Cockercombe tuff
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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.
Coordinates: 51°05′N 3°12′W / 51.09°N 3.20°W / 51.09; -3.20