A revised model for the last deglaciation of eastern Scotland.

M McCabe, P.U Clark, D.E Smith, P Dunlop

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Abstract

Accelerator mass spectrometry 14C ages on monospecific marine microfauna from raised mud record initial deglaciation of the eastern coast of Scotland before 21.0 cal ka bp. Two subsequent ice-margin readvances occurred prior to the Loch Lomond Advance and are identified from ice-contact deposits overlying marine mud. The Lunan Bay Readvance dates to
Original languageEnglish
Pages (from-to)313-316
JournalJournal of the Geological Society
Volume164
Issue number2
DOIs
Publication statusPublished - Mar 2007

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