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The Giant's Causeway (Irish: Clochán an Aifir) [1] is an area of approximately 40,000 interlocking basalt columns, the result of an ancient volcanic fissure eruption. [3] [4] It is located in County Antrim on the north coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills.
Basalt columns seen on Porto Santo Island, Portugal. Columnar jointing of volcanic rocks exists in many places on Earth. Perhaps the most famous basalt lava flow in the world is the Giant's Causeway in Northern Ireland, in which the vertical joints form polygonal columns and give the impression of having been artificially constructed.
Cary is a historic barony in County Antrim, Northern Ireland. [2] To its north is the north-Antrim coast, and it is bordered by three other baronies: Dunluce Lower to the west; Dunluce Upper to the south; and Glenarm Lower to the south-east. [2] The Giant's Causeway is situated on the north coast of Cary.
The Carrick-a-Rede Rope Bridge (locally pronounced carrick-a-reed) is a rope bridge near Ballintoy in County Antrim, Northern Ireland. The bridge links the mainland to the tiny island of Carrickarede (from Irish Carraig a' Ráid, meaning 'rock of the casting'). [1] It spans 20 metres (66 ft) and is 30 metres (98 ft) above the rocks below. [2]
Columnar jointing in Giant's Causeway in Northern Ireland Columnar jointing in the Alcantara Gorge, Sicily. Columnar jointing is a geological structure where sets of intersecting closely spaced fractures, referred to as joints, result in the formation of a regular array of polygonal prisms (basalt prisms), or columns.
Much of the northeast of Ireland is a basalt plateau. An area of particular note is the Giant's Causeway on the north coast, a mainly basalt formation caused by volcanic activity between 50 and 60 million years ago. [21] The basalts were originally part of the great Thulean Plateau formed during the Paleogene period. [22]
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