Llangolman
Llangolman () is a village and parish in the southeastern Preseli Hills in Pembrokeshire, Wales. It is part of the community of Mynachlog-ddu. There are prehistoric remains nearby and the parish has a history of slate and clay quarrying. History 
Llangolman lies in a historic landscape near the upper part of the valley of the Eastern Cleddau and its tributaries. The village place name derives from the church dedicated to St. Golman, or in Irish, St Colman. Colman is attributed to Colmán of Dromore, a 6th-century saint. On old maps, one will often see the east-west road from Llangolman to Maenclochog via Llandilo, marked as a Roman road. This is the so-called Via Julia that was proposed by a number of 18th- and 19th-century antiquaries and was based on a 1757 forged document by Charles Bertram called The Description of Britain. As a result, it is doubtful that the road is actually Roman. Instead, the Via Julia is now considered to be much further south and passes via Wiston. Anglican church 

Llangolman church stands on high ground just to the south of the main village. The current building is Victorian or early Victorian, with little to show for the original medieval building that once stood on the site. Of historical interest is the recording in the 19th century of a stone gate post about  from the churchyard. This stone, known as the Maen-ar-Golman (the stone upon Colman) is about  tall with a number of cross markings carved on the stone. The stone appears to have no inscriptions. The local belief is that Colman is buried nearby. The earliest recorded tombstone in the graveyard is for Stephen Lewis from Llangolman with the date 1778. Local chapels 

There are two local chapels in the area, Llandeilo and Rhydwilym. Rhydwilym (English: William's Ford) is the oldest active Welsh Baptist chapel in the world and was founded in 1668. Funds to build the first chapel were provided by the gentleman farmer John Evans of Llwyndwr in 1701. There was a chapel on the site in 1763; a plaque on the front wall indicates that the 1763 chapel was rebuilt in 1841, and further enlarged in 1875. The current Llandeilo chapel was built in 1882, though earlier chapel structures are recorded in the immediate vicinity. The name Llandeilo comes from the local church dedicated to the 5th-century saint, Teilo. Historical buildings 
Two gentry houses from the 18th century include Plas-y-Meibion and Llangolman Farm. There is also the house called Temple Druid (c. 1795) which was designed by John Nash, architect to King George IV, and is located roughly halfway between Llangolman and Maenclochog. Llangolman Farm has some architectural interest. Although most of the current house probably dates from the 17th/18th century, the rear wing of the house has an older structure that includes barrel vaulting. There are two vaults, one above the other. The lower vault covers the underlying cellar, which has three rooms. The end room in the cellar, and deepest, includes a freshwater well. The first room, entered from an open arched doorway, includes square holes in the vaulted ceiling that allowed butter to be easily dropped into the cellar for storage. Above the cellar vault is a second vaulted ceiling that currently houses the bathroom. The farm was a centre of production, including clay, slate, salted bacon, butter, and a large mill for grinding corn. The earliest recorded date of Llangolman Farm goes back at least to 1638 when the Griffiths were said to reside at the location. In 1721, the High Sheriff of Pembrokeshire, Stephen Lewis lived at Llangolman Farm. There is little doubt that the farm itself is older than the 17th century but how old, is unknown. The presence of vaulting in the back portion of the house suggests the existence of an older structure. A legend known to the locals is that the house is haunted by a young girl who had an affair with a monk. She is said to have drowned herself in the millpond out of guilt and remorse. Location and terrain 
The area surrounding the village is riddled with steep wooded valleys, presumably cut during one or more of the glacial episodes of the Pleistocene. The village itself sits on a plateau where two valleys meet, the Eastern Cleddau and a tributary that originates near the small village of Llandelio. The underlying geology consists of interbedded Ordovician shales and sandstones with extensive slate outcrops. Evidence of glaciation is also seen from banks of gravel and sand to the east of the village, which form deep drainage seeps from which discharges excellent spring water. The springs emerge in boggy land at the base of the gravel banks, where deposits of blue boulder clay, known by the natives as "indiarubber clay", can also be found. Claypits close to the farmhouses of Llangolman Farm (still visible) and Llyn are evidence that the clay was once extracted on a significant scale. The study by Jehu mentions that the clay pit at Llyn was down to a depth of 15 to 20 feet, and ladders were required to get in and out. His report goes on to state that the clay is bluish in color and very tough (hence the nickname indiarubber clay). The clay covers the valley bottom from Llyn to Llangolman Farm at a level of over 400 ft. The valley sides have largely been saved from deforestation due to their steepness, and there is some evidence of old forest along the western side of the Llandelio tributary. Otters have been seen in the rivers. Of historical interest is a surviving and working hydraulic ram that pumps water to the local farm called Ffynnon Sampson ("Sampson's Well"). Industry
The current landscape around the village is entirely rural; the local economy is mostly based on farming (dairy, cattle and sheep) and tourism (bed and breakfasts and rented cottages). Of more interest and of historical importance is the slate quarrying industry. There is a seam of green slate running roughly east–west along the Taf Valley. This slate is of volcanic ash origin and of Ordovician date. The slate is generally of a greenish-grey or light blue colour. This slate was often used, in addition to roofing, for covering exposed walls to keep out moisture. Until the 1970s, the outer walls of Llangolman Farm were covered in hanging slates. The slate itself was exploited at least as early as 1860; the largest quarry was Dandderwen quarry (known as Whitland Abbey Slate quarry after the name of the company which exploited it). There is some suggestion that the Gilfach quarry may have been worked as early as the 16th century. It is also claimed that the slate used on the roof of the Houses of Parliament, when rebuilt in the 1830s, originated from the Gilfach quarry. Much of the slate industry went into decline after the 1890s, and by the 1930s most were closed due to competition from cheaper sources. Gilfach quarry on the eastern side of the Eastern Cleddau was still in operation until 1987. There are many smaller workings dotted amongst the landscape; some of the quarries are in the steep-sided valley that carries the western tributary from Llandeilo that joins the Eastern Cleddau; some are near Llangolman Farm, with one immediately north of the farmhouse. Tucker and Tucker published a review of many of the quarries in Pembrokeshire including a number around Llangolman Farm. They discuss the quarry to the north of the Farmhouse and add further information in their subsequent review. They state that this quarry (at SN 110262) was quarried by Lily Quarries Slate and Slab Co. Ltd. In their 1979 review, Tucker and Tucker also give more details on the large Gilfach and Dandderwen quarries mentioned above. Schools
There are no schools in Llangolman village. Children from Llangolman would either go to Maenclochog about 2.5 miles away or, until 1964 they would walk to the slightly closer school at Nant y Cwm (1.7 miles away). Nant y Cwm closed in 1964 but reopened in 1979 as a Steiner School. Archaeological sites
A number of sites at Llangolman are recorded in the 1925 Inventory of Ancient Monuments. One of the most obvious sites still visible today is the Iron Age enclosure located to the south of the village between the farms Bryn Golman and Pencraig Fawr. The site, locally called the Gear (in the field called Gear Meadow) is an enclosure that has a roughly level interior with measurements c.63m E-W and 66m N-S. The bank down-slope side stands up to 2 m high externally and 0.25 m internally. There appears to be a slight ditch on the northeast side. An entrance may be present that faces west. A second highly visible site is an enclosure called Castell Blaenllechog, located just to the west of the farm Pengawsai (itself located to the northwest of the village). It is not certain what the enclosure is, but suggestions include a medieval castle site, a medieval homestead or even an older Iron Age defensive site. What is particularly noticeable are the massive ramparts which stand 3.3 m high. Internally the height is less at about 1.5 m. Traces of a ditch 0.3 m to 0.6 m can be found to the west and south. This enclosure is particularly noticeable on the aerial views from Google Maps. References

External links
Historical and further sources on GENUKI
Cadw Description of Area

Slate industry in Wales
Villages in Pembrokeshire