Hengistbury Head

Hengistbury Head is a peninsula 1.5km long on the south-east coast of Dorset. Exposed to the sea to the south, to the north it encloses a vast bay of Christchurch Harbour into which empty the rivers Stour and Avon. There is some evidence of Early Iron Age occupation. The ‘Double Dykes’ barring the neck of the headland are thought to be late Middle Iron Age in construction, but it is not known whether they are of more than one phase of construction. In the Late Iron Age, about 100 BC, the site emerges as a major port, maintaining trading links with Brittany and Normandy (Cunliffe 1987).

Excavation History
The two major investigations that have ben undertaken to examine the Iron Age occupation of the site were those of J.P. Bushe-Fox 1911-1912 (Bushe-Fox 1915) and B.W. Cunliffe 1979-1984 (Cunliffe 1987). Unpublished excavations conducted by H.St George Gray 1918-1924 have left only a limited archive. Small-scale investigation by Dr.D. Peacock in 1970-1 on the shore of Christchurch harbour revealed well-stratified Iron Age and Roman occupation.

Defensive Earthworks
The Double Dykes cut off the neck of the headland from north to south and comprise a larger inner earthwork, (originally 5m high and 14m wide with a ditch 5m deep), and a smaller outer earthwork (a bank 10m wide and 1.5m high, the ditch 7m wide and 2m deep). The outer ditch is now obscured by blown sand. The bank has an eastward recurve to the North. Early records (Grose 1779) show the southern end similarly curving along the sea front, but since the late 18th century, a substantial amount of land on the seaward side of the headland has been lost to coastal erosion. Only 290m now survives of the original 520m length. The ramparts are of simple dump construction. It is thought that a gap at the northern end used by the modern road is an original entrance.
200m behind the Double Dykes is a second line of defences, now concealed at the surface by blown sand but exposed in the beach section; in the first stage it comprises a dump rampart 5.5m wide with a flat-bottomed U-shaped ditch, being replaced by enlarged rampart with a shallower, wider ditch. No dating evidence is associated with this rampart, but based on the spread of eighth–sixth century BC occupation identified on the headland, Cunliffe has tentatively proposed late Bronze Age/Early Iron Age date (Cunliffe 1987).

The occupation
The site has been in use since the Paleolithic. A large later Neolithic and early Bronze Age flint assemblage has been accumulated, with pottery from the same periods. At least 13 Bronze Age burial mounds are known, indicating that the headland was used as a cemetery in the first half of the second millennium BC. Excavations and general finds scatters attest intensive occupation in the Late Bronze Age/early Iron Age and from the late Iron Age into the Roman period, but the Middle Iron Age is poorly represented.
The modern excavations revealed dense traces of successive occupations characterised by ring ditches (penannular ditches and gullies), scatters of post holes and other gullies. The nature of the earlier first millennium BC occupation is not entirely clear, but might be characterised as a number of nucleated settlements, occupied over a period of time, separated by open areas (Cunliffe 1987). There appears to be a rupture in settlement 400-100 BC, possibly nuanced by a late Middle Iron Age occupation development circa 150 BC.

Late Iron Age 1
The late Iron Age occupation is divided into two periods: 100-50 BC and 50 BC-43 AD. Considerable evidence of levelling, land consolidation and construction activity is identified for the first period. The occupation, characterised by timber buildings, extended along a seashore roadway, from the Double Dykes for a distance of 1km. Evidence of possible harbour works are found at the two ‘inlets’ of Barnfield and Rushy Piece. Evidence for bronze and glass-working is found, and evidence for iron-working may be datable to this phase. Environmental evidence suggests the large-scale handling and processing of crops, and an unusual concentration of cattle on the site which may have been intended for slaughter and leather production. Coins and amphorae testify to exchange with the continent, with the import of wine, figs, coloured glass, metal, and Armorican pottery being attested. Despite the quantity of material recovered, Fitzpatrick (2001) has questioned whether the site was occupied all year round, suggesting instead that it may have been seasonally occupied by traders.

Late Iron Age 2
The occupation is now characterised by a series of palisaded enclosures along the shore-line road. Internal building activity is testified, but few structures can be identified from the evidence. The early harbour works are abandoned and overtaken by peat levels. The occupied and activity-associated areas appear to be more extensive than in phase one, and iron-working is positively attested. Long distance trade appears however to be much diminished. The decline of the seaport is connected (Cunliffe 1987) to the Roman conquest of Gaul deflecting the principal trade routes from the Roman entrepreneurs of southern Gaul via the Atlantic, to the Belgic area of Roman Gaul within easy reach of the the east coast of Britain.

Roman
Roman occupation continued on the site with no sign of a significant break through to the fourth century, the roadway being maintained throughout this period. Much of the headland was given over to arable farming. A gradual decline of occupation is detected through the late third and fourth centuries and the site is abandoned sometime in the late Roman period, until comparatively recently.


SITUATION ADMINISTRATIVE

Nom usuel : Hengistbury Head

Commune : Hengistbury Head

Lieu-dit : -

Nom antique : -

Département : Dorset

Région : South West

Pays : Royaume-Uni

Civitas : Durotriges

TOPOGRAPHIE ET REMPARTS

Superficie : 300 ha

Topographie :  Éperon barré

Nb de phases du rempart : 2

Nb de portes connues : 1 ?

Nb de portes fouillées : -

Architecture de rempart : 

1 - Talus massif 

2 - Talus massif 

OCCUPATION INTERNE DE L'OPPIDUM

Voirie place | Zone d'habitat


ENVIRONNEMENT DE L'OPPIDUM

-


CHRONOLOGIE DU SITE

Chronologie relative :  LT D1, LT D2, Augustéen

Occupation du site : 
Néolithique
Bronze ancien-moyen
Bronze final (Bz. D, Ha A-B)-Hallstatt ancien (Ha C)
Hallstatt moyen-final (Ha D)-La Tène ancienne (LT A)
La Tène finale (LT D)
Haut-Empire
Antiquité tardive


Chronologie absolue : -


BIBLIOGRAPHIE

Bushe-Fox J.P., Excavations at Hengistbury Head, Hampshire in 1911-12, (Society of Antiquaries Res. Rep. 3), Oxford, 1915.
Collis J.R., Defended sites of the Late La Tène in Central and Western Europe, (British Archaeological Reports, Intl. Ser. 2), Oxford, 1975.
Collis J.R., Oppida, Earliest Towns North of the Alps, H.Charlesworth and Co. Ltd, Huddersfield, 1984.
Cunliffe B., Hengistbury Head, Elek Books Ltd, London, 1978.
Cunliffe B., Hengistbury Head Dorset Vol.I: The Prehistoric and Roman settlement, 3500BC - AD 500, Oxford University Committee for Archaeology, Monograph 13, 1987.
Cunliffe B., de Jersey Ph., Armorica and Britain. Cross Channel relationships in the late first millennium BC, Oxford University Committee for Archaeology, Monograph 45, Oxford, 1997.
Fitzpatrick A.P., Cross-Channel exchange, Hengistbury Head and the end of hillforts, in Collis, J.R. (ed.), Society and Settlement in Iron Age Europe, Actes du XVIIIe Colloque de l'AFEAF, Winchester 1994, Sheffield Academic Press, 2001, 82-97.
Grose F., A description of ancient fortifications near Christchurch, Hampshire, Archaeologia, 5, 1779, 237-40.
Haselgrove C., Iron Age brooch deposition and chronology, in A. Gwilt and C. Haselgrove (eds), Reconstructing Iron Age Societies, Oxford, (Oxbow Monograph 71), 1997, 51-72.
Peacock D.P.S., Roman Amphorae in Pre-Roman Britain, in Jesson M., Hill D., The Iron Age and its Hill Forts, department of Archaeology, Southampton, 1971.


GESTION ET MISE EN VALEUR

L'oppidum d'Hengistbury Head est librement accessible. C'est un parc public appartenant au Council de Bournemouth Borough. Espace naturel situé à proximité de la station balnéaire de Bournemouth, il est très fréquenté (près d'un million de visiteurs par an).
Les vestiges du double fossé ont été perturbés par la fréquentation et l'érosion, mais ils sont à présent protégés. Le visiteur peut les découvrir en suivant les sentiers aménagés. D'autres vestiges ont été localisés, mais ne sont pas ou plus visibles.

L'accès au site en voiture est interdit et les cyclistes doivent suivre un itinéraire précis. Un parking à proximité permet de laisser son véhicule pour emprunter un petit chemin de fer pour se rendre sur la plage de Mudeford Spit. Il y a aussi un accès par ferry à partir du port de Christchurch.

Au niveau du parking se trouve un petit café qui permet de se restaurer mais aussi de se documenter sur le site archéologique : panneaux d'information, vente de guides et d'ouvrages. Cet établissement est le seul équipement d'accueil sur place.

Le « Red House Museum » à Christchurch présente quelques vestiges de l'oppidum et une maquette du site dans son exposition archéologique. Le musée est dirigé par le service des musées d'Hampshire en partenariat avec les « Councils » de Dorset et de Bournemouth Borough.
Ouvert du mardi au dimanche, son entrée est gratuite pour tous.
Pour plus de renseignements : Red House Museum - Quay Road, Christchurch - Dorset BH23 1BU / tel: +44 (0)845 603 5635

Voir aussi :
« Hengistbury Head » : http://www.hengistbury-head.co.uk

(Camille Daval – ArchéoMédia, mars 2008)


PHOTOTHEQUE

Vue aérienne depuis l'ouest Vue aérienne depuis l'est

Pip Stephenson / Colin Haselgrove