|
Moelwyn Bach
Moelwyn Bach is a mountain in Snowdonia, northern Wales and forms part of the Moelwynion. It is connected to its parent peak Moelwyn Mawr via the Craigysgafn ridge. It overlooks the town of Blaenau Ffestiniog and the Vale of Ffestiniog The Vale of Ffestiniog is a valley in the Snowdonia National Park in Gwynedd, North Wales. It stretches from Ffestiniog in the east and runs in a westerly direction towards Tremadog Bay, terminating near Porthmadog. The Afon Dwyryd runs throug ....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 Moelwyn Bach and surrounding rea Ffestiniog Llanfrothen Mountains and hills of Gwynedd Mountains and hills of Snowdonia Hewitts of Wales Nuttalls {{Gwynedd-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moelwyn Mawr
Moelwyn Mawr is a mountain in Snowdonia, North Wales and forms part of the Moelwynion. Its summit overlooks the Vale of Ffestiniog and has views in all directions. Site of Special Scientific Interest In 1990, Moelwyn Mawr was designated a Site of Special Scientific Interest of national scientific importance. The glaciated landscape of the mountain provides fine examples of two specific Pleistocene features. On the north-east flank of the mountain is a terrain of patterned ground, consisting of small-scale vegetated stripes. On the west side, a debris tongue formed by a rock glacier extends into Cwm Croesor. Quarrying Slate quarrying was a major industry for many years in the Moelwynion. Moelwyn Mawr's flanks have several major quarries on them. To the west is Croesor Quarry perched high above Cwm Croesor. To the north west is Rhosydd Quarry on the col between Cwm Croesor and Cwm Orthin. Within Cwm Orthin, Conglog and Wrysgan quarries are located on the north ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Llanfrothen
Llanfrothen () is a hamlet and community in the county of Gwynedd, Wales, between the towns of Porthmadog and Blaenau Ffestiniog and is 108.1 miles (174.0 km) from Cardiff. In 2011 the population of Llanfrothen was 437 with 70.1% of them able to speak Welsh. Parc, a Grade II* Listed Building is within the community, as are the village of Garreg and the hamlet of Croesor. The church at Llanfrothen is dedicated to St Brothen and is a Grade 1 listed building and is in the care of the Friends of Friendless Churches The church and parish achieved prominence throughout Wales in 1888 when David Lloyd George, then a young local solicitor, took a case involving burial rights in Llanfrothen churchyard on appeal to the Divisional Court of the Queen’s Bench Division. The case became known as the , and decision of the Divisional Court established the right of the family of a deceased nonconformist to have his body buried in the parish churchyard, by a Baptist minister, and without ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vale Of Ffestiniog
The Vale of Ffestiniog is a valley in the Snowdonia National Park in Gwynedd, North Wales. It stretches from Ffestiniog in the east and runs in a westerly direction towards Tremadog Bay, terminating near Porthmadog. The Afon Dwyryd runs through the Vale; pastoral farming is practised along its length. The Vale is chiefly famous for the Ffestiniog Railway, a narrow gauge railway running from Porthmadog to 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 12,00 .... Once used for transporting slate mined in Blaenau to docks on the coast, the line is now a major tourist attraction. References Ffestiniog Maentwrog Talsarnau Valleys of Gwynedd Valleys of Snowdonia {{Gwynedd-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Craigysgafn
Craigysgafn is a rocky ridge and a top of Moelwyn Mawr that leads south from Moelwyn Mawr to Moelwyn Bach in Snowdonia, 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 common .... It has several gullies which lead directly down to the scree slopes above Llyn Stwlan. Some scrambling is needed in places.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 Craigysgafn and surrounding area Ffestiniog Llanfrothen Mountains and hills of Gwynedd Mountains and hills of Snowdonia Hewitts of Wales Ridges of Wales Nuttalls {{Gwynedd-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moelwynion
The Moelwynion (a Welsh language, Welsh plural, sometimes Anglicisation, anglicised to Moelwyns) are a group of mountains in central Snowdonia. They extend from the north-east of Porthmadog to Moel Siabod, the highest of the group. The name derives from the names of two of the largest mountains in the group, Moelwyn Mawr (''great white hill'') and Moelwyn Bach (''little white hill''), 770m and 710m, respectively. Moel Siabod, to the north, is the highest at 872m. The group includes the following summits: *Moel Siabod *Moelwyn Mawr *Moelwyn Bach *Allt-fawr *Cnicht *Craigysgafn *Cnicht North Top *Moel Druman *Ysgafell Wen *Ysgafell Wen North Top *Manod Mawr *Manod Mawr North Top *Ysgafell Wen Far North Top *Moel-yr-hydd *Moelwyn Mawr North Ridge Top *Moel Penamnen *Moel Meirch *Y Ro Wen {{Coord, 53.036, -3.980, dim:20000_region:GB, display=title External links Walking Routes in the Moelwynion Beddgelert Bro Machno Capel Curig Dolwyddelan Ffest ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nuttall (hill)
This is a list of Nuttall mountains in England and Wales by height. Nuttalls are defined as peaks above in height, the general requirement to be called a "mountain" in the British Isles, and with a prominence above ; a mix of imperial and metric thresholds. The Nuttall classification was suggested by Anne and John Nuttall in their 1990 two–volume book, "The Mountains of England and Wales". The list was updated with subsequent revised editions by the Nuttalls. Because of the prominence threshold of only , the list is subject to ongoing revisions. In response, Alan Dawson introduced the Hewitts, with a higher prominence threshold of . This was the prominence threshold that the UIAA set down in 1994 for an "independent" peak. In 2010, Dawson replaced his Hewitts with the fully "metric" Simms, consisting of a height threshold of , and a prominence threshold of . However, both the Nuttall and Hewitt classifications have become popular with peak baggers, and both remain in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
.jpg "Click for more on -> Vale Of Ffestiniog")
.jpg "Click for more on -> Blaenau Ffestiniog")
