Aberwheeler

Bodfari railway station was opened on 6 September 1869 by the Mold and Denbigh Junction Railway. Following the Railways Act 1921 the line became part of the LMS. The station was located to the west of the road bridge on the A541 close to the village. Station buildings were on the Chester bound platform and there was a shelter on the Denbigh platform. The station closed in April 1962.The station site today is a private residence but the station building is still standing.

Bodfari is a village and community in Denbighshire, Wales. Until the local government reorganisation of 1974, Bodfari was in the historic county of Flintshire. The ancient parish of Bodfari comprised the townships of Bodfari, which was in historic Flintshire, and Aberwheeler, in historic Denbighshire.

Moel y Gaer (Welsh for "bald hill of the fortress") is an Iron Age hillfort at the northern end of the Clwydian Range, located on a summit overlooking the valley of the River Wheeler, near the village of Bodfari, Denbighshire, Wales, five miles north-east of Denbigh. The site is a scheduled monument, classified as a prehistoric defensive hillfort.The hillfort is one of a chain of six hillforts in the Clwydian Range, which are, from north to south, Moel Hiraddug, Moel y Gaer Bodfari, Penycloddiau, Moel Arthur, Moel y Gaer Llanbedr, and Moel Fenlli. Moel y Gaer Bodfari is the lowest of these hillforts, being just 200 m (656 ft) above sea level. The hill on which it stands is surrounded by lower land and is strategically situated at the confluence of the River Wheeler and the Clwyd. Offa's Dyke Path passes along the foot of the hill. The fort at Moel y Gaer is one of the smallest of the chain of defensive works found along the Clwydians. It probably dates from the Iron Age, although there is no definitive evidence to establish the exact period during which it was occupied. It has a single entrance on its northern side and is defended by a steep slope on the eastern side of the hill.Excavation started in 2011 and is ongoing as of 2016. The area enclosed by the ramparts is about two hectares. Various anomalies have been targeted in the excavations, including what is possibly a group of pits and other features where the ground seems to have been dug out, as well as what seems to be a roundhouse on a levelled piece of land. Examination of the middle rampart began in 2013, and it seems that there may have been several phases in its construction.

Lleweni Hall (Welsh: Plas Lleweni; sometimes also referred to as Llewenny Palace) was a stately home in Denbighshire, northeast Wales, around 2 miles (3.2 km) north-east of Denbigh on the banks of the River Clwyd. It was the principal seat of the Salusbury family and their descendants from 1289 until 1748, and the present territorial designation of the most senior branch of the family.

Aled was a rural district in the administrative county of Denbighshire, Wales, from 1935 to 1974. The district was created by a county review order in 1935 which reorganised districts in the county. It was formed by merging the bulk of St Asaph (Denbigh) Rural District with the Nant Conwy area previously administered by Conway Rural District in neighbouring Caernarfonshire. The district was named after the River Aled. The district contained the following civil parishes: Abergele Rural CP (part to Abergele UD, gained part of abolished St. George CP) Betws Abergele CP (part to Abergele UD, gained part of abolished Llanddulas CP) Bylchau Cefn Llaneilian yn Rhos Llanefydd Llanfair Talhaearn Llansantffraid Glan Conwy Llansannan TrefnantThe former parishes of St George and Llanddulas were abolished, being split between an enlarged Abergele Urban District and other parishes in Aled RD. The rural district was abolished by the Local Government Act 1972 in 1974. Its area passed to the Borough of Colwyn in the new county of Clwyd with the exception of Llansantffraid Glan Conwy which was included in the Borough of Aberconwy in Gwynedd.

The River Wheeler (Welsh: Afon Chwiler) is a tributary of the River Clwyd in north-east Wales. Rising on the east side of the Clwydian Range, it is a "misfit stream" occupying a deep valley cutting westwards through the range into the Vale of Clwyd. The river enters the Clwyd west of the village of Aberwheeler (Welsh: Aberchwiler), the name of which signifies "the mouth or confluence of the Wheeler". The river is followed for its entire length by the A541 road running from Mold to Trefnant and was formerly followed by the Mold and Denbigh Junction Railway. Besides Aberchwiler, the river passes through or beside the villages of Nannerch, Afon-wen and Bodfari.There are numerous workings, both active and abandoned, for sand and gravel within the Wheeler valley, a legacy of the last ice age, when the valley carried considerable quantities of glacial meltwater.

The Vale of Clwyd (Welsh: Dyffryn Clwyd) is a tract of low-lying ground in the county of Denbighshire in north-east Wales. 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).

Ffynnon Beuno and Cae Gwyn Caves are two Scheduled Ancient Monuments, in Denbighshire, Wales, which are also designated a Site of Special Scientific Interest (SSSI). The site has two caves, with entrances close to each other high on a valley side, above the Vale of Clwyd. They were first excavated in 1883–5. Human tools have been found on the site dating back to around 36,000 BC, and a mammoth bone has been dated back to 16,000 BC. These very early discoveries were significant in providing one of the first direct associations between stone tools of paleolithic people and the bones of extinct pre-iceage animals such as mammoth and woolly rhinoceros.In 1963 it was designated as an SSSI for the palaeontological interest described above and for its species interest as a winter roost of lesser horseshoe bat.

Moel y Parc (sometimes written as Moel-y-Parc) is a hill on the border between Denbighshire and Flintshire in Wales. It is one of the Clwydian Hills, rising 398 metres (1,306 ft) above sea level and is located at OS grid reference SJ114703. There is a television mast near the summit. The summit marks the boundary of Aberwheeler and Ysceifiog communities, and is the site of a cairn and tumulus.

Brynbella is a neoclassical villa built near the village of Tremeirchion in Denbighshire, northeast Wales, by Hester Piozzi and her husband, Gabriel Piozzi. It was the seat of the Salusbury family from 1794 until 1920. The name is part Welsh and part Italian, meaning "Beautiful Hill" (bryn + bella).

Tremeirchion (previously known as Lleweni) is a small residential community in Denbighshire, Wales. It lies on the B5429 road, to the north east of Denbigh and to the east of St Asaph. The community includes the village of Rhuallt. The town was part of the traditional lands of the Salusbury family and the Cotton baronets. It was dominated by these two families until the early part of the 20th century. It briefly became well known during the fin de siècle after a series of dinosaur bones were found in the area.

The Moel-y-Parc transmitting station is situated on Moel y Parc, a hill in north-east Wales at the northern end of the Clwydian range, close to the town of Caerwys and several miles (kilometres) north-east of Denbigh. It was built in 1962/1963 by the IBA to bring 405-line VHF ITV television to North Wales and it has been on the air since 1963. Its original height of 229 metres (751 ft) made it the tallest structure in North Wales and it stands on land that is itself about 335 metres (1,099 ft) above sea level. In 1965, VHF television transmissions from the BBC commenced from the site. With the addition of the UHF aerials in 1969, the mast height increased to 235 metres (771 ft) high. Its official coverage area includes parts of Flintshire, Denbighshire and Wrexham (although the majority of Wrexham is in a blindspot of direct transmission from Moel-y-Parc, its analogue transmissions were relayed via the Wrexham-Rhos transmitting station). A network of relay stations extends television coverage as far as Colwyn Bay in the west and Bala in the south. VHF television services from both BBC and ITV were discontinued in January 1985 as the 405-line TV system was switched off across the UK as a whole. Moel-y-Parc's UHF channel allocation made it a "Group B" transmitter, but with the roll-out of the UK's first digital TV services in 1998, a "Group W" wideband aerial was needed. The site reverted to being a "Group B" transmitter at digital switchover (DSO). Technically, with the advent of the temporary MUXES 7 and 8 Moel Y Parc became a K group, and is due to remain so at its 700 MHz clearance. However most B group aerials will still work on all Moel's transmitted DTT channels (see graph). The site is currently administered by Arqiva.