The amazing rock formation of Giant’s Causeway in Ireland

The Giant's Causeway in northeast coast of Northern Ireland is an area of about 40,000 interlocking basalt columns—the result of an ancient volcanic eruption. 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 and eight sides.

The remarkable geological features of the region have earned it the title of the Eight Wonder of the World and established it as a major part of Ireland's heritage. For 300 years, the causeway and the cliffs of the Causeway Coast have attracted thousands of visitors from around the world. Travellers have marvelled at the beauty of the formations while scientists have sought to describe and explain them.

The causeway was formed during the early Paleogene period, some 50 to 60 million years ago, over a long period of intense volcanic activity. Highly fluid molten basalt intruded through chalk beds to form an extensive lava plateau. As the lava cooled rapidly, contraction occurred. While contraction in the vertical direction reduced the flow thickness (without fracturing), horizontal contraction could only be accommodated by cracking throughout the flow. The extensive fracture network produced the distinctive columns seen today. The basalts were originally part of a great volcanic plateau called the Thulean Plateau, which was formed during the Paleogene period.


The Giant's Causeway 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.