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The Geology of Yorkshire in northern England shows a very close relationship between the major topographical areas and the geological period in which their rocks were formed. The rocks of the Pennine chain of hills in the west are of Carboniferous origin whilst those of the central vale are Permo-Triassic.
Yorkshire is drained by several rivers. In western and central Yorkshire, the many rivers empty their waters into the River Ouse, which reaches the North Sea via the Humber Estuary. [1] The most northerly of the rivers in the Ouse system is the River Swale, which drains Swaledale before passing through Richmond and meandering across the Vale of ...
The geology of the Yorkshire Dales National Park in northern England largely consists of a sequence of sedimentary rocks of Ordovician to Permian age. The core area of the Yorkshire Dales is formed from a layer-cake of limestones , sandstones and mudstones laid down during the Carboniferous period.
Pages in category "Geology of Yorkshire" The following 9 pages are in this category, out of 9 total. This list may not reflect recent changes. ...
Yorkshire (/ ˈ j ɔːr k ʃ ər,-ʃ ɪər / YORK-shər, -sheer) is an area of Northern England which was historically a county. [1] Despite no longer being used for administration, Yorkshire retains a strong regional identity. [2] The county was named after its county town, the city of York.
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The Ingleton Group is a group of Ordovician turbiditic sandstones, siltstones, conglomerates found within inliers in the Craven district of North Yorkshire, England.The two inliers are exposed in the valley of the River Doe northeast of Ingleton and at Horton-in-Ribblesdale to the east.
Geology of Yorkshire (4 C, 9 P) L. Lakes of Yorkshire (5 C, 1 P) Landforms of Yorkshire (1 C) Leeds City Region (20 P) N. Geography of North Yorkshire (18 C, 9 P) P.