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The Giant's Causeway (Irish: Clochán an Aifir) [1] is an area of approximately 40,000 interlocking basalt columns, the result of an ancient volcanic fissure eruption. [3] [4] 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.
Dunseverick Castle is situated in County Antrim, Northern Ireland, near the small village of Dunseverick and the Giant's Causeway.Dunseverick Castle and earthworks are Scheduled Historic Monuments in the townland of Feigh, in Causeway coast and Glens district council, at grid ref: C9871 4467.
Basalt columns seen on Porto Santo Island, Portugal. Columnar jointing of volcanic rocks exists in many places on Earth. Perhaps the most famous basalt lava flow in the world is the Giant's Causeway in Northern Ireland, in which the vertical joints form polygonal columns and give the impression of having been artificially constructed.
Dunseverick (from Irish Dún Sobhairce 'Sobhairce's fort') [3] is a hamlet near the Giant's Causeway in County Antrim, Northern Ireland. The name is also the alias for the townland of Feigh . [ 4 ] It is most notable for Dunseverick Castle .
Dunluce Castle (/ d ʊ n ˈ l uː s /; from Irish Dún Libhse) [3] is a now-ruined medieval castle in Northern Ireland, the seat of Clan MacDonnell.It is located on the edge of a basalt outcropping in County Antrim (between Portballintrae and Portrush), and is accessible via a bridge connecting it to the mainland.
View from the depths of the cave with the island of Iona visible in the background, 2008 Basalt columns inside Fingal's Cave, 2022. Fingal's Cave is formed entirely from hexagonally jointed basalt columns within a Paleocene lava flow [2] and is similar in structure to both the Giant's Causeway in Northern Ireland and Ulva.
The interlocking basalt columns on the north-east side of Fingal Head were called the "Giants Causeway", named after the famous Giants Causeway between Northern Ireland and Western Scotland. The Fingal Caves located on the south side of Fingal Head, were destroyed and used in the early 1900s for the Tweed Break water.
Google Maps' location tracking is regarded by some as a threat to users' privacy, with Dylan Tweney of VentureBeat writing in August 2014 that "Google is probably logging your location, step by step, via Google Maps", and linked users to Google's location history map, which "lets you see the path you've traced for any given day that your ...
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