Felindre Farchog

St Andrew's Church, Bayvil, is a redundant church standing in an isolated position in the hamlet of Bayvil, some 2 kilometres (1.2 mi) to the northeast of Nevern, Pembrokeshire, Wales. It has been designated by Cadw as a Grade II* listed building, and is under the care of the Friends of Friendless Churches. It is listed Grade II* because it is "a scarce rural example of an unaltered Anglican church of its date".

Bayvil (Welsh: Y Beifil) is a hamlet and parish in Pembrokeshire, Wales. It is situated in the north of the county, 5 kilometres (3.1 mi) east of Newport. It is in the Pembrokeshire Coast National Park. The parish includes most of the village of Felindre Farchog. Together with the parishes of Monington, Moylgrove and most of Nevern, it constitutes the community of Nevern.

Pentre Ifan (literally "Ivan's Village") is the name of an ancient manor in the community and parish of Nevern, Pembrokeshire, Wales. It is 11 miles (18 km) from Cardigan, Ceredigion, and 3 miles (4.8 km) east of Newport, Pembrokeshire. Pentre Ifan contains and gives its name to the largest and best preserved neolithic dolmen in Wales. The Pentre Ifan monument is a scheduled monument and is one of three Welsh monuments to have received legal protection under the Ancient Monuments Protection Act 1882. The dolmen is maintained and cared for by Cadw, the Welsh Historic Monuments Agency.

Tŷ Canol Woods are an ancient woodland in the Tŷ Canol National Nature Reserve which lies south of the village of Felindre Farchog, Pembrokeshire, Wales, between the Preseli Mountains and the north Pembrokeshire coast. The site is designated as an SSSI (Site of Special Scientific Interest), NNR (National Nature Reserve) and SAC (Special Area of Conservation). After the glaciers made their final retreat from Wales around 11,500 years ago, it took time to transform the barren landscape into a lush woodland. But gradually Arctic plants were joined by shrubs, then progressively birch, Scots pine, oak, alder and hazel trees colonised. By around 6,000 years ago, an extensive deciduous woodland may have covered even the uplands of Wales. 1,000 years later the woodlands started to diminish in size and number thanks to natural and human influences. With trees over 800 years old, Tycanol is one of the few remaining ancient woodlands in Wales. The site is important not only for its ancient oaks, but also for the many rocky outcrops. Both trees and rocks are covered with mosses and nearly 400 species of lichen, many of which are rare.

Castell Henllys (Welsh, "castle of the old court") is an archaeological site near Nevern in north Pembrokeshire, Wales. The Iron Age hillfort has been the subject of an ongoing excavation since the start of the 21st century, accompanied by an exercise in reconstruction archaeology whereby experiments in prehistoric farming have been practised. Four roundhouses and a granary have been reconstructed on their original Iron Age foundations – some 2,000 years old – the hillfort the only site in Britain where this has been done. The Castell Henllys site includes significant earthworks and fortifications.During the summer the site provides training for young archaeologists and is a popular visitor attraction. It is owned by Pembrokeshire Coast National Park.

The Church of St Dogfael, Meline, Pembrokeshire, Wales is a redundant church dating from the 19th century. A Grade II listed building, the church is now in the care of the Friends of Friendless Churches.

Tŷ Canol National Nature Reserve is a national nature reserve which lies south of the village of Felindre Farchog, Pembrokeshire, Wales, between the Preseli Mountains and the north Pembrokeshire coast. The volcanic rock of the moor of Carnedd Meibion Owain, the mossy boulders and gnarled oaks of Tŷ Canol Wood and the nearby presence of the Pentre Ifan burial chamber contribute to the reserve's prehistoric atmosphere. Buzzards and ravens are a common sight in the area.

Meline (also recorded as Meliney and Melinau) is a parish in the Diocese of St David's in north Pembrokeshire, Wales. There is no settlement of this name.

Nevern Bridge (Welsh: Pont Nanhyfer) spans the River Nevern (Welsh: Afon Nyfer) in the centre of Nevern, Pembrokeshire, Wales. This Grade II listed bridge, 220 yards (200 m) south of the church, was built in the late 18th or early 19th century. Constructed of rubblestone and ashlar, this humpback bridge has two unequal arches—the south arch is larger—and is recessed with keystones.

Nevern (Welsh: Nanhyfer) is both a parish and a community in Pembrokeshire, Wales. The community includes the settlements of Felindre Farchog, Monington, Moylgrove and Bayvil. The small village lies in the Nevern valley near the Preseli Hills of the Pembrokeshire Coast National Park 2 miles (3 km) east of Newport on the B4582 road.

Cemais (sometimes spelled Kemes after one of the several variations found in Medieval orthography) was an ancient cantref of the Kingdom of Dyfed, from the 11th century a Norman Marcher Lordship, from the 16th century a Hundred, and is now part of Pembrokeshire, Wales. It occupied the coastal area between the Teifi estuary and Fishguard, and the northern and southern slopes of the Preseli Hills, covering an area of approximately 140 square miles (360 km2). The Afon Nyfer divided it into two commotes: Cemais Is Nyfer to the north and Cemais Uwch Nyfer to the south.: 25 

Craig Rhos-y-felin is a rocky outcrop on the north side of the Preseli Mountains in Wales, which is designated as a RIGS site on the basis of its geological and geomorphological interest. It is accepted by some in the archaeological community that it is the site of a quarry, used together with one at Carn Goedog, for gathering stones used at Stonehenge, most notably as the source of some of the foliated rhyolite found in the Stonehenge "debitage". This is disputed by others, who believe that all of the features at the site, apart from evidence of intermittent occupation over a long period, are of natural origin. Some believe that the site was used as a quarry in both the Neolithic and Bronze Ages, around 4000 to 5000 years ago, and the rock's shape, like a pillar, allowed the stones to be quarried with relative ease compared to stones taken from other places. Others argue that if prehistoric men had wanted to obtain monoliths for use as standing stones, all they had to do was collect them from the abundant glacial erratics littering the landscape. Craig Rhos-y-felin was first claimed to be the site of a quarry in 2011. The cited evidence was disputed in two journal articles published in 2015 by Brian John, Dyfed Elis-Gruffydd and John Downes.