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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
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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.
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.
Geological Survey Ireland is a division of the Department of Communications, Climate Action and Environment and is based in Booterstown in Dublin. [4] Its multidisciplinary staff work in sections such as groundwater, bedrock mapping (consisting of bedrock and quaternary/geotechnical), information management, heritage, marine and minerals.
Column 4 indicates on which sheet of the Geological Survey of Ireland's 1:50,000 scale geological map series of Ireland, the fault is shown and named (either on map/s or cross-section/s or both). Column 5 indicates a selection of publications in which references to the fault may be found. See references section for full details of publication.
Jukes lectured in Dublin as professor of geology for many years, first at the Royal Dublin Society's Museum of Irish Industry, and afterwards at the Dublin Royal College of Science. During this period he wrote an article On the Mode of Formation of some of the River-valleys in the South of Ireland (Quarterly Journ. Geol. Soc. 1862).