Mount Caburn is a 480-foot (146m) prominent landmark in East Sussex, England, about one mile (1.6 km) east of Lewes overlooking the village of Glynde. It is the highest part of an outlier of the South Downs, separated from the main range by Glynde Reach, a tributary of the River Ouse.
On the summit of Caburn are the remains of an Iron Age hill fort. The hill fort has been repeatedly excavated, by Augustus Pitt Rivers (1877–78), the Curwens (1925—26), the Curwens again (1937–38), and the Sussex Archaeological Society (1996–98). It may have the most excavations per site in Britain, with 170 trenches.
Pollen records (from peat at the southern base) indicate that prior to 2000 BC the hill was covered with dark yew woodlands. The fact that a single Neolithic leaf-shaped arrowhead is the only pre-Bronze Age find on Caburn, despite the extent and duration of excavations, suggests that there was little permanent occupation then.
The summit was initially enclosed in the middle Iron Age (c. 400 BC), with a deep V-shaped ditch and a bank of dumped spoil. Originally the ditch was 8m wide at the top, 2.7m deep, and enclosed an area of 1.9 ha.
Since before the first excavations, it has been assumed that this enclosure was defensive, making a conventional hill fort. However the most recent excavators have challenged this assumption, arguing instead that the site was a religious enclosure, rather than a military fort or fortified farmstead. They point to the contents of the small pits, the insubstantial rampart, and its weak defensive attributes.
There are over 140 burial pits on Caburn: some are circular, some triangular and some rectangular. Each pit was found to be full of artefacts. Deposits included weapons, tools, pottery, coins, querns, and disarticulated human and animal bones. The most recent excavators argue that these are not random, or mere domestic rubbish, but are structured deposits and appear "ritually charged". The NE corner of the enclosure seemed to have special significance, because the high-status objects were mostly deposited there.
Outside the original rampart, on the northern side, there is a great ditch cut into the chalk. This is the side most vulnerable to attack.
This outer ditch has long been assumed to be a late Iron Age (re-)fortification, perhaps in response to the threat from Rome. That assumption has now been disproved. The excavation of trenches through the chalk dump (the spoil had been dumped in the adjacent valley instead of being used to build a bank) and a small internal bank turned up Romano-British pottery. Therefore the outer ditch is Romano-British or later, perhaps a Saxon measure against Viking raids.
It appears that the Caburn was densely grazed during the Roman period, when the hill slopes around were a patchwork of rectangular ploughed fields. Then the hill probably returned to scrub, but by the Norman Conquest the Caburn was heavily grazed again and the hill slopes were ploughed into strips. Both the Roman rectangular fields and the medieval strips are still visible today.
Conservation and recreation
Mount Caburn is now legally protected. It lies within the Lewes Downs SSSI (designated in 1953) and the Mount Caburn National Nature Reserve was established in the mid-1980s. It has been designated a Special Area of Conservation as an example of orchid-rich chalk grassland. It is home to a good population of stonechats.
Caburn is unusual within the South Downs for having a south-facing scarp slope. The site has the largest British population of burnt-tip orchid. There is also the rare small-leaved sweet-briar, and the typical fragrant and pyramidal orchids. Invertebrates include Adonis and chalkhill blue butterflies and the scarce forester moth. Populations of stonechats live in scrubby bushes such as gorse near the golf club and in the valley below, along with other song birds such as blue tits. Herring gulls and carrion crows often fly overhead and hundreds of domestic sheep graze the area. There is a sheltered cave with a water trough where lost sheep can rest safely if they stray away from the flock on a dark night when the farmer is rounding up the animals.
In fiction Caburn appears as Wealden Hill in the novel of the same name by Graeme K Talboys. Caburn also features prominently in the novels and short stories of John Whitbourn (e.g. The Royal Changeling and Bury My Heart At Southerham (East Sussex)). Caburn also appears in the children's story Elsie Piddock Skips in Her Sleep (first published in 1937) by Eleanor Farjeon. It is mentioned in Kipling's poem "The Run of the Downs."
It has only been called Mount Caburn since the end of the 18th century. The origins of the name are disputed.
- It has long been suggested that Caburn may come from Caer Bryn (Welsh - Stronghold hill), though this is widely discredited
- A rival explanation is that it was originally Calde burgh (Old English - Cold Fort - 1296), then Mount Carbone (late 18th century).
- Some local accounts allege that by the 18th century it was called Carber, and before that it was called Calborough Hill.
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- Drewett, P., and Hamilton, S., 1999: Marking time and making space: Excavations and Landscape Studies at the Caburn hillfort, East Sussex, 1996–98. Sussex Archaeological Collections, 137: 7-37.
- Drewett, P., and Hamilton, S., 2001: Sacred mount or classic hillfort? Current Archaeology, 174: 256-262
- M.P. Waller and S. Hamilton. 2000. Vegetation history of the English chalklands: a mid-Holocene pollen sequence from the Caburn, East Sussex. Journal of Quaternary Science, 15, 253-272.
- English Nature, 2002: Five Thousand Midsummer Days: the Caburn, its people and wildlife.
- Russell, M., 2006: Roman Sussex. Tempus. p60
- e.g. Drewett, P., Rudling, D., Gardiner, M., 1988: The South-East to AD 1000. Longman. p. 155
- Hampden. A., 1997: A Glimpse of Glynde. The Book Guild. p. 1
- Lusted, A., 1989: A pit-worker's story. Glynde Archivist 9.