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Glacial geomorphological research at Mýrdalsjökull, Iceland, 1977–86. I

The northern margin

Bibliographic Data

ID9850143
AuthorsJohannes Krüger (University of Copenhagen, corresponding author)
Year1988
Volume88
Issue1
Pages68-77
Publication date1988-01-01
Peer ReviewedYes
Open AccessNo
TypeARTICLE
VenueGeografisk Tidsskrift-Danish Journal of Geography (JOURNAL)
Journal identifiersISSN: 0016-7223 • E-ISSN: 1903-2471
PublisherInforma UK Limited (PUBLISHER • GB)
DOI10.1080/00167223.1988.10649259
OpenAlexW2404282254
LanguageEN
Citations received3
References cited15

Krüger, J.: Glacial geomorphological research at Mýrdalsjökull, Iceland, 1977–86. I: the northern margin. Geografisk Tidsskrift 88:68–77. Copenhagen. 1988. The lithostratigraphic divisions of the glacier forefield are tentatively interpreted as responses to a glacier advance about the middle of the 18th century, a following retreat, and oscillations have been succeeded by a continuous retreat in the present century. Most recently the glacier is re-advancing. During periods of deglaciation the marginal and the exposed subglacial landsystem were modified by glaciofluvial processes in the direction of a proglacial landsystem. Subsequent flows of ice across the area have led to deposition of lodgement tills and renewal of the subglacial landsystem

Deglaciation · Geography · Geomorphology · Glacial period · Glacier · Margin (machine learning · Moraine · Physical geography · Tidewater glacier cycle · Cryospheric studies and observations · Geological formations and processes · Geology · Geology and Paleoclimatology Research

  • Aktuelle thermische Klimaveränderungen am Polarrand der Ökumene Europas - Ausmaß, Ursachen und Auswirkungen

    Open Access•Ekkehard Schunke•Erdkunde•1979

Citation velocityhistorical
Highly citedNo

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