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Cefn Manmoel
Cefn Manmoel is the name given to the broad ridge of high ground between the Sirhowy Valley and Ebbw Vale in the Valleys region of South Wales. It straddles the boundary between the unitary areas of Caerphilly and Blaenau Gwent. The NNW-SSE aligned ridge achieves a height of above sea-level at OS grid ref SO 166072. To the south it drops away to a broad saddle southeast of the village of Manmoel, beyond which lies Mynydd Pen-y-fan. Parts of both its eastern and western flanks are afforested with conifer plantations such as at Coed y Rhyd and at Coed y Llanerch. Geology The entire hill is composed of sandstones and mudstones dating from the Carboniferous Period. There are also numerous coal seams within the sequence, most of which have been worked. The upper part of the hill including the summit plateau is formed from the Pennant Sandstone, a rock assigned to the Carboniferous Upper Coal Measures. The flanks of the hill owe their steepness in part to the action of glacial ice ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sirhowy Valley
The Sirhowy Valley ( ) is an industrialised valley in the eastern part of the Valleys region of Wales. It is named from the Sirhowy River () which runs through it. Its upper reaches are occupied by the town of Tredegar within the unitary area of Blaenau Gwent. The valley initially heads south-southeast between the ridges of Cefn Manmoel to the east and Mynydd Bedwellte to the west before turning to a more southerly direction. Its central section is one of the least populated of the Welsh coalfield valleys. The valley enters the unitary area of Caerphilly which contains the towns of Blackwood () and Pontllanfraith. It then turns east and joins the valley of the Ebbw River, Ebbw Vale at Crosskeys. History The valley's industrial history began with ironworks before evolving to meet the demand for coal and the expansion of coal mining. This process was led by companies such as the Tredegar Iron and Coal Company. Coal mines used to be located throughout the valley, including ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacier
A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. It acquires distinguishing features, such as crevasses and seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between latitudes 35°N and 35°S, glaciers occur ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains And Hills Of Blaenau Gwent
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ebbw Valley Walk
The Ebbw Valley Walk is a -long recreational walk which runs from Festival Park in Ebbw Vale southwards to the Sirhowy Valley Country Park west of Risca in South Wales. The route is managed and maintained by Caerphilly County Borough Council Caerphilly County Borough Council ( cy, Cyngor Bwrdeistref Sirol Caerffili) is the governing body for Caerphilly County Borough, one of the Principal Areas of Wales. The last full council elections took place 5 May 2022. Political control The ... who published a 24-page booklet promoting the route in 1996 though this is no longer in print.Ordnance Survey Explorer map series sheet nos 152 ''Newport & Pontypool'', 166 ''Rhondda & Merthyr Tydfil'' References {{reflist Recreational walks in Wales Geography of Caerphilly County Borough Tourist attractions in Caerphilly County Borough Ebbw Vale ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sirhowy Valley Ridgeway Walk
The Sirhowy Valley Ridgeway Walk (also referred to as the Sirhowy Valley Walk) is a -long recreational walk which runs from the southwestern outskirts of Newport north to the eastern edge of Tredegar in South Wales. The route is managed and maintained by Caerphilly County Borough Council Caerphilly County Borough Council ( cy, Cyngor Bwrdeistref Sirol Caerffili) is the governing body for Caerphilly County Borough, one of the Principal Areas of Wales. The last full council elections took place 5 May 2022. Political control The ..., which publishes a free A3 leaflet describing it. ldwa.org.uk; accessed 9 March 2015. References Recreational walks in Wales[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rights Of Way In England And Wales
In England and Wales, other than in the 12 Inner London 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 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 boroughs. Rights of way outside L ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Public Footpath
A footpath (also pedestrian way, walking trail, nature trail) is a type of thoroughfare that is intended for use only by pedestrians and not other forms of traffic such as motorized vehicles, bicycles and horses. They can be found in a wide variety of places, from the centre of cities, to farmland, to mountain ridges. Urban footpaths are usually paved, may have steps, and can be called alleys, lanes, steps, etc. National parks, nature preserves, conservation areas and other protected wilderness areas may have footpaths ( trails) that are restricted to pedestrians. The term footpath can also describe a pavement/sidewalk in some English-speaking countries (such as Australia, New Zealand, and Ireland). A footpath can also take the form of a footbridge, linking two places across a river. Origins and history Public footpaths are rights of way originally created by people walking across the land to work, market, the next village, church, and school. This includes Mass pa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
CRoW Act
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 Gloucestershire ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Open Country
"Open Country" is a designation used for some UK access land. It was first defined under the National Parks and Access to the Countryside Act 1949 (and extended by the Countryside Act 1968), and was land over which an appropriate access agreement had been made. In particular significant upland areas of the northern Peak District, where there had been much dispute over access prior to World War II, were so designated (see '' Mass trespass of Kinder Scout''). The term is also used in the 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 imp ... to describe 'areas of mountain, moor, heath and down' that are generally available for access under that Act. (It appears that the rights conferred by this new definition are in general less comprehensive than ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quaternary Glaciation
The Quaternary glaciation, also known as the Pleistocene glaciation, is an alternating series of glacial and interglacial periods during the Quaternary period that began 2.58 Ma (million years ago) and is ongoing. Although geologists describe this entire period up to the present as an " ice age", in popular culture this term usually refers to the most recent glacial period, or to the Pleistocene epoch in general. Since Earth still has polar ice sheets, geologists consider the Quaternary glaciation to be ongoing, though currently in an interglacial period. During the Quaternary glaciation, ice sheets appeared, expanding during glacial periods and contracting during interglacial periods. Since the end of the last glacial period, only the Antarctic and Greenland ice sheets have survived, with other sheets formed during glacial periods, such as the Laurentide Ice Sheet, having completely melted. The major effects of the Quaternary glaciation have been the continental erosio ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coal Measures
In lithostratigraphy, the coal measures are the coal-bearing part of the Upper Carboniferous System. In the United Kingdom, the Coal Measures Group consists of the Upper Coal Measures Formation, the Middle Coal Measures Formation and the Lower Coal Measures Formation. The group records the deposition of fluvio-deltaic sediments which consists mainly of clastic rocks ( claystones, shales, siltstones, sandstones, conglomerates) interstratified with the beds of coal. In most places, the coal measures are underlain by coarser clastic sequences known as Millstone Grit, of Namurian age. The top of the coal measures may be marked by an unconformity, the overlying rocks being Permian or later in age. In some parts of Britain, however, the coal measures grade up into mainly coal-barren red beds of late Westphalian and possibly Stephanian age. Within the Pennine Basin these barren measures are now referred to as the Warwickshire Group, from the district where they achieve their thic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ebbw Vale
Ebbw Vale (; cy, Glynebwy) is a town at the head of the valley formed by the Ebbw Fawr tributary of the Ebbw River in Wales. It is the largest town and the administrative centre of Blaenau Gwent county borough. The Ebbw Vale and Brynmawr conurbation has a population of roughly 33,000. It has direct access to the dualled A465 Heads of the Valleys trunk road and borders the Brecon Beacons National Park. Welsh language According to the 2011 Census, 4.6% of Ebbw Vale North's 4,561 (210 residents) resident-population can speak, read, and write Welsh, and 5.7% of Ebbw Vale South's 4,274 (244 residents) resident-population can speak, read, and write Welsh. This is below the county's figure of 5.5% of 67,348 (3,705 residents) who can speak, read, and write Welsh. Early history There is evidence of very early human activity in the area. Y Domen Fawr is a Bronze Age burial cairn above the town and at Cefn Manmoel there is a demarcation dyke believed to be of neolithic or medieval ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
