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Historic Walking Area Attractions In County Cavan

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County Cavan is a county in Ireland. It is in the province of Ulster and is part of the Border Region. It is named after the town of Cavan and is based on the historic Gaelic territory of East Breffny . Cavan County Council is the local authority for the county, which has a population of 76,092 according to the 2016 census.
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Historic Walking Area Attractions In County Cavan

  • 1. Killeshandra Looped Walking Trail Killeshandra
    Killeshandra or Killashandra - Irish place name Cill na Seanrátha meaning Church of the Old Rath , population 1,143, is a small town in County Cavan, Ireland. It is 20 km northwest of Cavan town and central to County Cavan's lakeland and geopark region, in the unique Erne catchment environment of rivers, lakes, wetlands and woodland. Together with the Lough Oughter Special Protected Area , it has been recognised by the EU programme for wildlife Natura 2000 since 2010. Killeshandra is specially noted by Failte Ireland as an Angling Centre of Excellence, as well as a hub for the Cavan Walking Festival which takes place in May each year. There are several looped walking and cycling trails in Killykeen Forest Park. The town also has a prominent football club called the Killeshandra GFC, known...
    From Wikipedia, the free encyclopedia.
  • 2. Wicklow Mountains National Park Glendalough Village
    The Wicklow Mountains form the largest continuous upland area in Ireland. They occupy the whole centre of County Wicklow and stretch outside its borders into Counties Dublin, Wexford and Carlow. Where the mountains extend into County Dublin, they are known locally as the Dublin Mountains . The highest peak is Lugnaquilla at 925 metres . The mountains are primarily composed of granite surrounded by an envelope of mica-schist and much older rocks such as quartzite. They were pushed up during the Caledonian orogeny at the start of the Devonian period and form part of the Leinster Chain, the largest continuous area of granite in Ireland and Britain. The mountains owe much of their present topography to the effects of the last ice age, which deepened the valleys and created corrie and ribbon la...
    From Wikipedia, the free encyclopedia.

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