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Giant's Causeway interlocking basalt columns Northern Ireland UK

La côte maritime avec des rochers, en Irlande du Nord

Panoramic shot of the Wall of Basalt Formations of the Giants Causeway, County Antrim, Northern Ireland

Basalt

Beautiful Giants Causeway Volcanic Landscape with famous Hexagonal Basalt Columns under dramatic skyscape. Giants Causeway, Northern Ireland, UK

Coastline at the Giants Causeway in Northern Ireland under a dramatic sky.

Northern Ireland, UK. Cliffs at Atlantic coast in County Antrim with visible geological strata and volcanic basalt formation of natural hexagonal poles resembling organ pipes. Aerial panorama

The Giant’s Causeway interlocking basalt columns natural beauty with a man with a Masai Blanket standing

Large rock formation on the coast of Northern Ireland, UK, near a body of water at Giant's Causeway, Bushmills, Northern Ireland, UK.

The Giant's Causeway is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic fissure eruption located in County Antrim on the north coast of Northern Ireland, about three miles northeast of the town of Bushmills

Bushmills, County Antrim, Northern Ireland, Ulster: Giant's Causeway (Irish: Clochán an Aifir) pattern of eroded hexagonal basalt columns entering the Atlantic Ocean - This area was mainly chalk when enormous amounts of highly fluid lava came to the surface from the depths some 60 million years ago. The constructive continental plate movement created rifts and oceanic spreading or sea floor spreading. This created a thick lava plateau. This lava cooled and shrank, so we still see the characteristic basalt columns today - UNESCO World Heritage Site 'The Giant's Causeway and Causeway Coast'.

Basalt columns rising from the sea. This geological feature results from erosion on ancient volcanic larva. This unique tourist attraction is the feature of some lovely Irish legends.

The Giants Causeway is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic fissure eruption. It is located in County Antrim on the north coast of Northern Ireland, about three miles northeast of the town of Bushmills. 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 some have four, five, seven or eight sides. The tallest are about 39 ft high.

County Antrim, Northern Ireland: -The Giant's Causeway is an area of some 40,000 interlocking basalt columns, the result of an ancient volcanic eruption.

North Ireland- Giant’s Causeway

The North Causeway Coast in Northern Ireland

Basalt rocks and a rough sea at the Giants Causeway in Northern Ireland.

Border of Ireland

Basalt Formations of the Giants Causeway, County Antrim, Northern Ireland

View during auto trip in West Iceland, Snaefellsnes peninsula, Snaefellsjokull National Park, Londrangar View Point. Spectacular black volcanic rocky ocean coast, landmark volcanic towers on cliff.

Giants Causeway in Northern Ireland.

Giant's Causeway Co. Antrim Northern Ireland

Hexagonal columns of basalt, cliff face and tourists (out of focus) at the shoreline of the Giant's Causeway, County Antrim, Northern Ireland. The site is a UNESCO World Heritage Site.

Des petites pierres sur le sol de la chaussée des géants, en Irlande du Nord

High angle view of a group of tourists walking along a road running next to a rocky coastline

Panoramic View of World Heritage site Giants Causeway bay on the northeast Irish coast in Northern Ireland

The Giants Causeway is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic fissure eruption. It is located in County Antrim on the north coast of Northern Ireland, about three miles northeast of the town of Bushmills. 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 some have four, five, seven or eight sides. The tallest are about 39 ft high.

Bushmills, County Antrim, Northern Ireland / Ulster: Giant's Causeway and the Atlantic - eroded hexagonal basalt columns entering the ocean - This area was mainly chalk when enormous amounts of highly fluid lava came to the surface from the depths some 60 million years ago. The constructive continental plate movement created rifts and oceanic spreading or sea floor spreading. This created a thick lava plateau. This lava cooled and shrank, so we still see the characteristic basalt columns today - UNESCO World Heritage Site 'The Giant's Causeway and Causeway Coast'

Free Images: "bestof:Northern Ireland banner Giants causeway.jpg en Wikivoyage banner for Northern Ireland Cropped from this PD-licensed picture http //commons wikimedia org/wiki/..."

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