||This article may be too technical for most readers to understand. (June 2011)|
Haig Fras is a 45 km long submarine granitic rocky outcrop in the southern part of the Celtic Sea, lying about 95 km northwest of the Isles of Scilly. It covers an area of 356.5 square kilometres (137.6 sq mi). At one point it reaches within 38 m of the sea surface. It is protected as a Special Area of Conservation (SAC) because of the diverse fauna developed in its bedrock reef habitat. It was discovered in 1962 and named by Smith and others in 1965.
The Haig Fras outcrop consists mainly of granite, forming a WSW-ENE trending elongate intrusion. The granite outcrop is surrounded by an area of Devono-Carboniferous sedimentary rocks. Evidence from gravity data suggests that the extent of the intrusion is greater than the observed outcrop, based on its association with a linear negative gravity anomaly. It is dated at 277 Ma, Early Permian in age, within the range of intrusion ages for the granites that make up the Cornubian batholith. Although the two intrusions have the same trend and are of similar age, they are not thought to be related. In detail three separate outcrops have been identified using a combination of radiometric data and seabed sampling. The granite is fine to medium-grained, unlike the megacrystic granite typical of the Cornubian batholith intrusions, although this may be due to the low level of sampling available. A foliated granite is locally developed as a marginal facies.
The granite is thought to be cut by a swarm of basic dykes inferred from magnetic and seismic reflection data. This swarm is interpreted to be 56 km long and 2.5 km across and at least six separate intrusive bodies have been identified. The proposed intrusions are though most likely to be of Mesozoic age.
The bedrock reef at Haig Fras supports a range of fauna. Jewel anemones (Corynactis viridis) and Devonshire cup corals (Caryophyllia smithii) are found at the top of the outcrop. Encrusting sponges, crinoids and Ross coral Pentapora fascialis are found near base of the outcrop. Mobile fauna observed include urchins such as Echinus esculentus, brittle stars and the squat lobster Munida.
Special area of conservation
The area of the proposed SAC is 481 square kilometres (186 sq mi), which includes a margin of 330 metres (1,080 ft) around the mapped bedrock area, derived from the maximum water depth of 110 metres (360 ft) and an assumed length to depth ratio of a fishing warp of 3:1. The area was first proposed in 2004 and was included in the first tranche of candidate SACs submitted to the European Commission in August 2008. It was selected on the basis of being an Annex I habitat, 1170 (reefs), in the terms of the EU Habitats Directive.
- Joint Nature Conservation Committee (2008). "Offshore Special Area of Conservation: Haig Fras SAC Selection Assessment". p. 14. Retrieved 10 January 2011.
- Smith, A.J.; Stride A.H. & Whittard W.F. (1965). "The geology of the Western Approaches of the English Channel IV. A recently discovered Variscan granite west-north-west of the Scilly Isles". In Whittard W.F. & Bradshaw R. Submarine geology and geophysics. Proceedings Colston Research Society 17. Butterworths. pp. 287–301. ISSN 0069-6277. Retrieved 25 January 2011.
- Edwards, J.W.F.; Briant, M. & Arthur, M.J. (1991). "Proposed Mesozoic dykes in the Celtic Sea". Proceedings of the Ussher Society 7: 344–349. Retrieved 10 January 2011.
- Edwards, J.W.F. (1984). "Interpretations of seismic and gravity surveys over the eastern part of the Cornubian platform". Variscan Tectonics of the North Atlantic Region. Special Publications 14. London: Geological Society. Retrieved 10 January 2011.
- Jones, D.G.; Miller J.M. & Roberts P.D. (1988). "A seabed radiometric survey of Haig Fras, S. Celtic Sea, U.K.". Proceedings of the Geologists' Association 99 (3): 193–203. doi:10.1016/S0016-7878(88)80035-X. Retrieved 10 January 2011.
- JNCC (2010). "Latest changes to the UK SAC list". Retrieved 12 January 2011.