Site of Special Scientific Interest | |
Location | Avon |
---|---|
Grid reference | ST588587 |
Coordinates | 51°19′33″N2°35′34″W / 51.32590°N 2.59267°W Coordinates: 51°19′33″N2°35′34″W / 51.32590°N 2.59267°W |
Interest | Biological |
Area | 48.7 hectares (0.487 km2; 0.188 sq mi) |
Notification | 2005 |
Natural England website |
Burledge Hill (grid reference ST588587 ) is on the southern edge of the village of Bishop Sutton, Somerset, England. It is the site of a Site of Special Scientific Interest and an univallate Iron Age hill fort.
The site comprises a mixture of flower rich grassland, scrub and mature hedgerows. Three fields are designated as Burledge Sidelands and Meadows a Site of Nature Conservation Interest (SNCI), [1] and, since November 2005, as a Site of Special Scientific Interest (SSSI) covering 48.7 ha the citation says:
These form part of a 3 km horseshoe of unimproved neutral grassland running around the top of Burledge Hill, forming the largest known concentration of this habitat recorded in Avon. Plant species found on the site include cowslip, Alchemilla (lady's mantle), saw-wort and devil's bit scabious. Birds such as willow warbler (Phylloscopus trochilus), garden warbler (Sylvia borin) and whitethroat (Sylvia communis) can be heard singing from the scrub areas. The site also falls within the Mendip Hills Area of Outstanding Natural Beauty (AONB) and has commanding views of the Chew Valley.
Hill forts developed in the Late Bronze and Early Iron Age, roughly the start of the first millennium BC. [3] 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. [4] 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". [5]
Burledge hill fort is a univallate Iron Age hill fort. [6] [7] The site was investigated three times: in 1955 by the University of Bristol Spelaeological Society and in 1959 and 1966 by field investigation. [8] In 1955, the excavating archaeologists found evidence of postholes, ditches, and pits inside the fort. They also found artefacts like a part of an iron fibula, animal bones, and pottery. One find which evidenced that metalworking was done at this site was the discovery of iron slag. [9]
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.
Bishop Sutton is a village on the northern slopes of the Mendip Hills, within the affluent Chew Valley in Somerset. It lies east of Chew Valley Lake and north east of the Mendip Hills, approximately ten miles south of Bristol on the A368, Weston-super-Mare to Bath road between West Harptree and Chelwood. Bishop Sutton and the neighbouring village of Stowey form the civil parish of Stowey Sutton.
Maesbury Castle is an Iron Age hill fort within the parish of Croscombe on the Mendip Hills, just north of Shepton Mallet, Somerset, England. It has been listed as a Scheduled Ancient Monument.
Plainsfield Camp is a possible Iron Age earthwork on the Quantock Hills near Aisholt in Somerset, England.
Cleeve Toot is an Iron Age univallate hillfort above Goblin Combe, Cleeve, Somerset, England. It is a Scheduled Ancient Monument.
Norton Camp is a Bronze Age hill fort at Norton Fitzwarren near Taunton in Somerset, England.
Kenwalch's Castle is probably an Iron Age hill fort that may have been converted into a Roman fortress, near Penselwood, Somerset, England, 6.6 kilometres (4 mi) east south east of Bruton at grid reference ST747335. It is a Scheduled Ancient Monument. It is believed to be named after Cenwalh of Wessex.
Kingsdown Camp is an Iron Age hill fort at Buckland Dinham 4.5 kilometres (3 mi) South East of Radstock, Somerset, England. It is a Scheduled Ancient Monument.
Banwell Camp is a univallate Iron Age hill fort in the North Somerset district of Somerset, England. The hill fort is situated approximately 1.6 miles (2.6 km) east from the Village of Banwell. Some artefacts found on the site dates back to the Bronze Age and the Stone Age. In places it is surrounded by a 4 metres (13 ft) high bank and ditch.
Burrington Camp, also known as Burrington Ham, is an Iron Age hill fort in the North Somerset district of Somerset, England. The hill fort is situated in the Mendip Hills approximately 0.6 miles (0.97 km) south from the village of Burrington.
Curdon Camp is a univallate Iron Age hill fort in the West Somerset district of Somerset, England. It is a Scheduled Ancient Monument.
Westbury Camp is a univallate Iron Age hill fort in the Mendip Hills in Somerset, England. The hill fort is situated in the parish of Rodney Stoke, approximately 1 mile (1.6 km) north-east of the village of Draycott and 1.5 miles (2.4 km) north-west of Westbury-sub-Mendip. The camp is largely situated in a hill slope. The north east defences have largely been destroyed by small quarries over the years. The narrow top of the hill bank suggests that it may have been surmounted by a dry stone wall. Along part of the east side of the camp there are traces of a berm between the bank and the outer ditch and at the western angle shallow quarry pits occur internally and externally set back from the 'rampart'.
Charterhouse Camp is a univallate Iron Age hill fort in the Mendip district of Somerset, England. The hill fort is situated approximately 0.6 miles (0.97 km) east from the village of Charterhouse. There is some evidence, in the form of burials in local caves, of human occupation since the late Neolithic times and the early Bronze Age. The site is associated with Charterhouse Roman Town and may have been the site of Iscalis.
Tunley Camp is an vallate Iron Age hill fort situated approximately 0.8 miles (1.3 km) north-east from the small village of Camerton in the Bath and North East Somerset district of Somerset, England. The hill fort comprises the slight earthwork remains of a univallate Iron Age hillfort which now nearly ploughed down.
Wain's Hill is an univallate Iron Age hill fort situated approximately 1 mile (1.6 km) south-west from the town of Clevedon in the North Somerset district of Somerset, England. The hillfort is defined by a steep, natural slope from the south and north with two ramparts to the east.
Broomfield Camp is a univallate Iron Age hill fort in the Taunton Deane district of Somerset, England. The hill fort is situated approximately 0.6 miles (0.97 km) south-east from the village of Broomfield. Broomfield Camp dates from late prehistoric or Roman times. The camp was searched in 1968 and the result uncovered a trench through a bank and ditch which produced Iron Age pottery.
Castles Camp is a univallate Iron Age hill fort in the Taunton Deane district of Somerset, England. The hill fort is situated approximately 1 mile (1.6 km) west from the village of Bathealton. A few trees a scattered around the camp's defences along with Roman coins being found in previous years.
Rodhuish Common is a univallate Iron Age hill fort in the West Somerset district of Somerset, England. There is a small oval enclosure which is thought to be of Iron Age date.
Dinies Camp is a univallate Iron Age hill fort enclosure in the Mendip district of Somerset, England. The hill fort is situated approximately 1 mile (1.6 km) south-west from the village of Downhead. The hill fort is considered to be medieval as it is on the site of earlier earthwork.
East Myne is a univallate Iron Age hill fort enclosure in the West Somerset district of Somerset, England. The hill fort is situated approximately 1.1 miles (1.8 km) west from the town of Minehead. The hill fort is considered to be a deserted post-medieval farmstead.