Giant's Causeway

Giant's Causeway, County Antrim, Northern Ireland (c) Ian Hay

Britain from the Air - Giant's Causeway

Volcanic lava that cooled 60 million years ago is today one of the geological wonders of the world.

The coastal landscapes around the UK are made up of rocks that vary in age. The oldest at around 3 billion years, are found in the hard rocky cliffs of the extreme northwest of Scotland and the Outer Hebrides. The youngest are the soft clays and sandstones on the coasts of East Anglia that are less than 3 million years old. The spectacular Giant’s Causeway is made of black volcanic rocks (basalt) some 60 million years old.

Hexagonal columns

The Causeway was created at a fascinating time in the Earth’s history, when the Atlantic Ocean was just beginning to form. The North Atlantic Ocean was created over millions of years through the steady widening of the ocean floor, either side of a submarine ridge in the middle of the sea.

As the land was being slowly torn apart by tectonic forces in the Earth’s crust, black molten lava began erupting over its surface. The lava cooled and shrank into the strange hexagonal columns that give the Giant’s Causeway - and its Scottish counterpart Fingal’s Cave - its impressive character. 

Legend of the giant’s causeway

According to legend, the columns were created by the mythical Irish giant Finn McCool in his argument with the Scottish giant Fingal.

After hurling insults and rocks at one another across the sea, Finn wrenched up giant blocks to create a causeway between Ireland and Scotland so that Fingal could come across and they could fight it out face to face. Fingal, frightened by a trick played by Finn, fled back to Fingal’s Cave, tearing up the causeway as he went, leaving only remnants behind on both shores.

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Location: Giant's Causeway, County Antrim, Northern Ireland, BT57 8SU
Grid reference: NR 13320 03356

Britain from the Air - Giant's Causeway credits

Thank you to -

Ian Hay for aerial photography

Text researched and written by the Royal Geographical Society (with IBG)

The size of the basalt columns, from a few centimetres to several metres, depends on the rate at which the lava cooled.