Irish Sea

The Irish Sea joins the North Atlantic at both its northern and southern ends. To the north, the connection is through the North Channel between Scotland and Northern Ireland and the Malin Sea. The southern end is linked to the Atlantic through the St George's Channel between Ireland and Pembrokeshire, and the Celtic Sea. It is composed of a deeper channel about long and wide on its western side and shallower bays to the east. The depth of the western channel ranges from to . Cardigan Bay in the south, and the waters to the east of the Isle of Man, are less than deep. With a total water volume of and a surface area of , 80% is to the west of the Isle of Man. The largest sandbanks are the Bahama and King William Banks to the east and north of the Isle of Man and the Kish Bank, Codling Bank, Arklow Bank and Blackwater Bank near the coast of Ireland. The Irish Sea, at its greatest width, is and narrows to . The International Hydrographic Organization defines the limits of the Irish Sea (with St George's Channel) as follows, :On the North. The Southern limit of the Inner Seas off the West Coast of Scotland, defined as a line joining the South extreme of the Mull of Galloway (54°38'N) in Scotland and Ballyquintin Point (54°20'N) in Northern Ireland. :On the South. A line joining St. David's Head in Wales () to Carnsore Point in Ireland (). The Irish Sea has undergone a series of dramatic changes over the last 20,000 years as the last glacial period ended and was replaced by warmer conditions. At the height of the glaciation, the central part of the modern sea was probably a long freshwater lake. As the ice retreated 10,000 years ago, the lake reconnected to the sea. ==History==

The Irish Sea was formed in the Neogene era. The Irish Sea was called Mare Hibernicus in the Roman Empire. Notable crossings include several invasions from Britain. The Norman invasion of Ireland took place in stages during the late 12th century from Porthclais near St. Davids, Wales, in Hulks, Snekkars, Keels and Cogs to Wexford Harbour, Leinster. The Tudors crossed the Irish Sea to invade in 1529 in caravels and carracks. ==Shipping==

Because Ireland has neither tunnel nor bridge to connect it with Great Britain, the vast majority of heavy goods trade is done by sea. Northern Ireland ports handle of goods trade with the rest of the United Kingdom annually; the ports in the Republic of Ireland handle , representing 50% and 40% respectively of total trade by weight. The Port of Liverpool handles of cargo and 734,000 passengers a year. Holyhead port handles most of the passenger traffic from Dublin and Dún Laoghaire ports, as well as of freight. Ports in the Republic handle 3,600,000 travellers crossing the sea each year, amounting to 92% of all Irish Sea travel. Ferry connections from Wales to Ireland across the Irish Sea include Fishguard Harbour and Pembroke to Rosslare, Holyhead to Dún Laoghaire and Holyhead to Dublin. From Scotland, Cairnryan connects with both Belfast and Larne. There is also a connection between Liverpool and Belfast via the Isle of Man or direct from Birkenhead. The world's largest car ferry, Ulysses, is operated by Irish Ferries on the Dublin Port–Holyhead route; Stena Line also operates between Britain and Ireland. "Irish Sea" is also the name of one of the BBC's Shipping Forecast areas defined by the coordinates: • • • • Iarnród Éireann, Irish Ferries, Northern Ireland Railways, ScotRail, Stena Line and Transport for Wales Rail promote SailRail with through rail tickets for the train and the ferry. The British ship LCT 326 sank in the Irish sea and was discovered in March 2020. In September 2021, the British Navy ship HMS Mercury was discovered; it sank in 1940. The British ship SS Mesaba was sunk by the Imperial German Navy U-118 in 1918 and discovered in 2022. This ship is well known for sailing near the Titanic and for attempting to warn the Titanic about dangerous icebergs. == Oil and gas exploration ==

Caernarfon Bay Basin The Caernarfon Bay basin contains up to of Permian and Triassic syn-rift sediments in an asymmetrical graben that is bounded to the north and south by Lower Paleozoic massifs. Only two exploration wells have been drilled so far, and there remain numerous undrilled targets in tilted fault block plays. As in the East Irish Sea Basin, the principal target reservoir is the Lower Triassic Sherwood Sandstone, top-sealed by younger Triassic mudstone and evaporites. Maximum burial of, and primary gas migration from, the source rocks could have terminated as early as the Jurassic, whereas many of the tilted fault blocks were reactivated or created during Paleogene inversion of the basin. It is not clear as yet whether aeromagnetic anomalies in the southeast of Caernarfon Bay are imaging a continuation of the dyke swarm into this area too, or whether they are instead associated with deeply buried Permian syn-rift volcanics. Cardigan Bay Basin The Cardigan Bay Basin forms a continuation into British waters of Ireland’s North Celtic Sea Basin, which has two producing gas fields. The basin comprises a south-easterly deepening half-graben near the Welsh coastline, although its internal structure becomes increasingly complex towards the southwest. Permian to Triassic syn-rift sediments are less than 3 km thick and overlain by up to 4 km of Jurassic strata, and locally up to 2 km of Paleogene fluvio-deltaic sediments. Reservoir targets include Lower Triassic Sherwood Sandstone, Middle Jurassic shallow marine sandstones and limestones (Great Oolite), and Upper Jurassic fluvial sandstone (Dragon Field reservoir). The most likely hydrocarbon source rocks are Early Jurassic marine mudstones. It comprises the integrated development of five offshore oil and gas fields in the Irish Sea: Douglas oil field Hamilton gas field Hamilton North gas field Hamilton East gas field Lennox oil and gas field Oil is produced from the Lennox and Douglas fields. PowerGen is the sole purchaser of gas from Liverpool Bay. Production started as follows: Hamilton North (1995), Hamilton (1996), Douglas (1996), Lennox (oil only, 1996), Hamilton East (2001). which became illegal in December 1988. East Irish Sea Basin With of gas and of oil estimated by operators (DTI, 2001), the basin is in a mature exploration phase. Early Namurian basinal mudstones are the source rocks. Production is from fault-bounded Lower Triassic Sherwood Sandstone reservoirs, sealed by Triassic mudstones and evaporites. Future exploration focuses on extending this play, with additional potential in Carboniferous fluvial sandstones. This requires intraformational mudstone seals because no top-seal exists where reservoirs subcrop the base Permian unconformity in the east; Carboniferous strata crop out at the seabed in the west. Dalkey Island exploration prospect Previous drilling in the Kish Bank Basin confirmed petroleum potential with oil shows in wells and hydrocarbon seeps from airborne surveys. New 2-D seismic analysis revealed a large undrilled Lower Triassic structural closure ~ offshore Dublin. The Dalkey prospect may be oil-prone, given prolific Lower Triassic reservoirs in the nearby eastern Irish Sea. It may contain ~ of oil in place. The prospect carries significant risk; partners are advancing a focused work programme to mitigate these risks. Its shallow-water location near shore may reduce drilling and development costs. ==Cities and towns==

Below is a list of cities and towns around the Irish Sea coasts in order of size: ==Counties bordering the Irish Sea==

• Listed are the islands in the Irish Sea which are either at least one square kilometre in area, or which have a permanent population. • Anglesey and Holy Island are included separately. == Environment ==

The most accessible and possibly the greatest wildlife resource of the Irish Sea lies in its estuaries: particularly the Dee Estuary, the Mersey Estuary, the Ribble Estuary, Morecambe Bay, the Solway Firth, the Firth of Clyde, Belfast Lough, Strangford Lough, Carlingford Lough, Dundalk Bay, Dublin Bay and Wexford Harbour. However, a lot of wildlife also depends on the cliffs, salt marshes and sand dunes of the adjoining shores, the seabed and the open sea itself. The information on the invertebrates of the seabed of the Irish Sea is rather patchy because it is difficult to survey such a large area, where underwater visibility is often poor and information often depends upon looking at material brought up from the seabed in mechanical grabs. However, the groupings of animals present depend to a large extent on whether the seabed is composed of rock, boulders, gravel, sand, mud or even peat. In the soft sediments seven types of community have been provisionally identified, variously dominated by brittle-stars, sea urchins, worms, mussels, tellins, furrow-shells, and tower-shells. Parts of the bed of the Irish Sea are very rich in wildlife. The seabed southwest of the Isle of Man is particularly noted for its rarities and diversity, as are the horse mussel beds of Strangford Lough. Scallops and queen scallops are found in more gravelly areas. In the estuaries, where the bed is more sandy or muddy, the number of species is smaller but the size of their populations is larger. Brown shrimp, cockles and edible mussels support local fisheries in Morecambe Bay and the Dee Estuary and the estuaries are also important as nurseries for flatfish, herring and sea bass. Muddy seabeds in deeper waters are home to populations of the Dublin Bay prawn, also known as "scampi". The open sea is a complex habitat in its own right. It exists in three spatial dimensions and also varies over time and tide. For example, where freshwater flows into the Irish Sea in river estuaries its influence can extend far offshore as the freshwater is lighter and "floats" on top of the much larger body of salt water until wind and temperature changes mix it in. Similarly, warmer water is less dense and seawater warmed in the inter-tidal zone may "float" on the colder offshore water. The amount of light penetrating the seawater also varies with depth and turbidity. This leads to differing populations of plankton in different parts of the sea and varying communities of animals that feed on these populations. However, increasing seasonal storminess leads to greater mixing of water and tends to break down these divisions, which are more apparent when the weather is calm for long periods. Plankton includes bacteria, plants (phytoplankton) and animals (zooplankton) that drift in the sea. Most are microscopic, but some, such as the various species of jellyfish and sea gooseberry, can be much bigger. Diatoms and dinoflagellates dominate the phytoplankton. Although they are microscopic plants, diatoms have hard shells and dinoflagellates have little tails that propel them through the water. Phytoplankton populations in the Irish Sea have a spring "bloom" every April and May, when the seawater is generally at its greenest. Crustaceans, especially copepods, dominate the zooplankton. However, many animals of the seabed, the open sea and the seashore spend their juvenile stages as part of the zooplankton. The whole plankton "soup" is vitally important, directly or indirectly, as a food source for most species in the Irish Sea, even the largest. The enormous basking shark, for example, lives entirely on plankton and the leatherback turtle's main food is jellyfish. A colossal diversity of invertebrate species live in the Irish Sea and its surrounding coastline, ranging from flower-like fan-worms to predatory swimming crabs to large chameleon-like cuttlefish. The estuaries of the Irish Sea are of international importance for birds. They are vital feeding grounds on migration flyways for shorebirds travelling between the Arctic and Africa. Others depend on the milder climate as a refuge when continental Europe is in the grip of winter. which are now considered to be almost extinct in eastern North Atlantic, sperm whale, northern bottlenose whale, long-finned pilot whale, orca, white-beaked dolphin, striped dolphin and Risso's dolphin. it has not been implemented as of 2013. The common or harbour seal and the grey seal are both resident in the Irish Sea. Common seals breed in Strangford Lough, grey seals in southwest Wales and, in small numbers, on the Isle of Man. Grey seals haul out, but do not breed, off Hilbre and Walney islands, Merseyside, the Wirral, St Annes, Barrow-in-Furness Borough, and Cumbria. == Radioactivity ==

The Irish Sea has been described by Greenpeace as the most radioactively contaminated sea in the world with some "eight million litres of nuclear waste" discharged into it each day from Sellafield reprocessing plants, contaminating seawater, sediments and marine life. Low-level radioactive waste has been discharged into the Irish Sea as part of operations at Sellafield since 1952. The rate of discharge began to accelerate in the mid- to late 1960s, reaching a peak in the 1970s and generally declining significantly since then. As an example of this profile, discharges of plutonium (specifically 241Pu) peaked in 1973 at falling to by 2004. Improvements in the treatment of waste in 1985 and 1994 resulted in further reductions in radioactive waste discharge although the subsequent processing of a backlog resulted in increased discharges of certain types of radioactive waste. Discharges of technetium in particular rose from in 1993 to a peak of in 1995 before dropping back to in 2004. Current rates of discharge for many radionuclides are at least 100 times lower than they were in the 1970s. Analysis of the distribution of radioactive contamination after discharge reveals that mean sea currents result in much of the more soluble elements such as caesium being flushed out of the Irish Sea through the North Channel about a year after discharge. Measurements of technetium concentrations post-1994 has produced estimated transit times to the North Channel of around six months with peak concentrations off the northeast Irish coast occurring 18–24 months after peak discharge. Less soluble elements such as plutonium are subject to much slower redistribution. Whilst concentrations have declined in line with the reduction in discharges they are markedly higher in the eastern Irish Sea compared to the western areas. The dispersal of these elements is closely associated with sediment activity, with muddy deposits on the seabed acting as sinks, soaking up an estimated of plutonium. The highest concentration is found in the eastern Irish Sea in sediment banks lying parallel to the Cumbrian coast. This area acts as a significant source of wider contamination as radionuclides are dissolved once again. Studies have revealed that 80% of current seawater contamination by caesium is sourced from sediment banks, whilst plutonium levels in the western sediment banks between the Isle of Man and the Irish coast are being maintained by contamination redistributed from the eastern sediment banks. The consumption of seafood harvested from the Irish Sea is the main pathway for exposure of humans to radioactivity. The environmental monitoring report for the period 2003 to 2005 published by the Radiological Protection Institute of Ireland (RPII) reported that in 2005 average quantities of radioactive contamination found in seafood ranged from less than for fish to under for mussels. Doses of man-made radioactivity received by the heaviest consumers of seafood in Ireland in 2005 was . This compares with a corresponding dosage of radioactivity naturally occurring in the seafood consumed by this group of and a total average dosage in Ireland from all sources of . In terms of risk to this group, heavy consumption of seafood generates a 1 in 18 million chance of causing cancer. The general risk of contracting cancer in Ireland is 1 in 522. In the UK, the heaviest seafood consumers in Cumbria received a radioactive dosage attributable to Sellafield discharges of in 2005. This compares to average annual dose of naturally sourced radiation received in the UK of . == Proposed fixed sea link connections ==

Discussions of linking Britain to Ireland began in 1895, with an application for £15,000 towards the cost of carrying out borings and soundings in the North Channel to see if a tunnel between Ireland and Scotland was viable. Sixty years later, Harford Montgomery Hyde, Unionist MP for North Belfast, called for the building of such a tunnel. A tunnel project has been discussed several times in the Irish parliament. The idea for a long rail bridge or tunnel continues to be mooted. Several potential projects have been proposed, including one between Dublin and Holyhead put forward in 1997 by the British engineering firm Symonds. At , it would have been by far the longest rail tunnel on earth with an estimated cost approaching £20 billion. == Wind power ==

An offshore wind farm was developed on the Arklow Bank, Arklow Bank Wind Park, about off the coast of County Wicklow in the south Irish Sea. The site currently has seven GE 3.6 MW turbines, each with diameter rotors, the world's first commercial application of offshore wind turbines over three megawatts in size. The operating company, Airtricity, has indefinite plans for nearly 100 further turbines on the site. Further wind turbine sites include: • The North Hoyle site off the coast from Rhyl and Prestatyn in North Wales, containing thirty 2 MW turbines. operated by NPower Renewables • Burbo Bank site off the north Wirral coast • Robin Rigg Wind Farm in the Solway Firth • Thirty 3 MW turbines are operating in a wind farm the coast of Walney Island. • The Warmley Extension west of Walney Island off the coast of Cumbria. As of 2018, it is the largest on Earth. ==In popular culture ==

• During World War I the Irish Sea became known as "U-boat Alley", because the U-boats moved their emphasis from the Atlantic to the Irish Sea after the United States entered the war in 1917. • The Port of Barrow-in-Furness, one of Britain's largest shipbuilding centres and home to the United Kingdom's only submarine-building complex, is only a minor port. • The Irish Sea figures prominently in the Mabinogion. In the second branch of the Mabinogi the Irish Sea is crossed from the south to Harlech by Matholwch, the Irish King, who has come to seek the hand of Branwen ferch Llŷr, sister of Bendigeidfran, King of the Island of the Mighty. Branwen and Matholwch marry, but when she becomes abused by Matholwch, her brother crosses the sea from Wales to Ireland to rescue her. Within the story the Irish Sea is said to be shallow; in addition, it contains two rivers, the Lli and the Archan. • The fictional Sodor, an island in both Wilbert Awdry's The Railway Series and the children's TV show, Thomas and Friends based on Awdry's books, is located in the Irish Sea. == See also ==