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Vale of Clwyd

Coordinates: 53°13′N 3°23′W / 53.21°N 3.38°W / 53.21; -3.38
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For the constituency of the House of Commons of the Parliament of the United Kingdom, see Vale of Clwyd (UK Parliament constituency). For the Senedd constituency, see Vale of Clwyd (Senedd constituency).

The Vale of Clwyd (Template:Lang-cy) is a tract of low-lying ground in the county of Denbighshire in north-east Wales.[1][2] The Vale extends south-southwestwards from the coast of the Irish Sea for some 20 miles (about 30 km) forming a triangle of low ground bounded on its eastern side by the well-defined 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 (Welsh: Afon Clywedog) and River Elwy (Welsh: Afon Elwy) and the smaller right bank tributary of the River Wheeler (Welsh: Afon Chwiler).

History

Dyffryn Clwyd was a cantref of Medieval Wales, and from 1282 was a marcher lordship.

Settlement and administration

At its seaward end are the coastal resorts of Kinmel Bay (Welsh: Bae Cinmel), Rhyl and Prestatyn whilst the town of Abergele and city of St Asaph (Welsh: Llanelwy) lie just inland. The other principal towns of the vale are Denbigh (Welsh: Dinbych) and Ruthin (Welsh: Rhuthun),[3] also Rhuddlan. Most of the area falls within the modern administrative county (and unitary authority) of Denbighshire and a portion is in Conwy County Borough; much of it lies within the Vale of Clwyd UK Parliamentary constituency.

Geology

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.[4] 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 mudstones and sandstones occur. The area was overrun by ice during the ice ages whose legacy is a covering of glacial till across the area and a swarm of drumlins along the western edge of the vale.[5] Alluvium is encountered across the floodplains of the River Clwyd and its tributaries.[6]

References

  1. ^ "THE VALE OF CLWYD". Clwyd-Powis Archaeological Trust. Retrieved 15 December 2021.
  2. ^ "Vale of Clwyd" (PDF). Natural Resources Wales. Retrieved 15 December 2021.
  3. ^ Ordnance Survey 1:50K Landranger sheet 116 'Denbigh & Colwyn Bay'
  4. ^ Williams, G.D.; Eaton, G.P. (1993). "Stratigraphic and structural analysis of the Late Palaeozoic-Mesozoic of NE Wales and Liverpool Bay: implications for hydrocarbon prospectivity". Journal of the Geological Society. 150 (3): 489–499. doi:10.1144/gsjgs.150.3.0489.
  5. ^ Lewis, Colin A.; Richards, Andrew E. (2005). The glaciations of Wales and adjacent areas (2nd ed.). Hereford: Logaston Press. pp. 41–42. ISBN 1904396364.
  6. ^ British Geological Survey, 1:50K map sheets 95 'Rhyl' & 107 'Denbigh'

53°13′N 3°23′W / 53.21°N 3.38°W / 53.21; -3.38

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