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		<updated>2015-07-11T19:21:40Z</updated>

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|description={{en|1=Tentative reconstructions of former proglacial lakes in north-east Scotland. a Creation of ‘50 m’ Lake Ugie shortly after the maximum of the second major expansion of the Main Late Devensian ice sheet (after 18 ka BP) and following the earlier ponding of the 80 m’ lake. Widespread glacial over-riding of glaciolacustrine deposits occured east of Lake Ugie. b Parting of East Grampian and ‘Logie-Buchan’ ice with the formation of Lake Ythan. c Diachronous ponding along the Banffshire coast and glaciomarine incursion around St Fergus at about 15 ka BP. From: Figure 42 in MERRITT, J W, AUTON, C A, CONNELL, E R, HALL, A M, and PEACOCK, J D. 2003. Cainozoic geology and landscape evolution of north-east Scotland. Memoir of the British Geological Survey, Sheets 66E, 67, 76E, 77, 86E, 87W, 87E, 95, 96W, 96E and 97 (Scotland).}}&lt;br /&gt;
|date=2015-07-11 20:15:08&lt;br /&gt;
|source=British Geological Survey&lt;br /&gt;
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