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		<updated>2017-07-29T14:53:28Z</updated>

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|description={{|1=Specimen of roofing slate quarried from Ballachulish, Argyllshire, Scotland. Very dark grey slate with minor pyrite and relatively smooth surface. It is a roofing slate quarried from Ballachulish, Argyll, Scotland. The specimen is of Precambrian, Dalradian age. British Geological Survey Petrology Collection sample number EMC 5759. This variety, known as&amp;#039;Oak&amp;#039;has a very fine grain on the cleavage surface. Slaty cleavage is formed by the re-alignment and growth of new minerals as a result of intense pressure and temperature deep in the Earth&amp;#039;s crust. Other minerals such as quartz and feldspar act as fillers giving the slate bulk and strength. Too much of these make a slate too thick with a coarse surface finish; too little and it is soft with low strength. Specimen size: 26x14cm. P519583.}}&lt;br /&gt;
|date=2017-07-29 15:51:27&lt;br /&gt;
|source=British Geological Survey&lt;br /&gt;
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