| Glanwydden | |
|---|---|
 The Queens Head public house, Glanwydden | |
  Glanwydden Location within Conwy | |
| OS grid reference | SH816802 |
| Community | |
| Principal area | |
| Country | Wales |
| Sovereign state | United Kingdom |
| Post town | LLANDUDNO JUNCTION |
| Postcode district | LL31 |
| Dialling code | 01492 |
| Police | North Wales |
| Fire | North Wales |
| Ambulance | Welsh |
| UK Parliament | |
| Senedd Cymru – Welsh Parliament | |
Glanwydden is a small village located between Llandudno and Colwyn Bay in Conwy county borough, north Wales.
The village has one pub and around 30 houses. It was the centre of the limestone quarry trade in the 17th century with most of the stone being used to build the hotels in Llandudno.
The village predates the quarries with a windmill and storage house whose charter dates from 1580. The Pub "the QueensHead" was votes Wales best pub 2009[ citation needed ]
The village played host to the Urdd Eisteddfod in May 2008. The village used to have a school from 1875-1905 until the new school opened on Derwen Lane. The village has a small chapel that dates back to 1790. The local dairy, opposite the Queens head, has been demolished.
There is a windmill that stands in the village, and is now a family home. There is evidence in Aberystwyth that the first Royal Charter, granted to the Wynne family for the construction of a windmill on the site in 1580. It is reputed to be the largest based windmill in wales. There is a key stone on the door of the mill that dates a rebuild in 1704. The keystone bears the inscription Sr RM and 66.8 which we believe is a reference to the psalm “Praise our God, all peoples, let the sound of his praise be heard” The Mill fell into disuse in the late industrial era, when steam powered mills in Manchester and Liverpool superseded most wind powered flour production. Local stories say the sails for the mill fell off during the later days of the first world war killing a pig. The mill was then plundered for its stone for local buildings. Only the base part of the mill remaining and used as a sheep fold by local farmers. In the 1980s the Windmill way sympathetically restored and is now a family home. There is still evidence of its working past in the gardens of the house with three large pieces of mill stone uncovered and on display.
Built in 1857 Glan Morfa house, on the outskirts of the village, was built by the Parry family using the local limestone. Lady Erskine lived at the property in the 1930s. The present owners (Griffiths family) great-great-grandfather was the local cobbler and would visit local houses to collect shoes to mend. In the 1980s "Bessie's" riding stable was a local hub for learner and experienced riders. This was next to the Queens head pub where some listed outbuildings remain. [1]
Blaenau Ffestiniog is a town in Gwynedd, Wales. Once a slate mining centre in historic Merionethshire, it now relies much on tourists, drawn for instance to the Ffestiniog Railway and Llechwedd Slate Caverns. It reached a population of 12,000 at the peak development of the slate industry, but fell with the decline in demand for slate. The population of the community, including the nearby village Llan Ffestiniog, was 4,875 in the 2011 census: the fourth most populous in Gwynedd after Bangor, Caernarfon and Llandeiniolen. The population not including Llan is now only about 4,000.
Llandudno is a seaside resort, town and community in Conwy County Borough, Wales, located on the Creuddyn peninsula, which protrudes into the Irish Sea. In the 2011 UK census, the community – which includes Gogarth, Penrhyn Bay, Craigside, Glanwydden, Penrhynside, and Bryn Pydew – had a population of 20,701. The town's name means "Church of Saint Tudno".
Penmaenmawr is a town and community in Conwy County Borough, Wales, which was formerly in the parish of Dwygyfylchi and the traditional county of Caernarfonshire. It is on the North Wales coast between Conwy and Llanfairfechan and was an important quarrying town, though quarrying is no longer a major employer. The population of the community was 4,353 in 2011, including Dwygyfylchi and Capelulo. The town itself having a population of 2,868 (2011).
The Great Orme is a limestone headland on the north coast of Wales, north-west of the town of Llandudno. Referred to as Cyngreawdr Fynydd by the 12th-century poet Gwalchmai ap Meilyr, its English name derives from the Old Norse word for sea serpent. The Little Orme, a smaller but very similar limestone headland, is on the eastern side of Llandudno Bay.
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Blisworth is a village and civil parish in the West Northamptonshire, England. The West Coast Main Line, from London Euston to Manchester and Scotland, runs alongside the village partly hidden and partly on an embankment. The Grand Union Canal passes through the village and the north portal of the Blisworth tunnel is near Stoke Road.
Penrhyn Bay is a small town on the northern coast of Wales, in Conwy county borough, within the parish or community of Llandudno, and part of the ecclesiastical parish of Llanrhos. It is a prosperous village, with a cluster of local shops, a pub, a parish church and a modern medical centre with doctors' surgery at the foot of the pass over the shoulder of the Little Orme from Llandudno Bay. Here there is a highschool called Ysgol y Creuddyn and a primary school called Ysgol Glanwydden. It is considered to be a residential suburb of Llandudno lying east of the Little Orme. It adjoins the resort of Rhos-on-Sea and covers a large part of the Creuddyn peninsula. The population of Penrhyn Ward at the 2011 census was 4,883.
Carboniferous Limestone is a collective term for the succession of limestones occurring widely throughout Great Britain and Ireland that were deposited during the Dinantian Epoch of the Carboniferous Period. These rocks formed between 363 and 325 million years ago. Within England and Wales, the entire limestone succession, which includes subordinate mudstones and some thin sandstones, is known as the Carboniferous Limestone Supergroup.
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Chesterton Windmill is a 17th-century cylindric stone tower windmill with an arched base, located outside the village of Chesterton, Warwickshire. It is a Grade I listed building and a striking landmark in south-east Warwickshire.
St. Andrew's Major is a village and parish in the community of Dinas Powys in the Vale of Glamorgan, between Barry and Cardiff in south-eastern Wales.
Bodysgallen Hall is a manor house in Conwy county borough, north Wales, near the village of Llanrhos. Since 2008 the house has been owned by The National Trust. It is a Grade I listed building, currently used as a hotel. This listed historical building derives primarily from the 17th century, and has several later additions. Bodysgallen was constructed as a tower house in the Middle Ages to serve as defensive support for nearby Conwy Castle. According to tradition, the site of Bodysgallen was the 5th century AD stronghold of Cadwallon Lawhir, King of Gwynedd, who had wide-ranging exploits as far as Northumberland.
Carew is a village, parish and community on an inlet of Milford Haven in the former Hundred of Narberth, Pembrokeshire, West Wales, 4 miles (6.4 km) east of Pembroke. The eastern part of the parish is in the Pembrokeshire Coast National Park.
The Barony of Giffen and its associated 15th-century castle were in the parish of Beith in the former District of Cunninghame, now North Ayrshire. The site may be spelled Giffen or Giffin and lay within the Lordship of Giffin, which included the Baronies of Giffen, Trearne, Hessilhead, Broadstone, Roughwood and Ramshead; valued at £3,788 9s 10d. The Barony of Giffen comprised a number of properties, including Greenhills, Thirdpart, Drumbuie, Nettlehirst and Balgray, covering about half of the parish of Beith. Giffen was a hundred merk land, separated from the Barony of Beith, a forty-pound land, by the Powgree Burn which rises on Cuff hill. The Lugton Water or the Bungle Burn running through Burnhouse may have been the Giffen barony boundary with that of the adjacent barony and lands of Aiket castle.
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The coastline of Wales extends from the English border at Chepstow westwards to Pembrokeshire then north to Anglesey and back eastwards to the English border once again near Flint. Its character is determined by multiple factors, including the local geology and geological processes active during and subsequent to the last ice age, its relative exposure to or shelter from waves, tidal variation and the history of human settlement and development which varies considerably from one place to another. The majority of the coast east of Cardiff in the south, and of Llandudno in the north, is flat whilst that to the west is more typically backed by cliffs. The cliffs are a mix of sandstones, shales and limestones, the erosion of which provides material for beach deposits. Of the twenty-two principal areas which deliver local government in Wales, sixteen have a coastline, though that of Powys consists only of a short section of tidal river some distance from the open sea. Its length has been estimated at 1,680 miles (2,700 km).
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