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FENNIA 66, N:o 1
5
In addition, during the Littorina time, five other well-marked
beaches were formed and traced palaeontologically and also
archaeolo-gically. Distinct shore features have come into existence also during
other times, namely three after the formation of the last Littorina
Fig. 2. Map of the initial stage of the Ancylus Lake.
shore-line, and four during the Ancylus period, besides the above
mentioned highest shore-line of this stage (Fig. 2). Thus, no less than
fifteen old water planes are known in the Baltic basin from the
postglacial epoch.
The late-glacial oscillations of level, again, are not recorded in
detail by the pollen-statistics, because the formation of peat and mud
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