Riv.Bas.Sur.
Pap. No. 4]
ADDICKS
BASIN— WHEAT 177
178
tationbeing345°.
As
intheDoering
site, agridsystemof 1 m. (3.28 feet) squareswas
staked off,and
excavationwas by
arbitrary levels of 15cm. (0.49 foot). Allthe materialwas
screenedand
theartifacts weresegregatedby
squareand
level. Profilesestablishedby
usingan architect's telescopic leveland
target rodwere
plottedon
standardgraph
paper,and from
this a contourmap was
prepared (fig. 14).Depth was measured from
thesurfacelevelof the designator stake for eachsquare.The uppermost
stratum of the site consists of sandymidden
soil, Ilighttanin color,
and
varyingin thicknessfrom
afew
centimeters at i the center of the site tosome
30 cm. (0.98 foot) about the perimeter(fig.15).
While
thecolormay
reflect,in part,aweatheringout of the organicstainscommon
tohuman
occupation, it is probablethat occu- pationwas
not constant, and, furthermore, thatsome
of the sandis the result of aggradation
by
natural agencies.Below
the light- colored sandy layer is a stratum of dark, sandymidden
deposit to a fmaximum
depth of 75cm. (2.46 feet). This deposit fans outtoward
• the perimeter of the site. Since this stratum produced the largest ;number
of artifactsand
animal bones, it seems likely that this zone >marks
theperiod of densest occupation.Conformably
underlying themidden
properis a knoll ofunknown
depthcomposed
of very light-colored, water-laid sand.As
in the Doering site, the precise transitionfrom
the knoll to the overlyingmidden
deposit ismasked by
theblending ofthesandcomposing
the knoll with the lower part of the midden.Although
artifacts occur but infrequently in this stratum, they nevertheless indicate limited occupation of the site during a periodwhen
the knollwas
stillaggrading.
Artifacts
from
theKobs
siteweremost numerous
inthedark mid- den zone.The
majorityoftheprojectilepoints in thisstratumwere
PerdizPointed Stem,Alba
Barbed,and Eddy and
ScalhoniStemmed.
At
the base of themidden
deposit thesewere
of about equal occur- rencewithGary Stemmed
points, indicating that the transitionfrom
the use of the large pointstothe smaller oneswas
already wellunder way. Pottery occurred frequentlyin this layer.All theproje<;tilepoints
from
thesandknoll arelarge,themajority beingGary Stemmed
points. Potterywas
quite rarein this stratum.Inthe
upper
part of the knollseveralsherds of aTchefuncteStamped
pottery jar were found,giving us one of ourmost
important chrono- logical cluesand
affording a tentative cross-dating with the early Tchefuncteculturesof theLower
Mississippi Valley.Three
burials werefound
in theKobs
site.Two
of these were flexed, while the thirdwas
semiflexed.Two
were buried in pitsdug
intothe sand knoll, easily recognizedbecause of the dark
midden
fill.Rlv.Bas. Sur.
P;il>.No.4] ADDICKS BASIN
— WHEAT 179
fI
i
OF
AMERICAN ETHNOLOGY
[Bull.154Figure
16—
Burials, Kobs site (42/66A6-3). A. Burial S. B, Burial 6. C, Burial 7.pS.N^o^.'4T'^'
ADDICKS
basinWHEAT 181 The
thirdburialprobablywas
alsointerred inapit, but inasmuch as therewas no
penetrationinto the whitesand of theknoll,none
could be defined. Burialnumbers
were continued seriallyfrom
those of theDoering
site.BurialNo.5 (fig. 16,a):
Location:9N/7W.
Depth:72cm. (2.36 feet) to skull.
Matrix:Middenfill inovalpit 85cm. (2.78 feet) longandofindeterminate width and depth. Pit well defined on south side by contrast of middenmaterial withwhite sandoftheknoll.
Position: Flexed on back; head oriented to southwest, facing southeast.
Arms: Right arm tightly folded against itself, hand to chin; left arm
foldedalongsidechest,handto left shoulder.
Legs:Thelegs werepulled closeto and ontop ofbody with lowerlegs rotated medially so that the feet crossed each other above the pelvis.
Age:Adult.
8eip: Female.
Associated Objects: Halfof a small turtle shellwith a few pebblesbeneath
it,found ontop of thechest,
may
have beenarattle.Remarks: Bone condition fair; some breakage due to groundpressure.
BurialNo.6 (fig. 16,6)
:
Location: 11N/7W-12N/7W-11N/8W-12N/8W, center of burial pit almost directlyunder designatorstake forsquare12N/8W.
Depth:70cm. (2.29 feet) to skull.
Matrix: Midden fill in elongated oval pit, 120 cm. (3.93 feet) long, 67 cm.
(2.19 feet) wide, 40 cm. (1.31 feet) deep, excavated from midden intowhite sandofknoll.
Position:Semiflexedonright side; headorientedtosoutheast,facing north- east.
Arms: Upper right arm across chest to front of body,lower arm and hand missing; left arm folded alongside body, hand to left shoulder.
Legs: Upper legs form approximately a 140° angle with the body, the lowerlegsfolded tightly againstthem.
Age:Adult.
Sex: Female.
AssociatedObjects:None.
Remarks:
A
number of bones were missing, including the left and right radii, left ulna,thelower vertebrae, pelvis,hand and foot bones, and mostof the ribs. Thelegbones were separatedfrom theupper body by a distance much greater than normal. This, together with the number of missing bones, suggests the possibility that the body was partly decomposedbefore burialand that someattemptat rearticula- tionhad beenmade.BurialNo.7(fig. 16,c)
:
Location:10N/9W.
Depth: 40 cm. (1.31feet) to skull.
Matrix:Middenfill.
182 BUREAU
OFAMERICAN ETHNOLOGY
[Bull.154 Position:Flexed onleftside, almost on itsback; head oriented north-north-east,facing southeast.
Arms: Right arm folded along side, hand (missing) between right shoulder and chin; left arm tightly folded beneath the left leg,
handunderleft side offace.
Legs: Pulledcloseto chest, feet atpelvis.
Age: Adult.
Sex: Male.
Associated Objects:None.
Remarks: Best preserved skeleton from the site. No burial pit visible be- causeofhomogeneityofmiddenearth.
THE GRISBEE
SITE (42/66A3-1)The
Grisbeesiteislocated atthenorthend
of awestward meander
ofLangham
Creek about 150m.
(492.12 feet) south of its junction withHorsepen
Creek (fig.5).At
thesouth endof themeander, pot- sherds, lithic artifacts,and
othercamp
debris are erodingfrom
a stratum about 10 cm. (0.32 foot) inthickness underlyingan
average 20 cm. (0.75 foot) of alluvial fill.The
areaencompassed by
themeander
supportsa cover of small pinetrees,many
ofthem
of second growth.Along
the stream are oaksand
otherhardwood
trees, as well aswillowsand
afew
larger pines.Approximately
20 m. (65.61 feet) abovethesitean
intermittent contributaryjoinsthemain
channel ofLangham
Creekfrom
the northeast.The
siteconsistsof amidden
deposit90 cm. (2.95 feet) thick over- lying a kidney-shaped knollwhich
parallels thebend
of the stream onthe southeastbank
asitturnsintothewestward meander
(fig. 17)FiGURE 17.—Sketch map, Grisbee site (42/66A3-1), showing test pit.
Kiv.Bas.Sill
Pap. No.4] ADDICKS BASIN
WHEAT
18^The
siteis 15m.
(49.21 feet) across its northeast-southwest axisand
27 m. (88.58 feet) across its northwest-southeast axis.The
north- easternend
rises sharply to approximately 45 cm. (1.47 feet) above the flood plainand
themidden
slopes gently to the southand
west.The
site is undergoingsome
lateral erosionon
the edge next to the creek in theform
of a miniatureguUey
cuttingheadward
into the central portion of the midden.The
remainder of the surface is sta- bilized by anundergrowth
of thorny vinesand
low bushes.Three
large oak trees aregrowing
on the lower slopes of the midden.A
stratigraphic test pit 1.20 m. (3.93 feet) squarewas
excavatedby
15 cm. (0.49 foot) arbitrary levels, approximately in the center of themidden
(fig. 18).From
the surface to a depth of 15 cm.(0.49 foot)
was
an indurated crust oftopsoiland
sparsemidden
de- posit, compacted, perhaps,by
the pressure of the hooves of grazing cattle (fig. 16, h).Below
this crust themidden
earthwas
cohesive.6
12 18
24 30 36
15
30 45 60 75 90
o 3
Indurated Crust
Midder)
Deposit
Sterile Clay Unexcavated
Figure 18.
—
Stratigraphicsection,Grisbeesite(42/66A3-1).From
45to75cm. (1.47 to 2.46 feet) the organiccontent of the deposit greatly increased,making
itmore
friableand
perceptibly darker in color.Most
of theartifactsobtainedat this sitecome from
thislevel,which
probabl}^ represents the period of heaviest occupation.Below
this levelthe