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Cadbury Castle, Somerset
Cadbury Castle is a Bronze and Iron Age hillfort in the civil parish of South Cadbury in the English county of Somerset. It is a scheduled monument and has been associated with King Arthur's legendary court at Camelot. The hillfort is formed by a plateau surrounded by ramparts on the surrounding slopes of the limestone Cadbury Hill. The site has been excavated in the late 19th and early 20th century by James Bennett and Harold St George Gray. More recent examination of the site was conducted in the 1960s by Leslie Alcock and since 1992 by the South Cadbury Environs Project. These have revealed artifacts from human occupation and use from the Neolithic through the Bronze and Iron Ages. The site was reused by the Roman forces and again from c. 470 until some time after 580. In the 11th century, it temporarily housed a Saxon mint. Evidence of various buildings at the site has been unearthed, including a "Great Hall", round and rectangular house foundations, metalworking, and a ...
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South Cadbury
South Cadbury is a village in the civil parish of South Cadbury and Sutton Montis, in the South Somerset council area of the English county of Somerset. The parish includes the village of Sutton Montis. It is famous as the location of the hill fort of Cadbury Castle, thought by some to be King Arthur's Camelot. History The name Cadbury means ''Cada's fort'' and refers to Cadbury Castle, which is immediately to the south west of the village. It is a vast Iron Age hill fort covering an area of around 20 acres (8 ha). The site has seen human occupation from Neolithic times until the late Saxon period. It was famously partially excavated by Leslie Alcock in the 1960s, when, amongst other things, an Arthurian period feasting hall was discovered. Since John Leland made reference to local traditions of a connection with King Arthur in the 16th century, there has been widespread speculation that this was the location of Camelot. King Arthur's Well sits at the foot of the hill and ...
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Leslie Alcock
Leslie Alcock (24 April 1925 – 6 June 2006) was Professor of Archaeology at the University of Glasgow, and one of the leading archaeologists of Early Medieval Britain. His major excavations included Dinas Powys hill fort in Wales, Cadbury Castle in Somerset and a series of major hillforts in Scotland. Early years Alcock was born at Cheadle Hulme, Stockport, near Manchester, son of clerk Philip John Alcock and Mary Ethel (née Bagley). He won a scholarship to Manchester Grammar School in 1935. Alcock left school in 1942, subsequently joining the army and going on to serve as a captain in the Royal Gurkha Rifles during World War II. After demobilisation in 1946, he won a scholarship to Brasenose College, Oxford, where he read Modern History from 1946 to 1949. He pursued his interest in archaeology through the Oxford Archaeology Society, becoming its president. He met his wife Elizabeth during this period, and they were married in 1950, shortly before he left Britain to become ...
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Somerset Levels
The Somerset Levels are a coastal plain and wetland area of Somerset, England, running south from the Mendip Hills, Mendips to the Blackdown Hills. The Somerset Levels have an area of about and are bisected by the Polden Hills; the areas to the south are drained by the River Parrett, and the areas to the north by the rivers River Axe (Bristol Channel), Axe and River Brue, Brue. The Mendip Hills separate the Somerset Levels from the North Somerset Levels. The Somerset Levels consist of marine clay "levels" along the coast and inland peat-based "moors"; agriculturally, about 70 per cent is used as grassland and the rest is arable. Willow and Dipsacus fullonum, teazel are grown commercially and peat is extracted. A Palaeolithic flint tool found in West Sedgemoor is the earliest indication of human presence in the area. The Neolithic people exploited the reed swamps for their natural resources and started to construct wooden trackways, including the world's oldest known tim ...
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Cadbury Hill
Cadbury Hill is a small hill, mostly in the civil parish of Congresbury, overlooking the village of Yatton in North Somerset. On its summit stands an Iron Age hill fort, which is a Scheduled Ancient Monument. Background Hill forts developed in the Late Bronze and Early Iron Age, roughly the start of the 1st millennium BC. The reason for their emergence in Britain, and their purpose, has been a subject of debate. It has been argued that they could have been military sites constructed in response to invasion from continental Europe, sites built by invaders, or a military reaction to social tensions caused by an increasing population and consequent pressure on agriculture. The dominant view since the 1960s has been that the increasing use of iron led to social changes in Britain. Deposits of iron ore were located in different places to the tin and copper ore necessary to make bronze, and as a result trading patterns shifted and the old elites lost their economic and social s ...
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Channel 4
Channel 4 is a British free-to-air public broadcast television network operated by the state-owned enterprise, state-owned Channel Four Television Corporation. It began its transmission on 2 November 1982 and was established to provide a fourth television service in the United Kingdom. At the time, the only other channels were the television licence, licence-funded BBC One and BBC Two, and a single commercial broadcasting network ITV (TV network), ITV. The network's headquarters are based in London and Leeds, with creative hubs in Glasgow and Bristol. It is publicly owned and advertising-funded; originally a subsidiary of the Independent Broadcasting Authority (IBA), the station is now owned and operated by Channel Four Television Corporation, a public corporation of the Department for Digital, Culture, Media and Sport, which was established in 1990 and came into operation in 1993. Until 2010, Channel 4 did not broadcast in Wales, but many of its programmes were re-broadcast ...
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Barry Cunliffe
Sir Barrington Windsor Cunliffe, (born 10 December 1939), known as Barry Cunliffe, is a British archaeologist and academic. He was Professor of European Archaeology at the University of Oxford from 1972 to 2007. Since 2007, he has been an Emeritus Professor. Biography Cunliffe's decision to become an archaeologist was sparked at the age of nine by the discovery of Roman remains on his uncle's farm in Somerset. After studying at Portsmouth Northern Grammar School (now the Mayfield School) and reading archaeology and anthropology at St John's College, Cambridge, he became a lecturer at the University of Bristol in 1963. Fascinated by the Roman remains in nearby Bath he embarked on a programme of excavation and publication. In 1966 he became an unusually young professor when he took the chair at the newly founded Department of Archaeology at the University of Southampton. There he became involved in the excavation (1961–1968) of the Fishbourne Roman Palace in Sussex. Anot ...
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Bronze
Bronze is an alloy consisting primarily of copper, commonly with about 12–12.5% tin and often with the addition of other metals (including aluminium, manganese, nickel, or zinc) and sometimes non-metals, such as phosphorus, or metalloids such as arsenic or silicon. These additions produce a range of alloys that may be harder than copper alone, or have other useful properties, such as ultimate tensile strength, strength, ductility, or machinability. The three-age system, archaeological period in which bronze was the hardest metal in widespread use is known as the Bronze Age. The beginning of the Bronze Age in western Eurasia and India is conventionally dated to the mid-4th millennium BCE (~3500 BCE), and to the early 2nd millennium BCE in China; elsewhere it gradually spread across regions. The Bronze Age was followed by the Iron Age starting from about 1300 BCE and reaching most of Eurasia by about 500 BCE, although bronze continued to be much more widely used than it is in mod ...
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Copper
Copper is a chemical element with the symbol Cu (from la, cuprum) and atomic number 29. It is a soft, malleable, and ductile metal with very high thermal and electrical conductivity. A freshly exposed surface of pure copper has a pinkish-orange color. Copper is used as a conductor of heat and electricity, as a building material, and as a constituent of various metal alloys, such as sterling silver used in jewelry, cupronickel used to make marine hardware and coins, and constantan used in strain gauges and thermocouples for temperature measurement. Copper is one of the few metals that can occur in nature in a directly usable metallic form ( native metals). This led to very early human use in several regions, from circa 8000 BC. Thousands of years later, it was the first metal to be smelted from sulfide ores, circa 5000 BC; the first metal to be cast into a shape in a mold, c. 4000 BC; and the first metal to be purposely alloyed with another metal, tin, to create ...
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Tin Mining In Britain
Tin mining in Britain took place from prehistoric times, during Bronze Age Britain, until the 20th century. Mention of tin mining in Britain was made by many Classical writers. Tin is necessary to smelt bronze, an alloy that played a vital cultural role during the Bronze Age. As South-West Britain was one of the few parts of Anglian stage England to escape glaciation, tin ore was readily available on the surface. Originally it is likely that cassiterite alluvial deposits in the gravels of streams were exploited but later underground working took place. Shallow cuttings were then used to extract ore. In the 19th century advances in mining engineering enabled the exploitation of much deeper mines. In a few cases these mines even extended both to multiple levels and workings below the seabed. See also *Tin sources and trade in ancient times *Dartmoor tin-mining *Mining in Cornwall and Devon Mining in Cornwall and Devon, in the southwest of England, began in the early Bronze ...
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Iron Ore
Iron ores are rocks and minerals from which metallic iron can be economically extracted. The ores are usually rich in iron oxides and vary in color from dark grey, bright yellow, or deep purple to rusty red. The iron is usually found in the form of magnetite (, 72.4% Fe), hematite (, 69.9% Fe), goethite (, 62.9% Fe), limonite (, 55% Fe) or siderite (, 48.2% Fe). Ores containing very high quantities of hematite or magnetite (greater than about 60% iron) are known as "natural ore" or "direct shipping ore", meaning they can be fed directly into iron-making blast furnaces. Iron ore is the raw material used to make pig iron, which is one of the main raw materials to make steel—98% of the mined iron ore is used to make steel. In 2011 the ''Financial Times'' quoted Christopher LaFemina, mining analyst at Barclays Capital, saying that iron ore is "more integral to the global economy than any other commodity, except perhaps oil". Sources Metallic iron is virtually unknown on ...
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Iron
Iron () is a chemical element with symbol Fe (from la, ferrum) and atomic number 26. It is a metal that belongs to the first transition series and group 8 of the periodic table. It is, by mass, the most common element on Earth, right in front of oxygen (32.1% and 30.1%, respectively), forming much of Earth's outer and inner core. It is the fourth most common element in the Earth's crust. In its metallic state, iron is rare in the Earth's crust, limited mainly to deposition by meteorites. Iron ores, by contrast, are among the most abundant in the Earth's crust, although extracting usable metal from them requires kilns or furnaces capable of reaching or higher, about higher than that required to smelt copper. Humans started to master that process in Eurasia during the 2nd millennium BCE and the use of iron tools and weapons began to displace copper alloys, in some regions, only around 1200 BCE. That event is considered the transition from the Bronze Age to the Iron A ...
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Prehistoric Britain
Several species of humans have intermittently occupied Great Britain for almost a million years. The earliest evidence of human occupation around 900,000 years ago is at Happisburgh on the Norfolk coast, with stone tools and footprints probably made by ''Homo antecessor''. The oldest human fossils, around 500,000 years old, are of ''Homo heidelbergensis'' at Boxgrove in Sussex. Until this time Britain had been permanently connected to the Continent by a chalk ridge between South East England and northern France called the Weald-Artois Anticline, but during the Anglian Glaciation around 425,000 years ago a megaflood broke through the ridge, and Britain became an island when sea levels rose during the following Hoxnian interglacial. Fossils of very early Neanderthals dating to around 400,000 years ago have been found at Swanscombe in Kent, and of classic Neanderthals about 225,000 years old at Pontnewydd in Wales. Britain was unoccupied by humans between 180,000 and 60,000 yea ...
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