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About: Cockercombe tuff     Goto   Sponge   NotDistinct   Permalink

An Entity of Type : yago:Substance100019613, within Data Space : dbpedia.org associated with source document(s)

Type: geo:SpatialThingyago:Abstraction100002137yago:IgneousRock114931879yago:Material114580897yago:Matter100020827yago:Part113809207yago:PhysicalEntity100001930yago:Relation100031921yago:WikicatIgneousRocksBandyago:Rock114696793yago:Substance100019613 New Facet based on Instances of this Class

Cockercombe Tuff is a greenish-grey, hard pyroclastic rock, formed by the compression of volcanic ash containing high quantities of chlorite, which gives it its distinctive colour. It is found almost exclusively in the south-eastern end of the Quantock Hills near Cockercombe, Somerset, England from where it has been quarried for centuries. Quantock Lodge is built from Cockercombe tuff.