Results obtained by mapping and special varved clay investigation show that the so-called Northeastern ice advance (13,500 B.P.) and the Low Baltic readvance (13.0W13.200 B.P.) are separated by a significant deglaciation phase, for which we propose ' Lockarp Interstadial' (13,200-13.500 B.P.) as a time-stratigraphic term to be used in the type area of southwestern Scania.
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