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Phoenix United Mine

1836 establishments in England1914 disestablishments in EnglandBodmin MoorBritish companies disestablished in 1914British companies established in 1836
Copper mines in CornwallEnergy companies established in 1836Non-renewable resource companies disestablished in 1914Non-renewable resource companies established in 1836Sites of Special Scientific Interest in CornwallSites of Special Scientific Interest notified in 1996Special Areas of Conservation in CornwallTin mines in CornwallUse British English from February 2023
Phoenix United mine
Phoenix United mine

Phoenix United Mine is a disused 19th century copper and tin mine in Cornwall, England, UK. Heavy metals left over in the soil from the mining operations have allowed mosses and lichens to flourish, and today the site is a Site of Special Scientific Interest (SSSI), noted for its biological characteristics. All of the land designated as Phoenix United Mine SSSI is owned by the Duchy of Cornwall.

Excerpt from the Wikipedia article Phoenix United Mine (License: CC BY-SA 3.0, Authors, Images).

Geographical coordinates (GPS)

Latitude Longitude
N 50.5261 ° E -4.4471 °
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Address


PL14 5BP
England, United Kingdom
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Phoenix United mine
Phoenix United mine
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Nearby Places

Cheesewring
Cheesewring

The Cheesewring (Cornish: Keuswask) is a granite tor in Cornwall, England, situated on the eastern flank of Bodmin Moor on Stowe's Hill in the parish of Linkinhorne approximately one mile northwest of the village of Minions and four miles (6 km) north of Liskeard. It is a natural geological formation, a rock outcrop of granite slabs formed by weathering. The name derives from the resemblance of the piled slabs to a stack of "cheeses" in a traditional cider press. Wilkie Collins described the Cheesewring in 1861 in his book Rambles Beyond Railways: If a man dreams of a great pile of stones in a nightmare, he would dream of such a pile as the Cheesewring. All the heaviest and largest of the seven thick slabs of which it is composed are at the top; all the lightest and smallest at the bottom. It rises perpendicularly to a height of thirty-two feet, without lateral support of any kind. The fifth and sixth rocks are of immense size and thickness, and overhang fearfully all round the four lower rocks which support them. All are perfectly irregular; the projections of one do not fit into the interstices of another; they are heaped up loosely in their extraordinary top-heavy form on slanting ground, half way down a steep hill. Located adjacent to the Cheesewring Quarry (which supplied the granite cladding for the structure of Tower Bridge, London) and surrounded by other granite formations, this landmark was threatened with destruction in the late nineteenth century by the proximity of blasting operations, but was saved as a result of local activism.