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		<updated>2017-07-29T14:53:23Z</updated>

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|description={{|1=Specimen of roofing slate quarried from Ballachulish, Argyllshire, Scotland. Darke grey slate with common cubes of yellow metallic pyrite, and a slight grain or lineation on the cleavage surface. British Geological Survey Petrology Collection sample number EMC 5755. This slate is marked as&amp;#039;Ballachulish Ordinary Variety&amp;#039;. The Ballachulish Slate Formation is a geological unit approximately 400 metres thick, that lies within the Appin Group of the Dalradian Supergroup. These rocks are Precambrian in age, and form some of the oldest rocks in Britain. The Scottish slate belts are found in the Grampian Highlands, forming part of the ancient Caledonian mountain system which once extended from the Appalachians to Scandinavia. P519579.}}&lt;br /&gt;
|date=2017-07-29 15:51:21&lt;br /&gt;
|source=British Geological Survey&lt;br /&gt;
|author=British Geological Survey&lt;br /&gt;
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