Stratigraphic evidence is presented for the commencement of solifluction at a site 850 m a.s.l. during the Early Subboreal Chronozone. at ca. 5500 years B.P. It is possible that this process was initiated as the result of a climatic deterioration, in which case the site examined provides one of only two examples of 14C-dated stratigraphic evidence currently available for such an event occurring at around this time in the mountains of Scandinavia.
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Stephen Ellis (1979) studied this question.
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