The
1935 investigations at the Lindenmeier site consisted of the digging oftwo
largetrenchesthroughtheareawhere
objectsattribu- table toFolsom man
arefound, of further excavationsinthedeeppit in theravinebankwhere
mostof the specimens obtained duringthe preliminary investigations were dug,and
of uncovering the remains of agroupof bisonat the locationwhere
Judge C. C. Cofifin, A. L.Coffin,and Maj.
Roy
G. Coffinmade
theiroriginal discoveries.The
collectionobtained
from
thework
containssome
750specimens, large quantities of chipper's debris,and numerous
bonesfrom
animals killedbythe former occupants ofthe region.The
artifacts comprise a series of tools and implements of which 11.3 percent are points, 32.8 scrapers,5.6gravers, i.ochisel-gravers,0.5choppers, 3.0 knives, 6.3 large blades, 0.8 hammerstones, 1.6 pieces of hematite which have been rubbedorshaped, 13.6channelflakesfrom
the longitudinal groovesinthe facesof thetypically fluted points,4.0 sandstonerub- bers, 0.5 pieces of bone showing evidences of workmanship, and 19 percentflakesshowingsignsofwork
but too nondescriptincharacter to permit classification as types of implements.The
artifacts as a groupshow
thatthelithiccomponent
inthelocal cultural patternwas
primarily aflake industry, slightly lessthan 1.5 percent of the imple- mentsbeing of the coretype.The
sizerangeinthe pointsinthecollection raisesa pertinent ques- tion, namely.On what
type ofweapon
weretheyused?The
general conception, based onknowledge of the Southwestand
theMexican
area,hasbeen thatthe
bow
andarrow was
a late developmentintheNew World and
that older cultures employed a spear and spear thrower. Archeologists occupied with theFolsom
problem have as-sumed
thattheflutedpoints,becauseoftheirsize,were usedin a shaft hurledfrom
a spear thrower.Many
of the smaller examples in the present groupcould easily have functioned as arrowheads and sug- gest thatthe earlybisonhuntersmay
on occasion have usedthebow.Definite conclusions should not be attempted solely on the evidence of stone points, but attention shouldbe called tothe fact that all of
them
arenot necessarily of asizerequiring a spearshaft.Interestingevidenceon one of the"burningissues " inthearche- ology of the western plains area, the
Folsom-Yuma
problem,was
obtainedfrom
theinvestigations. Stratigraphicmaterialdemonstrated that as far astheLindenmeiersite isconcernedtherewas
only avery late contemporaneity betweenFolsom
andYuma
points, theYuma
appearing toward the end of the
Folsom
occupationand
survivingNO. lO
SECOND
REPORTOX FOLSOM COMPLEX
ROBERTS 35 longer. Furthermore,Yuma
points constitute so small a factor thatit isquestionablewhetherthey should be consideredasbelonging to the complex.Fivespecies ofanimals are representedinthebones
from
the site.Only
one, the bison, is an extinct form.Nine
species ofmoUusks
were foundand whilenone of these is extinct,two
are considerably north oftheirpresent range. Theirpresenceatthe Lindenmeiersite is considered an indication that the climatewas somewhat warmer
andmoisterwhen Folsom man was
therethanitisnow.The
large trenches revealed in cross-section the deposits overlying the oldlevelof occupationand demonstratedthatwhatnow
constitutes a terracewas
at onetime an old valley bottom.The
ridge that bor- dered its southern side has been erodedaway
since the areawas
abandoned by its aboriginaloccupants.The
nature of the valley fill, as exposed in the trenchwalls, suggests that the changes whichcul- minatedinthe presentstateof the sitecould nothave been extremely rapid ones. Considerable timemust
haveelapsed sincethe layer con- tainingtheman-made
objectswas
laiddown. Evidenceinthe trenches also indicated that themakers
of the tools and theFolsom
points stopped for atime along the slope above the old valley bottom. If the trenches did not cross a portion of therealcampsite,theyat least bordered on it. Thiswas shown
by the finding of cut and burned bones,charcoal andwood
ashes, hammerstonesand
chipper'sdebris, and implements brokeninthemaking. Allwereso situated thattheir locations could not be attributedto drift or tothe washingdown
of materialfrom
higherlevels.The
broken implements,when
the frag- mentsarefittedtogether andthe originalflakeisrestored, givegood evidence of the techniqueusedinthe manufactureoftools.The
trenches didnotproducedata that are of aidindeterminingthe age of thesite. Despitetheirestablishingthe factthat thesoil layer inwhichthe objects arefoundwas
produced bythe naturaldecay and break-up of the top of the Oligocene bed underlyingthe area, they gavenoclue either totheagencythatoriginallyerodedaway
the over- burden, thus laying bare the Tertiary stratum and forming the old valley,or to the timewhen
the actiontook place. Conditions atthe Clovis lakebeds aresomewhat
betterfrom
the standpoint of dating, and Dr. Ernst Antevs has reached the conclusion,from
extensive studiesof the area,that theFolsom
artifacts found there represent anantiquityoffrom
12,000to 13,000years."" Since the Clovis mate-rial indicates that it comprises the relics of a people
whose
material Antevs, 1935,p.311.36 SMITHSONIA^-
MISCELLANEOUS
COLLECTIONS VOL. 95 culturewas
similar to that of the group occupyingthe Lindenmeiersite, it
may
be suggested that the latterwas
approximately thesame
age. This shouldnot be regarded asanestablished fact; it is merely a postulationbasedonanalogy. Subsequentwork may show
thetwo
sites to have been as widely separated in time as they arein space.
There
isstill anopportunitytoobtaina geologic date for the Linden- meiersite througha study of the terrace systemof the South Platte River and therelation of its terracestothe glaciation intheRocky
]\Iountains to the west.The
Lindenmeier terracecan be correlated withthose of theSouthPlatte,but as yet there hasbeenno determina- tion of the ages of the latter.An
attempt to solve this particular problemwillconstitutea part of theprogram
for futurework
inthe region.No human
remains have been found, and so far as his physical characteristicsareconcerned,Folsom man
isstillapersonaincognita.There
is no evidence as towhat
type of shelter hemay
have used.On
the otherhand
it seems obviousthathewas
a typicalhunter de- pendingentirelyupon
the bison for hismaintenance andsustenance.He no
doubt supplementedhispreponderantmeatdietwithwild seedsand
"greens" but did notcultivate hisown
vegetal food.He
prob- ably didnotsettlelong inone placebut traveled whereverthe bison moved,in ordertosupport himself.For
thatreason itisnot likely that his dwelling consisted of anythingmore
substantialthan a tentmade from
the skinsof that animal. Traces of the placeswhere
he pitched his shelter will be extremely hard to find at this late date.A
hardpackedfloor andhearth,perhapssome
post molds,isthemost that canbe expected.He
probablytarriedas longattheLindenmeiercamp
ashedidatanyofhissettlements, possibly longerthanatmost ofthem when
itsadvantagesarerecalled.Hence
thechancesoflocat- ing a lodge siteor even of uncovering hisown
remains are notal- togetherbeyond
thebounds oflikelihood.The
old valley bottom with itsnumerous meadows,
marshes, and bogs undoubtedly attracted bison because of the reeds and sedge grasses forfeedand
themireinwhichtowallow. Itisnotlikelythat largeherds frequentedthe district—
rather that small groups drifted infrom
the plains to the east.The
presence of the animalswould
draw Folsom man
intothe area,butinaddition therewerethe assets ofraw
material for useinmaking
implements,agood
supply of water, firewood,anda pleasantcamping
spot.Here
hecouldstalkhisgame, cutand
drythemeatnotwanted
forimmediate consumption,tan the skins,make
his tentsand suchclothing ashisneeds required,fashionXO. lO
SECOND
REPORTON FOLSOM COMPLEX
ROBERTS 37 histoolsfrom
theavailable stone,andpreparehisequipment for the inevitabletrekwhen
the bison shiftedto other pastures.Presentindicationsare that the Lindenmeiersite
was
notoccupied continuously bya largegroup of people. Itprobablywas
an annualsummer
and fall camping grounds visitedregularly over a period of yearsbysmallerparties.That
theintervalsbetweenoccupationswere not protracted isshown
bythehomogeneous
nature of the layer in whichtheartifactsarefound.
Dalam dokumen
Smithsonian miscellaneous collections - Smithsonian Institution
(Halaman 44-47)