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Red River, Cornwall

 

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Red River, Cornwall



 
 
The Red River is a small river in north-west Cornwall
Cornwall

Cornwall , constitutional Duchy and palatine, is a metropolitan and non-metropolitan counties of England of England, United Kingdom, located at the tip of the south-western peninsula of Great Britain....
, UK which issues into St Ives Bay
St Ives Bay

St Ives Bay is a bay on the Atlantic coast of north-west Cornwall in the United Kingdom. It is in the form of a shallow crescent, some 4 miles or 6 km across, between St Ives, Cornwall in the west and Godrevy in the east....
 at Godrevy
Godrevy

Godrevy is an area of west Cornwall, United Kingdom, found on the north coast within St. Ives, Cornwall and is popular with both the surfing community and walkers....
 on Cornwall's Atlantic
Atlantic Ocean

The Atlantic Ocean is the second-largest of the world's oceanic divisions; with a total area of about 106.4 million square kilometres . It covers approximately one-fifth of the Earth's surface....
 coast.

The Red River is approx 8 miles (13 kilometres) long and gets its name from the mineral
Mineral

A mineral is a naturally occurring solid formed through Geology processes that has a characteristic chemical composition, a highly ordered atomic structure, and specific physical properties....
 deposits associated with tin mining
Mining in Cornwall

Mining in Cornwall first began in the early Bronze Age approximately 2,150 BC and ended with the South Crofty tin mine closing in 1998....
 which formerly coloured its water red. The river's gradient is relatively steep; it falls 170 metres from source to sea.

The Red River rises from springs near Bolenowe on the Carnmenellis
Carnmenellis

File:Carnmenellis Down.jpgCarnmenellis hill in Cornwall gives its name to the area between Redruth, Helston and Penryn, Cornwall. The term 'Carnmenellis Granite' refers to the plateau of high ground in this area, one of several granite batholiths in Cornwall ....
 granite batholith
Batholith

A batholith is a large emplacement of igneous Intrusion rock that forms from cooled magma deep in the Earth's Crust . Batholiths are almost always made mostly of felsic or intermediate rock-types, such as granite, quartz monzonite, or diorite ....
, an upland plateau (see also Geology of Cornwall
Geology of Cornwall

The Geology of Cornwall is dominated by its granite backbone formed during the Variscan orogeny. Around this is an extensive Metamorphism#Contact metamorphism formed in the mainly Devonian slates that make up most of the rest of the county....
).






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The Red River is a small river in north-west Cornwall
Cornwall

Cornwall , constitutional Duchy and palatine, is a metropolitan and non-metropolitan counties of England of England, United Kingdom, located at the tip of the south-western peninsula of Great Britain....
, UK which issues into St Ives Bay
St Ives Bay

St Ives Bay is a bay on the Atlantic coast of north-west Cornwall in the United Kingdom. It is in the form of a shallow crescent, some 4 miles or 6 km across, between St Ives, Cornwall in the west and Godrevy in the east....
 at Godrevy
Godrevy

Godrevy is an area of west Cornwall, United Kingdom, found on the north coast within St. Ives, Cornwall and is popular with both the surfing community and walkers....
 on Cornwall's Atlantic
Atlantic Ocean

The Atlantic Ocean is the second-largest of the world's oceanic divisions; with a total area of about 106.4 million square kilometres . It covers approximately one-fifth of the Earth's surface....
 coast.

The Red River is approx 8 miles (13 kilometres) long and gets its name from the mineral
Mineral

A mineral is a naturally occurring solid formed through Geology processes that has a characteristic chemical composition, a highly ordered atomic structure, and specific physical properties....
 deposits associated with tin mining
Mining in Cornwall

Mining in Cornwall first began in the early Bronze Age approximately 2,150 BC and ended with the South Crofty tin mine closing in 1998....
 which formerly coloured its water red. The river's gradient is relatively steep; it falls 170 metres from source to sea.

The Red River rises from springs near Bolenowe on the Carnmenellis
Carnmenellis

File:Carnmenellis Down.jpgCarnmenellis hill in Cornwall gives its name to the area between Redruth, Helston and Penryn, Cornwall. The term 'Carnmenellis Granite' refers to the plateau of high ground in this area, one of several granite batholiths in Cornwall ....
 granite batholith
Batholith

A batholith is a large emplacement of igneous Intrusion rock that forms from cooled magma deep in the Earth's Crust . Batholiths are almost always made mostly of felsic or intermediate rock-types, such as granite, quartz monzonite, or diorite ....
, an upland plateau (see also Geology of Cornwall
Geology of Cornwall

The Geology of Cornwall is dominated by its granite backbone formed during the Variscan orogeny. Around this is an extensive Metamorphism#Contact metamorphism formed in the mainly Devonian slates that make up most of the rest of the county....
). The river flows north, passing through a gorge in the granite ridge west of Carn Brea
Carn Brea

Carn Brea is a civil parish and hilltop site near Redruth in Cornwall, England, United Kingdom, famous for its long history of human occupation....
. Beyond the gorge, the river passes Tuckingmill
Tuckingmill

The parish of Tuckingmill was constituted in 1845 being carved out of a western section of the parish of Illogan and an easterly section of Camborne parish and it covers 1,300 acres....
, once a centre of mining and associated industries. At the hamlet of Combe, the Tehidy
Tehidy Country Park

Tehidy Country Park is located near Camborne, Redruth and Portreath. It was once part of a created estate that was owned by the wealthy Basset Tin mining family....
 Stream joins the Red River which then turns west towards Godrevy.

The Red River's catchment area includes the major mining areas of Tuckingmill, Pool
Pool, Cornwall

Pool is a village in Kerrier district, Cornwall between Redruth and Camborne.Cornwall College is based here.The Cornish Main Line railway passes through the village....
, and Camborne
Camborne

Camborne was once one of the richest mining areas in the world and is located in north Kerrier, Cornwall in the United Kingdom, forming the western end of the greater Camborne, Pool, Cornwall and Redruth conurbation....
. Thus:
"The Red River catchment has been subjected to mining and mineral working for many centuries, particularly during the eighteenth and nineteenth centuries. It has been extensively tin streamed and its water used for mineral processing, both for use in the mineral separation processes and as a source of power. As a result of past mining activities the river has undergone many modifications and for significant parts of its course the river has been diverted, canalised, and, in places, embanked. Very little, if any, of the river can be considered to be in a truly natural condition." Quoted from


Since mining finished, the Red River has lost its distinctive colour and natural ecology and biodiversity are re-establishing.

The river gives its name to the Red River Inn public house (formerly The Pendarves Arms) in nearby Gwithian
Gwithian

Gwithian is a village in the parish of Gwinear-Gwithian, located in the district of Penwith, in Cornwall, UK. It is located to the east side of St Ives Bay....
.