Beads:
Bone
beads.— Bone
beads, relatively scarce in theAdena
complex, are representedfrom Natrium Mound by
a string of 33 disk beads(pi. 25c) recovered
from
across the knees of a burial in feature 46.These
beads, verycrumbly and
poorly preserved, weremade
of flat,smoothed
bone,presumably
ofmammal. The
averagebead
is 1.6cm.in diameter
and
0.3 cm. thick.The
circumferences are notperfectly circular,and
the thicknesses rangebetween
0.2and
0.4 cm.The
holes,
which
are often slightly ovoid in shape, appear tohave
been boredfrom
both sides. Their diameters are slightly over 0.4 cm.and
less than 0.5 cm.Bone
beads arean Adena
trait (No. 160) according toWebb and Snow
(1945, p. 96).Pearl
and
shell beads.—
Thirty-six pearland two
shell beads were found draped over aNatrium Mound
burial (feature 40).These
beads are representedby
six dimensional sizes as listed below. All were drilledfrom
both sides.These
beads were strung on thesame
cord with copper beads (pi. 25e, lower).The
copper saltsfrom
the latterstained the outer surfaces of these beads.Table 1.
—
Beadsfroma Natrium
Mound
burial NumberofBarite bead.
— One
baritebead
(pi. 25d)was
recoveredfrom
feature51. This
bead
is aflat circular diskperforatedfrom
bothsides. Its diameter is 1.7 cm. It is ofuneven
thickness, varyingbetween
ex- tremesof 0.2and
0.7cm.The
hole, imperfectly drilledand
centered,is 0.5 cm. in diameter. Barite beads are apparently a
new Adena
trait, although
Webb and Snow
(1945,p.90, traitNo.
136) note that therehave
been aboriginal attempts tomake
beads of barite.Worked
bones.— A
fragment 10.3 cm. longand
2.4 cm. wide ofworked mammal bone was
found associatedwith feature46, aburial.This piece, 0.6cm. thick,isplano-convexincross section.
Both
ends of this objecthave
been broken.One
end narrowssomewhat,
as thoughfora point. Despite the checksand
condition ofpoorpreser- vation,it isevident that thebone had
beenwell finished,judgingfrom
the polishon
the surfaces.There
is a small area of red ochrelike stainon
the flat undersurface.An
over-all patchy discoloration of black matter is also present.The
origin ofthe latterwas
not ascer- tained.Another worked-bone
artifact, representedby
a small handful of extremely brittlebone
fragments,was
found in association with feature 35, a burial.Three
sections of the specimen total 10 cm. in lengthwhen
pieced together.Two
fragmentsshow
polish. Since the conditionofthespecimenissofragmentary, thereissome
question regarding itsform and
probable use.Bear canine
tooth.— One
fragmentary bearcanine toothwas
found associatedwith a cacheofbladesinfeature21. Thistooth fragment, alittleover2 cm.long,represents thecrown
only. Unfortunately,no
evidence ofwork
can be discernedon
it.However,
its presence is significant sinceWebb and Snow
(1945, p. 334) claim thatno
per- forated or cut animal teeth are found in theAdena
complex.Worked
coal.— A
rectangular pieceof hard coal, 1.5by
1.3by
0.4 cm.,was
foundin the centerofoneofthebead
strings associatedwith a copper reel in feature 34 (fig. 24^).The
coal seems tohave
been carefully trimmed.There was no way
of determining exactlyhow
this object could
have
been tied to the string of copper beads, since holes for suspension or other indications of fastening are absent.White
pebbles.—
Sixty-eight white quartz pebbles were found as- sociated with a burial in feature 47.These
pebbles were found in alittlearea about IK inches indiameter, as though they
had
been con- tained in a bag.The
pebblesdo not appear to be ofany
distinctive kind, being very similar to those gatheredon any
beach or stream bank.With
the exception oftwo
largerpebbles,theymeasure
about 0.9 cm. long with proportionate widthsand
thicknesses.The two
largerpebblesare 2.0 cm. long. It ishighlyprobable that thesepeb- bles
may have
beencontainedinabag
ofsome
kind ashad
beenmen-
nS!^40?^'^'''''
ADENA MOUND AT NATRIUM —
SOLECKI373
tioned, or perhaps in
some more
solid container equally vulnerable to decay. William C. Mills (1916, pp. 366-369) reports the finding of pebbles about thesame
size,which
were recovered in the hollow of copper boatstonesand
coppercones atTremper Mound. The
useof the pebblesis problematical.They may have formed
partofa setof appurtenances, such asfetishes, forpromoting thepersonal welfare of the owner.Natural sandstone pendant. — A
single-holedflat,ovatestonewas
found unassociated in themound
fill. This specimenis quitesmooth and
lacking in sharpand
abrupt edges, as though ithad
been water- worn.A
hole, 1.1 cm.wide,was
perforatedfrom
onesideonly,taper- ing toadiameter of 0.9cm.on
the reverseside.There
issome doubt
regarding the originofthe hole, sinceitsinnerdimensions areslightly belled out, aphenomenon
not usually encountered in drilled holes.Even
the striae one normally finds in drilled holes are absent.Con-
sidering this pieceofsandstone
from
allpoints, itappears thatitmay
have
beena naturally perforated,water-worn pebblewhich
eithermay
have
attracted the curiosity of themound
builder orwas
casually in- cluded in themound
fill.Pottery.
— Fragments
ofwhat
were originallytwo
small sherds identifiedby James
B. Griffin ^* as FayetteThick ware
were found in squareN13E2
atan
elevation of2.2 feetfrom datum. These
sherds were not associated with other artifacts or feature data,and may
have
been accidentally included in themound
fill.The
pottery isreddish
brown
in color, 1.3 cm. thick, heavily tempered with coarse fragmentary stone particlesand
very friable.The
outer surface bears cord-marked impressions while the inner surfaceshows
a slight roughening. Griffin (inWebb and Snow,
1945, p. 244) suggests that FayetteThick
pottery,an Adena
trait (ibid., p. 102,No.
200),may
be equated with
an
early manifestation of theAdena
complex.Pottery,
odd fragments. — A
small fillet ofgrit-tempered potterywas
found in the excavationspoils. Thisfillet, 2.5cm. long,was
evi- dently finger-modeled. Itisdarkredincolor,rather coarseintexture,and
does notseem
tohave
been subjected to firing, judgingby
itssoftness.
Another
larger piece ofhand-modeled
light-brown clay, fashioned intoan
oblong shape,was
found in themound
fill. It is unfiredand
coarsely sand-tempered.The
specimen is 6.0 cm. long, 3.5 cm. wide,and
2.0cm. thick.The
surfaceswhich have
notbeenbrokenor other- wise eroded are rudelysmoothed
asthough
this artifacthad
been consciouslymodeled
into shape. Since this objectwas
found in themound
fill, nothing definite can be said concerning it, except that it"Director,MuseumofAnthropology,UniversityofMichigan,AnnArbor,Mich.
seemstobelongtotheclassof so-called Poverty Point type problemat-
ical clay objects found torangein time
from
Tchefuncteto the ColesCreek
stage in Louisiana (Fordand Quimby,
1945, pp. 31-32).These, however, werefired.
Shells.
— One
large piece of shellwas
found in feature 46. Thisshell isa fresh-water mussel shell of local origin.
Several other fragments of local fresh-water mussel shells were found in
mound
featuresand
inthemound
fill.These
shellsmay have
been worked, although they are so fragmen- tary that certain identification cannot bemade.
Textile
remains.—One
solitaryfragmentofwoven
textile (pi. 256)was
preservedby
thecoppersaltsfromacoppergorgetfoundinfeature 34. This bit of fabric, 8by
12 cm.,presumably
theremnant
of a largerexample of textile art, lay under the gorget, assuming the out- lineshape of the latter inits preservation.The warp and
weftcords are both distinctenough
tomake
the identification of the weave.The warp
cordwas
the poorerpreserved of thetwo
cords.The
type ofweave
is called "plain twining" according toMiner
(1936, p. 186,fig. 3)
and
"single twinedweave"
according toWebb and Funkhouser
(1931,p. 383, fig. 84). Itisaverysimpleweave. Single
heavy warp
cords are held in parallel positionby
lighterpaired weft cordswhich
pass at right angles to the warp, one cordon
either side.The warp
cords arebound
close togetherby
the weft cords,which
in thisexample are 0.3 cm. apart
from
center to center.The
weft cord, alittleless than 0.1 cm. in diameter, is
composed
oftwo
strandswhich
are twisted in a clockwise direction.The
coarserwarp
cord, about 0.15 cm. in diameter, seems tohave
beenmade from
one strand twisted slightly in a counterclockwise direction.The
weft cord isthe stronger
and more
flexibleofthetwo
cords. Thispliantcordmay
have
beenmade from
the silkyfibersofaspecies ofmilkweed
(Carey, inWebb,
1941, p. 187), although this is purely conjectural thinking, sinceno analysis of the cordwas made. The
coarser structureof thewarp
strandsindicatesthatanotherkindofmaterialwas
used,althoughit is also unidentified.
There
is a small 3-by-6-cm. patch or impressionof light furlikema-
terial extending along the width edgeof thispiece of textile. It isof
parchment
thinness. Itmay have
been abitofthehideofsome
small furredmammal.
One
ofthecordsof the heaviercopperbeadsisespeciallynoteworthy, since itrepresents a deviationfrom thecommoner
cordage type found atNatrium Mound.
It iscomposed
oftwo
strands of vegetalma-
terial twisted togetherin acounterclockwisedirection, forming acord 0.15 cm. thick.
A
third single strand (0.10 cm. thick) of thesame
fibrous material is
wound
around the heavier cord in a clockwiseNo!^40]^"^'^^'
ADENA MOUND AT NATRIUM — SOLECKI 375
direction.
The
strands of the cord are twisted approximately five turns to the centimeter, while the single outside strand iswound
ap- proximately oneand
ahalf turns to the centimeter.Fragments
ofcordsofanotherkindofmaterialwere foundpreservedby
the copper beads.These
cords,up
to approximately 0.4 cm.thick, appear to