38
SMITHSONIAN MISCELLANEOUS COLLECTIONS
VOL.99
NO. 23
SANDIA
CAVE,NEW MEXICO — HIBBEN 39
the site.
The
Sandia layer is less consolidated than theFolsom
and contains fire areas or hearths.Below
the Sandia occupation, between the Sandiaand
bedrock, lies an intermittent layer of disintegrated limestone of claylike consistency.Artifacts of the
Folsom
layer comprise a series of toolsand
imple- ments, includingFolsom
pointsand
other objects considered typical ofFolsom
times. ClassicFolsom
points are represented bytwo whole
pointsand two
bases.Three
unchanneledFolsom-shaped
points are present, as well as one lanceolate Southern Plains type.Five large blades, six gravers, seven snub-nosed scrapers, four side scrapers, ten flake knives, one ivory shaft,
and two worked
splinters ofbone make up
the rest of theFolsom
series.The
Sandia layer is equally distinctive. Sandia points are gen- erally larger than typical Folsoms,and
not so well chipped.These
earlierpoints aredistinguished
by
a side shoulder or notch suggestive of Solutrean points, althoughno
contemporaneity or connection betweenthem and
theOld World forms
is necessarily implied by such comparison.The
Sandia points are further divided intotwo
subtypes, both possessing the side-shouldered feature.Type
i islanceolate
and rounded
in outline.Type
2 is straight-shafted with paralleling sides.Type
i is apparently slightly older than type 2.The
rest of the Sandiacollectioncomprises three snub-nosed scrapers, one side scraper,numerous
flakeswhich may
ormay
not have been used as knives,and two bone
points.Twelve
species of animals are present in all the strata of Sandia Cave. In the recent layer, only theground
sloth is an extinctmem-
ber. Sloth remains
were found
only in the lowermostportions of the recent depositand
in the rear of the cave.The Folsom
layer is dis- tinguishedby
horse, camel, bison,mammoth, ground
slothand
wolf.The
Sandia stratum includes in its faunal assemblage horse, bison, camel, mastodon,and mammoth. The
paleontological grouping of SandiaCave
is chiefly valuable as contributing toknowledge
of late Pleistoceneand
early Recent times.None
of the species are par- ticularly distinctive nor are the associations new.The
sloth is again indicated as one of the last survivors of themany
large Pleistocenemammals which became
extinct at the end of that periodand
in the beginning of the Recent.Sporadic testing in other caves of the
Sandia-Manzano
area, especially at the siteknown
asManzano
Cave, has produced further results. InManzano Cave
stratawere found which
correspond roughly with Sandia material. In addition, a cultural levelwas
segre- gatedwhich may
be described as early Recent, i.e., following the40 SMITHSONIAN MISCELLANEOUS COLLECTIONS
VOL.99
Folsom. This later-than-Folsom culture is identified by a type of projectile point similar to those ofGypsum
Cave, Nevada. In addi- tion toadistinctivetype of projectile,theManzano Cave
alsoproduced sphericaland
sometimesgrooved stoneballs identifiedas bolaweights.In this region, then,
and
perhaps with validityapplicable to amuch
largerarea, a sequence has been erected. This is especially important as it involves the
famous Folsom
culture, already the center of a controversy concerning the antiquity of the Paleo-Indian inNorth
America.The
variouscomponents
of the sequence occur in the fol-lowing order
:
Recent Pueblo occupation Considerable time interval
Manzano (Gypsum Cave) Early Recent
Wet
period End of PleistoceneFolsom Late Pleistocene or
early Recent
Wet
period Late PleistoceneSandia Late Pleistocene
This sequenceinvolvinganearlier-than-Folsom cultureagainbrings to the fore the question of
Old World
connections. Thisproblem
isrendered the
more
pressing by reason of the remarkable resemblancebetween
the Sandia pointsand
certain Solutrean examplesfrom
theOld World.
It has alreadybeen pointed out bymany
of those inter- ested(McCown,
1939, pp. 150-152) that Solutrean cultural relation- ship is notto be suggested in the case ofFolsom man
because of the remoteness of true Solutrean (almost entirely within continentalEurope) and
the complete lack of demonstrable connection between Solutrean regionsand
theNew World
across the as yetunknown
reaches of Asia.
The
perhaps fortuitous circumstancethat the Sandia projectile points evenmore
closely resemble certain Solutrean ex- amples brings this question evenmore
prominently to the fore. It iswell
known
bythosewho
have studied Solutrean collections inEurope
thatthebulkof the material is not distinguishedby fine ripple flaking
and
delicatelymade
points a cran. Indeed,European
Solutrean ismuch
closer totheSandia thanto theFolsom, especially astheFolsom
is distinguished by a specialized facial channel unparalleled in
Euro-
pean or Asiatic horizons.However,
it is fruitless to discuss Solu- trean connections or contemporaneity until Asiatic gaps ofawe-
inspiringmagnitude
have been bridged, a possibility at the present time extremely remote.A
schoolofthought advocatinga Neolithic basis forallNew World
cultures exhibits an equal academic
myopia
concerning cultural phe-NO. 23
SANDIA
CAVE,NEW MEXICO HIBBEN
4Inomena
as they arenow known. Although some
"Neolithic" cultures areknown which
existed on a huntingand
fishingeconomy,
their inclusion in Neolithic categories is dependentupon
agriculturaland
animalhusbandry
centers in adjacent territoriesknown
to be con- temporaneous. In other words, the classic text-book sequence of culture forEurope
has already been demonstrated to be invalid for Asia, especially Siberia. Furthermore, rudimentary studies of agri- cultureshow
that of theNew World
to be distinctfrom
that of theOld World
both in the matter of species of plantsand
of methods.It
must
not be forgotten that theword
Neolithicwas
coined forEuropean
problems originallyand was
brought into theNew World
to describe the status of the recent
American
Indian,which
appar- ently paralleled certainEuropean and
Asiatic groups. This status in theOld World
included agriculture, animal domestication,perma-
nenthabitations,bow and
arrow, pottery,etc., all ofwhich
are lacking in the culturesnow
in question. Furthermore, the Neolithic even in Mesopotamia, its supposable point of origin,was
definitely subse- quent to the pluviationsand
climatic fluctuations attendant on the last retreat of theWiirmian
glaciation in its various stadia.There
is
no
reason to believe that the continental glaciations inNorth America were
notcontemporaneous
with those ofEurope
(Daly, 1934) stage for stage, althoughminor
variationsmay have
been localized in one hemisphere.Folsom
and Sandia have been definitely associated with extinctmammal
formsand
with climatic changes coincident with the lastphases of the
Wisconsin
glaciation.There
is no reason todeny
theseNew World
cultures an antiquity comparable withEuropean and
Asiatic culturalphenomena
occurring under similar climatic circumstancesand accompanying
a like fauna.There
isno
need for correlations with definiteEuropean
cultures especially byname,
or even Asiatic ones. Horizons roughly corresponding toFolsom and
Sandia have been describedfrom
southernand
eastern, but not as yet northeastern, Siberia.These
are usuallylumped
under an"Upper
Paleolithic" category
which
is descriptive of a cultural statusand
time rather than of aEuropean
connectionby name,
although the blade industries of theEuropean
levelsand
theNear
East are also represented in Asia (elaborationsand
variations of Aurignacian, Aurignacian-Magdalenian,and
Gravettian).There
seems little need to connectNew World
cultures, whether Sandia, Folsom, orany
other, with Asiatic or