Mynydd Marchywel
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Mynydd Marchywel
Mynydd Marchywel is a high hill in the Neath Port Talbot area in South Wales. Its summit is marked both by a cairn and a trig point. The larger part of the hill is cloaked in modern forestry through which numerous streams fall away westward to the River Tawe, eastward to the River Dulais and southward into the Clydach, the latter two being tributaries of the River Neath. Geology The hill is formed from multiple layers of Pennant Sandstone with intervening mudstone layers and occasional coal seams. All are tilted to the south and southwest towards the axis of the South Wales Coalfield syncline. Parts of its slopes are mantled by glacial till. The coal seams have been worked extensively in the past. One of the last operations was that at Gleision Colliery under the northwestern side of Mynydd Marchywel. Scheduled monuments ;Mynydd Marchywel summit cairn: This Round cairn dating to the Bronze Age is north of the trig pont. The heap of stones, now gradually spreading, has trac ...
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Fan Gyhirych
Fan Gyhirych is a mountain in the Fforest Fawr section of Brecon Beacons National Park in south Wales. It lies within the county of Breconshire, and administered as part of the unitary authority of Powys. Its highest point at 2379 feet (or 725 m) is marked by a trig point which is located towards the western side of the summit plateau. The hill drains to the north into the catchment of the Afon Crai and to the south and west into that of the River Tawe. Fan Fraith is a nearby hill which can be considered a subsidiary top of Fan Gyhirych. Geology The hill is formed largely from sandstones of the Brownstones Formation of the Old Red Sandstone laid down during the Devonian period. A part of the summit plateau is capped by sandstones of the overlying Plateau Beds Formation which also occur on the nearby peak of Fan Fraith. The Cribarth Disturbance, a north-east to south-west aligned zone of faulting and folding, passes through the hill. The hill's finest feature is its nort ...
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South Wales Coalfield
The South Wales Coalfield ( cy, Maes glo De Cymru) extends across Pembrokeshire, Carmarthenshire, Swansea, Neath Port Talbot, Bridgend, Rhondda Cynon Taf, Merthyr Tydfil, Caerphilly, Blaenau Gwent and Torfaen. It is rich in coal deposits, especially in the South Wales Valleys. Description It comprises a fully exposed synclinorium with a varying thickness of coal measures (Upper Carboniferous/Pennsylvanian) with thick, workable seams in the lower parts and generally thinner and sparser seams in the upper parts, together with a development of sandstones (Pennant Sandstone). These sandstones have been much used in building construction (including the characteristic terraces of former miners' houses) and give rise to bleak uplands rising 300–600 metres above sea level between the steep-sided valleys in which most deep mines were developed. The coal generally increases in grade or "rank" from east to west, with bituminous coals in the east, and anthracite in the west, mostly to ...
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Countryside And Rights Of Way Act 2000
The Countryside and Rights of Way Act 2000 (c. 37), known informally as the CRoW Act or "Right to Roam" Act is a United Kingdom Act of Parliament affecting England and Wales which came into force on 30 November 2000. Right to roam The Act implements the so-called "right to roam" (also known as ''jus spatiandi'') long sought by the Ramblers' Association and its predecessors, on certain upland and uncultivated areas of England and Wales. This element of the act was implemented in stages as conclusive maps of different regions were produced. The act refers to areas of 'mountain, moor, heath and down' in addition to registered common land; not all uncultivated land is covered. Rights of way A staged review of public rights of way, including limited rights to create new public footpaths where needed, is being conducted under the Act. Again, this is being conducted in a staged manner, which can produce anomalies – of the two administrative areas of the County of Gloucestershir ...
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Freedom To Roam
The freedom to roam, or "everyman's right", is the general public's right to access certain public or privately owned land, lakes, and rivers for recreation and exercise. The right is sometimes called the right of public access to the wilderness or the "right to roam". In Scotland, Finland, Iceland, Norway, Sweden, Estonia, Latvia, Lithuania, Belarus, Austria, Czech Republic and Switzerland, the freedom to roam takes the form of general public rights which are sometimes codified in law. The access is ancient in parts of Northern Europe and has been regarded as sufficiently basic that it was not formalised in law until modern times. However, the right usually does not include any substantial economic exploitation, such as hunting or logging, or disruptive activities, such as making fires and driving offroad vehicles. In countries without such general rights, there may be a network of rights of way, or some nature reserves with footpaths. Europe Nordic countries Ancient traces p ...
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Rights Of Way In England And Wales
In England and Wales, other than in the 12 Inner London London boroughs, boroughs and the City of London, the right of way is a legally protected right of the public to pass and re-pass on specific paths. The law in England and Wales differs from Scots law in that rights of way exist only where they are so designated (or are able to be designated if not already), whereas in Scotland any route that meets certain conditions is rights of way in Scotland, defined as a right of way, and in addition, there is a general presumption of access to the countryside ("right to roam"). Private rights of way or easements also exist (see also Highways in England and Wales). Inner London Definitive maps of public rights of way have been compiled for all of England and Wales, as a result of the National Parks and Access to the Countryside Act 1949, except the 12 Inner London boroughs, which, along with the City of London, were not covered by the Act. Definitive maps exist for the Outer London bo ...
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Crynant
Crynant ( cy, Y Creunant) is a village and community in the Dulais Valley in Wales. It lies 7¾ miles north-east from the town of Neath in Neath Port Talbot, situated between the mountains of Mynydd Marchywel to the west, Hirfynydd to the east and Mynydd y Drum to the north. Crynant is a long village, lying on the narrow valley floor and lower slopes of Hirfynydd. Originally there were separate villages (essentially separate farms), such as the region of Treforgan, but all have now merged into a single village. The River Dulais flows through the village. Etymology The name Y Creunant has its etymology, like many Welsh place names, in description. 'Creu' (or nghreu) meaning the creation, or beginning, and 'nant' meaning stream or brook. A different interpretation of the prefix is 'crai', implying a narrow place signifying a brook that has to make its way through a narrow place. Another explanation states that the place name is a contraction of Croyw-nant, the clear brook. Creu ...
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Saint Illtyd's Walk
Saint Illtyd's Walk is a waymarked long-distance footpath in South Wales. It runs from Pembrey Country Park, west of Burry Port, through rural eastern Carmarthenshire and Neath Port Talbot to end at Margam Country Park, south of Port Talbot. The walk is named after Illtyd (or Illtud), a late-fifth / early-sixth century Welsh saint. The route The route skirts the fringes of Burry Port, heading east to the Lliedi reservoirs then to Pontarddulais. It then turns northeast heading up via Graig Fawr onto Mynydd y Gwair then heads southeast via Bryn Mawr and Mynydd Carnllechart to the Swansea Canal north of Pontardawe following the towpath past Ynysmeudwy and Cilmaengwyn. The route then climbs east over the northern end of the Mynydd Marchywel ridge and down to cross the River Dulais at Crynant. From there it climbs steeply up through forestry to Sarn Helen which here runs along Hirfynydd and then steeply down to Resolven in the Vale of Neath. Passing Melincourt Falls it clim ...
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Bronze Age
The Bronze Age is a historic period, lasting approximately from 3300 BC to 1200 BC, characterized by the use of bronze, the presence of writing in some areas, and other early features of urban civilization. The Bronze Age is the second principal period of the three-age system proposed in 1836 by Christian Jürgensen Thomsen for classifying and studying ancient societies and history. An ancient civilization is deemed to be part of the Bronze Age because it either produced bronze by smelting its own copper and alloying it with tin, arsenic, or other metals, or traded other items for bronze from production areas elsewhere. Bronze is harder and more durable than the other metals available at the time, allowing Bronze Age civilizations to gain a technological advantage. While terrestrial iron is naturally abundant, the higher temperature required for smelting, , in addition to the greater difficulty of working with the metal, placed it out of reach of common use until the end o ...
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Round Cairn
A bowl barrow is a type of burial mound or tumulus. A barrow is a mound of earth used to cover a tomb. The bowl barrow gets its name from its resemblance to an upturned bowl. Related terms include ''cairn circle'', ''cairn ring'', ''howe'', ''kerb cairn'', ''tump'' and ''rotunda grave''. Description Bowl barrows were created from the Neolithic through to the Bronze Age in Great Britain. A bowl barrow is an approximately hemispherical mound covering one or more Inhumations or cremations. Where the mound is composed entirely of stone, rather than earth, the term cairn replaces the word barrow. The mound may be simply a mass of earth or stone, or it may be structured by concentric rings of posts, low stone walls, or upright stone slabs. In addition, the mound may have a kerb of stones or wooden posts. Barrows were usually built in isolation in various situations on plains, valleys and hill slopes, although the most popular sites were those on hilltops. Bowl barrows were first ident ...
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Gleision Colliery
The Tarenni Colliery ( cy, Gloddfa Tarenni) and its associated workings, are a series of coal mines and pits located between the villages of Godre'r Graig and Cilybebyll located in the valley of the River Tawe, in Neath Port Talbot county borough, South Wales. Primrose Colliery Primrose Colliery was developed from the mid-1800s, close to the village of Rhos. After the disaster of 1853, it was redeveloped as the New Primrose Colliery, owned by Sir Ralph Howard, and by 1896 employed 307. It closed in the early 1900s, but from 1908 was revived as a pumping station for the Tarenni Colliery. Tirbach Slants The major coal seams are located close beneath the valley floor, but mean accessing steeply declining seams which run in high geological fault structures, running directly under the River Tawe. This makes the coal easily accessible, but also dangerous to extract. The first drift mine workings occurred in the late 1800s, at a site referred to at the time as the Tirbach Slants. The Pwl ...
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