Abstract
In western Norway pre Late Weichselian sediments (older than 15,000 B.P.) are limited except at a few locations. Ålfjord (Fig. 1) is a coast parallel fjord with up to 250 ms TWT thick sediment sequences. Ice movement was towards the Norwegian Channel [Holtedahl 1975] and the area has been ice free during Mid Weichselian [Sejrup & Larsen 1991].
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References
Holtedahl, H., The Geology of the Hardangerfjord, West Norway, Norges geologiske Undersokelse 323, 87 pp. 1975.
Sejrup H.P., and E. Larsen, Eemian-early Weichselian N-S temperature gradiants; North Atlantic-NW Europe, Quaternary International 10–12, 161–166. 1991.
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© 1997 Chapman & Hall
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Aarseth, I. (1997). Glacial Erosion of Sediments in the Ålfjord, western Norway. In: Davies, T.A., et al. Glaciated Continental Margins. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-5820-6_10
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DOI: https://doi.org/10.1007/978-94-011-5820-6_10
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