Cornwall is a historic county and ceremonial county in South West England. It is recognised as one of the Celtic nations, and is the homeland of the Cornish people. Cornwall is bordered to the north and west by the Atlantic Ocean, to the south by the English Channel, and to the east by the county of Devon, with the River Tamar forming the border between them. Cornwall forms the westernmost part of the South West Peninsula of the island of Great Britain. The southwesternmost point is Land's End and the southernmost Lizard Point. Cornwall has a population of 568,210 and an area of 3,563 km2 (1,376 sq mi). The county has been administered since 2009 by the unitary authority, Cornwall Council. The ceremonial county of Cornwall also includes the Isles of Scilly, which are administered separately. The administrative centre of Cornwall is Truro, its only city.
Perranporth is a seaside resort town on the north coast of Cornwall, England, United Kingdom. It is 1 mile east of the St Agnes Heritage Coastline, and around 8 miles south-west of Newquay. Perranporth and its 2 miles (3 km) long beach face the Atlantic Ocean. It has a population of 3,066, and is the largest settlement in the civil parish of Perranzabuloe. It has an electoral ward in its own name, whose population was 4,270 in the 2011 census.
North Cornwall is an area of Cornwall, England, United Kingdom. It is also the name of a former local government district, which was administered from Bodmin and Wadebridge 50.516°N 4.835°W. Other towns in the area are Launceston, Bude, Padstow, and Camelford.
Mount's Bay is a large, sweeping bay on the English Channel coast of Cornwall, United Kingdom, stretching from the Lizard Point to Gwennap Head. In the north of the bay, near Marazion, is St Michael's Mount; the origin of name of the bay. In summer, it is a large, benign, scenic, natural harbour. However, in winter, onshore gales present maritime risks, particularly for sailing ships. There are more than 150 known wrecks from the nineteenth century in the area. The eastern side of the bay centred around Marazion and St Michael's Mount was designated as a Marine Conservation Zone in January 2016.
Porthtowan is a small village in Cornwall, England which is a popular summer tourist destination. Porthtowan is on Cornwall's north Atlantic coast about 2 km (1.2 mi) west of St Agnes, 4 km (2.5 mi) north of Redruth, 10 km (6.2 mi) west of Truro and 15 km (9.3 mi) southwest of Newquay in the Cornwall and West Devon Mining Landscape, a World Heritage Site.
Crackington Haven is a coastal village in Cornwall, England, United Kingdom. It is in the civil parish of St Gennys at grid reference SX140972 at the head of a cove on the Atlantic coast. The village is seven miles (11 km) south-southwest of Bude and four miles (7 km) north-northeast of Boscastle.
Aire Point to Carrick Du SSSI is a Site of Special Scientific Interest on the Penwith Peninsula, Cornwall, England. It is 5.98 square kilometres in extent, stretching from grid reference SW360279 to grid reference SW513410. The site is designated both for its biological and its geological interest.
Geevor Tin Mine, formerly North Levant Mine is a tin mine in the far west of Cornwall, United Kingdom, between the villages of Pendeen and Trewellard. It was operational between 1911 and 1990 during which time it produced about 50,000 tons of black tin. It is now a museum and heritage centre left as a living history of a working tin mine. The museum is an Anchor Point of ERIH, The European Route of Industrial Heritage. Since 2006, the mine has been part of the UNESCO World Heritage Site Cornwall and West Devon Mining Landscape.
Carnewas and Bedruthan Steps is a stretch of coastline located on the north Cornish coast between Padstow and Newquay, in Cornwall, United Kingdom. It is within the parish of St Eval and is part-owned by the National Trust. The trust maintains a shop and café, and the cliff–top views of rocks stretching into the distance along Bedruthan beach make the area a popular attraction for tourists and painters. The property affords walks along the coast path and the steep steps at Bedruthan allow access to a series of rocky beaches at low tide. Signs at the top of the steps down to the beaches warn visitors not to risk swimming in these waters due to heavy rips, fast tides, and submerged rocks.
Mining in Cornwall and Devon, in the southwest of England, began in the early Bronze Age, around 2150 BC. Tin, and later copper, were the most commonly extracted metals. Some tin mining continued long after the mining of other metals had become unprofitable, but ended in the late 20th century. In 2021, it was announced that a new mine was extracting battery-grade lithium carbonate, more than 20 years after the closure of the last South Crofty tin mine in Cornwall in 1998.
St Agnes is a civil parish and a large village on the north coast of Cornwall, UK. The village is about five miles (8 km) north of Redruth and ten miles (16 km) southwest of Newquay. An electoral ward exists stretching as far south as Blackwater. The population at the 2011 census was 7,565.
Joseph Carne was a British geologist and industrialist.
The geography of Cornwall describes the extreme southwestern peninsula of England west of the River Tamar. The population of Cornwall is greater in the less extensive west of the county than the east due to Bodmin Moor's location; however the larger part of the population live in rural areas. It is the only county in England bordered by only one other county, Devon, and is the 9th largest county by area, encompassing 3,563 km² (1,376 mi²). The length of the coast is large in proportion to the area of the county. Cornwall is exposed to the full force of the prevailing south-westerly winds that blow in from the Atlantic Ocean. To the north is the Celtic Sea, and to the south the English Channel.
The Cornubian batholith is a large mass of granite rock, formed about 280 million years ago, which lies beneath much of Devon and Cornwall, the south-western peninsula of Great Britain. The main exposed masses of granite are seen at Dartmoor, Bodmin Moor, St Austell, Carnmenellis, Land's End and the Isles of Scilly. The intrusion is associated with significant quantities of minerals particularly cassiterite, an ore of tin which has been mined since about 2000 BC. Other minerals include china clay and ores of copper, lead, zinc and tungsten.
Zennor Head is a 750-metre (2,460 ft) long promontory on the Cornish coast of England, between Pendour Cove and Porthzennor Cove. Facing the Atlantic Ocean, it lies 1 kilometre north-west of the village of Zennor and 1.6 kilometres east of the next promontory, Gurnard's Head. The granite (Killas) cliffs rise over 200 feet (60 m) from the sea and the highest point of the headland is 314 feet (96 m) above sea level, with an Ordnance Survey triangulation station. Zennor Head is on the South West Coast Path, which follows the cliff edge closely, skirting the entire perimeter of the headland. The promontory is part of the Penwith Heritage Coast, and is the largest coastal feature in the United Kingdom that begins with the letter "Z". It gets its name from a local saint, Senara. Zennor Head was mined for copper and tin in the Victorian Era. There is no longer any residential or commercial occupancy on the headland, but it is occupied by a variety of coastal animals and plants, such as kestrels and gorse.
The following outline is provided as an overview of and topical guide to Cornwall: Cornwall – ceremonial county and unitary authority area of England within the United Kingdom. Cornwall is a peninsula bordered to the north and west by the Celtic Sea, to the south by the English Channel, and to the east by the county of Devon, over the River Tamar. Cornwall is also a royal duchy of the United Kingdom. It has an estimated population of half a million and it has its own distinctive history and culture.
Presented below is an alphabetical index of articles related to Cornwall:
The geology of Maine is part of the broader geology of New England and eastern North America.
This article describes the geology of Dartmoor National Park in Devon, in south-west England. Dartmoor gained national park status in 1951 but the designated area of 954 km2 (368 sq mi) extends beyond the upland of Dartmoor itself to include much of the surrounding land, particularly in the northeast. The geology of the national park consists of a 625 km2 (241 sq mi) core of granite intruded during the early Permian period into a sequence of sedimentary rocks originating in the Devonian and Carboniferous periods. These rocks were faulted and folded, sometimes, intensely, during the Variscan orogeny. Thermal metamorphism has also taken place around the margins of the granite pluton altering the character of the sedimentary rocks whilst mineral veins were emplaced within the granite. A small outlier of Palaeogene sediments occurs on the eastern boundary of the national park.
