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Washover ridges and lagoons developed during the transgression after 0.7 ka BP.

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Basedon the location of Thule Culture Eskimo ruins of different ages in relation to the present shoreline it has been suggested that RSL was relatively high before 0.4 ka BP, that it was relatively low between 0.4 and 0.2 ka BP, and that it has been rising since (Mathiassen in Gabel-Jørgen sen & Egedal 1940; Weidick 1993).

The purpose of this investigation is to reconstruct the trend of the early-middle Holocene emergence of western Disko and to point out possible transgression phases during late Holocene.

Morten Rasch, Danish Polar Center, Strandgade 100H, 1401 Copenhagen K, Denmark; Bjarne Holm Jakobsen & Niels Nielsen, Institute of Geography, University of Copenhagen, Øster Voldgade 10, 1350 Copenhagen K., Denmark.

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