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Distant from the ice margin, however, red colluvium is extensively exposed on interfluves.
Furthermore we refined the location of the eastern LGM ice margin, by new sub bottom profiles.
Lake level subsequently fell > 35 m as the ice margin retreated northward during the Twocreekan Interstadial.
This approach relies on the assumption that the distribution of moraines in the modern landscape is an accurate reflection of former ice margin positions during climatically controlled periods of ice margin stability.
Mean annual temperatures near the ice margin were about −6 °C or colder and increased away from the ice margin to about 0 °C near the southern extent of the permafrost.
Deposition took place during deglaciation but was punctuated by minor readvances of the ice margin that deformed the sediment pile.
Off the southwest coasts, the ice margin was maintained for up to 1.5 ka at fiord mouths.
West of the Last Glacial Maximum (LGM) ice margin in Denmark ages reflect exposure from the Middle Weichselian.
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Our seven ice-margin samples act as geological blanks.
This stage was succeeded by a second phase in which a fluvial system formed as a result of ice-margin retreat farther to the SE (postglacial stage).
This paper presents a detailed analysis of high-resolution facies architecture of glaciolacustrine ice-margin deposits, which formed at the southern margin of the Scandinavian ice shield.
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