:Clwydian Range
{{Short description|Hill range in north Wales, Great Britain}}
{{For2|the area of oustanding natural beauty|Clwydian Range AONB|other Clwyds|Clwyd (disambiguation)}}
{{Use dmy dates|date=April 2022}}
{{Infobox mountain
| name = Clwydian Range
| other_name = Clwydian Hills
| photo = North from Jubilee Tower - geograph.org.uk - 1716315.jpg
| photo_size = 250px
| photo_upright =
| photo_alt =
| photo_caption = Northern section of the Clwydian Range towards Liverpool Bay
| map =
| highest = Moel Famau
| highest_location =
| elevation =
| elevation_m = 554
| coordinates = {{coord|53.1544|N|3.25602|W|scale:50000|display=inline}}
| coordinates_ref =
| length =
| length_km =
| length_mi = 20
| length_orientation =
| length_ref =
| width =
| width_km =
| width_mi = 4
| etymology =
| nickname = Clwyds
| native_name = {{native name|cy|Bryniau Clwyd}}
| native_name_lang =
| translation =
| pronunciation =
| authority =
| location = Wales (Great Britain)
| country_type =
| country =
| state_type =
| state =
| region_type =
| region = North Wales
| formed_by = upstanding block of deep sea sediments
| orogeny =
| age = ~ 443.8 million years ago
| type =
| geology = debris slurries laid down during the Silurian period
}}
The Clwydian Range ({{langx|cy|Bryniau Clwyd}}; also Clwydian Hills or Clwyds{{Cite news|date=2010-03-04|title=A bird's eye view of Clwyds|language=en-GB|url=http://news.bbc.co.uk/local/northeastwales/hi/people_and_places/nature/newsid_8545000/8545570.stm|access-date=2021-09-20}}) is a series of hills in the north-east of Wales that runs from Llandegla in the south to Prestatyn in the north; the highest point is {{convert|554 |m|abbr=on}} Moel Famau. The range forms the north-western part of the Clwydian Range and Dee Valley Area of Outstanding Natural Beauty.
Geology
File:Jubilee Tower - geograph.org.uk - 1325231.jpg is strewn with Turbidite]]
The Clwydian Hills are formed from an upstanding block of deep sea sediments formed during the Silurian period as debris slurries originating on the nearby continental shelf. The older mudstones and siltstones of the Nantglyn Flags Formation form parts of the west-facing scarp slope and the overlying Elwy Formation, which consists of mudstones and siltstones deposited in deep marine conditions with numerous sandstone beds, forms most of the higher ground.{{cite web |title=BGS: Geology of Britain |url=https://mapapps.bgs.ac.uk/geologyofbritain/home.html |website=Geology of Britain Viewer |publisher=British Geological Survey |access-date=29 December 2019}} Both formations are of Ludlovian age. The range's rocks are intensely faulted; the major Vale of Clwyd Fault is responsible for the impressive west-facing scarp of the Clwydian Range. It downthrows the rocks to the west and separates the younger Carboniferous and Permo-Triassic rocks of the Vale of Clwyd from those of the hills.{{cite book |title=1:50K map sheets 107 Denbigh & 108 Flint |publisher=British Geological Survey |location=Keyworth, Nottingham}}
Ice from the Welsh ice-sheet moved eastwards over the Clwydian Hills during the last ice age, impinging on the Irish Sea Ice to the east of the range. Numerous glacial meltwater channels occur around the range whilst the valley of the River Wheeler which cuts the range in two was a significant drainage channel.{{cite book |title=Map sheet (England and Wales) 108 Flint |date=1999 |publisher=British Geological Survey |location=Keyworth, Nottingham |edition=Solid and Drift Geology}}
Geography
The hills in the Clwydian Range provide extensive views across northern Wales, to the high peaks of Snowdonia, eastwards across the Cheshire Plain to the Peak District, and towards Manchester and Liverpool in England to the northeast. The Offa's Dyke National Trail traverses the range's high ground from Llandegla to Prestatyn.{{cite web |url=http://www.visitwales.com/explore/north-wales/borderlands/clwydian-range-dee-valley |title=Exploring the Clwydian Range and Dee Valley |work=Explore Wales |publisher=Welsh Government |access-date=25 April 2016}}
Image:Moel Arthur, Sir Ddinbych 02.JPG from Moel Llys-y-Coed]]
The hills, which are mainly heather-clad upland above pastures, have six Iron Age hillforts including Y Foel (Moel Hiraddug), Moel-y-gaer, Penycloddiau, Moel Arthur, a second Moel y Gaer and Foel Fenlli. There are several tumuli and cairns on the hills.{{cite map |title=265 Clwydian Range/Bryniau Clwyd |publisher=Ordnance Survey |scale=1:25000 |series=Explorer }}
=Summits=
File:Clwydian range from abergele.jpg showing from left to right: Prestatyn Hillside, Gop Hill, Moel Hiraddug and Mynydd y Cwm]]
class="wikitable sortable" style="text-align: center; width: 450px;" |
#
!Peak !Elevation (m) !Grid reference |
---|
1
|Bryn Coed yr Esgob |211 |{{gbmappingsmall|SJ068812}} |
2
|265 |{{gbmappingsmall|SJ063785}} |
3
|300 |{{gbmappingsmall|SJ073768}} |
4
|Moel Maenefa |290 |{{gbmappingsmall|SJ085745}} |
5
|206 |{{gbmappingsmall|SJ095708}} |
6
|398 |{{gbmappingsmall|SJ114703}} |
7
|440 |{{gbmappingsmall|SJ127678}} |
8
|Moel Plas-yw |420 | {{gbmappingsmall|SJ152669}} |
9
|456 |{{gbmappingsmall|SJ145661}} |
10
|Moel Llys-y-coed |465 |{{gbmappingsmall|SJ145655}} |
11
|Moel Dywyll |475 | {{gbmappingsmall|SJ151632}} |
12
|554 |{{gbmappingsmall|SJ161626}} |
13
|339 |{{gbmappingsmall|SJ148617}} |
14
|511 | {{gbmappingsmall|SJ162600}} |
15
| Moel Eithinen |434 | {{gbmappingsmall|SJ168592}} |
16
| Gyrn |384 |{{gbmappingsmall|SJ165586}} |
17
|467 |{{gbmappingsmall|SJ171575}} |
18
| Moel Llanfair |447 | {{gbmappingsmall|SJ169566}} |
19
|Moel y Plâs |440 |{{gbmappingsmall|SJ170554}} |
20
| Moel y Gelli |361 | {{gbmappingsmall|SJ166545}} |
21
| Moel y Waun | 412 | {{gbmappingsmall|SJ168534}} |
22
| Moel yr Acre |400 |{{gbmappingsmall|SJ169525}} |
Area of Outstanding Natural Beauty
{{main|Clwydian Range and Dee Valley}}
The Clwydian Range was designated as an Area of Outstanding Natural Beauty in 1985, one of only five in Wales. The original area was {{convert|167|km2}}, but in 2011 the area was extended southwards by a further {{convert|229|km2}} to include the Dee Valley, Moel y Gamelin, the Horseshoe Pass and Castell Dinas Bran, the towns of Llangollen and Corwen, the Pontcysyllte Aqueduct, Chirk Castle and Valle Crucis Abbey.{{cite web |url=http://www.clwydianrangeanddeevalleyaonb.org.uk/ |title=Clwydian Range and Dee Valley Area of Outstanding Natural Beauty |publisher=Denbighshire Countryside Services |access-date=25 April 2016}}
The AONB now extends to {{convert|389|km2}}.{{cite web|url=http://www.clwydianrangeanddeevalleyaonb.org.uk/exploring-the-clwydian-range-and-dee-valley/|publisher=ClwydianRangeandDeeValleyaonb.org.uk|title=Clwydian Range and Dee Valley AONB |access-date=November 4, 2014}}
A wide range of wildlife thrives in the range, including red kites and red foxes, which both prey on rabbits and voles. There is also one of the few Welsh populations of black grouse and there is a project to conserve the European water vole, which is suffering a large decline in numbers across the United Kingdom. Another project is trying to get rid of the non-native Himalayan balsam which has invaded the Alyn Valley area.{{cite web |url=http://www.clwydianrangeanddeevalleyaonb.org.uk/wildlife-projects/ |title=Wildlife projects |publisher=Clwydian Range and Dee Valley AONB |access-date=25 April 2016}}
Recreation
The Offa's Dyke Path follows the Clwydian Range, although Offa's Dyke itself was not constructed on it. The Clwydian Way long distance footpath passes through the Clwydian Range, and the North Wales Path follows the foot of the scarp between Prestatyn and Dyserth.{{cite web |url=http://www.clwydianway.co.uk/ |title=Clwydian Way |publisher=North Wales Area of The Ramblers Association |access-date=25 April 2016}}
References
{{Reflist}}
External links
- [https://www.clwydianrangeanddeevalleyaonb.org.uk/ Clwydian Range and Dee Valley AONB]
- [http://www.visitclwydianrange.co.uk Clwydian Range Tourism Group]
{{Coord|53|11|N|3|15|W|region:GB_type:mountain|display=title}}
{{Denbighshire}}
{{Flintshire}}
{{Authority control}}
Category:Areas of Outstanding Natural Beauty in Wales