Bryn y Neuadd Hospital

Llanfairfechan railway station serves the town of Llanfairfechan, Wales, and is located on the Crewe to Holyhead North Wales Coast Line 51+1⁄4 miles (82.5 km) west of Chester.

St Winifred's School was a school for girls in Llanfairfechan, Conwy County Borough, Wales.

Llanfairfechan (Welsh for 'Little St Mary's Parish') is a town and community in the Conwy County Borough, Wales. It is known as a seaside resort and had a population at the 2001 Census of 3,755, reducing to 3,637 at the 2011 Census. The history of the area dates back to at least Roman times, as demonstrated by the discovery of a large second century milestone, which is now preserved in the British Museum.

Pen y Bryn is a two-storey manor house, in Abergwyngregyn, Gwynedd, in north-west Wales, adjacent to the A55, five miles east of Bangor and eight miles west of Conwy. It is constructed mainly of broken stone, with roughly dressed quoins and a slate roof. The house is situated within Garth Celyn, a double bank and ditch, overlooking the Menai Strait to Anglesey. A smaller house was immediately adjacent in 1811 when Sir Richard Colt-Hoare recorded it; this was demolished by 1815. The present structure incorporates a four-storey stone tower. The present roof timbers were dated by dendrochronology to 1624, when the house was refurbished. There is evidence of long use with multiple rebuildings before 1624, but there is disagreement on the duration and nature of its mediaeval use.

The Anafon River, or Afon Anafon, is a river in Gwynedd, Wales, that flows into the Afon Aber. It originates on the slopes of Foel-fras and the Drum of the Carneddau. It flows into Glyn Anafon. then north-west along the Anafon Valley, flowing past monuments of the Iron Age and the Bronze Age. It joins with the Aber Estuary just above the New Bridge, the bridge over the river on the way to the back of Abergwyngregyn.

The Penmaenmawr & Welsh Granite Co. owned and operated a major granite quarry on the north Wales coast located between Conwy and Llanfairfechan. Granite axe-heads and other implements from Neolithic quarries at Penmaenmawr have been found throughout Britain. In the 1830s commercial granite quarries were opened on Penmaenmawr to meet the growing demand for granite setts. The granite was lowered from the quarry by self-acting inclines to the 3 ft (914 mm) narrow gauge tramway which ran to jetties from where the setts were loaded into ships. The standard gauge Chester to Holyhead railway reached Penmaenmawr in 1848, after which the majority of the quarry output was sent by rail. The quarry and its internal narrow gauge railway continued to thrive during the nineteenth century. Production at the quarry continues in 2006, though the railway was replaced by trucks in the 1960s.

Braich-y-Dinas was an extensive hillfort at the summit of Penmaenmawr, one of the northernmost peaks of the Carneddau mountain range on North coast of Wales. It was once considered the best preserved and most complete hillfort in North-West Wales, but completely disappeared in the first half of the 20th century due to a massive quarrying effort by the Darbishire family, which overwhelmed and eventually destroyed all traces of it, despite efforts by the Royal Commission to save the site.

The Kingdom of Ceredigion was one of several Welsh kingdoms that emerged in post-Roman Britain in the mid-5th century. Cardigan Bay to the west and the surrounding hilly geography made it difficult for foreign invaders to conquer. Its area corresponded roughly to that of the county of Ceredigion. Ceredigion transparently means "the people of Ceredig." The kingdom as an independent entity ceased to exist around the year 872.

Powys Wenwynwyn or Powys Cyfeiliog was a Welsh kingdom which existed during the high Middle Ages. The realm was the southern portion of the former princely state of Powys which split following the death of Madog ap Maredudd of Powys in 1160: the northern portion (Maelor) went to Gruffydd Maelor and eventually became known as Powys Fadog; while the southern portion (Cyfeiliog) going to Owain Cyfeiliog and becoming known, eventually, as Powys Wenwynwyn after Prince Gwenwynwyn ab Owain, its second ruler. Powys Wenwynwyn and Gwynedd became bitter rivals in the years that followed, with the former frequently allying itself with England to further its own aims of weakening the latter.

The Kingdom of Powys (Welsh: Teyrnas Powys; Latin: Regnum Poysiae) was a Welsh successor state, petty kingdom and principality that emerged during the Middle Ages following the end of Roman rule in Britain. It very roughly covered the northern two-thirds of the modern county of Powys and part of today's English West Midlands (see map). More precisely, and based on the Romano-British tribal lands of the Ordovices in the west and the Cornovii in the east, its boundaries originally extended from the Cambrian Mountains in the west to include the modern West Midlands region of England in the east. The fertile river valleys of the Severn and Tern are found here, and this region is referred to in later Welsh literature as "the Paradise of Powys" (an epithet retained in Welsh for the modern UK county).

Seisyllwg (Welsh: [sɛiˈsəɬʊɡ]) was a petty kingdom of medieval Wales. It is unclear when it emerged as a distinct unit, but according to later sources it consisted of the former Kingdom of Ceredigion plus the region known as Ystrad Tywi. Thus it covered the modern county of Ceredigion, part of Carmarthenshire, and the Gower Peninsula. It is evidently named after Seisyll, king of Ceredigion in the 7th or early 8th century, but it is unknown if he was directly responsible for its establishment. In the 10th century Seisyllwg became the centre of power for Hywel Dda, who came to rule most of Wales. In 920 Hywel merged Seisyllwg with the Kingdom of Dyfed to form the new kingdom of Deheubarth.

Glywysing was, from the sub-Roman period to the Early Middle Ages, a petty kingdom in south-east Wales. Its people were descended from the Iron Age tribe of the Silures, and frequently in union with Gwent, merging to form Morgannwg.