Moel Penamnen
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Moel Penamnen
Moel Penamnen is a mountain just north of Blaenau Ffestiniog, North Wales and forms part of the Moelwynion. It may be climbed from the Crimea Pass via Moel Barlwyd, from Blaenau Ffestiniog or Cwm Penamnen to the north. A circular of Cwm Penamnen can be done taking in Y Ro Wen Y Ro Wen is a mountain just north of Blaenau Ffestiniog, North Wales and forms part of the Moelwynion. It may be climbed from Dolwyddelan or Cwm Penmachno. The popular climbing crag of Craig Alltrem can be found on its western slope. The summ .... It may also be combined with its parent peak Manod Mawr, however the pass between these peaks is extremely boggy and there are many mines, air shafts and open quarries in the area.Nuttall, John & Anne (1999). The Mountains of England & Wales - Volume 1: Wales (2nd edition ed.). Milnthorpe, Cumbria: Cicerone. . References External links www.geograph.co.uk : photos of Moel Penamnen and surrounding area Dolwyddelan Ffestiniog Mountains and hills of Conw ...
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Manod Mawr
Manod Mawr is a mountain in North Wales and forms part of the Moelwynion. Although known as a mountain in the eastern Moelwyns, it and its sister peaks are sometimes known as the Ffestiniog hills. Manod Mawr is a mountain which has been extensively quarried. The now-closed Graig Ddu Quarry is to be found on the contour, in the hollow between Manod Mawr's summit and Manod Mawr North Top. Manod Mawr's summit is in the exclusion zone of the Snowdonia National Park around Blaenau Ffestiniog, while Manod Mawr North Top's summit only just misses out on the national park's protection. There were fears the quarry would eventually remove the North Top.Nuttall, John & Anne (1999). The Mountains of England & Wales - Volume 1: Wales (2nd edition ed.). Milnthorpe, Cumbria: Cicerone. . During the Second World War, quarry tunnels in the Manod range were used to store and protect, in secret, valuable paintings from the National Gallery in London London is the capital and largest c ...
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Crimea Pass
The Crimea Pass ( cy, Bwlch y Gorddinan) is a mountain pass in North Wales, on the A470 road between Blaenau Ffestiniog and Dolwyddelan connecting the counties of Gwynedd and Conwy. Geography At its highest point, it is above sea level, and is sometimes closed in winter because of snow. At one time there was an inn at the summit of the pass, called the "Prince Llewellyn Inn" but it was popularly known as "the Crimea", because of its reputation for fights. The inn closed in 1881 because the police opposed the renewal of its licence and the justices thought that there was no need for the Inn when the railway to Ffestiniog was completed. Industry In the mid 1870s, Owen Gethin Jones opened the Bwlch Gordduant quarry near the summit of the pass. The quarry was not a great success and it was sold to the owner of the Prince Llewellyn quarry in late 1876. There is a track above the road which follows the route of the old road across the pass, described as a cleverly constructed ...
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Mountains And Hills Of Snowdonia
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 and ...
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Mountains And Hills Of Gwynedd
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 ...
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Mountains And Hills Of Conwy County Borough
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 and ...
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Ffestiniog
Ffestiniog () is a community in Gwynedd in Wales, containing several villages, in particular the settlements of Llan Ffestiniog and Blaenau Ffestiniog. It has a population of 4,875. History Ffestiniog was a parish in Cantref Ardudwy; in 1284, Ardudwy became part of the county of Merionethshire, which became an administrative county in 1888. Mary Evans (1735–89) founded a sect in Ffestiniog around 1780, whose believers held that she had married Christ in a ceremony held in Ffestiniog church. The sect soon died out after her death. The parish was created an urban district in 1894. Welsh ''-og''. The form ''-iog'' with an additional /i/ can be explained by the preceding element, which is a personal name ending with ''-i-us'' : ''Festinius''. The whole name should be ''*Festiniākon''. Probably same name as Festigny (France, e.g.: Festigny, Marne, ''Festiniacus'' in 853) See also * Festiniog and Blaenau Railway * Ffestiniog power station * Ffestiniog Railway The Ffestini ...
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Dolwyddelan
Dolwyddelan ( ; ; ) – in Victorian times, often spelled Dolyddelen – is a village and community in Conwy county borough, Wales, on the main A470 road between Blaenau Ffestiniog and Betws-y-Coed. As a community, the population of Dolwyddelan was recorded in the 2001 Census as 427, and 55.8% of those residents could speak Welsh. The population increased to 474 in the 2011 census with the proportion of Welsh speakers falling to 50.8%. Name The spelling of the village's name has varied over the years, though there appear to be two primary spellings with two primary meanings. The common modern spelling "Dolwyddelan" is translated as "Gwyddelan's meadow", referring to Saint Gwyddelan, an Irish missionary of the 6th century, after whom the parish church is named. There is some question as to which came first, the castle or the name. Saint Gwyddelan is believed to have arrived around 600 AD. A variant of this spelling is Dolwyddelen, which was particularly used by the ...
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Y Ro Wen
Y Ro Wen is a mountain just north of Blaenau Ffestiniog, North Wales and forms part of the Moelwynion. It may be climbed from Dolwyddelan or Cwm Penmachno. The popular climbing crag of Craig Alltrem can be found on its western slope. The summit has a shelter cairn, with views of Moel Penamnen, Manod Mawr North Top, Y Gamallt and Moel Siabod Moel Siabod ( Welsh for "bare hill" with unknown meaning of 'Siabod'), is a mountain in Snowdonia, North Wales, which sits isolated above the village of Dolwyddelan. At , it is the highest peak in the Moelwynion mountain range. The UK National Mo ....Nuttall, John & Anne (1999). The Mountains of England & Wales-Volume 1: Wales (2nd edition ed.). Milnthorpe, Cumbria: Cicerone. . References External links www.geograph.co.uk : photos of Moel Penamnen and surrounding area Bro Machno Dolwyddelan Mountains and hills of Conwy County Borough Mountains and hills of Snowdonia {{Conwy-geo-stub ...
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North Wales
, area_land_km2 = 6,172 , postal_code_type = Postcode , postal_code = LL, CH, SY , image_map1 = Wales North Wales locator map.svg , map_caption1 = Six principal areas of Wales commonly defined to be North Wales, for policing, fire and rescue, health and regional economy. North Wales ( cy, Gogledd Cymru) is a region of Wales, encompassing its northernmost areas. It borders Mid Wales to the south, England to the east, and the Irish Sea to the north and west. The area is highly mountainous and rural, with Snowdonia National Park ( and the Clwydian Range and Dee Valley (), known for its mountains, waterfalls and trails, wholly within the region. Its population is concentrated in the north-east and northern coastal areas, with significant Welsh-speaking populations in its western and rural areas. North Wales is imprecisely defined, lacking any exact definition or administrative structure. It is commonly defined adminis ...
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Hewitt (hill)
This is a list of Hewitt mountains in England, Wales and Ireland by height. Lists of mountains and hills in the British Isles#Hewitts, Hewitts are defined as "Hills in England, Wales and Ireland over two thousand" feet in height, the general requirement to be called a Lists of mountains and hills in the British Isles#Elevation, "mountain" in the British Isles, and with a prominence above ; a mix of imperial measures, imperial and metric system, metric thresholds. The Hewitt classification was suggested by Alan Dawson in his 1992 book, "The Relative Hills of Britain". Dawson originally called his Hewitts "Sweats", from "Summits - Wales and England Above Two thousand", before settling on the label Hewitt. In a series of three booklets edited by Dave Hewitt, the list of English Hewitts was published in 1997, and the list of Welsh Hewitts was also published in 1997, and the list of Irish Hewitts was published in 1998. Hewitts were designed to address one of the criticisms of ...
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Blaenau Ffestiniog
Blaenau Ffestiniog is a town in Gwynedd, Wales. Once a slate mining centre in historic Merionethshire, it now relies much on tourists, drawn for instance to the Ffestiniog Railway and Llechwedd Slate Caverns. It reached a population of 12,000 at the peak development of the slate industry, but fell with the decline in demand for slate. The population of the community, including the nearby village Llan Ffestiniog, was 4,875 in the 2011 census: the fourth most populous in Gwynedd after Bangor, Caernarfon and Llandeiniolen. The population not including Llan is now only about 4,000. Etymology and pronunciation The meaning of Blaenau Ffestiniog is "uplands of Ffestiniog". The Welsh word ' is the plural of ' "upland, remote region". Ffestiniog here is probably "territory of Ffestin" (Ffestin being a personal name) or could possibly mean "defensive place". The English pronunciation of Blaenau Ffestiniog suggested by the ''BBC Pronouncing Dictionary of British Names'' is , but the f ...
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Mountain
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 (topography), 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 Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, 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 Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosys ...
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