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Chanctonbury Ring

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Through England, Iron Age and World War II

Consisting of a roughly circular low earthen rampart surrounded by a ditch, Chanctonbury Ring is thought to date to the late Bronze Age or early Iron Age. The purpose of the structure is unknown but it could have filled a variety of roles, including a defensive position, a cattle enclosure or even a religious shrine. After a few centuries of usage, it was abandoned for about five hundred years until it was reoccupied during the Roman period. Two Romano-British temples were built in the hill fort's interior, one of which may have been dedicated to a boar cult.

After its final abandonment around the late fourth century AD, the hill fort remained unoccupied save for grazing cattle until a mid-18th-century landowner planted a ring of beech trees around its perimeter to beautify the site. They became a famous local landmark until largely being destroyed in the Great Storm of 1987. Periodic replanting on a number of occasions to replace old or destroyed trees has afforded archaeologists the opportunity to carry out a series of excavations which have revealed much about the history of the site.

Description

Chanctonbury Ring is in a commanding position looking across the Sussex Weald to the north, on the edge of a steep natural escarpment to the northwest and northeast. It is at the middle point of a long, narrow and otherwise treeless plateau, approached via ridges to the east and west. A trig point is located about 400 metres (440 yd) west of the Ring, recorded by the Ordnance Survey as 238 metres (781 ft) above sea level. Although this was originally recorded as the top of Chanctonbury Hill and thus the Marilyn summit, recent measurements suggest that the area of the Ring is higher, about 241 metres (791 ft) above sea level. The Ring lies just to the north of an ancient ridgeway which has been in use since prehistoric times and is now part of the South Downs Way.

The hill fort is roughly circular, enclosing about 1.5 hectares (3.7 acres). The bank around the enclosure is about 10 metres (33 ft) wide and up to 0.8 metres (2 ft 7 in) high, with a circumference of about 400 metres (1,300 ft). It is surrounded by a ditch approximately 8 metres (26 ft) wide and 0.7 metres (2 ft 4 in) deep. The bank was constructed from chalk rubble, flint and clay excavated from its surrounding ditch. They would originally have been much wider and deeper, and would have had prominent lines of sight to other prehistoric landmarks in the area. The fort is defined by archaeologists as a "slight univallate hill fort", indicating a single-walled earthwork with a low rampart.

The original entrance to the hill fort was provided by a gap of approximately 6 metres (20 ft) on the south-eastern side, where the remains of a causeway are visible. Another gap through the rampart is visible on the south-western side but was probably created much later after the hill fort had gone out of use, as no causeway is visible there. The rampart and outer ditch have largely been preserved on the southern side, though slightly damaged by two small quarries dug into it. Erosion and soil creep have reduced the earthworks on the northern side and only traces remain of the ditch in this area. The perimeter and interior of the hill fort are occupied by a planted stand of beech trees.

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