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Ynys Môn (Senedd constituency)

1999 establishments in WalesConstituencies established in 1999EngvarB from June 2018Politics of AngleseySenedd constituencies in the North Wales electoral region
Ynys Môn (Assembly constituency)
Ynys Môn (Assembly constituency)

Ynys Môn is a constituency of the Senedd. It elects one Member of the Senedd by the first past the post method of election. Also, however, it is one of nine constituencies in the North Wales electoral region, which elects four additional members, in addition to nine constituency members, to produce a degree of proportional representation for the region as a whole. It was represented from 1999 by Ieuan Wyn Jones, the former leader of Plaid Cymru. Jones resigned from the Assembly on 20 June 2013, triggering a by-election, which was held on 1 August 2013. Plaid Cymru's candidate Rhun ap Iorwerth comfortably held the seat for the party with a majority of over 9000 votes.

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Ynys Môn (Senedd constituency)

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N 53.284 ° E -4.361 °
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LL77 7PZ
Wales, United Kingdom
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Ynys Môn (Assembly constituency)
Ynys Môn (Assembly constituency)
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GeoMôn

GeoMôn UNESCO Global Geopark is a Geopark covering the entire island of Anglesey in north Wales. It was admitted to the European Geoparks Network and to the UNESCO-assisted Global Network of National Geoparks in May 2009. It was the second Geopark to be designated in Wales, the seventh within the United Kingdom and the thirty-third in Europe. The UNESCO Geopark designation reflects the diversity of the island's geology, which encompasses solid rocks from the Precambrian to the Neogene with some Miocene sediments and extensive Pleistocene glaciation features from the Quaternary period. GeoMôn covers 720 square kilometres and has 125 miles of coastal walks.The Isle of Anglesey lies off the north coast of Wales, UK. It is known as Ynys Môn in Welsh. Around 67,000 people live on the island. The local culture is very distinctive, with around 60% of the population using Welsh as their first language. The island is known for its diverse tectonic geology. South Stack exhibits particular folding and faulting that have made it a site of interest for many years, having been first identified as the oldest Precambrian rock then the youngest and now said to be from the Cambrian period. It is a common location for students and schools who come here to study folding and faulting as well as examining the evidence for the birth of the Atlantic. Llanddwyn Island on the west Anglesey coast is a small, but complete oceanic plate, with the pillow lavas at its eastern end created at a Precambrian constructive plate margin. The plate interior on the northern coast is composed of mudstones and sandstones, some containing ‘dropstones, the remnants of the Gaskier's Ice Age that occurred at the end of Precambrian times. Anglesey is the type locality for a rock type named "mélange" by Edward Greenly when he first mapped the geology of Anglesey in the early years of the twentieth century. GeoMôn publishes a series of local trails to guide the visitor around the coastal areas of the island served by the 125 mile long coastal path. The trail at Beaumaris illustrates the use of rocks in the building of the 13th century castle, roofs and roads as well as more ornate carvings on high-status buildings. The castle built by King Edward I was intended to ‘tame’ the local Welsh people and keep them in order. It is part of the Castles and Town Walls of King Edward in Gwynedd World Heritage Site. Oriel Ynys Môn is the municipal art gallery and museum dedicated to local artists and crafts. Anglesey’s two most important artists have exhibitions there. Firstly, there is an exhibition of the work of Charles Tunicliffe RA, the wildlife artist, and then Sir Kyffin Williams RA, whose work is shown in a new gallery dedicated to him. He was a founder member of the Geopark and its first patron. His great uncle, Sir Andrew Ramsay, was the second Director General of the British Geological Survey and a ‘Father’ of Welsh Geology; he died in Beaumaris and is buried in the churchyard at Llanddwyn, under a glacial erratic, a boulder of Shap Granite. Originally geoconservation on Anglesey was administered by the Gwynedd and Môn RIGS group, but a decision was taken to apply for Geopark membership. GeoMôn is administered by GeoMôn-Anglesey Geopark Limited, a company registered at Companies House, and a registered charity.GeoMôn produces books on the geology of the island as well as leaflets detailing a number of self-guided trails. There is a Geopark visitor centre open from 10am to 4pm every day except Monday, at the Watch House in Porth Amlwch. Porth Amlwch was created mainly to facilitate the export of copper ore from the mines on Parys Mountain. The Watch House was originally the waiting place for the pilots guiding sailing ships in and out of the tiny harbour.

Roman conquest of Anglesey
Roman conquest of Anglesey

The Roman conquest of Anglesey refers to two separate invasions of Anglesey in North West Wales that occurred during the early decades of the Roman conquest of Britain in the 1st century CE. The first invasion of North Wales began after the Romans had subjugated much of southern Britain. It was led by the Provincial governor of Britannia, Suetonius Paulinus, who led a successful assault on the island in 60–61 CE, but had to withdraw because of the Boudican revolt. In 77 CE, Gnaeus Julius Agricola's thorough subjugation of the island left it under Roman rule until the end of Roman rule in Britain in the early 5th century CE. Anglesey, which was recorded in Latin as Mona and is still known as Môn in modern Welsh, was a place of resistance to Roman rule because it was an important centre for the Celtic Druids and their religious practices. After the conquest, there are no surviving Roman sources that mention Anglesey. Archaeologists have located a fort dated shortly after the first conquest near Cemlyn Bay; a trading settlement on the shore of the Menai Strait; and a village of huts huddled together on a hill for defence. In the last decades of Roman rule in Britain several military forts were built on the northern and western coasts to defend the island against Irish sea raiders. However, despite more than three centuries of Roman rule, archaeologists have found no evidence of major civic centres or villas on the island indicating that Romano-British culture lacked the influence it had in other parts of the Roman province of Britannia. The only Roman source for the island's two invasions is the Roman historian Tacitus. His last work The Annals, written as a history of the Roman Empire from Tiberius until Nero, mentions the first invasion by Suetonius Paulinus. The second invasion is detailed in Tacitus' work The Life of Gnaeus Julius Agricola, which was written to record and extol the life and accomplishments of his father-in-law. Tacitus may have used first-hand accounts from Agricola, who had been present with the Roman forces on both occasions.