Manod Mawr North Top | |
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![]() Manod Mawr North Top from Manod Mawr | |
Highest point | |
Elevation | 658 m (2,159 ft) |
Prominence | 65 m (213 ft) |
Listing | Hewitt, Nuttall |
Naming | |
English translation | great snowdrift |
Language of name | Welsh |
Pronunciation | Welsh: [ˈmanɔd ˈmauɾ] |
Geography | |
Location | Gwynedd, Wales |
Parent range | Moelwynion |
Topo map | OS Landranger 124 |
Manod Mawr North Top is a mountain in North Wales and forms part of the Moelwynion.
A mountain is a large landform that rises above the surrounding land in a limited area, usually in the form of a peak. A mountain is generally steeper than a hill. Mountains are formed through tectonic forces or volcanism. These forces can locally raise the surface of the earth. Mountains erode slowly through the action of rivers, weather conditions, and glaciers. A few mountains are isolated summits, but most occur in huge mountain ranges.
North Wales is an unofficial region of Wales. Retail, transport and educational infrastructure are centred on Wrexham, Rhyl, Colwyn Bay, Llandudno and Bangor. It is bordered to the rest of Wales with the counties of Ceredigion and Powys, and to the east by the English counties of Shropshire, Merseyside, and Cheshire. People from North Wales are sometimes referred to as "Gogs", derived from "gogledd" - the Welsh for "north".
The Moelwynion 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 the two largest mountains in the group, Moelwyn Mawr and Moelwyn Bach.
It lies directly to the north of its parent Manod Mawr, separated by the Graig Ddu Quarry. Crossing the quarry to reach the main summit can be dangerous. There are also a few mine adits on the northern slopes. [1] There were fears that the top may eventually be removed.
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.
Graig Ddu Quarry is a disused slate quarry in North Wales, originally opened as Manod Quarry in about 1800, but developed as Graig Ddu in the 1840s. Although output was only about 3,000 tons a year, it reputedly has 36 saw tables and the same number of dressing machines on site. As with others in the area, the quarry suffered from a lack of water, resulting in the siting of the mill some distance away, at a lower level.
Blaenau Ffestiniog is a historic mining town in Wales, in the historic county of Merionethshire, although now part of the unitary authority of Gwynedd. The population of the community of Ffestiniog was 4,875 according to the 2011 census, including the nearby village of Llan Ffestiniog, which makes it the fourth most populous community in Gwynedd, after Bangor, Caernarfon, and Llandeiniolen. Llan Ffestiniog's population of 864 puts the population of Blaenau itself at around 4,000. Blaenau Ffestiniog was at one time the second largest town in North Wales, behind only Wrexham. After reaching 12,000 at the peak development of the slate industry, the population fell with the decline in the demand for its slate. Today the town relies heavily on tourists, who come for attractions that include the nearby Ffestiniog Railway and Llechwedd Slate Caverns.
Penmaenmawr is a town and community in Conwy County Borough, Wales, which was formerly in the parish of Dwygyfylchi. It is on the North Wales coast between Conwy and Llanfairfechan and was an important quarrying town, though quarrying is no longer a major employer. The population of the community was 4,353 in 2011, including Dwygyfylchi and Capelulo. The town itself having a population of 2,868 (2011).
Tanygrisiau is a village and area within Blaenau Ffestiniog in the upper end of the Vale of Ffestiniog in the county of Gwynedd, north-west Wales. It can be found along the southern side of the Moelwyn mountain range and dates to around 1750. It joins onto the semi-urban area of Blaenau Ffestiniog, and is in the community of Ffestiniog; located between 650 feet (200 m) and 750 feet (230 m) above sea level.
The Croesor Tramway was a Welsh, 2 ft narrow gauge railway line built to carry slate from the Croesor slate mines to Porthmadog. It was built in 1864 without an Act of Parliament and was operated using horse power.
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.
Craigysgafn is a rocky ridge and a top of Moelwyn Mawr that leads south from Moelwyn Mawr to Moelwyn Bach in Snowdonia, North Wales. It has several gullies which lead directly down to the scree slopes above Llyn Stwlan. Some scrambling is needed in places.
Moel-yr-hydd is a subsidiary summit of Moelwyn Mawr in Snowdonia, North Wales and forms part of the Moelwynion.
Moel Penamnen is a mountain just north of Blaenau Ffestiniog, North Wales and forms part of the Moelwynion.
Rumney is a district and community in the east of the city of Cardiff, Wales. It lies east of the Rhymney River, and is historically part of Monmouthshire. On 1 April 1938 the Cardiff Extension Act 1937 incorporated it into the county borough of Cardiff, although it remained part of Monmouthshire, and England.
Y Fron, also known locally as Cesarea, after the chapel, is a country village on the south-west side of Moel Tryfan, overlooking the Nantlle Valley, in North Wales, near Rhosgadfan and Carmel, on the tail of Mynydd Mawr, with epic views of Trum Y Ddysgl and Craig Cwm Silyn. It is in the community of Llandwrog.
Tan-y-Manod railway station was just under one route mile south of the present day Blaenau Ffestiniog station in what was then Merionethshire, now Gwynedd, Wales.
Moelwyn Mawr North Ridge Top is a top of Moelwyn Mawr in Snowdonia, North Wales and forms part of the Moelwynion. From its summit, which directly overlooks Bwlch Rhosydd, can be seen Cnicht, Allt-fawr and Moel-yr-hydd. A recently discovered 'top' has only received attention from Nuttall baggers.
Y Ro Wen is a mountain just north of Blaenau Ffestiniog, North Wales and forms part of the Moelwynion.
Y Gamallt is a mountain located in the Migneint in Snowdonia, North Wales. It forms part of the Arenig mountain range being separated from the Moelwynion range at the head of Cwm Teigl.
The car gwyllt is a Welsh invention used by quarrymen to ride downhill on the steep inclined planes of a slate quarry.
Fron-Boeth and Pant Mawr Quarries were two closely related and interconnected quarries on the western slopes of Moelwyn Mawr in Gwynedd, North Wales. Pant Mawr operated from around 1850 to 1879, and was partly re-opened in 1886 when it was amalgamated with Fron-Boeth. Both quarries closed during the First World War. Finished product was transported to the slate quays of Porthmadog by the Croesor Tramway.
Mawr is a community in south Wales. Mawr means big or great in Welsh and may also refer to the following Wales-related topics:
Coordinates: 52°59′01″N3°54′13″W / 52.98348°N 3.90360°W
A geographic coordinate system is a coordinate system that enables every location on Earth to be specified by a set of numbers, letters or symbols. The coordinates are often chosen such that one of the numbers represents a vertical position and two or three of the numbers represent a horizontal position; alternatively, a geographic position may be expressed in a combined three-dimensional Cartesian vector. A common choice of coordinates is latitude, longitude and elevation. To specify a location on a plane requires a map projection.
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