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Rhigos RFC Players
Rhigos () is a village and community in Rhondda Cynon Taf, Wales. The village is located on the saddle of higher ground between the Vale of Neath and the Cynon Valley. It was part of Neath Rural District, in the county of Glamorgan, until 1974. The village then came under the jurisdiction of Cynon Valley Borough, which subsequently became Rhondda Cynon Taf in 1996. It lies just off the Aberdare road that was the main link between Aberdare and Glynneath, before the A465 road was extended in the 1960s. The hamlets of Cefn Rhigos and Cwm-Hwnt lie to the west of the main village. The population of the community in the 2011 census was 894. The postal the town is Aberdare, although it is some from Aberdare town centre, and from Glynneath. It was noted as a township in the parish of Ystradyfodwg in several historical references and people moved to this rural area to work in local industries. Today the village is a quiet place to live with views of the Brecon Beacons National Park t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tower Colliery
Tower Colliery ( Welsh: Glofa'r Tŵr) was the oldest continuously working deep- coal mine in the United Kingdom, and possibly the world, until its closure in 2008. It was the last mine of its kind to remain in the South Wales Valleys. It was located near the villages of Hirwaun and Rhigos, north of the town of Aberdare in the Cynon Valley of South Wales. History With coal located so close to the surface, it was known by locals to be possible to drift mine coal from Hirwaun common. This activity increased from 1805, until in 1864 the first drift named Tower was started, named after the nearby Crawshay's Tower, a folly built in 1848 and named after Richard Crawshay. In 1941, a new shaft was sunk to a depth of 160 metres. From 1943 until closure, this shaft was used as the main "return" ventilation shaft and for the transport of men. In 1958 Tower No. 3 was driven to meet the No. 4 colliery workings, and was used as the main "intake" airway, conveying coal to the surface and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ystradyfodwg
Ystradyfodwg or Ystrad Dyfodwg (Vale of Tyfodwg) was an ancient upland parish in Glamorgan, Wales. It is believed to have been named after Dyfodwg (or Tyfodwg) a 6th-century saint or chieftain. The parish included most of the area which would later be known as Rhondda named for the parish rivers, Rhondda Fawr and Rhondda Fach. Extent The parish of Ystradyfodwg covered a vast area of 10,127 Hectares, but only had 542 inhabitants in 1801. It stretched from the confluence of the Rhondda rivers at Porth, over the mountain as far as the Vale of Neath. It was divided into four townships: *Home (between the rivers) *Clydach (south of the Rhondda Fawr) *Middle (the upper part of the valley) * Rhigos (north of the mountains). History The small village of Ystradyfodwg was centred on its parish church, at the site now occupied by the church of St John the Baptist in Ton Pentre. Prior to the industrial revolution, Ton Pentre (then just called Ton) was a hamlet a short distance to the we ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sites Of Special Scientific Interest
A Site of Special Scientific Interest (SSSI) in Great Britain, or an Area of Special Scientific Interest (ASSI) in the Isle of Man and Northern Ireland, is a conservation designation denoting a protected area in the United Kingdom and Isle of Man. SSSI/ASSIs are the basic building block of site-based nature conservation legislation and most other legal nature/geological conservation designations in the United Kingdom are based upon them, including national nature reserve (United Kingdom), national nature reserves, Ramsar Convention, Ramsar sites, Special Protection Areas, and Special Area of Conservation, Special Areas of Conservation. The acronym "SSSI" is often pronounced "triple-S I". Selection and conservation Sites notified for their Biology, biological interest are known as Biological SSSIs (or ASSIs), and those notified for geological or Physical geography, physiographic interest are Geological SSSIs (or ASSIs). Sites may be divided into management units, with some a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Llyn Fawr
Llyn Fawr (large lake''' in Welsh) is a reservoir that occupies one of a series glacial cirques that form the northern escarpment of the South Wales Coalfield uplands, overlooking the heads of the Vale of Neath and the Cynon Valley, South Wales. It is known as the site of an important hoard of weapons and tools from the late Bronze Age and early Iron Age. It lies on the northern flanks of Craig-y-Llyn, a mountain that is designated as a Site of Special Scientific Interest. The western cirque contains Llyn Fach (small lake'''). While in government terms, it falls in the unitary authority of Rhondda Cynon Taf, in geographic terms it is actually in the Vale of Neath and its excess waters (all its water before conversion) flow into Nant Gwrelych, which flows into the River Neath at Pont Walby near Glynneath. Less than 1 km to the southeast and south lie the headwaters of the Rhondda Fawr and Rhondda Fach rivers, while 1.5 km to the southwest lie the headwaters of Rive ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tarn (lake)
A tarn (or corrie loch) is a mountain lake, pond or pool, formed in a cirque (or "corrie") excavated by a glacier. A moraine may form a natural dam below a tarn. Etymology The word is derived from the Old Norse word ''tjörn'' ("a small mountain lake without tributaries") meaning pond. In parts of Northern England – predominantly Cumberland and Westmorland (where there are 197), but also areas of North Lancashire and North Yorkshire – 'tarn' is widely used as the name for small lakes or ponds, regardless of their location and origin (e.g. Talkin Tarn, Urswick Tarn, Malham Tarn). Similarly, in Scandinavian languages, a ''tjern'' or ''tjørn'' (both Norwegian) or ''tjärn'' or ''tärn'' (both Swedish) is a small natural lake, often in a forest or with vegetation closely surrounding it or growing into the tarn. The name of the Tjörnin in Reykjavik, Iceland is also from a related word. The specific technical use for a body of water in a glacial corrie comes from the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pennant Measures
The Pennant Measures is the traditional name for a sequence of sedimentary rocks of the South Wales Coalfield. They were also referred to as the Upper Coal Measures and assigned to the Westphalian 'C' and Westphalian 'D' stages of the Carboniferous Period. The Pennant Measures were divided into the Lower Pennant Measures and the Upper Pennant Measures, differing from the underlying Middle and Lower Coal Measures in being principally of sandstone units – known collectively as the Pennant Sandstone – with mudstone being the subsidiary rock type. Numerous coal seams occur within the Pennant Measures though they are less common than in the underlying Coal Measures.British Geological Survey 1:50,000 map sheet 231 'Merthyr Tydfil' & accompanying memoir. However recent reclassification of the sequence has resulted in the definition by the British Geological Survey of the Pennant Sandstone Formation as a sub-unit of the newly established Warwickshire Group. The formation is recognis ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacial Cirque
A (; from the Latin word ) is an amphitheatre-like valley formed by Glacier#Erosion, glacial erosion. Alternative names for this landform are corrie (from , meaning a pot or cauldron) and ; ). A cirque may also be a similarly shaped landform arising from fluvial erosion. The concave shape of a glacial cirque is open on the downhill side, while the cupped section is generally steep. Cliff-like slopes, down which ice and glaciated debris combine and converge, form the three or more higher sides. The floor of the cirque ends up bowl-shaped, as it is the complex convergence zone of combining ice flows from multiple directions and their accompanying rock burdens. Hence, it experiences somewhat greater erosion forces and is most often overdeepening, overdeepened below the level of the cirque's low-side outlet (stage) and its down-slope (backstage) valley. If the cirque is subject to seasonal melting, the floor of the cirque most often forms a tarn (lake), tarn (small lake) behind a d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Craig Y Llyn
is a mountain situated to the south of the village of Rhigos in the Cynon Valley on the south side of the upper Vale of Neath and north of the Rhondda Valleys in South Wales; it is the highest point in the ancient kingdom and, later, county of Glamorgan (Morgannwg), and the South Wales Coalfield, southern Welsh coalfield plateau. Description The summit of Craig y Llyn lies within the borough of Neath Port Talbot whilst its eastern slopes are within Rhondda Cynon Taf, the boundary running in a north - south direction to the east of the summit. The name derives from the sandstone cliffs which drop steeply down to the lake on its northern side. The hill is covered by forestry, except for the steep north and northeast faces, and is crowned with a trig point. Several trail, footpaths cross near the summit of the hill, including the Coed Morgannwg Way. The highest point in Neath Port Talbot, Craig y Llyn, is commonly known as the Rhigos Mountain after the village of Rhigos located ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Calluna
''Calluna vulgaris'', common heather, ling, or simply heather, is the sole species in the genus ''Calluna'' in the flowering plant family Ericaceae. It is a low-growing evergreen shrub growing to tall, or rarely to and taller, and is found widely in Europe and Asia Minor on acidic soils in open sunny situations and in moderate shade. It is the dominant plant in most heathland and moorland in Europe, and in some bog vegetation and acidic pine and oak woodland. It is tolerant of grazing and regenerates following occasional burning, and is often managed in nature reserves and grouse moors by sheep or cattle grazing, and also by light burning. Description ''Calluna'' can reach in height. It has small-scale leaves (less than 2–3 mm long) borne in opposite and decussate pairs, whereas those of '' Erica'' are generally larger and in whorls of 3–4, sometimes 5. Clive Stace, (2010) ''New Flora of the British Isles'', 3rd edition. Cambridge University Press. It flowers fr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gwenhwyseg
or (also called " Gwentian" in English) is a Welsh dialect A dialect is a Variety (linguistics), variety of language spoken by a particular group of people. This may include dominant and standard language, standardized varieties as well as Vernacular language, vernacular, unwritten, or non-standardize ... of South East Wales. The name derives from an old term for the inhabitants of the area, . One of Gwenhwyseg's characteristics is the change in the long ''a'' vowel to a long ''e'' e.g. rather than the standard ("the Father, the Son and the Holy Spirit"). The diphthong ''ae'' is changed in the same way: This is a diphthong which varies in pronunciation over the Gwenhwyseg territory and not realised with same phoneme; it is also found in words like , etc. This does not occur in monosyllabic words containing a short ''a'' like and as happens in some of the dialects of Montgomeryshire. Gwenhwyseg has influenced the English spoken in the area with English speakers usin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cardiff
Cardiff (; ) is the capital city, capital and List of urban areas in the United Kingdom, largest city of Wales. Cardiff had a population of in and forms a Principal areas of Wales, principal area officially known as the City and County of Cardiff (). The city is the List of cities in the United Kingdom, eleventh largest in the United Kingdom. Located in the South East Wales, southeast of Wales and in the Cardiff Capital Region, Cardiff is the county town of the Historic counties of Wales, historic county of Glamorgan and in 1974–1996 of South Glamorgan. It belongs to the Eurocities network of the largest European cities. A small town until the early 19th century, its prominence as a port for coal when mining began in the region helped its expansion. In 1905, it was ranked as a city and in 1955 proclaimed capital of Wales. The Cardiff urban area covers a larger area outside the county boundary, including the towns of Dinas Powys and Penarth. Cardiff is the main commercial ce ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Machynlleth
Machynlleth () is a market town, community and electoral ward in Powys, Wales and within the historic boundaries of Montgomeryshire. It is in the Dyfi Valley at the intersection of the A487 and the A489 roads. At the 2001 Census it had a population of 2,147, rising to 2,235 in 2011. It is sometimes referred to colloquially as ''Mach''. Machynlleth was the seat of Owain Glyndŵr's Welsh Parliament in 1404,''The Welsh Academy Encyclopaedia of Wales''. John Davies, Nigel Jenkins, Menna Baines and Peredur Lynch (2008) pg527 and as such claims to be the "ancient capital of Wales". However, it has never held any official recognition as a capital. It applied for city status in 2000 and 2002, but was unsuccessful. It is twinned with Belleville, Michigan. Machynlleth hosted the National Eisteddfod in 1937 and 1981. Etymology The etymology of the name Machynlleth derives from ield, plainand . The ending 's' of is the cause of the 'c' of becoming 'ch': reflecting a stand ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
