Tor Enclosure
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Tor Enclosure
A tor enclosure is a prehistoric monument found in the southwestern part of Great Britain. These monuments emerged around 4000 BCE in the early Neolithic. Tor enclosures are large enclosures situated near natural rock outcrops, especially tors, on hilltops or the sides of hills. They consist of one or more roughly circular stone walls built around the tor. They are comparable to the causewayed enclosures found elsewhere in the British Isles and many are of similar Neolithic date although others are from later in prehistory. Examples The best known examples are Carn Brea in Cornwall, the first to be identified, following excavations in the early 1970s, and Helman Tor between Bodmin and Lostwithiel in the same county. Other possible examples are: * Rough Tor on Bodmin Moor, Cornwall * Stowe's Hill, also on Bodmin Moor * Whittor on Dartmoor. See also * Tor cairn A tor cairn is a prehistoric cult site occurring in the British Isles, especially in Cornwall and Devon ...
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Helman Tor
Helman Tor ( kw, Torr Helman) is a granite hill in mid Cornwall, UK with several separated tors, and is designated as a (non-statutory) County Geology Site (with similar criteria to a County Wildlife Site). The hill also has a Scheduled Ancient Monument. Helman Tor is also the name of the nature reserve managed by the Cornwall Wildlife Trust which includes Breney Common (a Special Area of Conservation) and Red Moor. Helman Tor, along with Breney Common, Red Moor and Belowda Beacon, is part of the Mid Cornwall Moors Site of Special Scientific Interest. It lies on the Saints' Way, a long-distance footpath completed in 1986. It is the northern end of a granite ridge. There are at least three rocking stones (logan stone) on the ridge. There is a prehistoric hill fort and a stone hut circle settlement on the site. There is evidence of walls constructed in Neolithic period, around 6,000 years ago, as well as some level platforms, thought to be house sites, one platform has a n ...
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Rough Tor
Rough Tor (), or Roughtor, is a tor on Bodmin Moor, Cornwall, United Kingdom. The site is composed of the tor summit and logan stone, a neolithic tor enclosure, a large number of Bronze Age hut circles, and some contemporary monuments. Toponymy In the 19th-century the hill was known as ''Router''. Geography Rough Tor is approximately one mile northwest of Brown Willy, Cornwall's highest point, on Bodmin Moor. Its summit is 1313 ft (400m) above mean sea level, making it the second highest point in Cornwall. Both hills are in the civil parish of St Breward and near the town of Camelford. The De Lank River rises nearby and flows between the two hills. Rough Tor and Little Rough Tor are twin summits of a prominent ridge of granite, though there are actually three tors at the site: Showery Tor (Also known as Flat Cap Ned), Little Rough Tor, and Rough Tor. Crowdy Reservoir and the Lowermoor Water Treatment Works are not far away from the hill. Hikes to the summit and to ne ...
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Stowe's Hill
Stowe's Hill is an elongated hill, high, located on the eastern edge of Bodmin Moor in the county of Cornwall, England.Ordnance Survey 1:25,000 ''Explorer'' map series, No. 109 Stowe's Hill is a prominent granite ridge located about 1500 metres north of Minions, the highest village in Cornwall. It is dominated by Stowe's Pound, a huge tor enclosure comprising two massive stone-walls. The smaller enclosure surrounds the tors at the southern end of the hill; the larger one encircles the rest of the ridge. At the southern end is a large, disused quarry, but the hill is best known as the site of the Cheesewring, the extraordinary granite formation that gave the quarry its name. Inside Stowe's Pound are two Bronze Age cairns, a stone round house and over 100 house platforms. The site is thought to be Neolithic or Bronze Age The Bronze Age is a historic period, lasting approximately from 3300 BC to 1200 BC, characterized by the use of bronze, the presence of writing in some ...
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Great Britain
Great Britain is an island in the North Atlantic Ocean off the northwest coast of continental Europe. With an area of , it is the largest of the British Isles, the largest European island and the ninth-largest island in the world. It is dominated by a maritime climate with narrow temperature differences between seasons. The 60% smaller island of Ireland is to the west—these islands, along with over 1,000 smaller surrounding islands and named substantial rocks, form the British Isles archipelago. Connected to mainland Europe until 9,000 years ago by a landbridge now known as Doggerland, Great Britain has been inhabited by modern humans for around 30,000 years. In 2011, it had a population of about , making it the world's third-most-populous island after Java in Indonesia and Honshu in Japan. The term "Great Britain" is often used to refer to England, Scotland and Wales, including their component adjoining islands. Great Britain and Northern Ireland now constitute the ...
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Neolithic
The Neolithic period, or New Stone Age, is an Old World archaeological period and the final division of the Stone Age. It saw the Neolithic Revolution, a wide-ranging set of developments that appear to have arisen independently in several parts of the world. This "Neolithic package" included the introduction of farming, domestication of animals, and change from a hunter-gatherer lifestyle to one of settlement. It began about 12,000 years ago when farming appeared in the Epipalaeolithic Near East, and later in other parts of the world. The Neolithic lasted in the Near East until the transitional period of the Chalcolithic (Copper Age) from about 6,500 years ago (4500 BC), marked by the development of metallurgy, leading up to the Bronze Age and Iron Age. In other places the Neolithic followed the Mesolithic (Middle Stone Age) and then lasted until later. In Ancient Egypt, the Neolithic lasted until the Protodynastic period, 3150 BC.Karin Sowada and Peter Grave. Egypt in th ...
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Tor (rock)
A tor, which is also known by geomorphologists as either a castle koppie or kopje, is a large, free-standing rock outcrop that rises abruptly from the surrounding smooth and gentle slopes of a rounded hill summit or ridge crest. In the South West of England, the term is commonly also used for the hills themselves – particularly the high points of Dartmoor in Devon and Bodmin Moor in Cornwall.Ehlen, J. (2004) ''Tor'' in Goudie, A., ed., pp. 1054-1056. ''Encyclopedia of Geomorphology.'' Routledge. London, England. Etymology Although English topographical names often have a Celtic etymology, the Oxford English Dictionary lists no cognates to the Old English word in either the Breton or Cornish languages (the Scottish Gaelic ''tòrr'' is thought to derive from the Old English word). It is therefore accepted that the English word ''Tor'' derives from the Old Welsh word ''tẁrr'' or ''twr'', meaning a cluster or heap. Formation Tors are landforms created by the erosion a ...
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Causewayed Enclosure
A causewayed enclosure is a type of large prehistoric earthwork common to the early Neolithic in Europe. It is an enclosure marked out by ditches and banks, with a number of causeways crossing the ditches. More than 100 examples are recorded in France and 70 in England, while further sites are known in Scandinavia, Belgium, Germany, Italy, Ireland and Slovakia. The term "causewayed enclosure" is now preferred to the older term, causewayed camp, as it has been demonstrated that the sites did not necessarily serve as occupation sites. Construction Causewayed enclosures are often located on hilltop sites, encircled by one to four concentric ditches with an internal bank. Enclosures located in lowland areas are generally larger than hilltop ones. Crossing the ditches at intervals are causeways which give the monuments their names. It appears that the ditches were excavated in sections, leaving the wide causeways intact in between. They should not be confused with segmented, or ...
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Carn Brea, Redruth
Carn Brea ( kw, Karnbre) is a civil parish and hilltop site in Cornwall, England, United Kingdom. The population of Carn Brea including Bosleake and Church Coombe was 8,013 at the 2011 census. The hilltop site is situated approximately one mile (1.6 km) southwest of Redruth. The settlements of Bosleake, Brea, Broad Lane, Carn Arthen, Carn Brea Village, Carnkie, Four Lanes, Grillis, Illogan Highway, Pencoys, Penhallick, Piece, Pool, Tolskithy, Tregajorran, Treskillard, Tuckingmill and West Tolgus are in the parish. Neolithic settlement The Neolithic settlement at Carn Brea was a tor enclosure occupied between around 3700 and 3400 BC. Roger Mercer directed archaeological excavations of the site in 1970. https://cornisharchaeology.org.uk/volume-9-1970/ and 1972. https://cornisharchaeology.org.uk/volume-11-1972/ A two-acre (0.8 ha) inner enclosure was surrounded by one of eleven acres (4.5 ha). The ramparts consisted of stone walls with an earth bank and ditch. T ...
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Cornwall
Cornwall (; kw, Kernow ) 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 and an area of . 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. Cornwall was formerly a Brythonic kingdom and subsequently a royal duchy. It is the cultural and ethnic origin of the Cornish dias ...
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Bodmin
Bodmin () is a town and civil parish in Cornwall, England, United Kingdom. It is situated south-west of Bodmin Moor. The extent of the civil parish corresponds fairly closely to that of the town so is mostly urban in character. It is bordered to the east by Cardinham parish, to the southeast by Lanhydrock parish, to the southwest and west by Lanivet parish, and to the north by Helland parish. Bodmin had a population of 14,736 as of the 2011 Census. It was formerly the county town of Cornwall until the Crown Courts moved to Truro which is also the administrative centre (before 1835 the county town was Launceston). Bodmin was in the administrative North Cornwall District until local government reorganisation in 2009 abolished the District (''see also Cornwall Council''). The town is part of the North Cornwall parliamentary constituency, which is represented by Scott Mann MP. Bodmin Town Council is made up of sixteen councillors who are elected to serve a term of four years. ...
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Lostwithiel
Lostwithiel (; kw, Lostwydhyel) is a civil parish and small town in Cornwall, England, United Kingdom at the head of the estuary of the River Fowey. According to the 2001 census it had a population of 2,739, increasing to 2,899 at the 2011 census. The Lostwithiel electoral ward had a population of 4,639 at the 2011 census. The name Lostwithiel comes from the Cornish "lostwydhyel" which means "tail of a wooded area". Origin of the name The origin of the name Lostwithiel is a subject much debated. In the 16th century it was thought that the name came from the Roman name ''Uzella'', translated as ''Les Uchel'' in Cornish. In the 17th century popular opinion was that the name came from a translation of ''Lost'' (a tail) and ''Withiel'' (a lion), the lion in question being the lord who lived in the castle. Current thinking is that the name comes from the Old Cornish ''Lost Gwydhyel'' meaning "tail-end of the woodland". The view from Restormel Castle looking towards the town sh ...
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Bodmin Moor
Bodmin Moor ( kw, Goon Brenn) is a granite moorland in north-eastern Cornwall, England. It is in size, and dates from the Carboniferous period of geological history. It includes Brown Willy, the highest point in Cornwall, and Rough Tor, a slightly lower peak. Many of Cornwall's rivers have their sources here. It has been inhabited since at least the Neolithic era, when primitive farmers started clearing trees and farming the land. They left their megalithic monuments, hut circles and cairns, and the Bronze Age culture that followed left further cairns, and more stone circles and stone rows. By medieval and modern times, nearly all the forest was gone and livestock rearing predominated. The name Bodmin Moor is relatively recent. An early mention is in the ''Royal Cornwall Gazette'' of 28 November 1812. The upland area was formerly known as Fowey Moor after the River Fowey, which rises within it. Geology Bodmin Moor is one of five granite plutons in Cornwall that make up pa ...
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