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		<updated>2015-07-22T16:51:53Z</updated>

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|description={{en|1=Cambro-Ordovician rocks of Ord on the Sleat peninsula, Skye. a Map showing the structural inlier of Cambro-Ordovician rocks within the Kishorn Thrust Sheet at the base of the Moine Thrust Belt. b Cross-sections illustrating alternative interpretations of the Ord structure by Clough (in Peach et al.,1907), Bailey (1939, 1955) and Potts (1982).The Clough and Bailey sections follow a common line whereas the line of Potts’ section lies slightly farther to the south.The detailed structure is very complex and there is no preferred model. Several contacts, interpreted as tectonic thrusts by both Clough and Bailey, have been re-interpreted as normal stratigraphical junctions by Potts, who has also re-interpreted some other thrusts as extensional faults; the Ord Syncline was interpreted as an antiform by Bailey, but as a synform by Potts. Figure 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=2015-07-22 17:48:30&lt;br /&gt;
|source=British Geological Survey&lt;br /&gt;
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		<author><name>Scotfot</name></author>
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