Tedbury Camp
Encyclopedia
Tedbury Camp is a multivallate Iron Age
promontory hill fort defended by two parallel banks near Great Elm
, Somerset
, England.
. 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 status. Power passed into the hands of a new group of people. Archaeologist Barry Cunliffe
believes that population increase still played a role and has stated "[the forts] provided defensive possibilities for the community at those times when the stress [of an increasing population] burst out into open warfare. But I wouldn't see them as having been built because there was a state of war. They would be functional as defensive strongholds when there were tensions and undoubtedly some of them were attacked and destroyed, but this was not the only, or even the most significant, factor in their construction".
and Fordbury Water.
It is also a site of Roman occupation between 337 and 366 which left behind a hoard of Constantine Junior
coins which were found in 1691.
Further excavations and explorations of the site were carried out in the 19th and 20th centuries, with a Quern-stone
being discovered between 1939 and 1945.
A quarry 500 metres (1,640.4 ft) north east of the camp actively extracted carboniferous limestone in the 20th century and demonstrates geological unconformity.
Iron Age
The Iron Age is the archaeological period generally occurring after the Bronze Age, marked by the prevalent use of iron. The early period of the age is characterized by the widespread use of iron or steel. The adoption of such material coincided with other changes in society, including differing...
promontory hill fort defended by two parallel banks near Great Elm
Great Elm
Great Elm is a village and civil parish between Mells and Frome in the Mendip district of Somerset, England. The parish includes the hamlet of Hapsford.-History:...
, Somerset
Somerset
The ceremonial and non-metropolitan county of Somerset in South West England borders Bristol and Gloucestershire to the north, Wiltshire to the east, Dorset to the south-east, and Devon to the south-west. It is partly bounded to the north and west by the Bristol Channel and the estuary of the...
, England.
Background
Hill forts developed in the Late Bronze and Early Iron Age, roughly the start of the first millennium BC1st millennium BC
The 1st millennium BC encompasses the Iron Age and sees the rise of many successive empires, and spanned from 1000 BC to 1 BC.The Neo-Assyrian Empire, followed by the Achaemenids. In Greece, Classical Antiquity begins with the colonization of Magna Graecia and peaks with the rise of Hellenism. The...
. 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 status. Power passed into the hands of a new group of people. Archaeologist Barry Cunliffe
Barry Cunliffe
Sir Barrington Windsor Cunliffe, CBE, known professionally as Barry Cunliffe is a former Professor of European Archaeology at the University of Oxford, a position held from 1972 to 2007...
believes that population increase still played a role and has stated "[the forts] provided defensive possibilities for the community at those times when the stress [of an increasing population] burst out into open warfare. But I wouldn't see them as having been built because there was a state of war. They would be functional as defensive strongholds when there were tensions and undoubtedly some of them were attacked and destroyed, but this was not the only, or even the most significant, factor in their construction".
Description
The inner bank is 4 feet (1.2 m) to 6 feet (1.8 m) wide and stand 10 feet (3 m) to 15 feet (4.6 m) high in places. There may have been a third bank. It covers an area of approximately 60 acres (24.3 ha) between the Mells RiverMells River
The Mells River flows through the eastern Mendip Hills in Somerset, England. It rises at Gurney Slade and flows east joining the River Frome at Frome.The river forms one of the boundaries of Mells Manor a country house estate in Mells....
and Fordbury Water.
It is also a site of Roman occupation between 337 and 366 which left behind a hoard of Constantine Junior
Constantine II (emperor)
Constantine II , was Roman Emperor from 337 to 340. Co-emperor alongside his brothers, his short reign saw the beginnings of conflict emerge between the sons of Constantine the Great, and his attempt to exert his perceived rights of primogeniture ended up causing his death in a failed invasion of...
coins which were found in 1691.
Further excavations and explorations of the site were carried out in the 19th and 20th centuries, with a Quern-stone
Quern-stone
Quern-stones are stone tools for hand grinding a wide variety of materials. They were used in pairs. The lower, stationary, stone is called a quern, whilst the upper, mobile, stone is called a handstone...
being discovered between 1939 and 1945.
A quarry 500 metres (1,640.4 ft) north east of the camp actively extracted carboniferous limestone in the 20th century and demonstrates geological unconformity.