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|description={{|1=Detail of the base of the clay-with-flints deposit filling the channel on the north face of the quarry. Note the abundance of hematised (reddened) flints which are internally heavily fractured, but still retain their original outline, suggesting that they have been subject to stress. The pinkish brown clay contains scattered lapilli indicating an air-fall ash component. The clast of weathered vesicular basalt (base, centre) is the only example found in the channel fill. (Trowel head 15cm long). From: Photograph 4C. Mitchell,W. I. (ed.). 2004. The geology of Northern Ireland-our natural foundation. Geological Survey of Northern Ireland, Belfast.}}&lt;br /&gt;
|date=2017-09-12 19:55:44&lt;br /&gt;
|source=Geological Survey of Northern Ireland&lt;br /&gt;
|author=Geological Survey of Northern Ireland&lt;br /&gt;
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		<author><name>Scotfot</name></author>
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