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The Mid Holocene Transgression on Alexandra Land, Franz Josef Land, Russia
Jens-Ove Näslund, Rolf Zale and Andrey Glazovskiy
Geografiska Annaler. Series A, Physical Geography
Vol. 76, No. 1/2 (1994), pp. 97-101
Stable URL: http://www.jstor.org/stable/521323
Page Count: 5
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14C datings of whalebone and driftwood samples from Alexandra Land, Franz Josef Land, Russia, indicate deglaciation before 8780 14C years BP. The absence of a prominent beach morphology at the highest marine limit suggests that the sea reached this level during a short period of time, the highest marine limit thus being formed during a transgression ending at 6800 BP.
Geografiska Annaler. Series A, Physical Geography © 1994 Swedish Society for Anthropology and Geography