County Wicklow
County Wicklow is a county in Ireland. The last of the traditional 32 counties, having been formed as late as 1606, it is part of the Eastern and Midland Region and the province of Leinster. It is bordered by the Irish Sea to the east and the counties of Wexford to the south, Carlow to the southwest, Kildare to the west, and South Dublin and Dún Laoghaire–Rathdown to the north.
Wicklow is named after its county town of Wicklow, which derives from the name Víkingaló. Wicklow County Council is the local authority for the county, which had a population of 155,258 at the 2022 census. Colloquially known as the "Garden of Ireland" for its scenerywhich includes extensive woodlands, nature trails, beaches, and ancient ruins while allowing for a multitude of walking, hiking, and climbing optionsit is the 17th largest of Ireland's 32 counties by area and the 16th largest by population. It is also the fourth largest of Leinster's 12 counties by size and the fifth largest in terms of population.
History
Missions and monasteries
During the 5th century Saint Palladius, a bishop from Britain or Gaul was sent to 'the Irish believing in Christ.' He and his companions landed at Wicklow harbour in the year 431 AD. Palladius founded three ancient churches at Donard, Tigroney and Colbinstown. Along with him came two clerics named St. Sylvester and Solonius who died and were buried at Donard. The local tribe in the area were called Cualann and their chief, a man named Naithi was opposed to these Christian missionaries. Despite this hostility however Palladius seems to have gained support elsewhere as he was able to erect those three churches in the Wicklow area. After a rather unsuccessful stay in the county St. Palladius departed Ireland and journeyed to Scotland.A large number of early Irish saints male and female founded churches, monasteries and convents in Wicklow. Among them were St. Kevin, St. Dagan, St. Ernan, St. Credan, St. Baotan and the holy women St. Cainnear, St. Ceoltigherna, St. Fledh, St. Tartinna, St. Coine and St. Croine. The ancient monastery of Glendalough is located in the county.
17th century onwards
County Wicklow was the last of the traditional counties of Ireland to be shired in 1606 from land previously part of counties Dublin and Carlow. Established as a distinct county, it was aimed at controlling local groups such as the O'Byrnes. The Military Road, stretching from Rathfarnham to Aghavannagh crosses the mountains, north to south, and was built by government forces to assist them in defeating the rebels still active in the Wicklow Mountains following the failed Irish Rebellion of 1798. It provided them with access to an area that had been a hotbed of Irish rebellion for centuries. Several barracks to house the soldiers were built along the route; in 1974 the Glencree Centre for Peace and Reconciliation was opened alongside the remains of Glencree barracks. Battalions of the Irish Army use firing ranges in County Wicklow for tactical exercises, especially the largest one in the Glen of Imaal which was previously used by the British Army prior to independence.There was a brief Wicklow gold rush in the year 1795 near the village of Woodenbridge that lasted for a month, during which as many as 80 kilograms of gold was recovered by unlicensed prospectors before the government took over.
During the Cromwellian conquest of Ireland, local authorities immediately surrendered without a fight. During the Irish Rebellion of 1798, some of the United Irishmen insurgents took refuge in the Wicklow Mountains, resulting in clashes between British forces and rebels commanded by Joseph Holt near Aughrim and later at Arklow.
The boundaries of the county were extended in 1957 by the Local Government Act which "detached lands from the County of Dublin and from the jurisdiction and powers of the Council of the County of Dublin" near Bray and added them to the County of Wicklow.
Irish language
Wicklow was the first county in Ireland to lose the Irish language, with only around 2% of people speaking it in the 1770s. It was spoken on the Western slopes of the Wicklow Mountains in the 1790s. Andrew and Hannah Byrne of Glenealy, who both died in 1830, were among the last native speakers in the county.Geography
Location
Wicklow is part of the Eastern and Midland Region of Ireland, within the province of Leinster. It is bounded by four counties, Dublin to the north; Kildare and Carlow to the west; Wexford to the south; and the Irish Sea to the east. Wicklow is the 17th largest of Ireland's 32 traditional counties by land area, and the 16th most populous. It is the fourth largest of Leinster's 12 counties by size and the fifth most populous. The county is named after the town of Wicklow, located approximately south of Dublin, the capital city of Ireland.The Wicklow Mountains are Ireland's largest continuous upland area and occupy a significant portion of the county, spanning the entire centre of Wicklow and stretching into Dublin and Wexford at their southern and northern fringes. Lugnaquilla, at above sea level, is the tallest peak in the range, the highest mountain in Ireland outside of County Kerry, and Ireland's 13th-highest mountain overall. The Wicklow Mountains National Park, located in the middle of the county, is a dedicated protected area covering, making it the largest national park in Ireland. The Wicklow Way was the first long-distance trail in the State, and crosses the range for.
Geology
The Wicklow Mountains are centred on the Leinster batholith and are primarily composed of granite surrounded by an envelope of mica-schist and much older rocks such as quartzite. Covering, the Leinster batholith is the most expansive mass of intrusive igneous rock in Ireland or Britain. The oldest rocks in the county are the quartzites of the Bray Group that include Bray Head and the Little Sugar Loaf and Great Sugar Loaf mountains. These metamorphosed from sandstone deposited in the deep waters of the primeval Iapetus Ocean during the Cambrian period.As with much of Ireland, Wicklow's terrain was sculpted by successive periods of glaciation during the quaternary. Weathering and erosion by ice carved out long valleys known as glens such as Glenmacnass, Glen of the Downs, Glenmalure, Glen of Imaal, Glencree and Glendalough. The Irish Sea Ice-Sheet began to retreat shortly after the Last Glacial Maximum ca. 20,000–23,000 years ago but significant ice masses persisted in the Wicklow Mountains for another 4,000–7,000 years.
Hydrology
Major rivers include the River Liffey, Ireland's 8th-longest river, which rises near Tonduff mountain and flows through the centre of Dublin City, reaching the Irish Sea at Dublin Bay. Its biggest tributary by volume, the River Dodder, rises along the northern slope of Kippure in the far north of the county, while the Kings River joins at Blessington Lakes. Multiple other Liffey tributaries flow within the county.The River Slaney, which starts at Lugnaquilla, flows west and then south before reaching St George's Channel at Wexford town. The Avonmore and Avonbeg rivers join to form the Avoca River at the Meeting of the Waters in the Vale of Avoca. The River Derreen in the south of the county defines a section of the border with Carlow.
File:Poulaphouca Reservoir, Co. Wicklow .jpg|thumb|The Poulaphouca Reservoir near Blessington is Ireland's largest artificial lake
Most of the county's lakes are glacially derived ribbon and corrie lakes found in scenic trough valleys surrounded by mountains, making them popular with tourists. Notable lakes in the county include Glendalough Upper Lake, Lough Tay, Lough Ouler, Lough Bray, Lough Dan and Lough Nahanagan.
Poulaphouca Reservoir is the largest of Wicklow's lakes, covering in the west of the county. It is the largest artificial lake in Ireland and was created following the damming of the River Liffey at Poulaphouca in 1940. The village of Ballinahown was completed submerged by the reservoir and its 70 families were relocated. Ruins of the old village including buildings, fences and farm machinery can be seen during droughts when water levels in the reservoir diminish. The lower Vartry Reservoir, constructed between 1862 and 1868, is the county's second largest lake.