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Bedrock geological map of Ireland. Layers of Upper Carboniferous sedimentary rocks, Loop Head, County Clare. The geology of Ireland consists of the study of the rock formations on the island of Ireland. It includes rocks from every age from Proterozoic to Holocene and a large variety of different rock types is represented.
Dún Briste (English: Dun Briste Sea Stack) is a natural sea stack or pilaster - in geomorphology called stack - that was formed in Ireland during the Carboniferous period, possibly Mississippian, approximately 350 million years ago. [1] Dún Briste sea stack
Ireland's geological history includes a wide range of elements, from volcanism and tropical seas to the last glacial period. Ireland was formed in two distinct parts, which slowly joined, uniting about 440 million years ago. As a result of tectonics and the effect of ice, the sea level has risen and fallen.
Ireland fields a single national rugby team and a single association, the Irish Rugby Football Union, governs the sport across the island. The Irish rugby team have played in every Rugby World Cup, making the quarter-finals in eight of them. [196] Ireland also hosted games during the 1991 and the 1999 Rugby World Cups (including a quarter-final).
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There is not agreement about whether the Great Glen Fault is "active" – accumulating seismic slip. [4] Some parts of the fault are moving in opposite directions, but the extent of displacement is not agreed on. The displacement could be at least the full length of the exposed fault on mainland Scotland. [5]
Pages in category "Geologic formations of Ireland" The following 37 pages are in this category, out of 37 total. This list may not reflect recent changes. *
While the tricolour today is the official flag of Ireland, it is not an official flag in Northern Ireland although it is sometimes used unofficially. The only official flag representing Northern Ireland is the Union Flag of the United Kingdom of Great Britain and Northern Ireland however its use is controversial. [ 75 ]