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

Northern Ireland

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

Waves crash on the steps of the Giants Causeway

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.

The Antrim Coastline in Northern Ireland is one of the most scenic and dramatic coastal areas in Europe, famous for its rugged cliffs, picturesque villages, and natural wonders.

Irish landscape in northern Ireland (County Antrim - United Kingdom - Europe)

Sunset at Giant's causeway in Northern Ireland

Abstract view of rock formations of basalt columns at Giant's Causeway in Northern Ireland

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

Basalt columns with flowers

The Giant's 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 (4.8 km) northeast of the town of Bushmills.

Giant's Causeway

Basalt columns stemming from the ground

Giant's Causeway Scenic Landscape Sunset Panorama under moody twilight skyscpe. Ultrawideangle 10mm Panorama Landscape Shot. Giants Causeway, Antrim County, Northern Ireland, United Kingdom, Northern Europe, Europe

Giants Causeway, an area of hexagonal basalt stones, created by ancient volcanic fissure eruption, County Antrim, Northern Ireland. Famous tourist attraction, UNESCO World Heritage Site.

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

Basalt

Basalt Column detail at Giant's Causeway in Northern Ireland

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

famous giants causeway stones infinity horizon over the atlantic ocean in northern ireland, europe.

Giant’s Causeway in Northern Ireland

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

Giant's Causeway in a beautiful summer day, Northern Ireland

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'.

Giants Causeway Volcanic Landscape, Ultrawideangle Landscape Shot. Giants Causeway, Northern Ireland, UK

Giants Causeway

Natural phenomenon “Giant’s Causeway” in Northern Ireland. The hexagonal basalt columns form a truly astonishing site, especially at dawn. There is just a single person in the background of the scene, providing a perspective on size.

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.

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