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Retreat pattern and dynamics of glaciers and ice sheets: reconstructions based on meltwater features

Margold, Martin, 1981- (författare)
Stockholms universitet,Institutionen för naturgeografi och kvartärgeologi (INK),Paleoglaciology
Jansson, Krister, Docent (preses)
Stockholms universitet,Institutionen för naturgeografi och kvartärgeologi (INK)
Stroeven, Arjen, Professor (preses)
Stockholms universitet,Institutionen för naturgeografi och kvartärgeologi (INK)
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Kleman, Johan, Professor (preses)
Stockholms universitet,Institutionen för naturgeografi och kvartärgeologi (INK)
Helmens, Karin, Docent (preses)
Stockholms universitet,Institutionen för naturgeografi och kvartärgeologi (INK)
Stokes, Chris (opponent)
Durham University, Department of Geography
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 (creator_code:org_t)
ISBN 9789174474299
Stockholm : Department of Physical Geography and Quaternary Geology, Stockholm University, 2012
Engelska 17 s.
Serie: Dissertations from the Department of Physical Geography and Quaternary Geology, 1653-7211 ; 30
  • Doktorsavhandling (övrigt vetenskapligt/konstnärligt)
Abstract Ämnesord
Stäng  
  • Glaciers and ice sheets covered extensive areas in the Northern Hemisphere during the last glacial period. Subsequently to the Last Glacial Maximum (LGM), they retreated rapidly and, except for Greenland and some other ice caps and glaciers, they vanished after the last glacial termination. This thesis examines the dynamics of deglacial environments by analysing the glacial geomorphological record with focus on the landforms created by glacial meltwater. The aims are (i) to evaluate the data available for mapping glacial meltwater features at the regional scale, and (ii) to demonstrate the potential of such features for regional ice retreat reconstructions in high-relief landscapes. Meltwater landforms such as ice-marginal meltwater channels, eskers, deltas and fossil glacial lake shorelines are used to infer former ice surface slope directions and successive positions of retreating ice margins. Evaluated high-resolution satellite imagery and digital elevation models reveal their potential to replace aerial photographs as the primary data for mapping glacial meltwater landforms. Following a methods study, reconstructions of the deglacial dynamics are carried out for central Transbaikalia, Siberia, Russia, and for the Cordilleran Ice Sheet (CIS) in central British Columbia, Canada, using regional geomorphological mapping surveys. Mapped glacial landforms in central Transbaikalia show evidence of a significant glaciation that possibly extended beyond the high mountain areas. Large glacial lakes were formed as advancing glaciers blocked rivers, and of these, Glacial Lake Vitim was the most prominent. Deglacial dynamics of the CIS reveals that the ice divide shifted to the Coast Mountains in north-central British Columbia and the eastern ice margin retreated towards the ice divide in late glacial time. This thesis demonstrates the potential to reconstruct ice retreat patterns and deglacial dynamics at regional scales by interpretation of the meltwater landform record.

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Naturgeografi (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Physical Geography (hsv//eng)

Nyckelord

Palaeoglaciology
Cordilleran Ice Sheet
deglaciation
glacial meltwater features
glacial lake
Physical Geography
naturgeografi

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