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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 .
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.
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 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 geology of the Peak District National Park in England is dominated by a thick succession of faulted and folded sedimentary rocks of Carboniferous age. The Peak District is often divided into a southerly White Peak where Carboniferous Limestone outcrops and a northerly Dark Peak where the overlying succession of sandstones and mudstones dominate the landscape.
A geologic map or geological map is a special-purpose map made to show various geological features. Rock units or geologic strata are shown by color or symbols. Bedding planes and structural features such as faults , folds , are shown with strike and dip or trend and plunge symbols which give three-dimensional orientations features.
Map modified from Irwin (1990) [4] showing distribution of Great Valley Sequence and Franciscan Complex (in blue). Diagram (modified from Fig 3.11 in Irwin, 1990) showing the depositional setting of the Franciscan Assemblage and the contemporaneous Great Valley Sequence,.
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 ...