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|description={{|1=Specimen of roofing slate from Aberfoyle Slate Quarries, Perthshire, Scotland. Dark grey-greenish slate, termed&amp;#039;green variety&amp;#039;showing very strong ribboning on the cleavage surface. The specimen is of Precambrian, Dalradian age. British Geological Survey Petrology Collection sample number EMC 5772. The Aberfoyle Slates occur in a structurally complex zone of geological deformation known as the Tay Nappe, close to the Highland Boundary Fault. The Tay Nappe is a vast flat-lying fold that overturns rocks of the Southern Highlands over an area of hundreds of square kilometres. The Aberfoyle Slate Formation occurs associated with a more sandsy unit termed the Bed Ledi Grit, named after the hill to the north of Aberfoyle. P519597.}}&lt;br /&gt;
|date=2017-07-29 15:51:38&lt;br /&gt;
|source=British Geological Survey&lt;br /&gt;
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