mont Blanc area (Western Alps). The larger …

  • Zur Gletscher- und Klimageschichte des alpinen Spätglazials

    Open Access•Max Maisch•ARTICLE•Geographica Helvetica•1982

    No abstract available

  • Combination of Numerical Dating Techniques Using 10 Be in Rock Boulders and 14 C of Resilient Soil Organic Matter for Reconstructing the Chronology of Glacial and Periglacial Processes in a High Alpin…

    Open Access•Filippo Favilli, M Egli et al.•ARTICLE•Radiocarbon•2009•Cited by: 1•References: 49

    Glacier fluctuations and paleoclimatic oscillations during the Late Quaternary in Val di Rabbi (Trentino, northern Italy) were reconstructed using a combination of absolute dating techniques ( 14 C and 10 Be) and soil chemical characterization. Extraction and dating of the stable fraction of soil organic matter (SOM) gave valuable information about the minimum age of soil formation and contributed to the deciphering of geomorphic surface dynamics…

  • Zur Gletscher- und Klimageschichte des alpinen Spätglazials

    Open Access•Max Maisch•ARTICLE•Geographica Helvetica•1982

    No abstract available

  • Die Gletscher um "1850" und "Heute" im Bünderland und in den angrenzenden Gebieten

    Open Access•Max Maisch•ARTICLE•Geographica Helvetica•1987

    An inventory of data for the extent of ice in 1850 is presented and compared to the extent of alpine glaciers in 1973 as recorded by the Swiss glacier inventory. Special attention is given to the position and spatial Variation of snowline altitudes based on data for the general ice retreat between 1850 and 1973. The ränge of snowline altitudes (as given by the 2 :1 -equilibrium line calculation) reflects the topography and the related change from…

  • Zur Gletscher-, Vegetations- und Klimageschichte der Schweiz seit der Späteiszeit

    Open Access•Gerhard Furrer, C Burga et al.•ARTICLE•Geographica Helvetica•1987

    A Statistical analysis of published and compilated snowline data for the late-glacial Stades of Gschnitz, Clavadel, Daun and Egesen is presented. The calculation of snowline and snowline-depression (compared to the extent of 1850) is based on the 2: 1 -equilibrium line method. The Interpretation does not show significant differences in snowline-depression between the Lower Engadin (Eastern Alps) and the Mont Blanc area (Western Alps). The larger …

  • Zum neuzeitlichen, gegenwärtigen und zukünftigen Gletscherschwund in Graubünden

    Open Access•Max Maisch•ARTICLE•Geographica Helvetica•1991

    No abstract available

  • Klimaänderung und Gletscherskitourismus

    Open Access•Bruno Abegg, U König et al.•ARTICLE•Geographica Helvetica•1994

    No abstract available

  • Mensch - Umwelt - Klima

    Open Access•Max Maisch, Frank Preusser•ARTICLE•Geographica Helvetica•2008

    No abstract available

  • Combination of Numerical Dating Techniques Using 10 Be in Rock Boulders and 14 C of Resilient Soil Organic Matter for Reconstructing the Chronology of Glacial and Periglacial Processes in a High Alpin…

    Open Access•Filippo Favilli, M Egli et al.•ARTICLE•Radiocarbon•2009•Cited by: 1•References: 49

    Glacier fluctuations and paleoclimatic oscillations during the Late Quaternary in Val di Rabbi (Trentino, northern Italy) were reconstructed using a combination of absolute dating techniques ( 14 C and 10 Be) and soil chemical characterization. Extraction and dating of the stable fraction of soil organic matter (SOM) gave valuable information about the minimum age of soil formation and contributed to the deciphering of geomorphic surface dynamics…

  • Multi-methodological reconstruction of the lake level at Morgarten in the context of the history of the Swiss Confederation

    Open Access•M Egli, Max Maisch et al.•ARTICLE•The Holocene•2015•References: 1

    In AD 1315, the Habsburgs fought against the Swiss Confederation at Morgarten. Since historical records are very limited, the battle has been the subject of very controversial discussions. Its location and outcome seem likely to have been influenced by the landscape and the size of the Aegeri lake, but only sparse and contradictory information are available. Numerical, semi-quantitative and relative dating techniques were applied to reconstruct t…

  • Piecing together the Lateglacial advance phases of the Reussgletscher (central Swiss Alps)

    Open Access•Max Boxleitner, Ivy-Och et al.•ARTICLE•Geographica Helvetica•2018

    Exposure dating has substantially improved our knowledge about glacier advances during the Younger Dryas (YD) and the early Holocene. The glacier development after the Last Glacial Maximum (LGM) and the timing of morphologically evidenced, earlier Lateglacial re-advances is, however, still widely unknown. In this study we used 10Be surface exposure and radiocarbon dating to address these phases and corresponding landforms in the catchment of the …

Geology (7 works) · Geography (5 works) · Geology (5 works) · Geology and Paleoclimatology Research (5 works) · Physical geography (5 works) · Geomorphology (4 works) · Glacier (4 works) · Radiocarbon dating (4 works) · Glacial period (3 works) · Moraine (3 works)

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