thanthat of 1934, althoughthe butt ends stillcomprise a large per- centage of theseries.
Most
of thetip endscame from
the bisonpit,andthe inferenceis that theyhad been
embedded
intheflesh of the animalswhose
boneswere
foundthere. In discussing the prevalence of buttendsinthepreviousfindsitwas
suggested that the circumstance could be attributedto the replacing ofdamaged
points.Many must
have snapped ofif in the killing of game. This is illustrated by the tipsinthebisonpitand bytheoneinthe vertebra.Undamaged
shafts were no doubtretrievedandcarriedbacktocamp
tobefittedwithnew
points.
The
fragmentof the oldone remaininginthe shaftwould
be the butt end, andinthe remountingprocess itwould
be tossed aside to remain in the debris of accumulation.Such
an explanation, of course, refers only to fragmentswhichshow
that they formed part ofacompleted point;itwould
notapply tobuttsfrom
thosebroken in themaking.The
basal portionswere
not always discarded,how-
ever,asexamplesinthecollection
show
thatitwas
notanuncommon
practice to take a buttwhich had lost its tipand rechip it so that it
again had a point capable of penetration. Specimens in this group are extremely stubbyand flat-pointed.
Thereare a
number
of pointsinthecollectionwhicharenot of the characteristicFolsom
form.One
type in the variant groupconsists of small pointsmade from
fortuitous flakes,oftenfrom
portions of channel flakes.None
of these has the fluting;as a matter of fact, they are too thintopermittheremovalof asidespall.They
definitely belongintheimplement complex, however, and their outlinesclosely follow the generalFolsom
pattern.The
other type of pointis repre- sentedby fragmentsonly,but the pieces are sodistinct intheirnature that theymust
be considered as representative of aform
found in theWest
which is frequently linked with the Folsom. This is the so-calledYuma. The
fragmentsarefrom
the trueYuma,
notfrom
anyof the multitudinous subtypevarieties.The
typicalYuma
point, inthe conceptionof the writer,isonewhichislongandslender.The
edges extend approximately parallelfrom
the base—
insome
cases thereisan almostimperceptiblenarrowing towardthe butt—
forabout two-thirds of the lengthand then taper toa sharp point (fig. 2). It isoval incross-section (fig. 2, b).The
basemay
bestraight across, slightly concave, ordeeply concave. Sporadic examples have a small shoulder on one or both sidesnear the base, thus forming a slight tang(fig. 2,/). In theshapingprocess themain
flakeswereremoved
so that the facets extend completely across the face of the blade, usuallyataslightangle directedtowardthetip.The
edgeswerethenNO. lO
SECOND
REPORTON FOLSOM COMPLEX
ROBERTS 21 refined bya retouchin which minute flakeswere removed,a process comparable tothesecondarychippingintheFolsom
group.A
large variety of bladesand pointshave been grouped under thename Yuma,
and atthe present time thereis considerable confusion as towhatconstitutessuchapoint. In factit seemsthat thetendencyis to callanything
Yuma
that is not a trueFolsom
or a barbed and tanged arrowheadof the recent Plainstype. Dr. E. B.Renaud,of the University of Denver,was
the first to describe theform
and gaveit the
name Yuma.
His discussion and classification, including his several subtypes,may
befoundin hisvarious publications." Dr. E. B.Howard
considers the Folsom-Yuma
problem atsome
length in his"Evidence of Early
Man
in North America,"'" and J. D. Figgins has written anumber
of articles on the subject."As
the situation.^^J:I%^^k^^j,^''Tih4^iJ^.
:.^M%ffMMi''
?"PA^Iff:
t^£'m
<ci> bed LJ UJ UJ ^ f
Fig.2.
— Yuma
point,a: Cross-section,/>,•andbasetypes,c-f. (Actualsize.) Stands today, it seems essential to reach an agreement on what is meant l)yYuma
and that its use be restricted to somethingmore
specificthan itspresentcatch-all connotation.
The
importance of the fragmentsfrom Yuma
type points found atthe Lindenmeier site lies intheevidence bearing ontheir position in the sequence.One came from
the latest old stream channel in section B-3. Itsposition distinctly indicated a later deposition than theblack stratumcontaining theFolsom
points.The
otherspecimencame from
the blacklayer. Thiswas
inA-23.where
indicationswere thatthe layerwas
thebottom of aswamp
orbogdeposit.The
exact positionof thisexamplewas
not obtained, as the pointwas
foundin the screenand notin situ. Indications were that it had been inthe black fairly highabovethecontact. Sincethiscannot be established withcertainty,itwillbe considered as beingonalevelwith theFolsom
'"Renaud,1931,1932,1934.
^^Howard, 1935.
='Figgins, 1934, 1935.
22
SMITHSONIAN MISCELLANEOUS
COLLECTIONS VOL. 95 material. Portions from twootherpoints,nottypicallythe trueYuma
type as described in thispaper but of a
form
usually calledYuma, were
also obtained.One was
above the black layer in section B-8.The
otherwas
abovetheblackintheareajust eastofA-4.The
situa- tionmay
then besummarized
as follows:Out
of four specimens attributed to theYuma
group, onewas
in a position thatmay
be regarded as evidence for contemporaneity with the Folsom, and threewerelater.The Denver Museum
party obtained,initslargepit,fourspecimens whichinabroad sense of theword
mightbecalledYuma. Two
of these werefrom
the contact line between the black and the basic substratum.The
others werefrom
a higher level in the black.The
situation in the deposit
where
these were foundwas
similar to that intrenchA from
section23 throughtothedeeppit.As
aconsequence thereisthe possibilityofsomewhat
later material sinkingto alowerlevel.
The
only conclusion which can bedrawn from
the evidence asitnow
standsisthattherewas
atbestonlyalate contemporaneity betweenYuma
andFolsom
atthe Lindenmeiersitewith alater sur- vivalof theYuma.
Subsequentwork may
throwmore
light on the subject and change the picture, but at present theYuma
must be considered comparatively late in this immediate district. Further- more,they are only aminor
factor,as only .05 percent of the pointsfrom
the site can be classified asYuma,
andsome
of these are of sucha nature thattheirinclusionishighly debatable.Implements of this type comprise 32.8 percent of the collection
from
the1935excavations (pis.5,6, 7,8).The
toolsfallintoseveral majorgroups.These
are the side scrapers, "snub-nosed" scrapers, end scrapers, "thumbnail" scrapers, and scraper edges.The
latter consist of piecesfrom
broken implements too indefinite in char- acter to warrant inclusion in one of the other classes.The
term"thumbnail" is occasionally used as a
synonym
for "snub-nosed."Inthisdiscussion they areregarded asdifferent types.
The
side scraper seriesrepresents 56percent of the group. Thereisconsiderable variationinthe type oftlakesused intheir manufac- ture,theirdegreeoffinish,andintheirgeneralquality.
Some
of the implementsarelight inweightand almostas thinasa sheet ofheavy paper. Othersare thickand cumbersome. Certainexamplesare littlemore
than rough flakes withaworked
edge alongone side only; insome
casesmerelya portion of theedge showschipping. Toolsin this fI
NO. 10