Bodmin Moor (Cornish: Goen Bren) is a granite moorland in northeastern Cornwall, England, United Kingdom. It is 208 square kilometres (80 sq mi) in size, and originally dates from the Carboniferous period of geological history.
Bodmin Moor is one of five granite plutons in Cornwall that make up part of the Cornubian batholith (see also Geology of Cornwall).
The name 'Bodmin Moor' is relatively recent, being an Ordnance Survey invention of 1813. I...
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Bodmin Moor (Cornish: Goen Bren) is a granite moorland in northeastern Cornwall, England, United Kingdom. It is 208 square kilometres (80 sq mi) in size, and originally dates from the Carboniferous period of geological history.
Bodmin Moor is one of five granite plutons in Cornwall that make up part of the Cornubian batholith (see also Geology of Cornwall).
The name 'Bodmin Moor' is relatively recent, being an Ordnance Survey invention of 1813. It was formerly known as Fowey Moor after the River Fowey which rises within it.
Dramatic granite tors rise from the rolling moorland: the best known are Brown Willy, the highest point in Cornwall at 417 m (1,368 ft), and Rough Tor at 400 m (1,300 ft). To the south-east Kilmar Tor and Caradon Hill are the most prominent hills. Considerable areas of the moor are poorly drained and form marshes (in hot summers these can dry out). The rest of the moor is mostly rough pasture or overgrown with heather and other low vegetation.
The Moor contains...
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