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Svendsen, John Inge; Landvik, Jon Y.; Mangerud, Jan; Miller, Gifford H. (1987)
Publisher: Co-Action Publishing
Journal: Polar Research
Languages: English
Types: Article
Subjects:
Lake Linnévatnet is situated near the mouth of Isfjorden, on thc west coast of Spitsbergen (Fig. 1A). According to Denton & Hughes (1981) and Mangerud et al. (1987) it lies within the Late Weichselian ice boundary. whereas according to Boulton (1979) and Troitsky et al. (1979) it is outside that boundary. The purpose of this paper is to describe the stratigraphy of the lake sediments and discuss the timing of the glacial retreat.
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    • Beyurn, A . & Kjensmo. J . 1978: Physiography of Lake LinnCvatn, Western Spitsbergen. Verh. Internat. Verein. Limnol. 20. 609-614.
    • Beyum, A . & Kjensmo, 3. 1980: Postglacial sediments in Lake Linnevatnet. Western Spitsbergen. Arch. HydrobioL 88,232- 249.
    • Boulton, G . 1979: Glacial history of the Spitsbergen archipelago and the problem of a Barents Shelf ice sheet. Boreas 8. 31- 57.
    • Denton, G. H . &Hughes, T. J. 1981:The Arctic Ice Sheet: An Outrageous Hypothesis. Pp. 437467 in Denton, G . H. & Hughes, T. J. (eds.): The Last Great Ice Sheets. John Wiley & Sons, New York.
    • Mangerud, J . , Landvik, I. Y., Salvigsen, 0. & Miller, G. H. 1985: Lake Linnevatnet, Svalbard, a possible 40,000 years continuous record of lacustrine and marine sedimentation. 14th Arctic Workshop. Arctic Land - Sea Interactions. Abstracts. Bedfurd Inrtitute of Oceanography, Dartmouth 1985, 82-85.
    • Mangerud, J., Bolstad, M., Elgersma, A , , Helliksen, D., Landvik, J. Y., Lycke, A. K., L@nne,I., Salvigsen. 0..Sandahl, T. & Sejrup, H. P. 1987: The Late Weichselian glacial maximum in western Svalbard. Polar Research 5n.s.(thisvolume).
    • Sandahl, T. 1986: Kuartergeologiske undersgkeker i omrddet Lewinodden - Kapp Starostin - Linnkoatnet, Ytre Isfiorden, Soalbard. Unpublished thesis, Univ. of Bergen.
    • Troitsky. L . , Punning, J.-M., Hutt. G . & Rajama, R. 1979: Pleistocene glaciation chronology of Spitsbergen. Boreas 8, 401-407.
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