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Aberglaslyn Pass
The Aberglaslyn Pass ( cy, Bwlch Aberglaslyn) is a narrow gorge of considerable beauty in Snowdonia, Gwynedd, north Wales. The A498 road/A4085 road follows a relatively level route along the Afon Glaslyn through the pass from Beddgelert to Prenteg and then continues at the edge of the Traeth Mawr via Tremadog to Porthmadog. River pass As recently as the early 19th century, the river Glaslyn was navigable for small boats at high tide as far as Pont Aberglaslyn, which is just south of Beddgelert, where a sixth-century monastery was succeeded in the twelfth by an Augustinian priory. In the Middle Ages Beddgelert was seen as a safe resting place before travelling further. The route from the coast via Beddgelert and overland to Caernarfon or Bangor via Llyn Cwellyn was often considered preferable to the long voyage round the Llŷn Peninsula. Edmund Vale: Snowdonia, National Park Guide Number 2 HMSO 1958/1960 (page 75) Pont Aberglaslyn is in the parish of Nantmor. From here t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aberglaslyn Pass
The Aberglaslyn Pass ( cy, Bwlch Aberglaslyn) is a narrow gorge of considerable beauty in Snowdonia, Gwynedd, north Wales. The A498 road/A4085 road follows a relatively level route along the Afon Glaslyn through the pass from Beddgelert to Prenteg and then continues at the edge of the Traeth Mawr via Tremadog to Porthmadog. River pass As recently as the early 19th century, the river Glaslyn was navigable for small boats at high tide as far as Pont Aberglaslyn, which is just south of Beddgelert, where a sixth-century monastery was succeeded in the twelfth by an Augustinian priory. In the Middle Ages Beddgelert was seen as a safe resting place before travelling further. The route from the coast via Beddgelert and overland to Caernarfon or Bangor via Llyn Cwellyn was often considered preferable to the long voyage round the Llŷn Peninsula. Edmund Vale: Snowdonia, National Park Guide Number 2 HMSO 1958/1960 (page 75) Pont Aberglaslyn is in the parish of Nantmor. From here t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Llyn Cwellyn
Llyn Cwellyn (''Llyn Quellyn'' in some antiquated texts) is a reservoir in North Wales which supplies drinking water to parts of Gwynedd and Anglesey. It lies on the Afon Gwyrfai in Nant y Betws between Moel Eilio and Mynydd Mawr in the northern part of Snowdonia National Park. It has an area of , and is over deep. At the southern end is the small village of Rhyd Ddu. Although it is now dammed at the northern end, below the Castell Cidwm ridge, near the village of Betws Garmon this has not substantially increased the size of the natural glacial moraine lake that has existed since the last ice age. The lake is very deep and is one of the few lakes in Wales to support a natural population of Arctic char. The lake also is home to brown trout and there are otters that are regularly seen at the Castell Cidwm end. The lake has shared ownership between Lawrence Jones (businessman) owner of the Castell Cidwm estate at the Northern end and Welsh water, who own the right hand side that ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Passes 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Passes 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] |
Canyons And Gorges Of Snowdonia
A canyon (from ; archaic British English spelling: ''cañon''), or gorge, is a deep cleft between escarpments or cliffs resulting from weathering and the erosive activity of a river over geologic time scales. Rivers have a natural tendency to cut through underlying surfaces, eventually wearing away rock layers as sediments are removed downstream. A river bed will gradually reach a baseline elevation, which is the same elevation as the body of water into which the river drains. The processes of weathering and erosion will form canyons when the river's headwaters and estuary are at significantly different elevations, particularly through regions where softer rock layers are intermingled with harder layers more resistant to weathering. A canyon may also refer to a rift between two mountain peaks, such as those in ranges including the Rocky Mountains, the Alps, the Himalayas or the Andes. Usually, a river or stream carves out such splits between mountains. Examples of mountain-type c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canyons And Gorges Of Gwynedd
A canyon (from ; archaic British English spelling: ''cañon''), or gorge, is a deep cleft between escarpments or cliffs resulting from weathering and the erosive activity of a river over geologic time scales. Rivers have a natural tendency to cut through underlying surfaces, eventually wearing away rock layers as sediments are removed downstream. A river bed will gradually reach a baseline elevation, which is the same elevation as the body of water into which the river drains. The processes of weathering and erosion will form canyons when the river's headwaters and estuary are at significantly different elevations, particularly through regions where softer rock layers are intermingled with harder layers more resistant to weathering. A canyon may also refer to a rift between two mountain peaks, such as those in ranges including the Rocky Mountains, the Alps, the Himalayas or the Andes. Usually, a river or stream carves out such splits between mountains. Examples of mountain-type c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
National Trust For Places Of Historic Interest Or Natural Beauty
The National Trust, formally the National Trust for Places of Historic Interest or Natural Beauty, is a charity and membership organisation for heritage conservation in England, Wales and Northern Ireland. In Scotland, there is a separate and independent National Trust for Scotland. The Trust was founded in 1895 by Octavia Hill, Sir Robert Hunter and Hardwicke Rawnsley to "promote the permanent preservation for the benefit of the Nation of lands and tenements (including buildings) of beauty or historic interest". It was given statutory powers, starting with the National Trust Act 1907. Historically, the Trust acquired land by gift and sometimes by public subscription and appeal, but after World War II the loss of country houses resulted in many such properties being acquired either by gift from the former owners or through the National Land Fund. Country houses and estates still make up a significant part of its holdings, but it is also known for its protection of wild lands ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ffestiniog Railway
The Ffestiniog Railway ( cy, Rheilffordd Ffestiniog) is a heritage railway based on narrow-gauge, located in Gwynedd, Wales. It is a major tourist attraction located mainly within the Snowdonia National Park. The railway is roughly long and runs from the harbour at Porthmadog to the slate mining town of Blaenau Ffestiniog, travelling through forested and mountainous terrain. The line is single track throughout with four intermediate passing places. The first mile of the line out of Porthmadog runs atop an embankment called ''the Cob'', which is the dyke of the polder known as Traeth Mawr. The Festiniog Railway Company, which owns the railway, is the oldest surviving railway company in the world. It also owns the Welsh Highland Railway, which was re-opened fully in 2011. The two railways share the same track gauge and meet at Porthmadog station, with occasional trains working the entire route from Blaenau Ffestiniog to Caernarfon. History The railway company is prope ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dinas, Gwynedd
Dinas is a large hamlet near Bontnewydd, Caernarfon, in Gwynedd, north-west Wales. It is in the ancient parish and modern community of Llanwnda and is served by the parish church of St. Gwyndaf in Llanwnda village, which is about a quarter of a mile to the south. The hamlet developed with the opening of the turnpike Toll roads from Caernarfon first to Pwllheli in 1805, then to Porthmadog in 1810. Two coaching inns were built to serve the roads, Y Mount, which is now an Indian restaurant and Tafarn Hen, which is now a private residence. The Carnarvonshire Railway was built in 1866 on the route of the horse drawn Nantlle Railway. The building in 1878 of the North Wales Narrow Gauge Railways (later part of the Welsh Highland Railway) resulted in the opening of Dinas Junction station complete with slate transshipment facilities, which brought the construction of houses for the railway staff. The 20th century saw the development of suburban housing for Caernarfon. The present Dina ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Welsh Highland Railway
The Welsh Highland Railway (WHR) or Rheilffordd Eryri is a long, restored narrow gauge heritage railway in the Welsh county of Gwynedd, operating from Caernarfon to Porthmadog, and passing through a number of popular tourist destinations including Beddgelert and the Aberglaslyn Pass. At Porthmadog it connects with the Ffestiniog Railway and to the short Welsh Highland Heritage Railway. In Porthmadog it uses the United Kingdom's only mixed gauge flat rail crossing. The restoration, which had the civil engineering mainly built by contractors and the track mainly built by volunteers, received a number of awards. Originally running from , near Caernarfon, to ,Boyd (1972), pages=283 the current line includes an additional section from Dinas to Caernarfon. The original line also had a branch to and the slate quarries around Moel Tryfan, which has not been restored. (This branch forms a footpath "rail trail", the lower section of which has been resurfaced and supplied with heri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cambrian Railways
The Cambrian Railways owned of track over a large area of mid Wales. The system was an amalgamation of a number of railways that were incorporated in 1864, 1865 and 1904. The Cambrian connected with two larger railways with connections to the northwest of England via the London and North Western Railway, and the Great Western Railway for connections between London and Wales. The Cambrian Railways amalgamated with the Great Western Railway on 1 January 1922 as a result of the Railways Act 1921. The name is continued today in the route known as the Cambrian Line. History Creation of the Cambrian Railways: 1864 The Cambrian Railways Company was created on 25 July 1864 when the Cambrian Railways Act of Parliament received Royal Assent. The company was formed by amalgamating most of the railway companies in mid Wales: the Oswestry and Newtown Railway, the Llanidloes and Newtown Railway, the Newtown and Machynlleth Railway and the Oswestry, Ellesmere and Whitchurch Railway. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Welsh Highland Railway At Aberglaslyn - Geograph
Welsh may refer to: Related to Wales * Welsh, referring or related to Wales * Welsh language, a Brittonic Celtic language spoken in Wales * Welsh people People * Welsh (surname) * Sometimes used as a synonym for the ancient Britons (Celtic people) Animals * Welsh (pig) Places * Welsh Basin, a basin during the Cambrian, Ordovician and Silurian geological periods * Welsh, Louisiana, a town in the United States * Welsh, Ohio, an unincorporated community in the United States See also * Welch (other) * * * Cambrian + Cymru Wales ( cy, Cymru ) is a country that is part of the United Kingdom. It is bordered by England to the east, the Irish Sea to the north and west, the Celtic Sea to the south west and the Bristol Channel to the south. It had a population in 202 ... {{Disambiguation Language and nationality disambiguation pages ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
