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|description={{en|1=Pre-Paleocene strata and Paleocene lavas at Creag a’Ghaill, Gribun, western Mull. Platy-jointed psammites of the Moine, Upper Shiba Psammite Formation (Morar Group) are overlain unconformably by Triassic basal conglomerates and sandstones. Upper Triassic strata consist of calcareous sandstones with carbonate concretions (cornstones), and the overlying sandy limestones of the Rhaetian Penarth Group are cut by basaltic sills of Paleocene age. Upper Cretaceous silicified limestone is largely obscured by scree and Paleocene basalt lavas form the upper cliffs.The top of the upper cliff is about 260 m elevation. (Photomosaic: B G J Upton; P532641.). Plate 4. Emeleus, C H, and Bell, B R. 2005. British regional geology: the Palaeogene volcanic districts of Scotland. Fourth edition. Keyworth, Nottingham: British Geological Survey.}}&lt;br /&gt;
|date=2010-03-05 13:14:43&lt;br /&gt;
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