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Beautiful Giants Causeway Volcanic Landscape with famous Hexagonal Basalt Columns under dramatic skyscape. Giants Causeway, Northern Ireland, UK
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.
Giants Causeway
Giant's Causeway interlocking basalt columns Northern Ireland UK
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
Dublin, Wild Atlantic Way, Northern Ireland
Utoro, Japan - June 6, 2016: Oronko Rock View from 60 m huge rock, Orankoiwa rock to the parking and rocky reef with big public parking and small pier on right side. the rock is surrounded with blue Okhotsk sea. On parking there are many cars, taxi and big bus with driver. It is north east Hokkaido, Japan.
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 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.
Basalt rocks and a rough sea at the Giants Causeway in Northern Ireland on a windy day
The Giant's Causeway (Irish: Clochán an Aifir) 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.\nIt was declared a World Heritage Site by UNESCO in 1986 and a national nature reserve by the Department of the Environment for Northern Ireland in 1987.
Basalt Formations of the Giants Causeway, County Antrim, Northern Ireland
Giants Causeway in Northern Ireland.
The nature hexagon columns at the beach called the Giant's Causeway, County Antrim, Northern Ireland. Selective focus, basalt formation.
Basalt
Basalt Column detail at Giant's Causeway in Northern Ireland
Des falaises verdoyantes et la côte maritime en Irlande du Nord
Sunset at Giant's causeway in Northern Ireland
Abstract view of rock formations of basalt columns at Giant's Causeway in 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.
Coast of 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.
Giant's Causeway, Northern Ireland
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'
Giants Causeway, N. Ireland
The Giant's Causeway Antrim Northern Ireland
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