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Carnedd Llechwedd-llyfn
Carnedd Llechwedd-llyfn is a subsidiary summit of Carnedd y Filiast on the border of Snowdonia National Park in Llandderfel, in Gwynedd. The northern slopes of the peak lie in Ysbyty Ifan, in Conwy. It is part of the Arenig mountain range, and rises from the shore of Llyn Celyn. It is also a peak in an area of moorland known as the Migneint. The views of northern Snowdonia are extensive. Arenig Fach, Arenig Fawr Arenig Fawr ( en, Great High Ground) is a mountain in Snowdonia, North Wales, close to Llyn Celyn reservoir, alongside the A4212 between Trawsfynydd and Bala. Location Arenig Fawr is the highest member of the Arenig range, with Arenig Fach ( ... and Waun Garnedd y Filiast can also be seen. The summit is marked by a small cairn next to a fence which runs across this boggy summit.Nuttall, John & Anne (1999). The Mountains of England & Wales - Volume 1: Wales (2nd edition ed.). Milnthorpe, Cumbria: Cicerone. . References Mountains and hills of Conwy C ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Foel Boeth
Foel Boeth is the twin top of Gallt y Daren in the southern half of the Snowdonia National Park in Gwynedd, North Wales, and forms part of the Arenig mountain range. Its parent peak is Moel Llyfnant. The peak is often known as Foel Boeth, however the Nuttall list includes both the twin tops resulting in the higher top being called Gallt y Daren and the lower top called Foel Boeth. The summit is grassy and is marked by a small pile of stones.Nuttall, John & Anne (1999). The Mountains of England & Wales - Volume 1: Wales (2nd edition ed.). Milnthorpe, Cumbria: Cicerone. . References Nuttalls Mountains and hills of Snowdonia Llanuwchllyn Mountains and hills of Gwynedd Trawsfynydd {{Gwynedd-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Llyn Celyn
Llyn Celyn () is a reservoir constructed between 1960 and 1965 in the valley of the River Tryweryn in Gwynedd, Wales. It measures roughly long by wide, and has a maximum depth of . It has the capacity to hold of water. It was originally to be named ''Llyn Tryweryn Mawr'' (meaning "great Tryweryn lake"), but in September 1964 Liverpool Corporation agreed to the name change following a letter from the Tryweryn Defence Committee. Construction and opposition Construction of the reservoir for Liverpool Corporation Waterworks involved flooding the village of Capel Celyn and adjacent farmland, a deeply controversial move. Much of the opposition was brought about because the village was a stronghold of Welsh culture and the Welsh language, whilst the reservoir was being built to supply water to Liverpool and parts of the Wirral peninsula, rather than Wales. Liverpool Corporation's Tryweryn Reservoir Bill was presented in Parliament as a private bill in January 1957; by obtain ... [...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] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waun Garnedd Y Filiast
Waun Garnedd-y-filiast is a top of Carnedd y Filiast on the border of the Snowdonia National park near Cerrigydrudion in North Wales. It is part of the Arenig mountain range. It is also a peak in an area of moorland known as the Migneint. The summit is marked by a few stones in an area of peat hags on a small plateau of bog. Foel Goch (Arenigs), Carnedd Llechwedd-llyfn Carnedd Llechwedd-llyfn is a subsidiary summit of Carnedd y Filiast on the border of Snowdonia National Park in Llandderfel, in Gwynedd. The northern slopes of the peak lie in Ysbyty Ifan, in Conwy. It is part of the Arenig mountain range ... and Mwdwl-eithin can be seen. The top was not included in the Nuttall's original list. However, in 1999 it was surveyed to have the following re-ascent 15.1295 m (49 ft 7.5in). Controversy arose due to it not being quite 50 ft. Some walkers choose only to include it in a Metric list along with 600–608 m sub Hewitt summits. However, most walkers r ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arenig Fawr
Arenig Fawr ( en, Great High Ground) is a mountain in Snowdonia, North Wales, close to Llyn Celyn reservoir, alongside the A4212 between Trawsfynydd and Bala. Location Arenig Fawr is the highest member of the Arenig range, with Arenig Fach ( en, Small High Ground), a smaller neighbouring mountain, lying to the north. It is surrounded by Moel Llyfnant to the west, Rhobell Fawr to the south and Mynydd Nodol to the east. Ascent The easy-to-moderate climb to the summit takes about 2½ hours from Llyn Celyn. There are no readily identifiable footpaths but the route is marked by an old wire boundary fence. Beneath the mountain is Llyn Arenig Fawr, a reservoir providing drinking water to Bala and the surrounding villages. The summit, which is also known as Moel yr Eglwys ( en, Bare hill of the church), has a trig point and a memorial to eight American aircrew who died when their Flying Fortress bomber B-17F #42-3124 crashed on 4 August 1943. Some of the crash wreckage is still sca ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arenig Fach
Arenig Fach is a mountain in southern Snowdonia, north Wales. It is a peak in the Arenig range and lies to the north of its parent peak Arenig Fawr. It lies close to Llyn Celyn alongside the A4212 between Trawsfynydd and Bala. Carnedd y Filiast and Foel Goch (Arenigs) is to the east, while Moel Llyfnant, Gallt y Daren and Arenig Fawr are to the south. The summit itself is known as Carnedd Bachgen, named after the ancient cairn, ''Carnedd y Bachgen'' (which lies just north-east of the summit), and is the highest point at the north end of a wide plateau. There is a trig point and a substantial shelter cairn. The mountain rises from the Migneint The Migneint () is a large expanse of moorland in central Snowdonia, north-west Wales. It is part of the ''Migneint-Arenig-Dduallt'' Special Area of Conservation, along with the mountains Arenig Fawr, Arenig Fach and Dduallt, covering a range of ... moorland and looks like a bulky heathery "lump" from most directions. However, its ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Migneint
The Migneint () is a large expanse of moorland in central Snowdonia, north-west Wales. It is part of the ''Migneint-Arenig-Dduallt'' Special Area of Conservation, along with the mountains Arenig Fawr, Arenig Fach and Dduallt, covering a range of nearly . It is either the largest area of blanket bog in Wales, or the second largest, after the Berwyn range, further to the east. The area includes a few small lakes, including Llyn Conwy, the source of the River Conwy, and is bisected by the B4407 road from Ffestiniog to Ysbyty Ifan. Plans have been suggested to hold water on the Migneint for longer, to help prevent flooding in the Conwy valley , name_etymology = , image = Boats in River Conwy.jpg , image_size = 300 , image_caption = Boats in the river estuary at Conwy , map = , map_size = , map_caption = , push ...; but local farmers have voiced concern that this could be harmful to livestock. References ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arenig
In geology, the Arenig (or Arenigian) is a time interval during the Ordovician period and also the suite of rocks which were deposited during this interval. History The term was first used by Adam Sedgwick in 1847 with reference to the "Arenig Ashes and Porphyries" in the neighbourhood of Arenig Fawr, in Merioneth, North Wales. The rock-succession in the Arenig district has been recognized by W. G. Fearnsides (“On the Geology of Arenig Fawr and Moel Llanfnant", Q.J.G.S. vol. lxi., 1905, pp. 608–640, with maps). The above succession is divisible into: # A lower series of gritty and calcareous sediments, the "Arenig Series" as it is now understood; # A middle series, mainly volcanic, with shale, the "Llandeilo Series"; and # The shale and limestones of the Bala or Caradoc Stage. It was to the middle series (2) that Sedgwick first applied the term "Arenig". In the typical region and in North Wales generally the Arenig series appears to be unconformable upon the Cambri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carnedd Y Filiast (Cerrigydrudion)
Carnedd y Filiast is a mountain near Cerrigydrudion on the border of the Snowdonia National Park, North Wales and is high. Location Carnedd y Filiast is part of the Arenig mountain range, and rises from the shore of Llyn Celyn. It is also a peak in an area of moorland known as the Migneint. The Conwy/Gwynedd boundary passes through the summit. Summit View From the summit, with good weather conditions, it is possible to see several notable mountains and mountain ranges: Arenig Fach and the Rhinogs in the west, with the Llŷn Peninsula and Bardsey Island in the far distance. Snowdon, Moel Siabod, the Great Orme and the Carneddau to the northwest, the Clwydian Range and Moel Famau to the northeast, east to the Berwyns, south west to Aran Fawddwy, and southward to Bala Lake, Rhobell Fawr and Arenig Fawr. In exceptional conditions the Isle of Man, the Blackpool Tower, summits of the Lake District, the Winter Hill Transmitter, and the Peak District can also be seen. The furt ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
