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⚫ | The '''Vale of Clwyd''' ''([[Welsh language|Welsh]]: Dyffryn Clwyd)'' is a tract of low-lying ground in the [[county]] of [[Denbighshire]] in northeast [[Wales]]. The Vale extends south-southwestwards from the coast of the [[Irish Sea]] for some 20 miles (about 30km) forming a triangle of low ground bounded on its eastern side by the well-defined [[escarpment|scarp]] of the [[Clwydian Range]] and to the west by numerous low hills. The [[River Clwyd]] ''(Welsh: Afon Clwyd)'' which rises within [[Clocaenog Forest]], southwest of Denbigh, runs the full length of the vale. It is joined by the two major left bank tributaries of the [[River Clywedog (Clwyd)|River Clywedog]] ''(Welsh: Afon Clywedog)'' and [[River Elwy]] ''(Welsh: Afon Elwy)'' and the smaller right bank tributary of the [[River Wheeler]] ''(Welsh: Afon Chwiler).'' |
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{{Short description|Valley in Wales}} |
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{{About||the constituency of the House of Commons of the Parliament of the United Kingdom|Vale of Clwyd (UK Parliament constituency)|the Senedd constituency|Vale of Clwyd (Senedd constituency)}} |
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{{Use dmy dates|date=April 2022}} |
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{{Use British English|date=July 2022}} |
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⚫ | The '''Vale of Clwyd''' ( |
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==History== |
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⚫ | At its seaward end are the coastal resorts of [[Kinmel Bay]] ''(Welsh: Bae Cinmel''), [[Rhyl]] and [[Prestatyn]] whilst the towns of [[Abergele]] and [[St Asaph]] ''(Welsh: Llanelwy)'' lie just inland. The other principal towns of the vale are [[Denbigh]] ''(Welsh: Dinbych)'' and [[Ruthin]] ''(Welsh: Rhuthun)''.<ref>Ordnance Survey 1:50K Landranger sheet 116 'Denbigh & Colwyn Bay'</ref> The area falls within the modern administrative county (and [[unitary authority]]) of [[Denbighshire]] and much of it lies within the [[Vale of Clwyd (UK Parliament constituency)|Vale of Clwyd UK Parliamentary constituency]] |
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[[Dyffryn Clwyd]] was a [[cantref]] of Medieval Wales, and from 1282 was a marcher lordship. |
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===Geology=== |
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⚫ | The Vale of Clwyd is a [[sedimentary basin]] which takes the form of a [[graben|half-graben]] whose eastern margin is marked by the Vale of Clwyd [[fault (geology)|Fault]]. Like the [[Cheshire Basin]] further to its east, it is mostly floored by thick deposits of [[Permian]] and [[Triassic]] [[sandstone]]. Around St Asaph, late [[Carboniferous]], [[Coal Measures]] [[mudstone]]s and sandstones occur. The area was over-run by ice during the [[ice age]]s whose legacy is a covering of [[glacial till]] across the area and a swarm of [[drumlins]] along the western edge of the vale. [[Alluvium]] is encountered across the [[floodplain]]s of the River Clwyd and its tributaries.<ref>British Geological Survey, 1:50K map sheets 95 'Rhyl' & 107 'Denbigh'</ref> |
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⚫ | At its seaward end are the coastal resorts of [[Kinmel Bay]] (Welsh: |
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===References=== |
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{{refs}} |
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⚫ | The Vale of Clwyd is a [[sedimentary basin]] which takes the form of a [[half-graben]] whose eastern margin is marked by the Vale of Clwyd [[fault (geology)|Fault]]. |
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==References== |
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{{reflist}} |
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{{coord|53.21|-3.38|dim:30000_region:GB|display=title}} |
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{{Regions of Wales|state=collapsed}} |
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{{DEFAULTSORT:Vale Of Clwyd}} |
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[[Category:Geology of Wales]] |
[[Category:Geology of Wales]] |
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[[Category:Sedimentary basins of Europe]] |
[[Category:Sedimentary basins of Europe]] |
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[[Category:Rifts and grabens]] |