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Introduction:
The fjord was carved by the action of glaciers in the ice ages and was flooded by the sea when the later glaciers retreated. The geology of Lysefjorden was thoroughly investigated and described by Professor Bjørn G. Andersen in his Master's thesis ”Om isens tilbaketrekking i området mellom Lysefjorden og Jøsenfjorden i Ryfylke” (On the glacial retreat in the area between the Lysefjorden and Jøsenfjorden in Ryfylke).
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