Killas is a Cornish language mining term for metamorphic rock stratum of sedimentary origin which was altered regionally by the Variscan orogeny and then locally by heat from the intruded granites in the English counties of Devon and Cornwall. The term is used in both counties.
The depositional environments of the killas were very varied, as is revealed by the fossil content and the sedimentary sequences. The fossils indicate changes from , deep ocean-basin environments to shallow sea environments. The deformed brachiopod fossil Cyrtospirifer verneuili, known to quarrymen as the Delabole Butterfly, was found in the upper Devonian beds of North Cornwall.
Shortly after the deposition of the sediments, the Variscan orogeny caused low grade regional metamorphism of the sediment followed by the intrusion of the Cornubian batholith and the subsequent contact metamorphism created the metamorphic rocks seen today. The orogeny put intense pressure on the sediments causing them to be folded and geologic fault. This is most apparent in the cliffs at Millook Haven on the north Cornwall coast, where the cliffs display an impressive series of recumbent angular folds.
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