Nyame Akuma Issue 004

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    W0.4 A

    NeWSmm OF

    FRIC N ARCRAPX WGY p r i l 194

    Edited by P.L. Shinnie and issued from the Department of Archaeology,

    the University of Calgary,

    Calgary,

    Alberta, T2N I ,

    Canada

    This number

    of

    Nyam A m i n addit ion t o the usual

    news items

    also

    contains the f i r s t at tempt t o provide a

    l i s t

    of pennit giving

    au tho rit ie s f o r aruhaeological work i n Africa.

    It

    had been intended

    t o publish t h i s i n number

    3

    but that

    k a m e

    becems s o bulky t h a t I

    decided t o postpone pu blicatio n u n t i l nwaber 4. The

    l i s t

    i s

    e t i l l

    very

    inaomphte, several iaportant countries

    am

    no t inoluded, and th

    d e ta i ls f o r some of those given are rather spa.rse.

    I

    h o p in future

    t o

    be

    able t o g i m more detailed information

    and

    a l so t o draw a t ten t ion

    t o any special regulat ions, and possibly t o snnrarise the various

    Antiquit ies

    l aws .

    TO do

    thie,

    need help and would be g ra te fu l i f

    those, with infornation would send it t o me.

    I note that wry l i t t l e news i s ever received except i n ansuer

    t o di re ct requests.

    I w i l l

    continue t o send

    a

    le t ter out about a

    month before publication

    date

    s o l i c i t i n g news, but

    I

    would a l so much

    appreciate

    i t

    i f

    news item,

    sh ort repor ts on research etc could

    be

    sen t t o

    me

    throughout

    the year,

    Please,

    it

    i s not neaessary t o

    w a i t

    t o be asked t o send

    i n

    your news. I

    ant

    always ready t o receive

    it.

    I t had been suggested that Calgary should be the soem of the

    next meeting of our s t i l l so far as I know, namrelass organisation.

    I s h a l l be away i n t he Sudan or Egypt on sabbaticral a t the n o d

    time

    for

    these meetings, which should be

    in

    April

    1975. I

    am

    therefore

    proposing

    t o

    the Steerin g Cormaittee ~ t h e r t o n ,Nelson, Robbins Shinnie

    ?) )

    t h a t i t should ei ther be held

    elsewhere

    o r t h a t

    the

    date should

    be

    changed t o sometime in the

    a U

    o 1975.

    P.L. Shinnie.

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    NOTICE OF FORTHCOMRSL C0 SFL;fRENCE

    The

    7th Annual Conference of the Student Archaeology Assmia tion

    of

    the

    l h ive rs i t y

    of

    Calgary

    w l l

    take place Prm Notbnber

    15th

    17th

    1974. t

    will take the form of

    a

    sylaposj umi on

    PrMtiw

    Teahnology and

    A r t

    Sessions

    and

    workshops

    re

    t o include:

    lithics ceramics

    metallurgy

    text i les basketry and other aspects of historic and pre-

    historic technology

    and

    art nhsm per tinent t o arahaeology.

    The

    conferenae

    w i l l

    be sponeored by both the Archaeology Associa-

    t ion

    and

    the

    eparlmnt

    of Archaeology.

    Correspondence should be add-

    ressed

    to:

    Progrermab Committee

    Departarsnt of Archaeology

    IFnimrsity of

    Calgary

    Calgary Alberta,

    Canada.

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    News of f i e ld ac t i v i t i e s i n Africa, or research subsequent t o

    f i e ld work,

    is

    l i st e d here with the countries

    arranged

    alphabetically,

    except tha t the countries i n which the Brit ish In st it ut e i n Eastern

    Africa works a m grouped toge ther, al so alph abe tic all y, under the head-

    irq

    of E a s t Africa.

    Algeria

    D r

    D

    Lubell of the University of Alberta, reports:

    For the past two

    years

    w have been working i n Alceria on an

    investiga tion of t he p re hi st or ic cu lt ur al ecology of Capsian esoargo-

    t i b r e s i n the region of Tbbessa. The 1973 season, which began i n mid-

    June

    and

    lasted until mid-November,

    was

    funded by the Canada Council

    and undertaken i n cooperation with the Centre Algdrienne de Reaherchee

    Anthropolo~iqwa, Prdhistoriquee e t Ethnographiques.

    O u r work consisted

    of archaeological geologiapl eoolqical survey, excavation,

    and analysis

    of excavated colleations. Personnel, i n addition t o Lubell

    as

    director ,

    were A

    Oautier ( ~ ikauniveraiteit-0snt: palaeontology)

    F.

    Hassan

    (Southern Methodist Univere i ty : archaeology

    sn

    geology)

    J L

    B a l l a i s

    (UniversitB de

    Cam

    geomorphology)

    A

    Close (Cambridge University:

    archmology),

    C

    Chippindale (Canbridge Unirsrsity: archmolagy) and

    A Bouzenoune Univsrsitd d Alger botany).

    O u r primary objective for the

    1373

    season was the collection of

    data on environmental conditions during the period of Capsian occupation

    i n order t o test

    a

    hypothesis of seasonal occupation.

    To

    t hi s end we

    located, mapped,

    and

    sampled several exposures of alluvial sediments

    whioh could be corr el at ed with Capsian s i t e s. One of the se , i n

    the

    Wadi

    e l Redif, i n f ac t conta ins a destroyed escargoti -e. Two radiocarbon

    sanples from these cu lt ur al deposits are dated a t 7340a15

    yrs

    BP

    1.7964:

    ~harcoal)

    nd

    7690s20

    yrs

    BP

    (1-7692: s n a i l sh el l, Helix

    mslanostama) Analysis of t h i s sect io n along with another

    in

    the

    Wadi

    Meeeraa

    and

    a th i rd a t the excavated

    site

    of Ain Mfsteheyia, in di ca te

    sev era l periods of deposition

    and

    erosion more or

    less

    contemporaneous

    with the Capsian occupation.

    There i s in

    addition, evidence i n the

    form of thiak black dep osi ts of clay s, f o r the wide-spread occurrence

    of swamps and/or nwshes which

    may

    dat e t o t he Capsian occupation but

    are mom l ik e ly post-Capsian.

    One radiocarbon sample from these depo-

    s i t s

    i n the

    Wadi

    Meseraa has been dated

    a t 583035

    yrs

    BP

    (1-7963: snail

    shell, species undetermined).

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    kcavations were oarried out a t one si t e , the eaaargotibre of ~

    Misteheyir,

    i n

    th T(rlild m

    Valley

    about 10

    k n south

    of the modern

    t m

    of CMria.

    An area

    of 6 x

    2

    meters w s opened and exoavated t o a depth

    of 50

    on

    with

    the exception of

    o

    square

    exaavated t o s te ri le s oi l

    a t

    1.55 m. wo radiooarbon samples give d a b s of 728N115 grrs

    BP

    (1-7960:

    snail

    shell, WU x

    nslanmtaara) for

    the 46-45 om level, snd 928e135,

    yrs

    BP

    (w n m e ~ xatlanostma) for fhs

    Us-135

    ar level.

    These dates confirm our observations of a brsak in the cultural strati-

    graphy (on the basis of rtif ct bobnology

    and

    typology) at about the

    5 s level, The horitontal exporsnre permitted the tentative identiflca-

    tion of possible wt i v i t y

    areas within th

    s i t e

    which w i l l

    be

    disausssd

    in de ta i l in

    a

    forthcanning report in Ubyca.

    The

    Ulitsd sample of

    l i t h ic a r t ifaots from

    the

    levels below 5 am suggests considerable typo-

    logical va ri ab il it y which

    m y

    reflect seasonally specific activ itie s,

    However,

    further

    exaavation w i l l

    be

    required to verify this .

    A t present work

    i s

    oontinuing on

    analpis

    of modern vegetation

    a-ties f rom collections mpade i n th field, palynology, sedimento-

    logy, palaeontology, and

    tsbulaticm

    of the result8

    of

    the ar t i faot ana

    lyees completed i n Algiere.

    We

    r unable, on the basis of this par's

    results, ei ther to aacept or reject a hypothassis of seasonal ocoupation.

    While

    wle are

    reaeonably carttident that

    land

    anails

    were

    a seasonally

    available resource to Capeian populations, they m y not have constituted

    the prfaaery source of

    protein

    i n

    the

    diet.

    Therefore, the question of

    seasonal habitation mat be deferred,

    Further f ie ld work

    is

    projected

    for 1975.

    All radiocarbon dates were aalculated with the Libby ha lf -l if e of

    5568 years

    and no corrections hatre been made for variations i n the

    atnospheric C 14,

    Botswana

    D r

    Wilrasen of the University of Michigan reports:

    conducted f ie ld msearch among the k ung Bushawn

    l iv ing

    at

    ai a i from August

    1973

    un t i l aid-Janxwy

    1974.

    he s of

    m y

    fieldwork

    is t o ge t a de tai led account of these peoples resourae procurement

    efforts and the way i n which these efforts

    are integrated

    w i t h

    other

    aspects of their

    lives.

    Field methods combine ethnographic techniques

    with those developed by

    n i m l

    ecologists. ham obtained reaords of

    ne rly

    5 kjlls and have

    caatplete

    information on

    all

    of these

    as t o

    species, sex, location of ki l l , date

    and

    time of k i l l method eaployed,

    hunter, and so forth.

    In addition, the

    l e f t

    mtacarpal

    aad

    phalanges

    of

    each

    specimen has been obtained fo r bioohemical Bnalpis,

    These

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    records mre obtained by partioipant observation tsahniques or by inter-

    view on

    day

    of kill.

    The

    pav~yspecies have Plso been monitored both

    within hunting m s and out6ide of

    thescb

    i n order to arrive

    at

    satiu.tes

    of speciea dsnai ties f m t iv i ty ohrrmter ia tias of eaeh speaier,

    The aia

    here

    is t o obtain

    d b

    for osmssing

    W

    ayMlria8 of

    i n t S x ~ ~ Z l l c

    tion batmen Ihrehman

    predators and their prey apeoies. To

    oonp kwn t

    those studies

    an

    ~ o l o g i o a l-y of

    the

    /ail

    area has

    begun

    i n

    the hops of

    determining

    ths extent to whioh

    th

    a p a t i a l patbms wN

    charmturize present day distributions of

    B w b n

    i n the area exten into

    the past.

    hope

    t o be

    able

    t o show s p e c i f i o ~ l yaw s w i n g

    and

    rsao\lrts

    procursmnt a re

    interrelated

    in

    k mg

    organisrrtional

    struoture.

    Ethiopia

    The expsdit ion of Cke Bri t i sh Institute in Eastern Airica has

    continued i t a excavation

    at Axum r X 0 0 ~Janaarg 1974.

    No detail s

    are at

    present

    available. t is

    r lso

    knam

    that F+rofessor

    emand

    Clark of

    the

    University

    of

    California

    Berkeley, has been

    in the fleld but

    again

    no

    details

    ars

    available.

    Mr

    aam

    Sassoon fomer1.y

    i n

    Uganda

    (see N p m e

    llktma no. 2

    (1973)

    8-10) is now ourator a t Fort Jeew Muse=, Hdbasa. He

    is

    also i n

    charge of

    docrm~snting

    sites on the Kenya coast, opening

    selected

    sites

    t o

    th public, and a9srgiag out

    researoh.

    e would 10 publiaations

    offp-hts etc. for tbe F ort

    Jesus

    library.

    Mr. Q r d y , of

    the

    Institute

    of

    Bir faaaStwi ies University of

    Nairobh

    report8

    on

    his

    exoavations,

    at

    Site

    QVJIU/~,

    ukenya

    Hill,

    Whakos distr iot , Kenya October Novembsr,

    1 9 3 .

    Tmnty-eight square meetres of deposit re excavated on th

    Wua

    slope of this site,

    whid ia

    a roaksheltar

    oonta ining

    a number of a m %

    line-paintingrexscuted i n the

    late

    19th century,

    The excavations

    revealed

    two

    wcupation

    aonssr an upper containing rouletted pottery,

    trade goods b o ~ e

    rnaments,

    and dmegtio

    an irrrl bones

    all

    19th

    w n t q

    artefacts,

    wh

    can be assmiatad with the

    I opsr i

    who were

    knawn

    t o ham

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    grased Uvsstoek at ukenya H i l l ;

    and a

    lower containing a

    d c r o l i t h i c ahipped stone assenblage

    and

    a

    ama l l

    proportion of

    macrolithic

    tools, ceranics,

    and

    domstic and non-dolpbstia

    aninal remabe.

    The pottery

    of th8

    lower occupation i s interes-

    ting since it

    is

    identical

    w i t

    the type recognised by Mary

    bakey

    s

    the nHyrax

    H i l l

    variant of Gumban n

    i n

    her excava-

    tions i n the lNeoli thfol midden a t Hyrax

    H i l l

    Another reaently

    discovered occurretnce of

    this distinotive

    type of potteryia

    the Seronera s i te Tansania, whioh

    wae

    investigated by John

    Bower

    The

    importance of

    s i b

    c3v~m/3

    s

    the evidence

    it brings

    t o

    be r

    on the economy of the so-aalled Neolithia rPakers of the

    yrax

    H i l l variant of

    Gumban

    N pottery Both cattle and

    ovicaprids w m present in

    the

    lower occupation at GVJ along

    with

    the bones of -bra and

    warthog

    Conparative data

    on

    the

    fauna of

    th

    neolithic midden

    at Hyrax H i l l

    is lacking but

    m y

    soon

    be

    forthaadng when

    the

    current excavations of John

    Onyango

    are

    conalded. There

    are

    no dates for

    the

    older occu-

    pation

    at

    G V J ~ / ~

    s the results of radio-carbon determinations

    on

    bone collagen

    are

    b i n g

    awaited.

    One might venture t o guess

    that these detsrminatione

    w i l l provide

    dates

    within the first

    millennium

    B.C. as a

    single

    dab

    for nGmaban

    AH from

    t

    Seronera site

    was

    7

    B c ~

    15

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    Hr

    oramly

    also aaka for

    the f

    l l ~

    nnounosnent to

    be

    inserted:

    Thirty

    ailes southeast of

    lairobi

    Kenya

    near

    Luksnya Hill is

    a

    house of six room

    available

    for visiting aruhmologieta and their

    staff Laboratory spuse beds

    lamps and

    p i p d

    water

    are provided

    t

    i s

    hoped that asabrndlogists w l l be able t o rake use of thibi

    faci l i ty regularly

    and

    th r is no charge for usage.

    In order to

    s ve las t

    mixmte

    oonhrsi

    n

    bookbgs nuat be nade two months in

    advance

    b l

    writing to:

    Keys t o t house y

    bO

    pioked

    up

    at the British Lnetitute i n as t ern

    Africa

    chi^ ]^ ,

    Nairobi.

    he following

    map shows

    the best route to

    ulcenya

    House

    Detailed information as t o the

    facilities avail

    to

    Lukenya

    House m y

    be

    obtained by writing

    to Hr

    Oramly.

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    Dr. Bcnrer

    of

    Lake

    l o m a t C o lle ge reports:

    I

    have rea en t ly spe nt s i x weeks i n Nai robi, Dar -esSalaam, en

    P r e t o r i a c o l b c t i n g a t t r i b u t e

    data

    on Oldowan toole.

    his

    work

    r e p r e s e n t s an e x t e n s i o n o f a p ~ o j e c t n i t i a t e d in 1971 oiPed essen-

    t i a l l y at o la riFgLng t a x ( ~ d c e l a t i onah ipe among the various occu-

    rrences of the Oldowan.

    I hope t o oonrplete the

    analysis

    o f t h e e n t i r e

    crorpus of a t t r ibute

    data within

    t he nex t

    eix

    months.

    Hr.

    H t u r i ,

    the

    Direc tor of Ant iqui t i es and Archives sends the

    following aaaount

    1 Lake Ndutu Stone Age S i t s : The Department of Antiquit ies,

    unde r t he d i r ea t i on o f

    A A. M t u r i

    undertook a f i v e m e k p r el im i n a ry

    i n m e t i g a t i o n o f t h e s i t e whioh i a s i t u a t e d n o rt h o f lduvai Gorge

    - ti

    i e

    a

    oont inuat ion of the

    lduvai

    Pleirrtooem depolsite.

    The site

    whioh

    is

    an

    e x h t l a k e, c o n ta in s

    eurf s Artifacts

    l i t t e red on the l a rge r pa r t o f t he Wea te rn shore of the M e ,

    and dur-

    i n g

    the

    r a i n y

    Season

    t h e

    re

    with

    artifwts

    is

    under

    water.

    One of

    the problems which needed t o

    be

    reedred

    w e s

    whether

    the

    a r t i f a c t s

    w r

    being

    t ransported from ou t s ide t he

    lake or =re

    being eroded

    from

    wi th in t he l ake

    bsds.

    An

    area

    approximately 16n x 16m

    w s

    excavated and

    an

    occupa-

    t i on f l oo r wh ich w s covered

    by

    t h e t o p m o s t

    unit

    a sandy c l ay , w s

    exposed, n s i t u a r t i f a c t s and f a a n a l material w r found and wi th in

    the

    occupat ion f loor

    w s

    found a hominid skull. The skull i s now be-

    i n g reaons t ruc ted by I . Ron Clarke

    and

    preliminary d e s c r i p t i o n

    wil l

    be published soon. The Research project oont int lbs

    and

    another season

    is

    planned

    during September

    and

    October,

    1974

    2. Ngorongoro

    Crater:

    The exis tence of burial Hounds i n Ngorongoro

    Cra t e r

    has

    been known ainoe 1907 when a G e m fanrer found them

    while

    qnorrying s t o n e s far

    his

    buildings.

    His a s s i s t a n t s x aa va te d a t l e a s t

    e i x t e e n

    soun s

    and

    he recovered skeletal materials atone bowls

    grind-

    i n g atorme, p e s tl e rubberer, obsid ian art ifmts and beads of semi-

    precious

    stones.

    A s3gtemat ic excavat ion

    of a

    iarther two burial

    mounds one by Dr.H.D. Leakey in 1941 and the seaond by Hamo Sassoon i n

    1967 confi r rmbd that the bur ial mounds contained mult iple inhumations

    and

    among the grave goods were s tone bowls gr i n i ng s t o n e s and p e s t l e

    rubbers

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    They

    ware

    therefore oorm lated w i t h e i a i l a r burials found in

    the Kenya

    R i f t Valley and aseigned t o the Stom Bowl C u l t u r e wh i

    in

    Kenya ware

    dated by Carban 14 t o be tman 900 B.C. 100 B C.. Saeeoon obtsined a

    Carbon

    14

    termination of 300 B.C. from

    bone

    recovered

    Prolp

    the

    burial

    In

    1969 70, the IMpartmnt of Antiq ui tie s

    under the

    direction

    of A A H t u r i excavated two more burial

    m o m ,

    The two

    noun wlere

    found t o conta in only singl e inhumations and they

    had

    no grave goods.

    Stone Bowls,

    grinding

    s toms es t le rubbers were not found,

    though

    pottery s h e d

    and

    obaidhn a r t i f aa t s

    w r

    fotmd f ro l a within

    the

    body

    of the mounds.

    The

    1969 70 excavations ra is ed

    the

    possibility of

    the existence of

    two

    groups of people who though sharing the common

    tradition of urying t h e i r dead

    i n

    mounds, had

    different

    bel iefs and

    material culture.

    In

    1972 and

    1973, the Department excavated another

    six

    burial

    mounds

    Five of these

    mounds were

    found t o be s imilar

    t o

    those excavated

    i n

    969

    70

    oontaining single

    inhumations

    in

    a lea r ly

    defined graves and with no grave goods. Ths si x th which belongs t o

    the

    group of burial mounds of which om waa excavated by Sassoon

    in

    1967

    contained nu lti pl e inhumations a t l e e s t four

    individuals were

    r e p s e n t e d and grave goods.

    Among the

    grave goods -re tcan stone

    bowls, two complete and

    four broken

    grinding

    stonee,

    six

    pestle rubbers,

    four chalcedony and one red ochre beads, and numerous obsidian arti-

    facts .

    An intriguing find

    w s that

    of tw ir on bracelet s found about

    45

    cm below

    the

    surface of the mound in

    an

    area which produced

    a

    f a i r

    concentration of ske le ta l materials. The iron bracel ets

    come

    from

    a

    mound

    similar

    t o

    that

    excavated by Hamo Sassoon

    i n

    1967

    and from whiah

    w s

    obtained a carbon 14 determination of 300

    B.C..

    It i s therefore

    l i k e ly

    that

    ir on technology

    was

    being

    practised

    i n

    East Afriaa long

    before the beginning of

    the

    ItIron Agen.

    Finally, the 1972

    and

    1973 excavations seem t o strengthen the

    po ss ib il it y t h a t the Ngorongoro bu ri al mounds belong t o two di ff er en t

    groups of people with di ff er en t material culture . The temporal

    rela-

    tionship of the two groups

    i s

    not yet de te m he d but samples fo r

    Carbon

    14 dehnnination have been submitted to the

    Oeochron

    Laboratory.

    The

    research project continues

    and

    another season is

    planned

    during

    1974.

    3.

    West Ki li um ja ro : Stone bowls,

    pin ing

    stones, pestle rubbers,

    bored stones (stone rings) and obsidian

    artifacts

    have been found dur-

    in

    farming activities in

    vvly

    farms

    i n

    West K i l ~ ~ a r o ,he circum-

    stances

    of

    the findings were such that

    it

    was not possible

    t o

    associa-

    t e the ffnds and t o determine th ei r cul tura l and chronological para-

    meters,

    nor their

    temporal

    relat ionship

    w i t h s lm i l a r

    fin s associated

    w i t h

    the Ngorongoro burial mounds.

    During

    December 1972, the Department of Antiquities undertook

    a three w ks

    reconnaissance of the

    re

    as well. as preliminary ex

    cavat ions i n one of

    the

    farms-

    dLla

    farm.

    The excavations

    were

    in a

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    i n

    a

    s ignif icant ly

    large

    enough ample

    and

    if

    they can be

    cul tura l ly and logically aesooiated

    w i t

    the rock art then

    i t

    might become reasonable t o in fe r subsistenoe

    patterns

    not

    only b a e d on hunting as

    depiated

    by some

    of

    the pictographs

    but on

    grain

    wild or cultiva ted). Activit y patterning must

    be

    r e la ted t o

    the

    bio-physical environment.

    4.

    Relate the Tamania rock art t o th

    general picture

    of Afri-

    can rock

    a r t

    by recourse t o ethnographic

    as well

    s

    archaeo-

    logical evidence.

    Dr Richard

    L Hay writes

    The present

    ph se

    of

    f i e l d

    work on the Olduvai stratigraphy

    was

    ooonp;ieted i n January, 1974, and

    my next

    a im i r p t o oorlsplete a

    nonograph

    on the O l d d geology.

    smphasis i s

    on

    ths subdivision of

    the

    major

    units

    into lithofaeies, whiah

    are

    i n t e r p ~ s t e d n t e r m of environraents

    see Hay, 1973,

    Quat

    Ree.

    , 3,

    91-560).

    Work

    i s s t i l l

    under

    w y

    by

    J. Buda Soripps

    Ins t

    on the

    racemisation of

    amain

    w id s f o r

    deter

    mining the late Pleistocsne temperature h tory and f o r d ting the

    Ndutu

    and

    Mask

    Beds.

    nd r ew Brook Uhiv. Nairobi) has worked out the

    g en e r a l i~ s dmragnetio atratigr)aphy,

    and

    Allan Cox

    Stanford Dhiv.

    is

    attempting

    t o

    l m a b the Matuyama Brunhea nagne tic tr an si ti on

    700,000

    pars B.P.

    within

    Bed

    N

    D r

    Peter Schmidt of Brown University

    sends

    the following

    report on his work:

    I am finishing

    up the

    major

    portion of the

    BFLhaya material and

    f ind that

    I need

    more comparative evidence on ea r ly ir on working

    before

    I

    fornailate any

    poeitfons

    about

    East AFrican

    linkage

    with

    Meroe.

    As

    a pob t of information, you

    m y

    be

    interested

    t o know t h a t

    I

    w l l be

    returning t o uhaya this

    coming susaarer to

    conduct ethno-

    graphic nd metall urgi cal experfarents

    i n iron

    srsltfng.

    A s ~ 1 1

    w i l l

    continue limited excavations of

    the

    ear ly

    iron

    age in

    the

    area.

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    Ghana

    r A Smith of the University of Ghana sends the following:

    A v i s i t

    was

    made with students from the Departnent of Archaso-

    logy, Univerrsity of Ghana over Chris t ras break 1973 t o Basumpra Cave,

    Abetifl. Since Professor Thur8h Shaw s excava tion in

    l*3

    ~raa .of

    the

    reh hi at.

    Soa. 1W Vol. 10:l-67) was performed p rio r t o th e

    advent of

    C 14

    dating we excavated

    a

    small witness seotion t o re t r ieve

    organic remains f o r dating.

    Samples of chasooal

    were

    r e t r l e r ed

    frau

    a l l

    l ev el s t o 1lOoaa.. e

    well

    as carbanieed

    remains

    of the o i l PalmA

    Elaesis

    ineensis, - i o a depth of

    at least 80cm

    The

    existence of Che

    o i lw i~ ~ ~ siem wa i t s

    opinion of

    mveral

    botanists.

    Charcoal samples have been sen t t o Rikrsgaka Kenkyasho, Japan

    for processing, O n e

    of

    th es e san ples from 100-110om. should give

    us

    a date for the

    pm-pottery

    niorol i thio industry/pot tsry wing transi-

    tion.

    Certainly th4 existenoe of the casbonised o i l palm kernels to

    a t l e a s t 80cm. suggests that the use of this plant gous back a long

    way

    These examples m y w e l l

    be

    the oldest known a r d w o l o g i c a l

    speeiaaens from West Africa.

    I

    would

    appreciate

    ny

    of the

    readers

    of

    Nyame Akuum who might know of any oth er exoqplerr ge tt in g i n touch

    with me .

    This report

    has

    been received from the Ghana National Musetnu:

    The 5th of January, 1974 saw th e o f f i c i a l opening of t he West

    African

    Historical Museum at Cape Coast by Commder J K medume

    deput is ing fo r the C d s s i o n e r fo r Education and Culture Col. Nyante.

    The Museum

    is

    t o be a Centre f o r Research in to West African History.

    Thus the exhibits refleet not only the period beginning with European

    contact with West Africa

    fr m

    about the 13th t o l a t e 19th century,

    D u t a ls o some Stone Age b p l e m n t s , that

    i a ;

    the period before the

    Buropeans i n West Mrioa.

    The museum is housed

    i n

    a ca st le of Danish or igi n and th i s adds

    t o the uniqueness of

    the

    Mueem

    and i t s

    task.

    The building i s i t s e l f

    a monmaent. A p a r t hm being a m u m u m part of wing is going t o

    be

    converted into a theatre t o o f f e r

    f u l l

    f a a i l i t i e s f o r c u l t u r a l a c ti vi -

    t i e s .

    Diorama show:

    On th e 5 th of March the National Museum mounted

    an

    exhibition

    i n

    i t s

    main building at Accra.

    This is

    an

    extraordinary exhib ition

    because, f o r the

    f i r s t

    time

    in

    the Museum s h is to ry si nc e

    1957,

    the

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    e x h i b i t i o n was mounted in

    a

    n a t u r a l e c o l o g i o a l s e t t i n g .

    It was an

    a t tempt t o d i ap l a y w e u m ob;iecta

    in

    a

    f m s i n d l e of t h e i r

    real

    l i f e

    s e t t in g t o afford

    an

    easy uomplrehension. It por t r ays an indigenow

    I r o n Smlting group aa p r a c t i s e d in t h e Upper Region of

    Ghana

    eoas

    40 5 p r ago. Everything w e d

    waa

    aa thsn t i e .

    The proueae was

    demonstrated by a blookwsith Woobari Angko of Tiaa villegs

    i n the

    Lawra d i s t r i c t of Upper Region,

    The l i f e - a i s e u s s t 8 o f the blenk-

    s n i t h h b e l f and his m a t s t a n t s

    were

    cade

    by Mr. Asa-Anakwa

    a

    diorama t echn i c i an o f

    the

    Museum, The

    display

    i t a e l f was the outuoine

    of the researuh

    work undertaken

    by ,

    L M

    Pole one of th e A ssi s ta nt

    Keepere of

    the

    Museum, The Museum of th e U niv e rs i ty of

    Ghana

    on 14th

    March had

    i t s

    new cramprehenaive exhibition o p m

    by

    Dr. OkucAmpofo

    t o

    nark

    t he s i l v e r Jub i l ee o f t he Univsra it y .

    New

    Apwintnmnts and Movemnts:

    M r .

    K A. Myhs

    Keeper, has

    been appointed

    Acting Director of

    the National Huseura and Mr. Jones Asante h w been appo inted A ssi s ta nt

    Keeper (His tory) for

    the

    West African Historiual Hnaetor.

    The Mreotor

    of the National Museum will soon be on

    t w o - p a r

    sabbatioal l e a v e in

    Canada.

    With the

    number

    of t he Cura to r i a l

    staff

    i n

    both

    Ethnology

    artd

    Arohaeology inmasing plans are a fo o t fo r f i eldwork . Mr, Leonard M.

    P ol e s work

    on

    Indigenow Iron Smelt ing,

    *oh

    culmina ted t o t he

    mounting of

    tbe

    diorama exhibit ion mentioned above, I hope is well

    k n m t o you

    An

    in t ro duc tory reseaah on beads n

    the

    Jasikan area of

    the

    Volta Region

    had been

    undertaken by

    Mr. E.K.

    Agorsah.

    It

    was a i m d a t

    recording th h i s t o r y , 1~(~1ufwture

    nd

    use of the beads, as a l s o t o

    know t he

    raw

    materials w e d , as

    w e l l

    as m y o t h e r r e l e v a n t

    data

    It

    is

    more or less a foundat ion work f o r future

    research.

    A t Efutu near

    Cape Coast, a pre l iminary a rchaeologica l exuavat ion has begun under

    W.

    E.K.

    Agorsah.

    Also

    in

    FO@ S8

    i s

    ~ a h a s 0 1 0 g i C d

    -y

    of

    once an Iron Szaelting village a t Okyirikoaf o

    near

    Accra by Dr. 1 N .

    Debrah.

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    Ivory Coast

    The

    following is supplied

    by

    Professor

    Hauny

    of

    the

    University

    of Paris:-

    Philippe Leclerc

    is

    at the Hission dfiAi de e t de Coophation,

    B.P. 1839, Abidjan since

    l a s t

    par

    st

    in bad conditions the

    shell-mounds of the Lower Ivory Coast lagoons.

    I

    saw hir and

    he

    prepared

    a

    paper

    on his work.

    These mound6 seem

    definitely

    a r t i f i c i a l ,

    but

    there

    exist alrao sans natural oms.

    I

    shoclld be very glad i f our

    Ghanaian colleagues would study those on their

    side

    of

    the

    border.

    Liberia

    In Nyam A k m no.1 1972). 12 D r Creighton Gabel of Boaton

    University announoed a forthcoming project

    i n

    Liberia.

    This pro*ct

    is

    now under way

    and

    the f irat p rt has been completed.

    Dr.

    Gabel

    sends this

    report:

    Beginning i n January 1973 three archamlogists frola Boston

    Univ ersity undertook an archaeolo gical survey which w s funded by the

    U.S. Educational

    and Cu l t u r a l

    Foundation in

    Liberia.

    Creighton Qabel

    w

    proj ect di re ct or , as si st ed by Ph.D stud ents Robert

    B

    Borden

    and

    Susan L Whits who w s also supported by

    a

    fellowship from the Canada

    Council). Gabel

    wa

    i n Liberia until late August, Borden until

    October, and White until

    early

    Dsoember.

    During

    the

    l a t e r montha of

    the program, Borden conoantrated primarily on lithic industries

    and

    Me. White on t r ad i t io n a l iron-working, combining th e moording of

    archaeological and ethnographic

    materials

    with col lect ion of ora l data

    obtained

    frow

    Lama,

    Bandi, Mandingo, Mano,

    and

    K i e s s i saitha.

    The

    areas

    of t he country i n which th e group worked ineluded t he western c oa st

    and

    hinterland, ce nt ra l Liberia, the northwest, the northeast, and

    Caps

    Palmas on th e southeast coast. The heavy fo re et cover i n la rg e sec to rs

    of

    the

    eastern and western interior

    and

    the lack of access by road t o

    mmt of the c e n t r a l and eastern ooasts made it di f f ic ul t t o do nuah in

    those regions.

    The coast between Buchanan and Harper deserves thorough

    survey by boat because of th e in te ns it y of European tr ad e

    fram

    the 14th

    o r 15 th centu ry onward

    and

    the many

    small

    is la .. de which have long been

    used

    as

    tribal burial grounds.

    The pote ntial richnesa of the la t t e r

    was

    amply bm onstr ated

    by

    examination of coastal cemeteries

    and

    one

    remarkable ossuary

    at

    Cape Palmas

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    Preeminent among

    th

    antiquit ies of the int erio r are vestiges

    of former towns

    and

    villages, although most

    are

    of no great antiquity

    and

    few disp lay much depth of Aidden accumulation (due to the prac tice

    of swidden rice cultivation

    and

    patterns of endemic tribal warfare).

    They are also abundant along the coast, whem erosion of beaahes

    lagoon bluffs, and tidewater riverbanks Irskes sites of these and

    ea rl ie r types easi er t o loaate.

    The earliest archaeological oacurrenoes noted were oms of

    broadly nSangoann appearance, charmte ri zed

    by

    heavy picks, choppers,

    and

    scrapera. About ten suoh

    sites

    were identified

    i n

    the vicinity of

    the lower St. Paul River weat of Monrovia, assoaiated with su bs ta nt ia l

    qu rtr

    dikes. Most are ordinary surface or road-cut sites although a

    couple

    of

    stratified ones

    were

    found on the river itself,

    and

    probably

    represent quarry workshops.

    Micro li thic e i te s without pot tery wewe observed in several

    instances, but with two or throe exceptions these also were surfaae

    occurrences.

    Single speaimns or

    small

    sca t te rs

    w r

    collected even

    i n areas of high bwh. t one rook s hel ter i n the far northwest,

    near

    the borders w i t Sierra hone and Quima, t e s t excavations produaed a

    miarolithia msemblage n strlatigraphio aaaooiation

    wit

    oarmias of

    rude fom.

    ocasparable si tu at io n was found t o p reval l a t another

    shelter in the northeast interior.

    These m y approximate somthlng on

    the order of

    the

    wI)uimaN ~ o l i t h i c . ~

    Microlithic assemblages include outils escruilldes

    burins,

    ir re gu la r sarapers, baoked flakes o r b-s occasional small unifa-

    c i a l or b i fac ial pointe, and rar e geoaaetria segments.

    None was associ

    ted with axes or other heavy impleaents of ground stone.

    C e r d c s i t e s abound i n most areas.

    oeae coastal ones incorpo-

    rate European trade goods such as crockery, gl ass, clay pipes, stone-

    ware

    beads and

    brass ornaments. Locally-made i ron a r t i fac t s al so

    occur, although their survival valw on the whole is limited.

    Most

    of the sites with or without European trade materials probably should

    be

    viewed

    as

    late prehistoric

    o r

    recent,

    a t

    lea st unt i l such

    a

    time

    as

    evidence t o the contrary

    is

    produced.

    Relative dating, especi al ly when

    European imports

    r

    absent, is difficult sinae there are few archaeo-

    logical or ethnographic ceramic colleotions available for comparison.

    The sca rc ity of habitable caves or sh el te rs and of deep settlement

    laiddens

    of

    any

    kind

    makes

    the problem worse.

    However

    the ceramic

    sansples which

    were

    obtained

    w i l l

    provide at l e a s t a preliminary frame-

    work fo r the later Iron Age and historic periods i n some

    areas.

    Apart

    from the Stone Age industrie s, the most fr u i t f u l opportunit ies fo r

    reeearoh a t the moment probably l i e i n tr ac ing of t r i b a l movements over

    the past few centuries, combining the evidence of o ra l tra di ti on with

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    ar ch ~o lo gi oa l nves tiga tion.

    The saw ccmmnts re generally applic-

    able t o the smelting sites seen.

    With two or three possible exceptions,

    these seem t o

    be

    of quite recent origin, although the procureiwnt

    and

    reduction of iron ore m y be somewhat more

    widespre d

    than formerly

    believed.

    In the project report being submitted t o the sponsoring agency

    and the Liberian Government, a number of recommsndations for the future

    are included.

    Among these re a plea for continued use of the SASES

    grid for recording sites

    and

    artifacts; the promotion of joint research

    by

    historians, linguists

    and

    archaeologists; recording and preserva-.

    tion of Liberian arts and crafts, with part icu lar reference t o th ei r

    sociological significance; identification and dist r ib ut ion s tudies of

    imported tr ade go ;

    and the

    preservation

    and

    protect ion of antiqui-

    t i e s .

    From Hr. A Smith, University of Ghanar

    I intend t o lead a j oint archaeological geological expedition

    t o the Azaouak Valley, Niger next December.

    An archaeological

    reconnaissance

    w i l l

    be made of the region Prom I n Abangarit t o th e

    M a l i

    border we i n i t i a l l y intended t o work in

    M a l i

    too but

    I

    have

    been informed by the I n s t i t u t

    des

    Sciences humaines, Bamako t h a t a l l

    researah i n the

    5 t h

    and 6th Regions of

    Mali

    has been provisionally

    suspended

    dw

    t o

    the

    current drought). We also

    intend

    t o excavate

    a t T a m p Nellet or Tafer j i t depending on which site

    w i l l

    give the

    most information.

    The expedition

    w i l l

    include

    Dr M.R.

    Talbot,

    Departmnt of Geology, Univsrsity of hana and Dr. M A J W i l l i a m s

    School of Earth Sciences, Maquarrie University,

    N.S.W.

    Australia.

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    tion near the mouth of the shelter.

    Although there was vir tua lly no

    vert ical s t rat igraphic different iat ion,

    i t

    ha8 been possible

    by

    seriat ion teohniquss t o divide

    this

    baad into three phases,

    A B

    and

    C.

    In the latest Phase,

    C

    lnicroliths

    are

    associated with pottery and, a t

    one point outside th dr ip li ne , two i ron f'rag~l~bnts. l here

    are

    f ive

    radiocarbon age-deterrainatims for th Phase, on from the bottom of

    i t

    fa l l ing ne r the middle of the th Century

    B.C.

    and four f r o m the

    top ranging

    f'rom

    the 15th t o the 17th Centuries A.D.

    It is clear that

    cultural.

    material

    i n the 10-15

    ca.

    Immediately below

    the surface

    is

    Plixed

    and

    probably includes,

    int r

    U a , pot te ry brought t o the s i t e

    by Fulani

    herdsmen

    sheltering re

    i n

    bad weather.

    I n

    Phase R where the lnicrolithlc

    industry

    reaches its grea tes t

    vertical concentration,

    there

    is

    als o som pottery, but

    there

    i s

    a

    ole ar diffe rence between this and th Phase C pottery; and a shallow

    but definite stratum exists between the two Phases which aontcrins no

    pottery at

    all.

    The Phase R pottery is i n

    v ry

    poor aondltion,

    and

    i s largely nondescript;

    where

    decoration is diaoernible,

    it is

    of

    the

    comb-impression type.

    Two radiooarbon age-determinations ex is t for

    this Phase, th upper falling in the la te

    rd

    Millennium

    B.C.

    and the

    lower in the l a t e

    5th

    Millennium

    B.C.

    Phase A i s distinguished

    from

    Phase

    B

    largely on seriation;

    the

    fmquency of ar t i f ac ts d r o p sharply,

    and

    the

    inbrfaoe

    between

    the

    two phases

    is

    marked a t one point by a large f l a t s l a b of rock 1.25

    x

    1

    m.

    in

    rsise aml about

    30m

    thick, which f e l l out of the roof a t the

    end of Phase

    A

    The cav ity i n the roof is s t i l l visible,

    Thereafter,

    this

    s l ab aas the focus of activity i n Phase B

    judging

    by the concen-

    tra tio n of factory w ste over and mound it There

    i s

    one radiocarbon

    age-detennination for Phrrse A which falls i n

    th

    mid&* Millennium

    B.

    C

    There is thus

    an

    inversion betmen the early Phaae

    B and

    the

    Phase

    A

    dotermhatione, but i t should

    be

    noted that the samples pro-

    cessed

    were

    s t r a t i f i e d i n the

    samo

    square without possibility of

    Phatse overlap.

    further age-determlnation exists for a louer level, below

    the cul tural

    noterial

    altogether and bove bedrook, which fa l l s i n

    the la te

    6th

    o r ea rl y 5th MUlennium B.C.

    The mlcrolithia indastry

    is

    homogeneous, and similar i n many

    respects t o t ha t exoavated

    a t

    Ropp Rockshelter by

    B.E.B.

    Fagg (I*)

    and E.O.

    Eyo

    (1964).

    soab

    50 km. southeast of h t a e n Kongba.

    Over

    9 of the material is quartz 8@ white opaque and 1 ranslucent

    colourless or smoky),

    whib

    other materials present are bssa l t

    and

    granite

    Taking

    the

    Ut hi c material i rm the three Phaaes together,

    a

    to ta l of 39 898 i t e m , the breakdown in to typea i s

    i n

    outline s

    f olloo~zr

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    Cores

    3 746

    Flakes 10.9

    Blades 4.0

    Borers, Sorapera,

    Points, Lunates 0.4

    Trapezes, Chieels

    Debitage 81

    0

    100 6

    Morphological. analysis i s

    s t i l l

    incoaaplete but the model range

    of

    blade

    siees, for example,

    i n

    Phase

    C

    is

    as

    follons:..

    Length:

    14

    ]BPI.

    Breadth: 5 - 7 m .

    It is noticeable that a high percentage of the

    smaller

    artifants

    a m nade of clear oolourless quarts although opaque

    white

    quartz is

    the dominant material

    n general.

    uring

    the oourse of the excavation, a rock-gong similar t o

    those first reported by Fagg (1956, 1957) w ~ r discovered i n a aorridor

    leading off the rook-shelter. It

    has

    two notes,

    ur a

    aeries of c l e w

    chatter-marks,

    and is unwual

    in being

    n a

    vertical rather

    than

    a

    horisontal

    plane;

    it uansists of a f l a t slab of grani te wedged upright

    i n

    a

    oleft between

    two massive boulders. A

    pressure-flaked hollow-

    based arruwhead i n whitish chert, very closely analegoue t o hollow-

    based mowheeds from Ntemso

    i n Ghana,

    was found washed out of the

    surface

    i n

    the corridor

    after

    r a n n July,

    1973, during a

    visit

    t o the

    site by

    the exeavatora

    after

    the

    r r jn

    excavation had been com-

    pleted.

    Supplementary exaavation wars therefore

    rried

    out in th

    corridor, and a third type

    of

    pottery,

    g r d

    tone axes and hammer-

    stones

    were

    discovered stratified in

    a

    single oultural layer.

    No

    her

    pressure-flaked ifacts

    wetre

    found.

    Two radiocarbon

    age

    detenrinatians were obtained

    for

    this material, falling i n

    the

    first

    and

    fourth

    quarters

    of

    the 2nd

    Millenniua

    B.C.

    The exoavators currently inter-t the ~ c r o l i t h i c ndustry

    in

    the

    main

    shelter

    as

    the prodnut of a nomadic hunting carraaunity who

    used

    the shelter s

    a

    fwtory s i t e at

    regular

    intervals

    from

    sose

    time

    i n

    the 4th HUennim

    B C

    onwards, until

    at

    least the Ist

    Millennium

    B C The upper age-limit of the aicroli thic industry i e diff icul t

    t o

    deteraim because of

    the mixing i n

    the upper levels;

    but

    it is

    worth remelnbsring that the age of similar material at Rop

    is

    thought

    t o

    be

    early

    1st

    llennium

    A D

    S

    radia w e of the rook-shelter

    at

    G

    uben

    Kongba

    by laaa l

    people8

    i n H

    tor ic

    tire is

    clearly indiaated.

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    It

    appears l ik el y tha t tihe rock-gong

    m y

    have been

    i n

    use by

    th

    2nd

    Millennium

    B.C., since hammrstonee dropped below it uere found streir

    t i f i e d in deposits of

    that

    age.

    A t

    th ia

    period

    also people wing

    ground stone axes and poarribly pressure fl d arrawhsub appear t o

    have freqwntod the oorridor and

    p s u r o b l y

    th shelter a8

    11.

    A series of samples of organia material was

    recovered

    by

    flotation From each level

    of

    the exaavation,

    and is

    ourrently being

    analgsed.

    EYO,

    E.O.

    1966.

    1972

    FMG B.E.B. 1944

    1964. Exoavations a t Rop Rookshelter.

    West Af r . ArcheAtol. Ihmlstter

    3r5-14).

    Rop Roakaheltsr,

    Nigeria.

    W. Mr. Arahaeol. Newsletter.

    2

    Rop Rock Sheltcbr Excavations 1964.

    W.

    Afr

    J Ardwology. 2~13-16)

    PreUdmry report

    on

    a

    n ic ro l i th ic

    industry a t Rop rockshelter, I Nigeria.

    roc Prohist. Soc. 10:68-69).

    The rockgong omplex today and i n pre-

    hi st or ic times.

    J . ~ i s t . SOC. Nig. : 27-42).

    Rockgongs and rock-slides .

    - 57: 112 .

    Rop Rook Shelter Excavations 1944.

    W.

    Air. J. Arohaeology. 2: 1-12).

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    South Afr ica

    NEW DISCOVERIES AT EARLY

    IRON

    AGE

    SITE

    24/73, BROEDERSTROOH

    TRANSVAAL,

    SOUTH AFRICA From Pro fesso r R.J. W o n , U n iv e rs it y

    of th Witwatererand.

    Fielduork

    in

    December,

    1973 and

    ~ a n u a r y / ~ e b r u a r y974 a t t h e

    A.D.

    460 site of Brmders t rooa UCWL l f91

    B Prof

    R. Protsoh) has

    increased

    th

    number of

    known

    h u t f l o o r s a t th

    site from

    t o W

    The appraximate area is over 10 acres.

    S i t e 24/73 may t h e r e f o r e , be

    t h e l a r g e s t

    and

    e a r l i e s t s e t tl e m e n t p re se rv ed i n Af rfca so u th of the

    Sahara

    Fzcravationa by

    D r A.

    van Genderen a t l o c a l i t y 24/73

    U

    on the

    s ou th e a s t psri lpster o f a i t e 24/73

    hare

    revealed an o r n m n t - m k e r a

    working f loor approximately x 3 getres i n area

    On the f l o o r

    Dr. van Genderen discovered a s in g le s h e l l o f Conus hebrcriow

    the

    only such shell known i n t he i n t e r i o r of South M o a i n d i o a t i n g

    c o n t a c t with t h e t r o p i c a l c o a s t l i n e

    several

    hmdmd k i lo ~ n e t re s o th

    eaert as we11 as

    oowrie

    s h e l l s , q u a n t i t i e s o f o s t r i o h e g g s h e l l b ea ds ,

    worked bone and t o r t o i s e s h e l l

    and

    i vo r y f rag rsn t s . La te r S tone Age

    s t y l e s t o n e a r t e f a c t s m s o c i a t e d w i t h the I r o n Age o r n m n t s

    suggest

    that Later

    Stone

    Age

    people were aatually working within the p a w i n c t s

    of the

    24/73

    I r o n

    Age

    v i l l age .

    I n Demmber 1973 site 105/73 was discovered near Thabaaimbo

    several hundred kilcmretres t o the north-west of 24/73, with p o t t e r y

    and

    furn ces

    sfsilar t o t ho se at 24/73.

    indicating

    a vide d i s t r i b u t i o n

    of the s me Early

    I r o n

    Age t r a d i t i o n .

    I R O N AGE RESEARCH WORK 1973-1974 I N THE EASTERN TRANSVAAL

    .AFRICA Fram

    T.M.

    Evers Depastaabnt of Archasology,

    Un ive rsity of t he W itwatersrand, Johannesburg,

    TW sets of excavations have been carr ied ou t .

    1

    I n t he Wunic ipal g rounds of W n b u r g ,

    partly

    f inanced

    by

    t h a t

    Municipali ty , excavations

    revealed a

    well-preserved

    E a r l y

    I r o n

    Age

    site w i t h c a t t l e and s he ep t e e t h and p o t t e r y i n p i t s .

    Burials, as y e t

    t o be completely exoavated, are probably aesociated.

    Dates are

    expec ted to

    be c

    A.D.

    500

    Exaavations of a Late r I ron Age s t o n e

    w a l l

    si te

    a l s o proved informative.

    h u t f l o o r w s c l e a r e d

    and

    was found t o

    be

    composed of atone paving: and

    mud

    p l a s t e r .

    P o t te r y ha s a f f i n i t i e s

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    w i t h

    the nearby s i b of Badfontein *oh has produoed a l a t e A.D.l%h

    Century date.

    2.

    A t the Mineral spring nd vicinity of Eiland, o the south

    bank

    of the Groot Utaba, a large s lt works w s discovered and ex-

    cavated. Excavations revea led a aomplete sequence of Early Late

    Iron Age i n three atages.

    The Early Iron ge pottery i s l i k e t h a t

    from the nearby

    si te

    of Hanaony. The Middle Iron Age has a f f in i t i e s

    with Schofieldls M pottery from Mapungubwle

    and

    has been d ted t o the

    12th Century

    at

    the

    site

    of Silver Leaves 40 ailes

    from

    Eiland.

    The

    l a t e s t pottery

    i s

    s imila r to th a t f r o m Phalaborwa

    and

    Harmony

    and pro-

    bably dates between 1300

    and

    1900 A.D.

    An

    iron

    smel ting Iturnace, associated forge

    and

    l iv ing

    site

    w s

    partly

    excavatsd. They

    lie

    about 5 miles south ea st of t he s lt works.

    A date i n

    th

    14 th Century

    A D.

    i s expwted.

    From A J B Humphreys Alexander Mcgregor Memorial Museum,

    Kimbsrley.

    A t

    the beginning of

    1973

    the Alexander

    HaOregor

    Xeaorial

    Mweum initiated a projeo t on the Later Stone Agen of th e Kfnbarley

    area. I n i t i a l attenti on h w been foauesed on

    a

    ser ies of ro k shel-

    ters occurring

    n

    th Kaap Escarpment, m a t of Kimrberley.

    To date

    preliminary inve stiga tions have been undertaken in two of the shelters.

    Radiocarbon dating

    has

    placed the base of epos it i n om of the

    shelters (Dikbosch) at between 12 and 14 thousand ye rs

    B.P.

    and

    although th samples of cultural m teri l from

    t is

    period h ve been

    rather ertuall s o far, the possibili ty does e x i e t of establishing a

    long seqmncm fo r the

    area.

    Some of the =ore recent levels

    i n

    t h i s

    sh el te r have produoe~d

    an

    in te res t ing

    range

    of non-li thic a rte fa ct s

    in

    addi tion t o the

    usual

    stone implements. Faunal remains

    are we11 pm-

    served nd

    are

    being

    analgsed by Prof. Richard Klein of the Unive rsity

    of Chicago.

    From H. J. Deacon University of Stellenbosch.

    The Archaeo1og;y DepartPrsnt of the University of Stellenbosch,

    Cape,

    is

    proceeding with

    i t s

    nLongkloof Archaeological ProJect:

    A

    study of later Q rnary environment and cu l tu r e r e l a t ionsh ip

    i n

    the

    Southern Cape.

    Reconnaissance surveys and excavations have been

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    focused on the e w te r n zone of th e Cape Folded mountains i n the l a s t

    two years

    and

    currently

    work

    has begun on the excavation of

    a

    major

    cave s i t e on Boomplaas ( l i t e r a l l y , Tree

    F arm)

    four miles f rom the

    Cango Caves i n the Oudtshoorn Dis t r ic t .

    This

    i s

    a pre-Cambrian

    lire

    s tone belt

    that

    offers advantages

    i n

    preservation

    and

    rate of accumula-

    ti on of sediasnts fo r the excavator over caves i n the are a underlain

    by th m i d roaks of t he Cape

    System

    The Boomplaas cave

    i s

    250 sq.

    w t e r s i n

    area

    and has a

    depth

    of deposit of five meters ranging i n

    ge

    from

    th

    Holocene t o t he Upper Pleistocene.

    The deposits include

    s slb

    seven di sc re te oocupation horizons separated

    by

    oul tura l ly

    s t e r i l e microfauna-rich layers.

    I n i t i a l indications are t h a t a good

    palaeolsnvironasntal control will be afforded by

    the micro-

    and

    macro

    fauna

    and

    sedjsasnts,

    and

    areacexcavation of living surfanes

    w i l l

    pro-

    vide useful data on behavioural

    patterning. n

    are a of

    25

    sq. meters

    of the uppermost maupation floor of Holoaene

    age

    at

    a

    depth of

    9 em

    below the surface, has been exposed

    showing

    a

    clustering of

    leaf-

    l ined s t o r w p it a nd seed caohes associated with hearths.

    This

    i s

    f a i r l y c l ea r ly a doms t ic area, the margin8 of whbh are jnst within

    the present excavated area.

    It is

    expected that excavation of the

    si te ,

    which will involve exposure of successive horizons over the

    f u l l

    area

    w i l l

    take a nlaber of years.

    The

    excavation

    i s

    being

    directed

    by

    H J

    Deacon

    in

    association with

    Mary

    Brooker, both of Stellenbosch

    University, and Ja net te Deacon and R G Klein.

    Professor Karl Butzer of the University of Chiaago, Kill

    carry out

    a

    f i f t h s e a o n of geo-archaeological work i n

    South

    Africa

    from July t o October, 1974.

    a)

    study of the m i c r d e p o s i t i o n a l environments, based on

    comprehensive sediment analgaes, of the various australopithecine

    breccias (Transvaal, Taung i e nearing completion, and the results

    were

    f i r s t p resented o r a l l y a t th ~enner .~ren/NSFonference on

    African PlickPleistocene

    haminidae

    New York, Jan. 26- Feb. 2,

    1974.

    Work on these very ea r ly

    sites

    has

    been complemented

    by

    geological.

    investigation of Pliocene faunal occurrsnces

    a t

    Virginia

    0. .

    s

    and

    Langeb-g

    .

    b)

    Study of varf us Acheulian

    sites

    (Aaanzi Springs, Geslhout-

    boom, Elandsfontein, Brakkloof Doornlaagte Rooidam, Cornelia) of

    the coastal and interior regions are now mafnly in press. Further,

    re-investigation of the aal River gravels has been concluded in a

    d is se r ta t io n by David Helgren.

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    Robin Derriaourt now ~ e c re t a ry / ~ n sp e c t o ror the H i s or ioa l

    Monuments C o d e s i o n i n Zambia rep or ts

    as

    follows on

    hi

    work

    i n

    South Africa:

    I have campleted the writing-up of th f i e l d d a t a f r o m

    my

    study

    From

    1971-3 of the

    later

    archaeology of th e Tranekei and Ciskei regions

    of South Africa. A W t e d nmanbr of oopies of th e monograph rep or t

    haw been distr ibut ed t o South African archasological i ns ti tu ti on s and

    it

    is

    hoped

    a

    publisher for this

    w i l l be

    found.

    We a b e d

    a t

    reviewing by surfac e survey

    nd

    museum

    st*

    s i t e s

    of the

    Later

    Stone Age (t he te rn in a l

    part

    especially) and th Iron

    Age

    This

    w s

    supplemented by excavations

    a t

    three

    sites

    (OaMeigh,

    AM

    Shaw M i d d l e d r i f t

    and

    Chalumna ~ o u t h ) epresenting mountain, r iv e r

    valley and coa stal exp loita tion i n the Ciskei, The purely archasolo-

    gi ca l evidence has been conpared with o ra l tra di ti on s and written

    his tory for the last 500 yeare.

    This (attempted) interdisciplinary approwh emphMlises notably

    how complex

    i s

    the var iab i l i ty

    in

    the human groupa of

    the

    area over

    the

    l a s t

    two millennia: the dif fi cu lt ie s of tying the cult ur al un its

    emergent

    from

    archaeology i n di fferen t soms

    with

    each other, and with

    the rock

    art

    sequence; the difficulty of collating a r W o l o g i a a l

    groups with social grou recognised i n hist or y

    and

    t rad i t ion Bushmen

    Hottentots,

    mi,

    t c r which

    nt

    themselves di i i er sn tl y cln ssii ieti

    when

    usin

    technological , economic, l ing uist ic or m i c a l data .

    This

    i s

    especially visible as the Cierkei

    i s

    the fr on ti er solhempar ex

    cellence,

    There

    w

    particular problems when

    tryin@:

    t o distinguish the

    elements which le d t o

    a

    pa sto ra lis t nHottentotN ociety.

    void in

    ISA industries of

    the

    Smithfie ld or Wilton complexes south of t he

    h a t o l a h i l ls

    w s

    f i l l ed by

    an

    industry

    w i t

    a crude battered flake/

    core hammer emphasis in technique

    sharing

    sonre sim ilar i t ies with

    coastal assemblages).

    h i s

    i s

    located without pott ery but

    presumably

    l a te r pot te ry

    i s

    acquired

    i n

    one of the

    sites

    at

    Ann

    Shaw Middledrift,

    of

    a

    s ty le d i s t inc t

    f r om

    t ha t i n the

    LSA

    rock s he lte rs t o the north

    and

    all but rare coastal asemblages.

    The stme pottery element seems

    associated with cattle

    and

    possibly sheep and a C.14 date in the

    eleventh century in s m a l l

    mounds

    elsewhere

    at Ann

    Shaw Middledrift.

    The burial of a caw i n one of these mounds is paralleled by an unusual

    burial apparently inrstrusive into tl e e a r l i e r

    s i b

    of a crouched

    elder ly Bush-type famale

    and

    an ar t icu la ted caw adjacent t o each other,

    with la C-14 date of the eighteenth century (when Gonqua nHottentotsn

    are

    know from his to ri ca l sources t o have been i n the area.

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    A t Oakleigh, a rook shelter i n the h i l l s of Queenstawn, a

    sequence gave a lower industry without pa ra ll el i n S8slpson s Orange

    River sequence but s o d a t simil r t o fiHawiesonls Poort n, followed

    by an IS industry of the Smithfield complex into whioh new elements

    were added: pottery sho rtl y a ft e r the mid tenth century, c a t tl e i n

    the fi fte en th or sixteen th century, sheep ther eaft er

    and

    items of

    European

    mufacture

    at ths end of the sequence.

    The donreaCic

    8niaaJ s

    r e f l ec t the pattern of stock th ef t (o r rath er hunting of

    gane

    namd

    dif feren t ly by i t s

    owners

    s h m both i n rock rt

    or

    h is to r i ca l

    sources, though at a

    rather ea r ly date i f the C-14 reading

    i s

    correct.

    Many

    different coastal

    ssewbl ges

    have been distinguished,

    associated w i t h shell micidens

    These

    suggest coastal (perhaps seasonal)

    ac t iv i t ies of

    inland

    hunter-gatherere and pe st or al is ts ; but al so

    sp ec ifi ca lly o oastal gr ou p who at

    both

    west

    and

    east of the coastline

    absorbed pottery into

    an

    otherwise unchanged pattern.

    n Iron A g e

    ceramic tra di tio n c lea rly linked t o the

    NC

    of Natal Iron workers has

    been located at t~llelve i t e s along the coast, but paral le l I ron

    Age

    sites before the eighteenth century seem rarely to have survived with

    evidence f or th e archaeologist inland.

    Here

    history and t r ad i t ion

    nt r t o a s s i s t and supplement.

    Sudan

    Kadero

    Dr. L Krzyzaniak of the Polish Centre of Archaeology

    i n Cairo

    and

    the Archaeological

    Efuseum

    of Poenan continued work i n

    the

    winter of 1973-74 a t

    this

    important pre-historic s i te .

    The

    material

    s

    simil r

    t o

    that

    from Shaheinab but

    th r

    is

    some

    evidence

    t o suggest t is r at he r l a t e r i n date.

    Meroe

    P.L.

    Shinnie

    and R. Heitmaam spent four weeks

    at

    the

    s i t e (~ecember 973 January 1974 w i t h a group from Education

    Expeditions International.

    During

    this time excavation

    w s

    car r ied

    out in

    an

    area where

    an

    i ron smiting

    furnaae

    had been found i n th e

    season o 1969-70.

    The

    new work led t o the discovery of three more

    furnaces, two of them enclosed in a srmll, brick building with a brick

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    1973 saw excavations by Joseph Vogel of Livingstone Museum a t

    the Iron ge s i t e at Chundu Farm

    near

    Livingatone

    and

    by Karla Savage

    of University of California, Berkeley,

    at

    Mulrbwa revealing

    MSA

    LS

    and L material.

    3iss Savage studied

    and

    malyaed finds hw e a r l i e r

    excavations a t Kmu~ongolwaand Chanzbabulele,

    and

    has now returned t o

    the States to continue writing up her work.

    After my ar ri va l a t the National Monuments C o d s s i o n mid-year

    I carried out some preliminary survey work

    in

    the Luxpula Province

    and

    around Lake Tanganyika, mainly locat ing later

    Iron

    Age s i t e s .

    h i s

    work is t o be expanded In 1974 with t r i a l

    d i g s a t

    two village

    sites

    i n

    Samf ya.

    There

    is no Sndication that there w i l l be any overseas-based

    archaeological expeditions t o Zambia i n 1974, which i s regrettable.

    The National Monuawnts C d s s i o n , which controls pe ra i t s for such

    work,

    i s

    keen t o enaourage foreign research workers i n Zambia. It

    is

    fair to suggest that Zambia i s one of the rast open and free of African

    countrie s f o r archaeological fieldwork,

    and

    eaholars who can guarantee

    institutional backing and a

    progr m

    for publioation of results )

    would expect no d if fi cu lt y i n receiving excavation

    and temporary

    export

    permits, Enquiries should be

    addressed

    t o

    re

    a t t National Monuments

    Caarmission, P.O. B o x 124, Livingstone, Zmbia.

    he National Monuments Cammission plans (gradually) to carry

    out the dull but necassary task of reorganiaing for quick and easy

    reference

    i t s ow

    and Livingstone Museum's records of sites and find

    spots i n the country. This w i l l , hopefully,

    aid

    the future research

    worker. Reviews of data by subject or

    area

    w i l l appear frora time t o

    time. supplement is

    being

    prepared t o David Phillipson's invaluable

    NAnnotatedBibliography of the Archaeology of Zanbi.aN,

    s t i l l

    available

    f r om

    the Commission for $1.

    Also available free t o professional

    readers of Ngcnae

    kmaa is

    the C d s s i o n l s occasional newsle tte r

    nArchaeologia Zambianag

    Robin Derricourt.

  • 8/10/2019 Nyame Akuma Issue 004

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    Depuis l a crba t io n, en 1970, de 1 ' I n s t i t u t des Musbes Nat ionaux

    du

    xr re

    B.P.

    4249, Kinshasa I I ) , qu i , parmi s e s a t t r i bu t i ons ,poss&de l a

    rdg lementa ti on e t

    1

    organi sa t ion des fo ui l l es a rch6ologiques en Rgpubl ique

    du za i r e , p lu s ie urs missions ont 6 tb mengee en col lab ora t io n e nt re c e t

    i n s t i t u t e t l a s e c t i o n d e P r d h i s t o i r e e t d tA r ch ol og ie d u Musde r o y a l d e

    1

    r iq ue ce nt ra le Tervuren (Belgique)

    .

    Ces missions rgpondaient

    B

    d i v e r s b u t s

    :

    Prospection des rbgions encore ma1 connues du pays.

    E l abora ti on d' un cad re chronolog ique e t s t r a t i g r a ph iqu e des i n dus t r i e s

    p rbh i s to r i ques .

    Dbveloppement de l 'btude de 1'8ge du fer.

    Format ion d 'archbologues zarrois .

    D r

    F.

    V&n Noten a p ro sp ec t6 l e nord du Zaire de d6cembre 1972

    B

    mars 1973.

    En Ubangi, l a dd cou vert u ne g r o t t e d on t l a s t r a t i g r a p h i e a l l a i t

    de l ' zge de l a p i e r re moyen

    B

    l ' z ge de l a p i e r re rdcent . Chaque n iveau

    pour r a S t r e da t6 .

    En bld,

    il

    a recherchd des s i t e s pouvant a ppa r te n i r au so i -d i sant

    ndol i thique Ubl ien,

    cb l sb re pa r s e s be l l e s haches po l i e s en hgmat i te .

    En t u r i e u t l i e u l a t r o u v a i l l e l a p l u s i mp or ta nt e.

    LB, une g r o t t e

    du Mont Hoyo, p rs s de Bunia, a rbv6ld une s t r at ig ra ph ie a l l a n t de 1 '8ge de

    l a p i e r re moyen (ou d 'une forme assez anc ienne de l t8 g e de l a p ie r r e rbcent )

    B

    un 3ge du fe r , sans doute rbcent .

    Les d i f f6 r en t s n iveaux pourron t 8 t r e

    dat6s . Chacun e s t assoc ib

    B

    d'abondants re s t es de faune;

    on y a ret rouv6

    au ss i que lques ossements humains. Out re l a prQs erva t ion des ves t ig es orga-

    n i qu e s, l ' i n t g r s t m ajeur de c e t t e g r o t t e r b s i d e d an s s a s i t u a t i o n P l a

    l i s i g r e e n t r e l a s avanne e t l a f o r s t , c e q u i p e rm et tr a s a n s do ut e d 'b t ud i e r

    l ' dvo lu t io n de l t c ol og ie e t l a rnanigre dont l'homme s ' e s t adapt6 ces

    deux milieux.

    Depuis janvier 1974, D r F. Van Noten a re pr i s l e s fo ui l l es dans

    c e t t e g r o t t e .

    D r . D Cahen a e f fec tu6 d iverse s fo ui l l es dans l a rbgion de Kinshasa , de

    j u i n

    B

    septembre 1973.

    En premier l i eu , l e s i t e de l a poi n te de Gombs (ex-poin te de

    Kal ina) a 6tb rbexaminb, apr ss l e s t ravau x que

    J .

    C o l e t t e y f i t e n 1925 e t

    1927. Tr oi s occupations B 1'8ge de

    l a

    p i e r r e , l e K al i ni e n, l e D jo ko ci en

    e t l e Ndol ien (de l a p lus anc ienne

    i

    l a p lus r6cen t e) on t l it 6 dbcouve rt e s

    a i n s i qu'un n iveau de l ' a ge du fe r . Le Kal in ien app ar t i en t

    B

    l ' z ge d e l a

    Les a r t i c l e s 36 41 de l 'o rdonnance l o i du 15 mars 1971 re la t i ve

    B

    l a '

    p r o t e c t i o n d e s bi e n s c u l t u r e l s o n t d o t 6 l e z a h e d 'u n ensemble d e d i s p os i -

    t i o n s l d g i s l a t i v e s p er me tt an t un c o n t r z l e s t r i c t d es f o u i l l e s e t d e s db-

    couvertes archbologiques.

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    pi e rr e moyen e t correspond vraisemblablement un s t ad e assez anc ien du

    complexe lupembien. Le Djokocien , l u i , a ss ure l a t r an s i t i on en t r e l '3g e

    d e l a p i e r r e moyen e t r b c e nt . I1 s ' a g i t sans doute d'un Liipembien r6 cen t

    ou du Lupembo-Tshitolien.

    Enf in l e Ndol ien qu i n ' e s t guSre abondant ,

    p e ut S t r e a s s i m i l e au T s h i t o li e n .

    Le n iv e au d e l ' 8 g e du f e r e s t un s o l

    d ' h a b i t a t j on ch d d e t e ss o n s d e p o t e r i e , d e fr ag me nt s d e t e r r e e t d e

    pi e rr es br i i lges , de quelques morceaux de meule e t de

    s c o r i e s ;

    i c e s o l

    s e r a t t a c h e n t d e g r an ds f o y e r s e t d e s f o s s e s p r of o nd e s do n t c e r t a i n e s

    con tena ien t pa r f o i s un vase p lus ou moins complet e t de r a r es f ragments

    d ' o b j e t s en f e r .

    La cbramique pe ut S t r e rapprochiie de po t er ie s d6cou-

    v e r t e s

    ii

    K in sh as a e t d a tg e s l e s u nes du I I I e s i P c l e a v an t n o t r e g r e , l e s

    a u t r e s du Ve s i e c l e a p r s s n o t r e S r e ; m ai s l a c o r r 6 l a t i o n e n t r e l e s

    c ha rb on s d e b o i s q u i o n t f o u r n i c e s deux d a t e s e t l a c 6r am iq ue r e s t e

    impr6cise.

    Ces nouveaux travaux

    2i

    l a po in te de Gombe ont permis de r 6c ol te r

    plus de 335 6chant i l lons de charbon de bois dest in6s au dosage du C14.

    Le Pr.

    J

    De Ploey, de l a Ka thol ieke Un iv er s i t e i t Leuven , a pa r t i c i pg aux

    f o u i l l e s e t s ' e s t c ha rg 6 d e 1 1 6 tu de giiomorphologique e t s t r a t i g r a p h i q u e .

    D r D

    Cahen a Bgalement ef fe ct quelques sondages au s i t e

    de

    Kingabwa, pr6c6dem ent fo ui l l B par l e

    R F H

    v an Moorsel q u i l e d a t a i t

    du 17e s i Sc le environ.

    L 'absence de to u t o b j e t d ' im por ta t ion europ6enne

    dans c e t impor tan t 6 tab li s sement de 1 '8ge du f e r p l a i de peut -Z tre en faveur

    d'un ^age plus ancien.

    L es d a t a t i o n s p a r l e r a d io c a rb o n e p e r m e t t r o n t

    peut-Etre de conf i rmer ce t t e hypoth2se.

    De mars

    2

    a v r i l 1 9 7 4 , D r D Cahen donnera l e s cours de prEhis toi-

    r e e t d 1 ar c h6 0 10 g ie a f r i c a i n e 1 1 U n iv e r s i t 6 N a t io n a l e du ~a: re

    Lubumbashi. Ensuite,

    l

    ef f ec t ue ra une p rospec t ion a rch6ologique de mois

    en compagnie

    de

    M M

    Muya Kamwanga, ar ch do lo gu e, e t de

    J

    Moeyersons,

    gbomorphologue, dans l e s regio ns au sud du pays (Bandundu, ~ a s a r t Shaba) ,

    a f i n d e t r o h e r de nouveaux o i t e s q u i p e rm e tr r ai e nt d e r e l i e r l e s r 6 s u l t a t s

    a rch6olog iques ob tenus dens l 'o ue s t du za i re ceux de l ' e s t du pays .

    M

    P de Maret a ef fe ct u6 une premi2re pr os pec tio n e n ddcembre 1972 au

    Bas-Zaire. De j u i n

    2

    s ep te mb re 1 9 7 3 , i l a p o u r s u iv i c e t t e p r o s p e c t i o n ,

    a x6 e p lu s p a r t i c u l i s r e m e n t s u r l e s g r o t t e s de l a r 6 gio n. On s a v a i t q ue

    c e r t a in e s r e c e l a i e n t d e l a c6ramipue a n c i en n e, d e s h a ch e s p o l i e s , d e s

    p e i n t u r e s

    e t

    d e s g r a v u r e s t u p e s t r e s q u 1 6 tu d iG re n t l e s P r . G Mortelmans

    e t

    R

    Monteyne lo rs de l a prep ara t io n du IVe Congrks Pa na fr i cai n d e

    Pr l i h i s t o i re e t d1Etude do Qua te rna i re ,

    Nombre de cavernes sont dEcor6es de pe in tu re s e t de g ravures

    a s s e z s e mb lab l es , d e s c r o ix , d e s p o in t s , d e s h a ch u ra g es , d e s t r i a n g l e s , p ar -

    f o i s des animaux ou des personnages t r 6 s sch6matiques. Le s o l des anfrac-

    tu os i t 6s a in s i o rn6es n l a r6v616 qu 'une seu le couche a rch6olog ique con tenan t

    2

    l a f o i s d e s rag-ments d e p o t e r i e , d e s p i e r r e s t a i l l g e s e t d es os se me nt s.

    Pu isque tou te s ces g r o t te s ne renfe rment qu 'une seu le couche a rch6olog ique

    aux ca r ac t g r i s t i qu es comparables , l a con temporan6 it6 des ve s t ig es

    i n d u s t r i e l s e t d e s d 6c o r at i o n s r u p e s t r e s p a r a i t v r ai s em b la b le .

    Une au t r e g ro t t e a se r v i de n6cropo le

    2

    l l ^age du fe r .

    On y tr ou ve

    des ossements humains e t des t es son s de c6ramique en s urf ace . Les sondages

    ont montr6 l ' ex is te nc e d 'une unique couche arch6ologique contena nt des

    tes son s de l a mgme dra rni que ,

    d e s p o i n t e s d e f l 6 c h e e n f e r e t d e s d e n t s

    humaines . Ce s t y l e de po te r i e e s t connu dans tou t l e

    as-~alre

    e t

    5

    Kinshasa.

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    Pre s de Mbanza Ngungu (ex-Thys ville) deux g r o t t e s re ce la ie nt une couche

    oh de l a c6ramique vo i si ne i t avec dea haches pol iee .

    Dans une de ces

    deux cavernee, sous ce t t c couche, un sondage a rCv6ld l ' ex is te nc e d 'une

    impo rtan te s t r a t ig ra p h ie d ' in d u s t r i e s l i t h iq u e s a v ec d e s r e s t e s d e fau ne .

    Une reconnaiss ance d e di ve r s s i t e s de l 'bpoque du royaume de Kongo f u t

    au ss i eff ectuge a i n s i qu 'un sondage ayst matique dans l e n iveau de 1 '2ge

    du fe r de l a poi nt e de Gombe (en co ll abo ra ti on avec

    D r . D

    Cahen) .

    De mars j u i l l e t 1974, M.

    P .

    de Maret ef fe ct ue ra une mission

    de p rospec t ion e t de f ou i l le s des s i t e s de l ' a ge des mdtaux du Shaba (ex-

    Katanga) e t p lu s pa r t i c ul i e re men t d es s i t e s k i sa l i e n s , a ve c l ' a i d e d e

    M.M.

    Kanyimba e t

    J

    De Buyst de 1 U.N.A.Z.A.

    En conc lus ion , on peu t e spdre r que , g r h e l a co l la bora t i on

    i n s ta u r de en t r e 1 ' I n s t i t u t d es Musdes Nationaux du ~ a h et l e Musde roy a l

    de l 'b f r ique c en t ra l e l e re ta rd accumul6 par

    1

    archdol ogie en Af ri qu e

    cen tr a l e pourra 8t r e rapidement combl6. Vers l a f i n de 1974, on dis pos era

    de plus d 'une soixantaine de dates au C14.

    C el l es - ci , s i e l l e s i n t dr e s se -

    ro n t s u r to u t l e s pd r iod e s a sse z rd c e n tes , j e t t e r o n t ndanmoins l e s ba se s

    d 'u ne c h ro n o-s t ra t ig ra p h ie p lu s p rd c ia e p ou r c e t t e v a s te p a r t i e d u c o n t in e n t

    a f r i c a i n .

    Out re l ' o rg a n i sa t io n e t l ' 6 tu d e d e ce s fo u i l l e s au Za' ir e, d i f f d -

    re n t s t r av au x se so n t p o u rsuiv i s l a sec t io n de Pr i ih is to i re e t d 'Arch6olo-

    gie du M. K. A

    C.

    (Tervuren)

    - D r . F.

    Van Noten, archdologue, chef de sec t ion au M.R.A.C.

    -

    AchGvement de son dtude des pei nt ur es e t gr avures ru pe st re s

    du Jebel Uweinat.

    - Poursuite de son 6tude du matdrie l archdologipue du Jebel

    Uweinat .

    -

    Pours u i te de l 'd tude du matdr ie l de l ' age du f e r rdco l td au

    Niger ia l o r s de l a Benue Valley Expedit ion.

    D r . D .

    Cahen, archGologue, a s s i s t an t au

    M.R.A.C.

    Achsvement de son i h d e du s i t e arch6ologique de l a Kamoa.

    P r ds e nt a t io n d 'u ne t h s s e d oc t o r a t s u r c e s i t e e t p rg p a r a ti o n d e l a

    pub l ica t ion .

    M.

    P. de Maret, archdologue, as pi r an t au Fonds Nation al de l a Recherche

    Sc ie n t i f iq u e .

    -

    Prg p a ra t io n d 'u ne th se d e d o c to ra t s u r l ' sg e du fe r a u z a i re .

    Achsvement d'un mdmoire de licence en Sciences Sociales

    (Univ ersi t d Libre de Bruxelles) Le forgeron dans l e monde bantou. St a t ut ,

    tec hni que e t symbolisme.

    Etude de l in gu is t i que comparat ive des termes de mdt al l urg ie

    dans l e s langues bantoues (en colla bor at i on avec M. F. ~ s u k t a ) .

    Etude de l a technologie d e l a cdramique au

    as-~azre.

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    M J. Moeyersons, gEomorphologue, assistant

    a

    la Katholieke Universiteit

    Leuven.

    Achsvement de son itude g6omorphologique du site de la

    Kamo

    PrEparation de sa thsse de doctorat (K.U.L.) consacrle une

    Gtude g6omorphologique du pays Mumuye au Nigeria.

    Contribution 1'6tude de la "culture mat6rielleU des

    utnuyc (en collaboration ave ?~. Maesen).

    Dr.

    E.

    Roche, palynologue, chargd de recherches F.N.R.S.

    Achsvement de son dtude palynologique du site de la Kamoa.

    Etude palynologique de divers sites arch6ologiques africains

    (Gwisho, Zambie; Jebel Uweinat, Lybie; Gongola, Nig6ria).

    Poursuite de la constitution d'une collection palynologique

    de rEfErence (recherches sur herbier, dchanges internationaux).

    Plusieurs dtudiants de l'universitd de Gand ainsi qu'une

    Etudiante de l'universitd de Likige ont effectu6 ou pr6parent leur mEmoire

    de licence d a m le cadre de la section.

    Le 10 mai 1973 eut lieu la section une rdunion consacrde

    lt6tude du ddbut de l'age du fer en Afrique. I1 s'agiesait d'une confron-

    tation des donnEes linguietiques, ethnologiques, anthropologiques et

    arch6ologiques.

    Publications rgcentes

    en

    arch4ologie du Musde Royal de l'bfrique Centrale

    CAHEN, D. et MARTIN, Ph. 1972. Classification formelle automatique

    et industries lithiques. Interprdtation des hachereaux de la

    Kamoa Ann, Mus. Roy A@ Centr., Tervuren, Sci,hum., s6r.in-8',

    n076.

    CAHEN,

    D.

    et MORTELMANS, G. 1973.- Un site tshitolien sur le plateau

    des Bateke (Rgpublique du zaire) Ann. Mus. Roy Afr. Centr.,

    Tervuren, Sci.hum., sdr. in-8', n081.

    FAGAN, B.M. and VAN NOTEN, F.L. 1971,- The Hunter-gatherers of Gwisho

    Ann. Mus.

    Rog A@ Centr.,

    Tervuren, Sci.hum., s6r. in-8', n074.

    HIERNAUX, J., LONGREE, E. de,

    t

    DE BUYST,

    J.

    1971.- Fouilles arch6olo-

    giques dans la vallEe du Haut-Lualaba I. Sanga, 1958

    Ann Mits

    Roy Afr. Centr., Tervuren, Sci.hum., s6r. in-8', n073.

    VAN NOTEN, F.L. 1972.- Les tombes du roi Cyirima Rujugira et de la

    reine-mSre Nyirayuhi Kanjogera Description archdologique

    Ann.

    Mus.

    Roy Afr Centr., Tervuren, Sci.hum., sEr. in-8', n077.

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    Cali forn ia Stat e lhniveraity, Fmsno:

    Information

    wanted

    on

    African Obsidian StuUiee.

    I

    m pr s ntly

    oonducting research

    on

    obeidian

    trade

    and

    teohno-

    logy

    i n

    California and Nevpda

    Through the me of obsidian hydration

    and X r a y

    fluorescrenere, attempts

    are being

    ma t o

    c t e c t

    souroes

    and

    trade networks of aboriginal populations.

    I n

    the future, I hope t o

    carry out similar s t i e s on m o a n ~ ~ ~ t e r i a l s .would therefore

    appreoiate information, caaarrenta, uggestions aoncerning previous

    and current researoh i n Af rican

    obidim

    studies, espeaially as

    related to

    my

    reseasch

    intarest,

    Send to:

    C U

    Ritchie,

    D/A

    CSUF,

    Fresno, Ca, 93740.

    nichigan

    tab

    University:

    The Lothagasl Late Stone Age site

    report

    w i l l

    appear i n

    the

    Hichigan State University Museum, Anthropologioal series later on this

    year.

    A related report on early Holooane

    ge

    huanan skel etal material

    om

    west

    of

    ake

    Rudolf

    is

    now

    being

    written

    by Dr 8. T

    Phenioe

    L

    Angel

    and

    L Robbins,

    n addition to

    the

    above, a report on the Late Stone ge site

    of Rangi

    s

    i n

    i t s final

    stages of preparation by L Robbins, J Browr

    and

    A.

    Hoffman. This is

    a

    very

    late

    site

    from

    Kadm mountain i n south-

    ern Karamoja

    Distr ic t ,

    Uganda.

    The

    microliths

    from

    the s i t e have

    proved to be especially interesting and

    a

    Masters

    thesis is being

    written

    by

    Ms C.

    rewster

    on

    the

    edge

    daaage

    patterns found on these

    tools.

    Larry Robbins.

  • 8/10/2019 Nyame Akuma Issue 004

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    Northweatern

    University:

    You

    nay lke to

    know

    that I

    have

    had prepared

    a listing

    of

    all

    the

    papers published

    in

    the

    VIdm

    C o d s

    Panaf ricafi

    de

    Pdhirctoire

    Da k a r 962 since the

    voluare

    i tsel f

    has

    neither

    a

    U t f oont;enb nor

    an index

    It

    amounts to six

    typewritten

    pages and i f anyone

    would like

    t o have aopies

    o f

    it I should

    be

    happy t o provide

    them

    If

    the dem nd

    ia

    erufficient, I should

    be able t o supply t h e m at

    q? 5

    whioh

    w i l l

    aovar

    the

    cost of

    postage

    Otherwise,

    it

    m y cost

    as mu h

    as

    75.

  • 8/10/2019 Nyame Akuma Issue 004

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    SOURCE

    OF PWMXTS FOR R C H E O W I C L WDRK

    It is hoped, as information becomes available t o l i s t

    a l l

    the

    organisations

    in

    APdoa m

    which

    th

    XlOC Sary pm f t s

    t o

    out

    archaeological work can

    be

    obtained

    and

    o

    l i s t

    inst i tut ions such

    as

    universities and research institutes

    where

    research

    and

    teaching

    are catried

    out 5 n

    ths African

    continent. If it

    seems usef'ul

    the

    next

    a t ep would

    be

    t o

    l t

    all those institutions outside Africa

    where

    suah

    msearoh

    and teaching is being done

    If

    the

    information

    is aade avail

    able to

    the

    &tor of

    Nyaare koaa

    and i f

    it

    seem useful the intention

    i~ t o publish a handbook giving all this Wonnation it would

    per

    haps appear as

    a

    special nmuber of

    Ny a ma Akmrcr

    The

    present

    listings

    give

    what

    infomation

    is

    at

    present

    avail

    able

    here

    concerning the issuing of permits.

    The

    gaps w i l l

    be

    obvious

    and those wh have Momation am urged

    t o send it

    in.

    In

    particular

    infomation concerning Francophone oountries

    is

    much

    more

    d i f f i cu l t t o

    aolm by

    and

    those working

    i n ny

    of those oountries

    are

    espeoially

    urged

    to make

    information

    available

    Botswana

    Penni