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Holy Island, Anglesey
Holy Island ( cy, Ynys Gybi, 'the island of (Saint) Cybi') is an island () on the western side of the larger Isle of Anglesey, Wales, from which it is separated by the Cymyran Strait. It is called "Holy" because of the high concentration of standing stones, burial chambers, and other religious sites on the small island. The alternative English name of the island is Holyhead Island. According to the 2011 UK Census, the population was 13,659, of which 11,431 (84%) lived in the largest town, Holyhead. History Irish pirates invaded Anglesey following the end of Roman rule in Britannia. Cunedda first began warfare against the Irish but ultimately Cadwallon Lawhir defeated the Irish on Holy Island. Natural features There are a variety of natural habitats on the island including mudflats, dunes, marshes, and beaches. Practically nothing is left of the oak forest that covered almost all of the island before the arrival of Neolithic farmers. The western side of the island is t ...
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Irish Sea
The Irish Sea or , gv, Y Keayn Yernagh, sco, Erse Sie, gd, Muir Èireann , Ulster-Scots: ''Airish Sea'', cy, Môr Iwerddon . is an extensive body of water that separates the islands of Ireland and Great Britain. It is linked to the Celtic Sea in the south by St George's Channel and to the Inner Seas off the West Coast of Scotland in the north by the North Channel. Anglesey, North Wales, is the largest island in the Irish Sea, followed by the Isle of Man. The term ''Manx Sea'' may occasionally be encountered ( cy, Môr Manaw, ga, Muir Meann gv, Mooir Vannin, gd, Muir Mhanainn). On its shoreline are Scotland to the north, England to the east, Wales to the southeast, Northern Ireland and the Republic of Ireland to the west. The Irish Sea is of significant economic importance to regional trade, shipping and transport, as well as fishing and power generation in the form of wind power and nuclear power plants. Annual traffic between Great Britain and Ireland amount ...
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Cadwallon Lawhir
Cadwallon ap Einion (c. 460-517 or 534), usually known as Cadwallon Lawhir ('Long Hand') and also called Cadwallon I by some historians, was a Welsh ruler around 500. Cadwallon was the son of Einion Yrth and Prawst ferch Deithlyn. He is often considered to have been king of Gwynedd from his father's death in about 500 until his own death some time between 517 and 534. He is credited with having driven the last Irish settlers off the island of Anglesey. According to one tradition, Cadwallon and his army padlocked their own feet to their stirrups so that they could not be tempted to flee the battle. Cadwallon's epithet, ''Lawhir'', may possibly refer to him having longer than usual arms or might also be a metaphor, referring to the extent of his authority. The late medieval poet Iolo Goch claims that he could "reach a stone from the ground to kill a raven, without bending his back, because his arm was as long as his side to the ground." According to Gildas, Cadwallon's son, Mae ...
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Beddmanarch–Cymyran
Beddmanarch–Cymyran is a site of special scientific interest (SSSI) on the Welsh island of Anglesey extending to just over , and centred on the Cymyran Strait. It was first notified in 1961 for its coastal botanical and ornithological interest. The site is also a marine protected area as it includes intertidal areas and contains marine components. Area The Beddmanarch–Cymyran site comprises the area of coastal salt-marshes, mud-flats and shallow coastal water lying between Holy Island and the mainland of Anglesey. This includes the Cymyran Strait (sometimes called the Holy Island Strait), the tidal reaches of the Afon Alaw to the east and extends northwards to Porth Penrhyn-Mawr. There are two crossings over the water that makes up the site, Four Mile Bridge (road and pedestrian) and the Stanley Embankment (road, rail and pedestrian). The area between the two bridges is known as the ''Inland Sea''. Importance The site includes four special areas of interest: *Marine biolog ...
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Shipwrecks
A shipwreck is the wreckage of a ship that is located either beached on land or sunken to the bottom of a body of water. Shipwrecking may be intentional or unintentional. Angela Croome reported in January 1999 that there were approximately three million shipwrecks worldwide (an estimate rapidly endorsed by UNESCO and other organizations). When a ship's crew has died or abandoned the ship, and the ship has remained adrift but unsunk, they are instead referred to as ghost ships. Types Historic wrecks are attractive to maritime archaeologists because they preserve historical information: for example, studying the wreck of revealed information about seafaring, warfare, and life in the 16th century. Military wrecks, caused by a skirmish at sea, are studied to find details about the historic event; they reveal much about the battle that occurred. Discoveries of treasure ships, often from the period of European colonisation, which sank in remote locations leaving few livi ...
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Penrhos Country Park
Penrhos Country Park (also known as Penrhos Coastal Park) () is a country park near Holyhead, on the island of Anglesey in Wales, United Kingdom. The park attracts approximately 100,000 visitors each year. It was opened in 1971 on the former Penrhos estate which was formerly owned by the Stanley family and at the time of opening the Anglesey Aluminium Anglesey Aluminium was a joint venture between Rio Tinto and Kaiser Aluminum. Its aluminium smelter, located on the outskirts of Holyhead, was one of the largest employers in North Wales, with 540 staff members, and began to produce aluminiu ... company. It is adjacent to the A55, on the Anglesey Coastal Path and also adjoins Beddmanarch Bay. References External links The park's page at the Anglesey Heritage website Country parks in Wales Parks in Anglesey Holyhead Protected areas established in 1971 1971 establishments in Wales {{Anglesey-geo-stub ...
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Trearddur Bay
Trearddur or Trearddur Bay ( cy, Bae Trearddur) is a village, seaside resort and community south of Holyhead on the west coast of Holy Island off the north-west coast of Anglesey in Wales. The community includes the small settlement of Penrhosfeilw and the Refail Farm estate. Name Historically the bay on which the village sits was known as Porth y Capel ( Welsh: ''bay of the chapel'') and the nearby dunes as Towyn y Capel (''dune of the chapel''). The village name is recorded variously as Treffyarddr, Tre Iarthur and Trefarthur with Trearddur first recorded in 1749. All versions signify the ''settlement of Iarddur'', a key figure in the Middle Ages. History At the centre of the beach lies an ancient burial ground known by the old names and which was excavated in 2003. At the 2001 census, the community had a population of 1,858, reducing to 1,686 at the 2011 census. As with many places on the Welsh coast Trearddur is quite Anglicized with 44% of the population born in Englan ...
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South Stack Lighthouse
The South Stack Lighthouse is built on the summit of a small island off the north-west coast of Holy Island, Anglesey, Wales. It was built in 1809 to warn ships of the dangerous rocks below. History The lighthouse has warned passing ships of the treacherous rock below since its completion in 1809. The -tall lighthouse on South Stack was designed by Daniel Alexander and the main light is visible to passing vessels for , and was designed to allow safe passage for ships on the treacherous Dublin–Holyhead–Liverpool sea route. It provides the first beacon along the northern coast of Anglesey for east-bound ships. It is followed by lighthouses, fog horns and other markers at North Stack, Holyhead Breakwater, The Skerries, the Mice, Point Lynas and at the south-east tip of the island Trwyn Du. The lighthouse is operated remotely by Trinity House. It has been visited by the team at ''Most Haunted''. Visitors can climb to the top of the lighthouse and tour the engine room and ex ...
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South Stack
South Stack ( cy, Ynys Lawd) is an island situated just off Holy Island on the northwest coast of Anglesey, Wales. Geology South Stack is an island known as a sea stack. It was formed by the wave erosion of sedimentary rocks that once connected the island to the mainland. The area is known geologically as the South Stack Formation. Its strata includes sandstones and interbedded shales which have been contorted by large folds and crumples. The folds can be seen in the seacliffs (best viewed from the steps leading down to the lighthouse). Thick beds of pure Holyhead Quartzite, which forms the bulk of Holyhead Mountain, lie above these folded sedimentary rocks. Recent studies suggests the rocks appearance was caused by large scale earth movements which is not a part of the normal sedimentary process; however, this theory remains controversial. Similar evidence of upthrusts can be seen in the cliffs to the south of South Stack. The fascinating geology of South Stack has be ...
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North Stack
North Stack ( Welsh: Ynys Arw, meaning "rugged island") is a small island situated just off Holy Island on the north-west coast of Anglesey. The area has been an important location in the development of traditional climbing in Britain and has several notable classic, and also extreme, climbing routes. Description North Stack is the site of a redundant fog warning station, comprising a number of buildings, including the Trinity House Magazine, built-in 1861, where shells for the warning cannon were stored. These buildings now house a bird-watching observatory,North Stack
holyhead.com. Retrieved 31 December 2010.
giving a view of lighthouse across Gogarth Bay, and the studio of artist Philippa J ...
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Holyhead Mountain
Holyhead Mountain (''Mynydd Twr'' in Welsh: from ''(pen)twr'', meaning "tower") is the highest mountain on Holy Island, Anglesey, and the highest in the county of Anglesey, north Wales. It lies about two miles west of the town of Holyhead, and slopes steeply down to the Irish Sea on two sides. Ireland can be seen from here on a clear day and the mountain is an important site for seabirds. The mountain Holyhead Mountain is located on Holy Island, Anglesey, jutting out into the Irish Sea. At , it is the highest mountain in the county of Anglesey, being higher than Bodafon Mountain () on the main island. On the east side of the mountain is the site of a late Roman watchtower called ''Caer y Tŵr'' (Tower Fortress), from which Holyhead Mountain's Welsh name is derived. Holyhead Mountain also has the remains of a group of Iron Age huts near its foot. This shows evidence of being occupied in the middle part of the Stone Age, the Neolithic Age, the Bronze Age and the Iron Age. There a ...
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Neolithic
The Neolithic period, or New Stone Age, is an Old World archaeological period and the final division of the Stone Age. It saw the Neolithic Revolution, a wide-ranging set of developments that appear to have arisen independently in several parts of the world. This "Neolithic package" included the introduction of farming, domestication of animals, and change from a hunter-gatherer lifestyle to one of settlement. It began about 12,000 years ago when farming appeared in the Epipalaeolithic Near East, and later in other parts of the world. The Neolithic lasted in the Near East until the transitional period of the Chalcolithic (Copper Age) from about 6,500 years ago (4500 BC), marked by the development of metallurgy, leading up to the Bronze Age and Iron Age. In other places the Neolithic followed the Mesolithic (Middle Stone Age) and then lasted until later. In Ancient Egypt, the Neolithic lasted until the Protodynastic period, 3150 BC.Karin Sowada and Peter Grave. Egyp ...
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Beach
A beach is a landform alongside a body of water which consists of loose particles. The particles composing a beach are typically made from rock, such as sand, gravel, shingle, pebbles, etc., or biological sources, such as mollusc shells or coralline algae. Sediments settle in different densities and structures, depending on the local wave action and weather, creating different textures, colors and gradients or layers of material. Though some beaches form on inland freshwater locations such as lakes and rivers, most beaches are in coastal areas where wave or current action deposits and reworks sediments. Erosion and changing of beach geologies happens through natural processes, like wave action and extreme weather events. Where wind conditions are correct, beaches can be backed by coastal dunes which offer protection and regeneration for the beach. However, these natural forces have become more extreme due to climate change, permanently altering beaches at very ...
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