Celtic Sea

History

The Celtic Sea receives its name from the Celtic heritage of the bounding lands to the north and east. E. W. L. Holt proposed the name at a 1921 meeting of fisheries experts from Great Britain, France, and the Republic of Ireland in Dublin. This sea's northern portion was considered part of Saint George's Channel, and the southern portion was an undifferentiated part of the Southwest Approaches to Great Britain. The desire for a common name came to be felt because of the area's common marine biology, geology and hydrology.

It was adopted in France before being common in English-speaking countries. In 1957, Édouard Le Danois wrote, "the name Celtic Sea is hardly known even to oceanographers." Marine biologists and oceanographers adopted it, and later, by petroleum exploration firms. It is named in a 1963 British atlas,; cited in

but a 1972 article states, "what British maps call the Western Approaches, and what the oil industry calls the Celtic Sea [...] certainly the residents on the western coast [of Great Britain] don't refer to it as such."

Seabed

The seabed under the Celtic Sea is referred to as the Celtic Shelf, part of the continental shelf of Europe. The northeast portion has a depth of between 90 and(-), increasing towards Saint George's Channel. In the opposite direction, sand ridges pointing southwest have a similar height, separated by troughs approximately 50 m deeper. These ridges were formed by tidal effects when the sea level was lower. South of 50°N, the topography is more irregular.

Oil and gas exploration in the Celtic Sea has had limited commercial success. The Kinsale Head gas field supplied much of Ireland's demand for gas in the 1980s and 1990s. The water is too deep for fixed wind turbines. The area has potential for 50 GW of floating wind farms, and TotalEnergies plans a project with almost 100 MW.

Ecology

The Celtic Sea has a rich fishery with total annual catches of 1.8 million tonnes as of 2007.

Four cetacean species occur frequently: minke whale, bottlenose dolphin, short-beaked common dolphin and harbor porpoise. Formerly, it held an abundance of marine mammals.

Limits

There are no land features to divide the Celtic Sea from the open Atlantic Ocean to the south and west. For these limits, Holt suggested the 200 fathom marine contour and the island of Ushant off the tip of Brittany.

The definition approved in 1974 by the UK Hydrographer of the Navy for use in British Admiralty Charts was "bounded roughly by lines joining Ushant, Land's End, Hartland Point, Lundy Island, St. Govan's Head and Rosslare, thence following the Irish coast south to Mizen Head and then along the 200-metre isobath to approximately the latitude of Ushant."

The International Hydrographic Organization defines the limits of the Celtic Sea as follows:

Notes

References

References

1. C. Michael Hogan. 2011. [http://www.eoearth.org/article/Celtic_Sea?topic=49523 ''Celtic Sea''. eds. P. Saundry & C. Cleveland. Encyclopedia of Earth. National Council for Science and the /environment. Washington DC.]
2. Le Danois, Edouard. (1957). "Marine Life of Coastal Waters: Western Europe". Harrap.
3. (19 March 2020). "Oil giant Total dives into offshore wind with 'world's biggest' floating array".
4. "Celtic Seas".
5. (2008). "1 Background information on marine mammals for Strategic Environmental Assessment 8". Sea Mammal Research Unit.
6. (1936). "Recent and older finds of the California grey whale in the Atlantic". Temminckia.
7. (1936). "Report on cetacea stranded on the British Coasts from 1927 to 1932.". British Museum (Natural History) No. 11, London, UK..
8. (1971). "Limits of Oceans and Seas, 3rd edition + corrections". International Hydrographic Organization.