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The intensity of waves decreases eastwards along Akulliit.The inner part of the fiord is a good natural harbour even during severe storms. The sea in Akulliit is usually frozen from the middle of December to the beginning of June.
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It is also well established that RSL, at least in some parts of West Greenland during the last c.
3 ka, has been lower than at present (Mathiassen in Gabel-Jørgensen & Egedal 1940; Roussel 1941; Weidick 1976, 1993; Foged 1979; Rasch & Nielsen 1994, 1995; Rasch et al.
The study area, Saqqarliit Ilorliit, is located in the inner part of Akulliit, which is the middle of three large fiords on western Disko (Fig. The bedrock in the fiord consists of Tertiary basalts. Generally, littoral deposits consist of beach gravel. The wave climate on western Disko is characterized by wind generated waves and swell caused by cyclones in Davis Strait and Baffin Bay.
The Holocene marine limit is situated between 60 and 65 m.a.s.l. Boulder beaches on the outer coasts indicate high energy conditions during storms.
1) is described, sediment core data from salt marshes and lagoons are presented, and a RSL curve for western Disko is constructed from published and new 14 dates.