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    BARRY CUNLIFFE

    BRITAIN, THE VENETI AND BEYOND

    Summary. Archaeological and documentary evidence f o r contact

    between north western France and central southern Britain

    n

    the firs t

    millennium B C is presented and discussed. T he tin trade ma y well have

    been the principal motivation

    or

    contact until the late second cen tury B C

    when, following the foundation

    o

    Provincia Gallia Transalpina, the

    Rom an-dom inated wine trade appears to have itensified cross-channel

    intercourse. T he position

    o

    Armorican middlemen is considered and por t

    sites such as Ale t and Hengistbury are discussed. A We ss ex Contact Zon e

    is defined w ithin w hich overseas trade and local industrialproduction were

    focu sed. Th e economic and social effec ts o these sys tem s on other par ts

    o

    Britain are briefly outlined.

    In two well-known texts Caesar and

    Strabo bring the Veneti and the Britons

    into relationship with each other. Caesar

    is concerned with Venetic military

    strength: now of all the peoples of the

    coastal part of that area, the Veneti are by

    far the strongest. They have a great many

    ships and regularly sail to and from

    Britain. When it comes to knowledge and

    experience of navigation, they leave all

    the other tribes standing B G iii 8).

    Strabo adds: The Veneti are those who

    fought at sea against Caesar, for they were

    prepared to hinder his voyage to Britain

    as they were using the emporion there

    Geog.

    iv.4.1).

    There has been much discussion of

    these two texts. To Stevens 1952, 8-15)

    the Venetic revolt against the Romans

    was designed to divert Caesar from

    attacking Britain in

    56

    BC in order to

    protect their trading monopoly - an

    attractive and plausible explanation;

    while more recently Melinda Mays has

    argued convincingly that the emporion,

    noted by Strabo, referred to a specific site

    which she has tentatively identified as

    Hengistbury Mays 1980, 55-7).

    It was a desire to explore the archaeo-

    logical reality reflected by the texts which

    lay behind the famous expedition to

    Brittany and Normandy organized by Sir

    Mortimer Wheeler in 1938-9 following

    his excavations at Maiden Castle. In the

    Maiden Castle report, published in 1943,

    Wheeler stated his belief in trading

    contacts between the Veneti andcornwal l

    in the pre-Caesarian era, and at the time

    O X F O R D J O U R N A L O F A R C H A E O L O G Y

    l 1 )

    1982

    39

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    B R I TA I N , T H E V E N E T I A N D B E Y O N D

    of the G all ic Wars, an d went on to explain

    the Maiden Castle development in

    historical terms: Th e urb an peasantry of

    Do rset , or at any rate of Maiden Castle,

    comfortably ensconced in their ancient

    and decaying hill-fort, offered a more

    attractive prize t o th e hom eless Vikings in

    Brittany; an d it is to the survivors of the

    masterful Veneti in the folk-wanderings

    which may be supposed to have followed

    Caesars vengeance in 56 BC tha t, on all

    grounds,

    I

    f ind i t easiest to at tr ibu te the

    new Iron Age

    B

    rttgime at Maiden

    Castle (Wh eeler 1943, 56-7).

    The present paper a t temp ts to explore

    the archaeological background afresh in

    the light of evidence which has become

    available in the last forty years.

    T H E A T LA N T I C S E A W A Y S IN T H E E A R LY

    F I R S T M I L L E N N I U M BC

    I t is not our purpose here to examine

    the systems of exchange which bound

    together the communities set t led along

    the Atlantic seaways in the later part of

    the Bronze Age. The archaeological

    evidence has been widely discussed by

    Burgess (1969) an d Briard (1965) a n d the

    actual m echanisms

    of

    exchange have been

    considered recently by Rowlands (1980,

    15-55). Suffice it to say that between the

    eighth and sixth centuries BC the com-

    munities f lanking the C han nel were

    closely bound in a complex

    of

    socio-

    economic systems which resulted in the

    widespread distribution

    of

    similar arte-

    facts on bo th sides of the Cha nnel. Th is is

    particularly clearly show n by the distribu-

    t ion of Armorican axes (Briard 1965,

    241-82 an d below Fig.

    5 )

    a n d

    of

    bronzes

    consti tut ing the Carps Tongue sword

    complex (Burgess 1969, fig. 14). Longer-

    distance contacts are reflected in more

    exotic pieces such a s the S icilian socketed

    axes from near Rennes a nd from Hengist-

    bury Head on the Dorset coast .

    C O N T A C T I N T H E L A T ER F IR S T

    M I L L E N N I U M BC

    With the collapse of the bronze-

    dependent econom y in the middle of the

    millennium direct evidence for contact

    becomes rarer (Fig. 6) . Do uble pyramidal

    i ron ingots of Euro pean or igin appear on

    the south coast of Britain at Port land

    (Grinsell 1958, 137). Their relatively

    widespread distribution in Brittany (Giot

    1964) suggests a likely origin in north-

    western France. It is also possible that

    some at least of the Hallstatt fibulae

    recorded from Britain and of the later

    Gree k a nd Ca rthaginian coins may reflect

    contemporary social contacts with the

    west an d so uth, bu t the f inds of this kind

    are notoriou sly difficult t o interpret since

    reliable contexts are almost invariably

    lacking.

    Wheeler th ou gh t he could see evidence

    of contact between Brit tany an d sou thern

    Britain in pottery finds, draw ing attention

    to c eramic traits such a s the internally-

    grooved r ims an d countersunk perforated

    lugs

    -

    techniques found extensively in

    Brit tany and sporadically in the south-

    west of B ritain (Wh eeler 1943, 204-18).

    Th ere is l it tle more tha t can be added to

    his analysis except to stress tha t evidence

    for the actual transp ort of pottery between

    Britain and Brit tany before the late

    second century BC is virtually unknown

    (Fig .7) . Two sherds f rom Carn Euny ,

    wi th a radiocarbon date of 420f70 bc

    (HAR-238), are of Breton type though

    one at least may be a Cornish product

    (Elsd on 1978, 402-4), while on e un-

    doubted Breton sherd

    -

    a micaceous

    fabric with haematite painting

    -

    has

    40

    O X F O R D J O U R N A L O F A R CH A E OL O G Y

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    B A RR Y C U N L I FFE

    recently been fo und at P oun dbu ry, just

    outside of Dorchester, in a context

    suggesting a third-century BC date (C.

    Green, personal communication). I t is

    closely similar t o vessels fou nd a t RuguCrC

    B

    Plouvorn (Finistkre) an d K ergourognon

    B

    Prat (Cate-du-Nord) ( G iot , Lecerf and

    OnnCe 1971, figs. liv and xxxvi).

    Altho ugh the list of imp orts is no t long

    it does not necessarily m ean th at the tw o

    areas were isolated from each other.

    Indee d it is hardly likely that the traditio n

    of south-western British dec orated w ares,

    called collectively Glastonbury ware,

    could have developed in total isolation

    from contemporary Breton decorated

    styles: the relationship is surely close

    each area developing in knowledge of the

    other.

    If the archaeological evidence is not

    particularly informative a bo ut the nature

    of contact in the later part of the first

    millennium, the doc um entary evidence is

    specific in its general message that a tin

    trade, involving the Cornish peninsula,

    remained in operation throughout this

    t ime. The

    Massiliot Periplus

    of the sixth

    century, quoted in the

    Ora Mari t ima

    of

    Avienus, me ntions the voyages of Tartes-

    sans an d C arthaginians to is lands in the

    west -

    Oestrymnis -

    close to Britain where

    tin and lead could be had and where

    natives sailed in skin boats. Pliny

    Nut .

    Hist .

    IV.30.16) derives elements of a

    similar story, though in garbled form,

    from Pytheas, a Greek who sailed the

    Atlantic seaways in c. 325 BC; bu t Poly-

    bius writing in the second century BC

    (quoted by Strabo IV.2.1) offers the

    observation that Scipio could get no

    direct information ab ou t Britain fro m the

    traders of Massil ia, Narbo and Corbilo

    when he made enquiries of them some

    time ab ou t 135 BC. Tha t the traders were

    uncom municative does not however mean

    that they had no information to com-

    municate: they may simply have been

    protecting their m onop oly. Th e difficulty

    of obta ining reliable inform ation is ampli-

    fied in th e story of Pub lius Crassus (surely

    not the contemporary of Caesar as

    Stevens argued ) who had to resort secretly

    to tracking Phoenician tra ders to f ind the

    route to the tin-rich Cassiterides of the

    north-west (quoted by Strabo 111.5.1 1 .

    Even if imprecise in its detail, the

    documentary evidence is sufficient to

    show that a complex, and well guarded,

    network of maritime contact existed by

    means of which tin was delivered from

    Britain and Brit tany into the hands of

    merchants acting for Mediterranean

    states. The exact working of the netw ork

    is beyond recovery but a combination of

    short-haul local traffic, transhipment at

    ports-of-trade and long distance expedi-

    tions by Mediterran ean ship-own ers seem

    to be implied. In such a network the

    comm unities of the south-west of Britain

    would have been b roug ht, inevitably, into

    direct an d regular relationship with their

    Breton neighbours.

    Th e actual routes used throu gho ut the

    latter pa rt of the first millennium may be

    dimly reflected in the w ritings of the first-

    cen tury au thor s S t r abo and Diodorus

    Siculus bot h of w hom rely heavily o n the

    works

    of

    Posidonius compo sed earlier in

    the first century (Tierney 1960).Four

    principal crossings were then in op eratio n

    springing from the mouths of the rivers

    Rhine, Seine, Loire and Ga ron ne (Strabo

    IV.5.2). Of the S eine route S tra bo tells us

    tha t cargoes passed via the RhGne an d its

    tr ibutaries overland to the Seine and

    thence it begins its voyage down to the

    ocean an d to the Lexobii a nd Caleti , and

    fro m these peoples it is less th an a days

    O X F O R D J O U R N A L

    O F

    A R C H A E O L O G Y

    41

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    B R I T A I N , T H E V E N E T I A N D B E Y O N D

    run to Britain (IV.1.14). A more likely

    route for goods passing to the west of

    Britain is specified: From Narbo traffic

    goes inland for a short dis tance by the

    River Atax, an d then ag rea ter distance by

    land to the River Garonne . . and the

    Ga ronne f lows to the ocean

    IV. I .

    14). If

    the starting p oint w as Massilia an alterna-

    tive ro u te was u p t h e R h h e an d over land

    to the head-waters of the Loire an d thence

    to the Atlantic. Of the commodities for

    which Britain was famed Strabo lists

    grain, catt le, gold, s ilver a nd iron . These

    things, he says, were exported from the

    island along with hides, slaves and

    hunting dogs (IV.5.2). D iodo rus mentions

    tin as a principal export, noting that

    it

    came from Belerium (Cornw all) and was

    taken on horseback through Gaul to

    Massilia a n d N ar bo (V.22.2; V.38.5).

    T h e difficulty in dealing with these later

    sources is one of chronology. Although

    they may be reflecting long-established

    trade-links, b y the time they were written

    the entire network would have been

    revolutionized by the foundation of the

    Ro m an province in south ern Ga ul in 124

    BC. It is therefore a distinct possibility

    that the works of St ra bo an d Diodo rus

    (building on Posidonius) are in reality

    recording the trade-networks set up by

    Roman merchants and have l i t t le to do

    with the situation before 124 BC. T hus

    strictly it would be anachronistic to use

    these accoun ts in any attem pt to discuss

    mercantile contact before the fou nda tion

    of

    the province of T ransalpina.

    THE R O M A N W I N E T R A D E

    Th e foun datio n of the Provincia in 124

    BC and in particular the creation of the

    Ro m an enclave at

    Colonia Nar bo Ma rtius

    (Narb onne ) in o r abou t 118 BC marked a

    turning point in trade-relations with the

    west . Am ong the wide range of commodi-

    ties passing through the province was

    Italian w ine produ ced in the region of

    Terracina a nd Ca pua an d t ransported in

    dist inctive amphorae of Dressel

    1

    type

    (m app ed a decade ago by Peacock 1971,

    fig. 36). A n interesting insight in to the

    wine tra de is offered by Cicero in his Pro

    Fonteio- a defence of M. Fonteius,

    prop raeto r of Tra nsa lpina in 75-3 (o r

    74-2).

    In

    it we learn of an unofficial tax

    charged per amphora as wine passed

    thro ugh the inland cit ies . This

    portorium,

    it was alleged, was exacted at the rate of

    fou r denari i per am ph ora at Tolosa, three

    victoriat i a t Cu odu nu m an d tw o victor iati

    at V ulchalo. A t Elesioduli six dena rii were

    charged to those who shipped wine to

    the enemy

    P r o

    Fonteio, 19-20). Evi-

    dently there were fortunes to be made at

    the t ime for those who controlled the

    export of wine to the barbarian west.

    Th e distribution of Dressel 1 am ph orae

    gives substance to this trade. The early

    type, Dressel

    1

    a, occurs in som e numbers

    in the region of N arbo nne an d is foun d on

    the route to Toulouse and along the

    Garonne. Considerable numbers have

    recently been noted in Armorica

    P.

    Galliou, personal comm unication), a few

    have been found in Lower Normandy

    (Deniaux 1980) an d the type recurs in

    quant i ty at Hengis tbury Head and in its

    hinterland (Cunliffe 1978 a nd Fig. 12

    below). It is temp ting to suggest tha t this

    was the trade in which the Veneti were

    employed.The use of Venetic middlem en

    would have had the obvious adv anta ge of

    allowing the sou thern m erchants to leave

    the difficult an d unfamiliar waters of the

    Arm orican peninsu la to local sailors used

    to, and equipped for , these potential ly

    rough passages. If such was the system,

    transhipment of wine would have been

    42

    OXFORD

    J O U R N A L

    O F

    A R C H A E O L O G Y

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    B A R R Y C U N L I F F E

    carried out somewhere in Venetic terri-

    tory at Vannes?) cutting out the need for

    intermediate bases like Corbilo on the

    Loire

    -

    a port which had lost its import-

    ance and ceased to be recognized between

    the time of Polybius in the late second

    century and that of Strabo writing in the

    early years of the first century AD

    IV.2.1). Indeed the demise of the em-

    porium of Corbilo may be directly related

    to the causes consequent upon the Roman

    domination of the western trade route.

    Some wine transhipped from the

    Venetic port would have been offloaded

    at other Breton ports; more would be

    taken across the Channel to Britain. One

    might suggest the Quimper region of

    Finistkre and the Rance estuary of the

    C6te-du-Nord as possible locations with

    the potential for serving considerable

    hinterlands. On the Rance a major Late

    Iron Age port later called Alet has been

    discovered on the Saint Servin peninsula.

    Evidence of contemporary Late Iron Age

    activity is well attested Langouet 1978a)

    as is the importation of amphorae

    Sanquer 1978). In Britain the main port

    of entry was clearly Hengistbury Head

    Cunliffe 1978) but it is not impossible

    that other ports in Poole Harbour below

    pp. 46) and Cornwall were also visited:

    evidence is, however, slight.

    Whether or not other Mediterranean

    commodities were transported along with

    the wine there is little evidence to say. The

    only evidence

    of

    exotics in the archaeo-

    logical record are lumps of raw purple

    glass found at Hengistbury, for which a

    Mediterranean origin is likely.

    S H O R T - H A U L T R A D E B E TW E EN

    B R IT T A NY A N D B R IT A IN

    If the analysis offered above is correct,

    Venetic shippers would have provided

    one element in a system of long-distance

    trade initiated, or reinvigorated, by

    Roman merchants. There is also ample

    evidence of short-haul traffic between the

    two sides of the Channel. The clearest

    indication for this comes in the form of

    pottery imported into Hengistbury from

    north-western France. Three categories

    of ware are relevant Fig. 1):

    a) Black Cordoned Wares Wheel-turned

    and finely finished, made in two similar

    fabrics. These types were called Hengist-

    bury Class B wares by Bushe-Fox 1915,

    pls. xvii and xviii) and have been re-

    categorized as Hengistbury Class

    1

    ware

    by Cunliffe 1978, 49). Fabric-analysis

    suggests a north-western France origin.

    The distribution of Black Cordoned

    wares in Britain is limited to the Hengist-

    bury region and t o Poole Harbour but the

    types were widely copied in local fabrics

    below p. 50). In France the distribution

    appears to be north-eastern Armorican

    Fig. 9).

    b)

    Graphite-Coated Wares

    Wheel-turned

    jars and bowls coated externally and

    sometimes internally with graphite

    Bushe-Fox Class H, Cunliffe Class 2).

    The fabrics are similar to those of the

    Black Cordoned wares. In Britain the

    distribution is based on Hengistbury and

    Poole Harbour while in France it concen-

    trates on western Armorica, particularly

    Finistkre Fig. 10).

    c)

    Rilled Wares

    Wheel-turned vessels of

    two basic types: jars with coarse rillings

    down the body and shouldered bowls

    with furrows on the shoulders Cunliffe

    Class 3) . The fabrics are petrologically

    similar, both containing copious mica,

    quartz and felspar suggesting an origin in

    the granitic areas of Brittany. The British

    distribution is much the same as that of

    the Black Cordoned ware but the Breton

    O X F O R D

    J O U R N A L

    O F A R C H A E O L O G Y

    43

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    B R IT A I N , T H E V E N E T I A N D B E Y O N D

    Figure

    1

    Imported north-western French pottery

    from

    Hengistbury. Nos. 1 3 Black Cordoned ware;

    4-7

    graphite coated ware;

    8-9

    rilled ware. Scale

    /+

    distribution appears t o centre

    a

    little to apparent differences are significant is

    the west. The type is not known in difficult to say. All three distributions

    Normandy Fig.

    11).

    overlap in the C6te-du-Nord and it is

    It will be noted that the Armorican most likely tha t from this region the

    distribution of the three pottery types contact with Hengistbury sprang. Of

    varies geographically though whether the possible French port sites we have already

    44

    O X F O R D J O U R N A L O F A R C H A E O L O G Y

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    B A R R Y C U N L I FFE

    ment ioned Ale t on the Sain t Serv in

    peninsula near St . Malo . On pres ent site-

    evidence i t would appear highly l ikely

    tha t

    a

    t rading axis exis ted between Alet

    and Heng i s tbu ry . Two fu r the r obs e rva -

    t ions suppor t th is v iew. On Guernsey a

    la rge se t t lement producing the three

    major Armor ican wares together wi th

    Dres s e l l a amphorae has been found a t

    Kings Road, St . Peter Por t (R. Burns ,

    personal communicat ion) . The Kings

    Road s i te evidently l ies as tr ide the pro-

    posed nor th-south route . Even more

    impressive evidence is provided by the

    dis tr ibution of coins of the Coriosoli tes -

    the t r ibe occupying the Cdte-du-Nord

    area of which Alet is a pr incipal port

    (Cu nliffe 1978, fig.

    35).

    Of the to ta l o f 62

    Arm or ican co ins recorded in Br i ta in ,

    45

    a re o f the Cor io s o l i t e s and

    13

    of these

    come f ro m H engis tbury , mos t of the res t

    f rom the Hengis tbury h in ter land . The

    impl ica t ion c lear ly sup por ts the idea of

    a

    Hengis tbury-Alet axis .

    This impress ive body ofevidence should

    not however obscure the possibil i ty that

    o the r no r th -wes te rn French po r t s may

    have t raded wi th Hengis tbury . Coins of

    the Abr incatu i and Baiocasses f rom

    Hengis tbury are a r eminder tha t o the r

    t r ibes of wes tern Normandy ( the area

    producing Black Cordoned wares ) may

    well have been in direct contact with

    Br i ta in , and Pro fes s o r Gio t has d rawn the

    writers at ten tion t o the imp ort an t , but i ll -

    known coastal s i te of Nacquevil le , a few

    ki lometres wes t of Cherb ourg o n the

    Cotant in where Black Cordoned vesse ls

    have been recorded (Rouxel 1912, 30)

    together wi th Dresse l la am ph ora e

    (D en iau x 1980, 50-1). It is the closest

    po in t o n the French ma in land to Heng i st -

    bu ry a nd a lmos t exac tly due s o u th f rom

    it - a dis t inct navigational advantage if

    sa i ling was regula ted by a n equivalen t to

    the no r th s t a r

    Suff icient wil l have been said to show

    that there mus t have ex is ted a complex

    network of short-haul traff ic plying be-

    tween Br i t tany and cent ra l southern

    Britain in the half century or so before

    Caesar s conques t o f Armor ica in 56

    B C - a far more in t r ica te pa t tern than

    Caesar wi th h is emphas is on the Venet i

    a lone would have led us to believe. It

    could , o f course , be argued tha t the

    appearan ce of French mater ia l in Br ita in

    was

    a

    direct result of fugit ives f leeing fro m

    Caesar . Agains t th is might be p laced the

    evident in f luence of the imp or ted pot tery

    on nat ive manufactur ing over a wide area

    (below p .

    50)

    and the f ac t tha t a more

    detai led analysis of the coins of the

    Cor ioso l i tes shows tha t the co ins f rom

    Hengis tbury inc lude ear ly types and

    do

    no t con form t o th e coin profi les reflected

    in the f ligh t hoards of Franc e an d Jersey .

    Th e impl ica t ion is tha t contac t had been

    main ta ined for some t ime before the

    Caesar ian wars (Gruel

    et

    a 1980 and

    Langouet 1978b).

    T H E W E S SE X C O N T A C T - Z O N E

    Th e d is t r ibu t ion of Armor ican pot tery

    and co inage i s concen t r a ted in an a r ea

    centred on Hengis tbury which we can

    refer to as the Wessex Contact -Zone (a

    concep t equ ally relevant to ear l ier per iods

    to be discussed elsewhere) . In the centre

    of

    the area l ies Chr is tchurch Harbour wi th

    its fine riverine links - the Stour lead ing

    in land in to Dorse t , the Avon in to Wil t -

    sh i re . The harbour i s dominated by the

    prom onto ry of Hengis tbury H ea d , de-

    fended in the Iron Age and intensively

    occupied in the f irs t century BC (Fig . 2) .

    Th e ev idence has been sum mar ize d e lse-

    where (Cunliffe 1978) and s ince

    a

    new

    O X F O R D J O U R N A L O F A R C H A E O L O G Y

    45

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    B R I TA I N , T H E V E N E T I A N D B E Y O N D

    H E N G I S T B l T R Y H E A D D O R S E T

    2 1 6

    8

    1 etres

    HENGIST URY H E D

    u w

    Figure 2

    Hengistbury Head, Dorset and its environment.

    programme of excavations is under way it

    would be premature to say more at this

    stage. Poole Ha rbour can a lso be regarded

    as par t of the contact zone Fig.

    3).

    Two

    sites deserve particular note. Hamworthy,

    on the north side of the harbour close to

    the medieval heart

    of

    Poole, was partially

    excavated before the last war Smith

    1930). Here, beneath Roman layers pre-

    sumably representing a Roman military

    base, the excavation come upon a late

    Iron Age horizon that has never been

    adequately published. The layer produced

    a

    number

    of

    sherds of Dressel

    la

    ampho-

    rae together with

    a

    range of pottery, much

    of

    it imported from France, and including

    Black Cordoned wares and graphite-

    coated wares.

    The second site of some significance lies

    on Green Island close to the south shore

    of the harbour. Here , in a comparatively

    limited excavation,

    a

    wide range of north-

    western French imports

    of

    Hengistbury

    type have been located together with

    sherds of Dressel la amphorae . In addition

    the excavator found

    a

    large number of

    46

    O X F O R D J O U R N A L O F A R C HA E O LO G Y

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    BARRY CUNLIFFE

    cores from the turning of Kimmeridge

    shale arm lets. Th e cores are exclusively of

    Calkin's Class A - a type with

    a

    single

    central square-cut hole for the chuck. The

    association is interesting, no t only because

    i t

    is evidence

    of

    armlet m anufacture, but

    because it is a clear indication that the

    Class A cores belong to the early part of

    the first century BC.

    Th e re la t ionship of the Poole Ha rbo ur

    sites to Hengistbury a nd i ts t rading axis

    remains uncer ta in . The Poole Harbour

    sites are by n o m eans as prolific of finds as

    Hengistbury; but this is, in part at least,

    due to the dispari ty in the size of the

    excavations: Hengistbury is however by

    fa r the largest site. Ta kin g the evidence at

    its face value we may suggest that

    Hengistbury was the port-of-trade and

    that Poole H ar bo ur provided subsidiary

    bases for the t ranshipm ent

    of

    commodit ies

    due to be t ransported in to the hear t of

    ~ ~~

    L A T E I R O N A G E S E T T L E M E N T A R O U N D P O O LE H A R B O U R , D O R S E T

    Figure

    3

    Poole Harbour, Dorset. The present land-forms, with alluvium stippled, showing I ro n Age discoveries.

    O X F O R D J O U R N A L O F A R C H A E O L O G Y

    47

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    B R I TA I N , T H E V E N E T I A N D B E Y O N D

    west Dorset by way of the River Frome.

    Products such as sa l t f rom the harbour

    fringes and shale from the Isle of Purbeck

    may well have been am on g comm odit ies

    brought f rom the immedia te region to

    Hengistbury for wider distribution.

    T he are a designated the contact-zone is

    geographically isolated from the rest of

    Wessex by the wide band of heathland

    spreading from the New F orest to Egdon

    H eat h an d consists of two comparat ively

    fert ile areas: the Purb eck pro mo ntory a nd

    the flood-plain in the immediate hinter-

    land

    of

    Hengistbury (Fig.

    16).

    Th e l inks

    to the densely populated areas of Wessex

    were by the Rivers Frome, S tour and

    Avon. Within the contact-zone raw

    materials abounded: Kimmeridge shale,

    sal t , good pott ing clay (around Poole

    H arb ou r) an d a readily accessible supply

    of high-grade iron ore on Hengistbury

    Head. Th ere can be l it tle doubt f rom the

    British evidence th at these pr od uc ts were

    widely exploited and traded inland, the

    sal t , in i ts briquetage c ontain ers, an d the

    shale, used fo r armlet m anu factu re, being

    the mo st readily recognizable. La ter in the

    first century BC pottery p rod uction took

    on an increasing importance . Whether

    any of these commodities were exported

    overseas is difficult yet to say; but

    lignite bracelets have been fou nd at

    Alet and quantities of roughcut lignite

    bracelets were recovered at Nacqueville

    (Rouxel 1912). In advance of analysis

    however it would be unwise to indentify

    them as Kimmeridge shale. When con-

    sidering exports we should however

    reme mbe r t hat St ra bo specifically refers

    to Bri t ish i ron.

    Th us the Wessex Co ntact -Zone emerges

    as an area i so la ted from the main

    pop ulat io n centres, r ich in natur al mineral

    wealth and provided with excellent com-

    municat ions, by river to Wessex and by

    sea to the m ari t ime regions of Fra nce and

    Bri tain. I ts fine, safe ha rbo urs a nd close

    proximity to F ranc e sui ted i t admirably as

    a region

    of

    maximum contact on the

    overseas t rade network.

    T H E C O N T A C T - Z ON E A N D S O U T H E R N B R I TA I N

    Certa in commodi t ies brought in to or

    produced in the Wessex Contact -Zone

    were distributed t o the W essex hinterland.

    Kimmeridge shale had been a major

    import th roug hou t the second hal f of the

    first millennium. Hand-cut armlets were

    mad e in quan t i ty on Pu rbeck (Calk in

    1955, and Cunliffe and Phillipson 1968)

    and t ransported in land from the e ighth /

    sixth century onwards: there is evidence

    that d is tr ibut ion cont inued throughout

    the fi rst century B C a nd into the early first

    century A D when fine wheel-turned shale

    vessels fo un d their way to the aristocratic

    households of eastern Britain (Fig. 15).

    Sal t

    too

    is a commodity l ikely to have

    been long prized among the Wessex

    arable farmers.

    The development of

    a

    long-distance

    trade and the inject ion of wine into the

    exchange system is well attested by the

    distribut ion of characterist ic Dressel la

    amphorae in Hampsh i re and Dorse t

    within what can be regarded as the

    prim ary distribut ion-zone from Hengist-

    bury (F ig .

    12).

    T h a t a m p h o ra e ( a n d t hu s

    presumably wine) reached Cornwall may

    reflect a secondary distribution pattern

    ema nat ing from Hengis tbury or , a l terna-

    tively, evidence of direct trade to the

    south-west pe ninsula using a po rt such as

    Mount Bat ten .

    Th e distribut ion of Arm orica n coins in

    Britain m ay well have owed som ething to

    the direct trade link: significantly a

    48

    O X F O R D J O U R N A L O F A R C H A E O L O G Y

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    B A R R Y C U N L l F F E

    majority of those from sou thern Bri tain

    l ie within the primary distribut ion zone

    arou nd Hengistbury (F ig.

    12).

    If products such as wine, iron, shale

    an d glass were being fed into the exchange

    systems via Hengistbury we might rea-

    sonably ask what was flowing the other

    way. Strabos list of exports gives some

    indication of what th e Con tinen t desired

    af ter the annexat ion of Gaul , but i t

    ca nn ot be tak en as direct evidence of pre-

    Caesarian t rade. The archaeological re-

    co rd how ever gives some indication, since

    Heng istbury has produced evidence of the

    desilvering of lead (presumably of Men-

    dip origin),

    a

    mass of argentiferous

    copper o re from th e C all ington region of

    Cornwall and Glastonbury-style pot tery

    manufactured in western Cornwall, east-

    ern Devon and the Mendips . I t i s

    tempting to suggest that the pottery is an

    indicator of the regions from which

    commodit ies came: lead from the Men-

    dips; copper/silver ore fro m east Cornwall

    or Dev on; and perhaps t in f rom Cornwal l

    (al tho ugh none has yet been fo und o n the

    site).

    To

    this we might ad d hides fro m the

    south-west, corn and woollen fabrics

    from the cent re south and s laves f rom

    practically anywhere in the region. Two

    maps (Figs.

    13

    a n d 14) sum up both the

    evidence a nd the reasonable speculat ions

    deriving from it .

    THE

    E F FE C TS O F L O N G - D I ST A N C E T R A D E :

    T E C H N O L O G I C A L

    T he mo st readily recognizable effects of

    the patterns of long-distance trade des-

    cribed a bove ar e technological

    -

    the intro-

    duction of the lathe and the potters

    wheel. Th e lathe ha d an imm ediate effect

    on the shale industry: armlets which h ad

    previously been cut by hand were now

    turned, giving rise to a more regular

    product and to the easi ly recognizable

    wastecores withch uck holes. T he industry

    has alread y been described in som e detail

    by Calkin (1955).

    To

    his assessment we

    can now add that the earl iest cores of

    Class A can be dated to the period

    100-50BC on the evidence of their

    association with north-western French

    pot tery on Green Is land (above p .

    46).

    Class

    A

    cores have been f ou nd extensively

    on Purbeck a t Tyneham, Povington ,

    Encombe Obelisk, Gallows Gore, Hers-

    ton , Ho barr ow and Studland, al l of which

    were within easy reach of the shale source

    at K immeridge an d must therefore repre-

    sent a con tinuat io n of the native industry.

    Significantly all but two of the Purbeck

    sites (Ty neh am an d Povington) produced

    the earlier hand-cut armlets as well.

    Outside th e Isle of Purbeck Class

    A

    cores,

    implying shale wo rking on site, have been

    recovered

    at

    Green Is land, Hengis tbury ,

    Glastonbu ry an d Ship ton G orge, suggest -

    ing that raw shale may have been

    exported f rom Purbeck to these locat ions.

    T he exact datin g of Calkins oth er classes

    of core (B-D) is in doubt; most can be

    shown t o be post-conquest but so me may

    represent pre-conquest improvements in

    methods of at tachment to the lathe.

    In add it ion to bracelets, shale was also

    being used to manufacture vessels. Two

    have been fo und on Purbeck a t Rempston

    and Kimmeridge. Fourteen o thers are

    recorded

    though not all

    can be demon-

    strated conclusively to be pre-R oma n) of

    which four occur in the rich Aylesford-

    Swarl ing graves of eastern Bri tain (G rea t

    Chesterford , Old W arden, Barnwell and

    Harpenden). The Somerset si tes of

    Glas tonbury , Meare and Wookey a re a l so

    represented (Fig.

    15).

    If it is assumed tha t

    the vessels were manufactured within the

    O X F O R D J O U R N A L O F A R C H A E O L O G Y

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    B R I T A I N , T H E V E N E TI A N D B E Y O N D

    W e s se x C o n t a c t - Z o n e a n d e x p o r t e d , th e

    tw o ma jo r concen t ra t i ons i n Somerse t

    an d ea s t e rn Eng land m ay repre sen t a rea s

    wi th which th e contac t -zone h ad es tabli -

    shed exchange l inks . There i s however

    uncer ta in ty over da t ing. Al thou gh e leven

    of t he vesse ls c an be sho w n t o da t e t o t he

    p r e - R o m a n p e r i o d n o n e c a n b e p ro v e d t o

    be p re -Caesa r i an . Indeed those f rom

    eas t e rn Eng land a re a lmos t c e r t a in t o be

    da t ed to t he ea r ly f i rs t c en tu ry A D . I t is

    sa fe r , the re fore , to see the sha le vessels a s

    the ev entua l resul t of the in t rodu c t ion of

    the la the wh ich con t inued t o be fel t long

    af te r the in i t ia l con tac t ph ase .

    A mo re widespread e ffect of the per iod

    of con tac t w as a d ram a t i c improvem ent in

    po t t e ry t e chno logy in cen t ra l sou the rn

    an d sou th -w es t ern Br i ta in. T h e impor t a -

    t ion of quant i t ies of f ine whee l - turned

    vesse ls an d the acco mpan y ing know ledge

    of t he po t t er s w heel a ppea r t o have had

    a n imm edia te e ffec t o n pot te ry s ty les over

    a cons ide rab l e a rea . Th e ev idence may be

    briefly considered.

    In D orse t an d ad j acen t a rea s t he ef fects

    of w hee l - turning on the na t ive s ty le

    -

    t he

    M aiden Cas t le -Marn hul l s ty le (Cunl i ffe

    (1974) 1978, 47-8)

    -

    l ead to a t ightening

    of the prof i les of the range of ja rs wi th

    beaded r ims. As might be expec ted the

    fo rm s a re m ore p rec isely t oo l ed an d the

    vesse ls tend to become smal le r . This

    change cha rac t er i z es t he D u ro t r igan s tyl e

    (Brai lsford 1958; Cunliffe (1974) 1978,

    382) . T h e prec ise process of evolut ion i s

    exemplified in a s t ra t i f ied sequence of

    depos i ts fou nd dur in g the 1980 sea son o f

    excava tion a t H en g i s tbury w hich demo n-

    s t ra t e s c e ramic deve lopment beg inn ing

    w i th t he appea rance o f F rench impor t s

    a n d l a s ti n g t o t h e e a r l y R o m a n p e r i o d .

    Severa l of the imported types were

    di rec tly copied by loca l pot te rs , the m ost

    po pu la r be ing the Black Co rdo ned vesse ls

    which give r i se to the necked cordoned

    bowls , typica l of D uro t r iga n assemblages ,

    some t imes ca l l ed H eng i s tbury C la s s B

    derivat ives. The type was suffic ient ly

    des i rab l e t o f i nd i t s w ay to beyond the

    fringes of Du ro trig an ter ri tory. Vessels of

    th i s k ind a re found in t he Somerse t

    region , qui te possibly reflect ing a recipro-

    ca l aspec t of the exchange ne twork by

    which Somerse t lead reached Hengis t -

    bury . Ano ther typ e less f requent ly copied

    is the tazza, while the la t t ice dec ora t ion ,

    foun d o n g raph i te -coa ted j a r s , becomes a

    c o m m o n m o t i f o n D u r o t r i g a n j a r s.

    In Ha m psh i re the effects of the contac t

    w i th nor th -w es te rn F ran ce a r e n o le ss

    appa r en t , g iv ing ri se t o t he N o r the rn a nd

    So uth ern Atreb a t ic s ty les (Cunl i f fe ( 1974)

    1978, 97-100). W heel-tu rning becomes

    widespread whi le cord oned necked ja rs

    and occas iona l ly t a zze a re a recurr ing

    com pon en t o f t he a s semblage . A l though

    it is possible that these areas received

    some in f luences f rom the A yle s fo rd -

    Swarl ing cul ture to the eas t , c lose s imi-

    l a r it y t o t he D u ro t r igan deve lopment s is a

    s t rong a rgu me nt i n favou r o f the st imulus

    emana t ing f rom the Wessex Con tac t -

    Z o n e

    -

    an obse rva t ion s t reng thened w hen

    it is reca l led t ha t e a r ly D re sse l am ph ora e

    are widespread in Atreba t ic te r r i tory .

    A n o t h e r a r e a of t he Sou th -w es t

    to

    deve lop a w hee l-made , co rdon ed ce ramic

    assemblage a t abo u t t h i s t ime is Cornw a l l ,

    where d is t inc t ive cord on ed ware has long

    been recogn ized(T hreip1 and 1957,58-63).

    At S t . Mawgan-in-Pyder severa l whee l -

    made types were c lassified (Types E-K)

    among w hich w e re p l a in bow ls E),

    cordoned bow ls (F ) , t azze

    G)

    a n d l a r g e

    c o r do n e d j ar s ( H , J, K). T he assem blage is

    well represented in Cor nw al l (F ig . 8) in

    the l a s t s t ages o f t he p re -Roman I ron A ge .

    50

    OXFORD

    J O U R N A L

    OF

    ARCHAEOLOGY

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    B A R RY C U N L I FFE

    Th e s imple s t exp lana tion f o r i t s sudden

    appea rance i s as a resul t of exchang e l inks

    wi th the Wessex Contac t -Zone a l ready

    exempl i f ied by the Kimmerdige sha le

    a rmle t s f rom Cornw a l l and poss ib ly by

    the Dresse l la amphorae . Whi le i t could

    be a rgued tha t t he Corn i sh co rdoned

    wares were the resul t of direct contact

    wi th Bri t tany i t should be remembered

    tha t t he A rmor i can cordoned w a re s

    which the Cornish examples evident ly

    copy a re concent ra ted in the eas te rn par t

    of the Armorican mass i f . I t i s s impler

    the re fo re t o see t he shor t rou t e t o

    Hengis tbury becoming the main axis of

    contact with Bri ta in, coastal Bri t ish

    shipping be ing responsible for t ransmi t -

    t ing ideas to Cornw al l . If these v iews a re

    accep ted then the Corn i sh co rdoned

    w are s cou ld have begun to deve lop in t he

    first half of the fi rs t century BC.

    F ro m th e br ie f d i scuss ion offe red here

    i t is c lear that the t rade axis with north-

    weste rn Fran ce , deve loping in the per iod

    100-50 BC, can be cons idered to be a

    format ive inf luence in th e chang ing cera -

    mic technologies of the Atreb a tes , Du ro -

    t r i ge s and the w es t e rn D umnoni i : on ly

    e a s t e r n D u m n o n i a ( D e v o n ) a n d t h e

    sou the rn D obunn i (Somerse t ) s eem to

    have cont inued in t radi t iona l s ty les

    though wi th imported exot ic types . The

    chronologica l hor izon provided by these

    changes is

    of

    so m e significance in asses-

    s ing the soc ia l and pol i t ica l changes

    consequen t upon the phase of con tac t .

    THE EFFECTS OF LONG-DISTANCE TRADE:

    SOCIAL AND POLITICAL

    I t i s not the a im

    of

    t he p re sen t pape r t o

    explore these m at te rs in an y de ta i l except

    to no t e t ha t in m uch of the region cov ered

    by the D uro t r ig i an an d A t reba t i c tr i be s,

    most of the h i l lfor t s, which h ad dom ina ted

    the count rys ide for centur ies , qui te sud-

    denly ceased to be occupied o n any sca le .

    Th e evidence for th i s genera l iza t ion will

    be cons idered e l sewhere toge ther wi th

    possible exp lanat ion s: suffice i t to say th at

    the pr inc ipa l cause i s thought to be the

    c h a n g e f r o m a s i m p l e e m b e d d e d e c o n o m y

    t o

    a

    marke t e conomy. The re a re conse -

    quent changes in o ther aspec ts of the of

    the se t t lement a rchaeology.

    The pol i t ica l s i tua t ion was evident ly

    compl ica ted by pol i tica l t ransfo rma t ions

    taking p lace a t th i s time in the South-eas t ,

    bu t the resul t was tha t , while the Atreb a t ic

    t r ibe deve loped

    a

    coinage cons is tent wi th

    the ir e a s te rn an d nor the rn ne ighbours ,

    t h e D u r o t r i g e s a d h e r e d t o

    a

    silver stan-

    da rd ref lect ing perh aps th e coinage of

    the i r A rm or i can a s soc ia t es . Th a t the

    con tac t w i th nor th -w es te rn F ran ce an d

    beyo nd had comp ara t ive ly l i tt l e e ffec t on

    the pol i t ica l s t ruc ture of the South-west ,

    when compared to the effects of Belgic

    contac t wi th the S outh-eas t , is an indica-

    t ion of the d i f fe rences be tween the na tur e

    of t he c ross -Channe l li nks. In t he Sou th -

    eas t Br i ta in was brought in to c lose

    pol i tica l re la t ionship wi th the C ont ine nt

    -

    a re la t ionship intensified by actual folk

    movement . The w es t e rn ax i s seems to

    have been based ent i re ly upon exchange

    mechan i sms . Th a t it evo lved no fu r the r i s

    a reflect ion of the socio-poli t ical develop-

    ment re ached by communi t i e s on e i t he r

    side of t he Channe l .

    The ques t ion of incoming refugees

    shou ld n o t be ove r looked . T ha t some

    refugees reached B ri ta in fro m the ravages

    of Caes ar in Arm orica i s not unl ike ly . Al l

    tha t can be sa id i s tha t there i s no

    a rchaeo log ica l ev idence to suppor t t he

    idea , unless the few sword bur ia l s of

    sou the rn Br i t ain a r e rega rded a s ev idence

    O X F O R D J O U R N A L O F A R C H AE O L OG Y

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    B R I TA I N , T H E V E N E T I A N D B E Y O N D

    of refugees or of returning mercenaries

    who had learnt new religious practices

    (Cunliffe forthcoming).

    A F T E R C A E S A R

    Th e Caesarian conquest of Armorica in

    56

    BC appears to have put an en d to d i rec t

    trade between the south-west of Britain

    an d north-western France. T he evidence

    is threefold: post-Ca esarian ceramic deve-

    lopm ents in A rm orica are no t reflected in

    Britain; British coinage which developed

    after Caesar is only very rarely found in

    Armor ica a nd N orm andy ; and the in flux

    of Ital ian wine in Dressel la amphorae

    ceases. T he virtual absence of the lb type

    of am ph or a in central southern Bri tain is

    in marked cont ras t to the large number

    now f oun d in the South-east . At the very

    least the d is t r ibut ion pat tern must mark

    a

    dislocation in th e Ital ia n wine trad e with

    Britain, which could be explained in terms

    of new monopolies negotiated between

    the R oma ns and the p ro -Roman t r ibes of

    eastern Britain (Cunliffe 1978, 78-9).

    It remains then to consider briefly the

    post-Caesarian development of the So uth-

    west. At Hengistbury there is clear

    evidence that the site continued to deve-

    lop and in its later stages

    c . 50

    BC-AD

    50)

    it may even have become the seat of a

    mint (C unliffe 1978, 44-7). T hu s its

    continuing function as a commercial

    centre seems likely. It

    is

    now known, as

    the result of th e excavation of 1980, tha t a

    certain level of overseas trade continued;

    bu t

    so

    far the only definite evidence is

    provided by sherds of Spanish , Pa sq ua l l ,

    amphorae ,

    a

    type also found at Cleave1

    Point on the southern s ide of Poole

    H a r b o u r

    D.

    Williams, personal com-

    munication). T he in tensity a nd d ura t io n

    of the t rade is uncertain, bu t no do ub t

    current excavation wil l throw further

    l ight on the problem. That i t appears to

    have h ad litt le effect on local comm unities

    suggests that the overseas links were

    probably not extensive.

    Th e general impression given by Dur o-

    trigan culture in the last century before

    the Roman invasion is of politically

    backward communit ies showing none of

    the socio-economicadvances of th es ou th-

    east . The Dumnoni i in the South-west

    were even w ithout coinage. Th us the post-

    Caesarian period in the South-west may

    have been

    a

    t ime of stagnat ion

    -

    a marked

    con trast to the previous half century.

    T H E C H A N G I N G P A T T ER N S

    If we stand back fro m th e detai l in an

    at tempt to see broad pat ter ns of change i t

    is possible t o suggest fo ur principal stages

    in the systems of contact and exchange

    linking the communities of the Atlantic

    seaways. They may be summarized thus:

    c.

    800

    -

    c.

    600

    BC. Complex con-

    tact involving short-haul exchange pro-

    bably linked ultimately to long-distance

    networks. This manifests itself in the

    regional distribution of bronzes.

    2 . c.

    600

    -c.

    120

    BC. Long-distance

    trading expedit ions for t in (and other

    metals?) involving Greek and Carthagi-

    nian merchants. I t

    is

    possible that the

    foundat ion of the Greek colony a t

    Massilia may have been

    a

    significant

    facto r in inst igat ing the movements. The

    archaeological record app ears to suggest

    that local exchange pat terns were not

    extensive: th ere is intense c ultu ral regiona-

    l ism in Bri t tany and southern Bri tain.

    Mediterranean trade may be reflected in

    the d is t r ibut ion of G reek a nd Carthagi -

    nian coins in barbarian territories.

    3. c. 120-c.

    SO BC. The intrusion of

    1.

    52

    O X F O R D JO U R N A L

    OF

    A R C H A E O L O G Y

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    B A RR Y C U N L I F F E

    Ro ma n merchants into the Atlant ic routes

    trading wine, following the fou nd atio n of

    the province of Tr ansa lpina. Th is pro-

    bably involved short-haul tra ns po rt using

    middlemen. Archaeologically it is seen in

    the d ist r ibut ion of am pho rae and no rth-

    western French pottery an d the develop-

    ment of ports-of-trade at Alet and Hen-

    gistbury.

    Locally in Britain the establishm ent of

    new exchange networks an d the intensi-

    fication of production o n an industrial

    scale took place at various foci , in par-

    ticular the entry-points.

    4. c. 50 BC-AD 43 A reorientation

    of the principal axis of trade. Following

    the conquest of Ga ul, a greater emphasis

    on the Seine and later the Rhine as the

    routes of communication with the Medi-

    terranean w orld, leading to adeve lopm ent

    of British east coast markets. The

    southern ports lose their monopoly but

    retain their l inks with the Atlantic com-

    munities an d remain centres of produ ction

    for their hinterland.

    T h e s u m m a ry ,

    so

    briefly stated, looks

    deceptively simple, but it provides a

    broa d model against which to com pare

    the available evidence.

    To

    complicate it

    with more sophisticated theoretical rea-

    soning would be to go far beyond the

    reasonable l imits imposed by the data

    deep into the realms of unacceptable

    speculation. What is now needed is the

    more detailed excavation of key sites, an

    analysis of changes in the set t lement-

    pa t t e rn and new approaches to the

    numismatic evidence. Much of this work

    is now in hand and the results will , we

    hope, ap pea r in the pages of this journ al .

    Acknowledgements

    This pa pe r is a revised version of a lectu re given

    at a conference entitled Britain an d Brittany held in

    Oxford in January

    1981.

    The text has benefited

    from discussion with Professor Giot both at the

    conference a nd subsequently. The a uth or wishes to

    express his grateful thanks to Professor Gio t and to

    other French colleagues who have

    so

    readily

    responded to requests for help, and to the curators

    of the Red Hou se Museum, C hristchurch and the

    Borough Museum of Poole . Th e maps a re the jo in t

    work of Alison Wilkins (Institute of Archae ology,

    Oxford) and the au thor .

    Institute o Archaeology,

    36 Beaumont Street,

    Oxford

    A P P E N D I X A : T H E M A P S

    A series of

    13

    maps a re offered here to

    provide support for the arguments laid

    ou t in the text. In orde r not t o clut ter the

    text w ith lists of site-names a n d references

    the relevant information is given in the

    extended captions to the maps.

    O X F O R D J O U R N A L O F A R C H A E OL O G Y

    53

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    BRITAIN,

    THE

    VENETI AND BEYOND

    Figure 4

    Amorican axes found in hoards. The French distribution is plotted after Briard 1965. The six British sites

    are mapped by OConnor 1980 map 77 with references p. 586). The sites are Eggardon, Dorset; Nether

    Wallop, Hants.; Danebury, Hants.; New Forest, Hants.; Ventnor, Isle

    of

    Wight; and Tintern, Mons.

    Note

    no attempt has been made to map the hundreds

    of

    isolated finds.

    54

    OX F OR D J OU R N AL

    OF

    ARCHAEOLOGY

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    BARRY CUNLIFFE

    Greek

    and Car thag inJan

    coins

    1 Slcl l lan a x e s

    y v a m i d a l

    i r on ingots

    c3

    Iberian l ibulae

    1

    LmS

    Figure

    5

    Exotic impo rts. Sho wn are various categories of non-local artefacts.

    Greek

    and Carrhaginian coins: based on

    informatio n supplied by Jo hn Taylor. Ma ny if not most of these finds are likely to have been deposited in

    the Rom an period but some must be contemp orary impo rts (Taylor forthcoming). Silician axes:

    Hengistbury Head (Cunliffe 1978, fig. 9) and Rennes region (Briard 1970, 25-2). Double Pyram idal Iron

    ingots: for the French examp les, Gio t 1964.. The British site is Portlan d Bill where tw o ingots were found

    (Grinsell 1958, 137). Fibulae o Iberian type (possibly western French ): the Breton sites are Kerancoa t en

    Erg ut Armel an d Roz-an-Tremen en Plomeur both in Finistbre (Giot 1958). The British sites are Mou nt

    Batten, Devon (Fox 1958, pl. 31) and Harlyn Bay, Cornwall (Whimster 1977, 77-8).

    OXFORD JOURNAL OF ARCHAEOLOGY

    55

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    BRITAIN. THE VENETI AN D BEYOND

    Figure

    6

    Selected pottery types: Early-Mid La T h e .

    Breton stamped wares

    are plotted after Schwappach 1969,abb.

    11. For the Breton style sherds from Carn Euny see Elsdon 1978, fig. 53. The distribution of British

    Glastonbury wares

    is assembled from various sources. The distributions reflect parallel developments of

    decorated pottery styles. The rarer and selected)

    haematire painted wares

    shown are from Poundbury,

    Dorchester inf. C. Green); Rugut re Plouvorn, Finis ttre; and Kergourognon Pra t, CGte-du-Nord

    discussed in Giot 1979, 314-8).

    56

    OX F OR D J OU R N AL OF A R C HAEOLOGY

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    B A RR Y C U N L I F F E

    Figure 7

    Cliff castles and souterrains. To emphasize certain similarities of settlement type in the second half of the

    first millennium we have plotted cliff castles and souterrains. The Breton souterrains differ structurally

    from the Cornish fogous while cliff castles though structurally alike are best seen as a similar response to

    defending a natural promontory. Souterrains see Giot 1979, 292-300 for a distribution map and general

    discussion.of he Breton sites. For the Cornish see Christie 1979 for a recent reassessment. tiff Castlesare

    plotted from various sources including Wheeler and Richardson 1957, G o t 1980, Bernier 1964,OS Map of

    Southern Britain in the Iron Age, Cotton 1958 and, in Guernsey, recent fieldwork.

    O X F O R D J O U R N A L O F A R C H A EO L O GY

    57

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    BRITAIN, THE VENETI AN D BEYON D

    -

    o r n i s h

    Cordoned w a r e

    Henglstbury derivat ives

    Figure 8

    Selected Late La Tene pottery. The distribution of north-western French Black Cordoned ware and its

    British derivatives.

    BIack Cordoned ware

    Cunliffe 1978, fig

    33

    with corrections and a dditions. S ites plotted:

    see list Appendix B p . 66. Hengistbury derivatives various sources summarized in Cunliffe 1978, fig. 32.

    Cornish cordoned ware Threipland 1957 with additions).

    58

    OX F OR D J OU R N A L

    OF

    ARCHAEOLOGY

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    B A R RY C U N L I FFE

    Figure

    9

    Selected Late La Tene pottery. The distribution of north-western French graphite coated wares

    Cunliffe 1978, fig. 33 with corrections). Sites plotted see list Appendix B p.

    66.

    O X F O R D J O U R N A L O F A R C H AE O L OG Y

    59

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    B R I TA I N , T HE V E N E T I A N D B E Y ON D

    Figure

    10

    Selec ted Late La T h e pottery. Th e distribution o f north-western French rilled wares Cun liffe 1978, Fig. 33

    with corrections). Sites plotted: see list Appendix B p.

    66.

    60

    OX F O R D J OU R N A L OF A R C HA EOL OGY

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    BARRY CUNLIFFE

    Figure 1 1

    Nam es and routes. Tribal and place names m entioned by the classical sources show n in capitals, modern

    place names in lower case. The principal routes to Mount Batten and Hengistbury Head are indicated

    assuming northward sailing on a north star equivalent.

    OXFORD JOURNAL OF ARCHAEOLOGY

    61

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    B R I TA I N , T HE V E N ET I A N D B E Y ON D

    Figure 13

    Resources in southern Britain. The Glastonbury ware distributions are based on various sources beginning

    with Peacock

    1969

    and updating.

    62

    OX F O R D J OU R N A L O F A R CHA E OLOGY

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    B A RR Y C U N L I F F E

    Figure

    12

    Imports in to southern Britain. The coins of the Coriosoli tes an d oth er Armorican tr ibes are plotted after

    Allen

    1961

    and Hase lgrove

    1978.

    Dressel

    1

    am pho rae are plotted after Peacock

    1971

    with additions. Sites

    plotted: Horndean, Hants . ; Winchester , Hants . ; Owslebury, Hants . ; Danebury, Hants . (current

    excavation); Knighton, Isle of Wight; Gills Cliff; Ventnor, Isle of Wight; Hengistbury Head, Dorset;

    Ham worthy, D orset; Green Island, Dorset; G ussage All Saints , Dorset (Peacock 1979,72); Ma iden Castle,

    Dorset; Weymouth Bay, Dorset; Carn E uny, Cornwall (Elsdon 1978,403): Trethurgy, Cornw all (current

    excavation).

    Figure 14

    Model for trade in south-west Britain.

    O X F O R D J O U R N A L

    OF

    A R C H A E O L O G Y

    63

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    E

    I

    S

    H

    E

    A

    1

    k

    m

    s

    u

    u

    m

    F

    e

    m

    p

    s

    r

    e

    a

    m

    p

    a

    r

    a

    u

    o

    g

    p

    a

    y

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    d

    y

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    ]

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    B R I T A IN , T H E V E N E T I A N D B E Y O N D

    A P P E N D I X B

    Sites producing north-western French

    la te L a T h e p otte ry

    of

    selected types:

    Black Cordoned ware, graphite-coated

    ware and rilled ware.

    France

    1 Petit Celland, Manche Wheeler and

    Richardson 1957)

    2 Camp dArtus, Huelgoat, Finisttre Wheeler

    and Richardson 1957)

    3 h e Gaignog, Landtda , Finistttre Giot and

    Bourhis 1964)

    4 Stang-Vihan, Concarneau, Fini sttr e Le Roux

    1967)

    Kermoysan, Plabennec, Finisttre Le Roux

    and Lecerf 1973; Le Bihan and Galliou 1974)

    6 Kercaradec, Penhars, Fin ist he Wheeler and

    Richardson 1957)

    7 Tronoen, Port lAbbe, Finistbre Wheeler and

    Richardson 1957)

    8 Kersigneau, Plouhinec, Finis ttre Wheeler

    and Richardson 1957)

    9 Kervedan, Ile de Groix, Morbihan Threip-

    land 1945)

    10 Plouhinec, Port Louis, Morbihan Threipland

    1945)

    11

    Pointe du Vieux Chitteau, Belle-he en Mer,

    Morbihan Threipland 1945)

    12 Saint-Jude en Bourbriac, CBtes du-Nord

    Briard and Giot 1963)

    13 Villers-sur-Mer, Calvados Caillaud and

    Lagnel 1964)

    14

    Saint Malo-dAlet, Ille-et-Vilaine Sanquer

    1975)

    15 Moulin-de-la-Rive, Locquirec, Finisttre

    Giot Deunff, Briard and LHelgouach 1958)

    16 Bellevue, Ploukgat-Moyson, Finist tre Giot,

    Le Roux and Onnee 1968)

    17 St. Donan, St. Brieuc, CBtes-du-Nord Giot,

    Lecerf and Onnee 1971)

    18 G r h e des Rosaires, Plerin, CBtes-du-Nord

    Giot, Lecerf and Onnee 1971)

    19 Bourg, St. Glen, CBtes-du-Nord Giot , Lecerf

    and Onnee 1971)

    20 Rugire , Plouvorn, Finistkre Gio t, Lecerf and

    Onnke 1971)

    21 La Fresnais, Marais de Dol, Ille-et-Vilaine

    Sanquer 1979)

    22

    23 Moulay, Mayenne Naveau 1972)

    Ile Agot, CBte-du-Nord Giot 1980)

    Channel Islands

    101 Mont O rgteil, Jersey

    102 Maitresse Ile, Minquiers, Jersey Hawkes

    103 La Hougue au Compte, Cgtel, Guernsey

    Cunliffe forthcoming)

    104 Les Issues, St. Saviour, Guernsey Cunliffe

    forthcoming)

    105

    Catioroc, St. Saviour, Guernsey Cunliffe

    forthcoming)

    106 Kings Road, Peter Por t, Guernsey inf. R.

    Burns)

    1937, 186-8)

    Britain

    201 Hengistbury Head, Dorset Bushe-Fox 1915;

    Cunliffe 1979)

    202 Mill Plain, Chris tchurch, Dorset Calkin

    1965)

    203 Burleigh Road, Bournemouth, Dorset

    Calkin 1965)

    204 Tuckton Farm, Bournemouth, Dorset

    Calkin 1965)

    205 Wick, Bournemouth, Dorset Calkin 1965)

    206 Hamworthy, Poole, Dorset unpublished:

    Poole Museum)

    207 Green Island, Poole, Dorset unpublished:

    private collection)

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    A L L E N ,

    D.

    F.

    1961: The Origins of Coinage

    in

    Britain:

    a

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    B E R N I E R , G.

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    B R A I L S F O R D , J.

    1958: Early I ro n Age C in

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    B R I A R D , J. 1965: Les Dip6ts Bretons et LAge du

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    Rennes).

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    de Bretagne 77, 11-35.

    B R I A R D ,

    J.

    and GIOT, P-R. 1963: Fouille dun tu mu hs

    de 1Age du Bronze a Saint-Jude en Bourbriac

    CBtes-du-Nord).

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    C.B.

    1969: The Later Bronze Age in the

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    Archaeo-

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