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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.
OneGeology is an international collaborative project in the field of geology supported by 118 countries, UNESCO, and major global geoscience bodies.It is an International Year of Planet Earth flagship initiative that aims to enable online access to dynamic digital geological map of the world for everyone.
The Conor Pass or Connor Pass (Irish: An Chonair, 'the way or path') [2] is one of the highest mountain passes in Ireland served by an asphalted road. [3] It is on the R560 road on the Dingle Peninsula in County Kerry .
Geological Survey Ireland produces maps, reports and databases, and acts as a knowledge centre and project partner in a number of aspects of Irish geology. [ 3 ] The organisation managed the Irish National Seabed Survey (INSS, 1999–2005), which on completion was the world's largest civilian marine mapping programme.
The Santa Susana Formation is a Paleogene period geologic formation in the Simi Hills and western Santa Susana Mountains of southern California. [1] [2] [3] The formation consists largely of light-gray shale and some fine-grained shaly sandstone, with a lens of heavy conglomerates in the lower part. [1] [4] Small beds of limestone are also ...
The Gap of Dunloe (from Irish Dún Lóich, meaning 'Lóich's stronghold'), also recorded as Bearna an Choimín (meaning "gap of the commonage" or "gap of the little hollow"), [3] is a narrow mountain pass running north–south in County Kerry, Ireland, that separates the MacGillycuddy's Reeks mountain range in the west, from the Purple Mountain Group range in the east.
The board also published (jointly with OSNI) a series of 1:50000 maps of the entire island known as the Discovery Series [5] and a series of 1:25000 maps of places of interest (such as the Aran Islands and Killarney national park) and the Geology of Ireland. [6]
Geological maps of County Donegal show rock alignments running south-west to north east across the Fanad peninsula. The underlying rock in the peninsula is mostly of Dalradian meta-sedimentary rocks, which have been exposed by weathering and erosion over the millennia There are areas of Granodiorite igneous rocks across the northern end of the peninsula from Ballywhoriskey to Fanad Head, but ...