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Croesor Tramway

2 ft gauge railways in WalesHorse-drawn railwaysIndustrial railways in WalesRailway inclines in WalesRailway lines closed in 1948
Railway lines opened in 1864Railway lines opened in 2010Slate industry in WalesUse British English from March 2018Welsh Highland Railway
CroesorTramwayTrackbbed
CroesorTramwayTrackbbed

The Croesor Tramway was a Welsh, 2 ft (610 mm) 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. The tramway was absorbed into the Croesor and Port Madoc Railway in 1865 and later became the Portmadoc, Croesor and Beddgelert Tram Railway in 1879. Part of its route, from Croesor Junction to Porthmadog, was taken over by the Welsh Highland Railway in 1922, and upgraded to allow the operation of steam locomotives. The remainder of the line continued as a horse-drawn tramway, and operated as such until the mid-1940s.

Excerpt from the Wikipedia article Croesor Tramway (License: CC BY-SA 3.0, Authors, Images).

Geographical coordinates (GPS)

Latitude Longitude
N 52.981944444444 ° E -4.0402777777778 °
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Address


LL48 6SR , Llanfrothen
Wales, United Kingdom
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CroesorTramwayTrackbbed
CroesorTramwayTrackbbed
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Nearby Places

Yr Arddu (South)
Yr Arddu (South)

Yr Arddu is a large hill in Snowdonia, Wales (Not to be confused with the 589 metre Yr Arddu (North) to the east of Snowdon). It lies approximately 2.5 km south east of the village of Beddgelert and just over 1 km from the rather more famous mountain Cnicht. It is a rugged hill with widespread rock outcrops and cliffs. A small lake, Llyn yr Arddu, is located on the flanks of the mountain. The recognised summit is at 388m to the South of the hill, but the highest point, named Cerrig-y-Myllt on only the most detailed UK Ordnance Survey mapping, is at 463m above the two small lakes to the North of the hill. The craggy nature of the hill is due to the presence of lavas and tuffs (volcanic ash deposits) dating from the Ordovician period when Snowdonia was characterised by numerous volcanic eruptions; Yr Arddu is a particularly good location to see the record of Ordovician volcanism. The Yr Arddu Tuffs may be the earliest eruptive phase of the Lower Rhyolitic Tuff Formation.The whole hill is a site of special scientific interest designated by the Countryside Council for Wales.Yr Arddu is commonly approached by a footpath leaving the minor road that links Nantmor to Nant Gwynant running along the valley of Blaen Nanmor, but the final 0.5 km has no paths marked on UK Ordnance Survey mapping. However, a marked path runs South East from Nantmor Mountain Centre at Gelli-Iago. From this an intermittent rough path runs from West of Clogwyn Coch up to the two small lakes. The hill can also be approached with more difficulty from its West flank up to the small lake Llyn yr Arddu.