giant causeway north ireland

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Detail of  basalt columns at Giant`s Causeway North Ireland, UK isolated on white background Royalty Free Stock Photo
Giant`s Causeway, North Ireland, UK during winters. The fierce waves batter the iconic coastline of North Ireland. Royalty Free Stock Photo
Giant`s Causeway in North Ireland Royalty Free Stock Photo
Giant`s Causeway in North Ireland Royalty Free Stock Photo
Giant`s Causeway in North Ireland Royalty Free Stock Photo
Giant`s Causeway in North Ireland Royalty Free Stock Photo
The Giant`s Causeway, UNESCO World Heritage Site, located on the north County Antrim coast of Northern Ireland. Royalty Free Stock Photo
Giant causeway in north ireland
Landscapes of the Giant`s Causeway against blue sky in North Ireland, United Kingdom Royalty Free Stock Photo
Landscapes of the Giant`s Causeway against blue sky in North Ireland, United Kingdom Royalty Free Stock Photo
The Giant`s Causeway, UNESCO World Heritage Site, located on the north County Antrim coast of Northern Ireland. Royalty Free Stock Photo
The Giant`s Causeway, UNESCO World Heritage Site, located on the north County Antrim coast of Northern Ireland. Royalty Free Stock Photo
Giant& x27;s Causeway, North of Ireland. Royalty Free Stock Photo
Cliffs and rock by the north ireland sea with giant causeway Royalty Free Stock Photo
North Ireland GIANT'S CAUSEWAY. Ocean coast landscape. Royalty Free Stock Photo
The Giant's Causeway is an area of about 40, 000 interlocking basalt columns, the result of an ancient volcanic eruption. It is also known as Clochán an Aifir or Clochán na bhFomhórach in Irish and tha Giant's Causey in Ulster-Scots. It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4. 8 km) northeast of the town of Bushmills. It was declared a World Heritage Site by UNESCO in 1986, and a national nature reserve in 1987 by the Department of the Environment for Northern Ireland. In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although there are also some with four, five, seven or eight sides. The tallest are about 12 metres (39 ft) high, and the solidified lava in the cliffs is 28 metres (92 ft) thick in places.


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