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Culture and Ecology of Chaco Canyon and the San Juan Basin

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The Preceramic Period 69tool production, <strong>and</strong> tool use. Vierra (1994) also used<strong>the</strong> types <strong>of</strong> materials <strong>and</strong> <strong>the</strong> locations <strong>of</strong> <strong>the</strong>ir sourcesto outline possible areas utilized during an annualround by groups using <strong>the</strong> central <strong>San</strong> <strong>Juan</strong> <strong>Basin</strong>.In summary, <strong>Chaco</strong> Project surveys covered allphysiographic situations within <strong>the</strong> park boundaries.A typology <strong>and</strong> criteria for cultural subdivisions <strong>of</strong> <strong>the</strong>Preceramic adaptation were established. The dataconfirmed Gordon Vivian's impression that Preceramicsites were present on Chacra Mesa, but <strong>the</strong>evidence included a few sites in <strong>the</strong> canyon bottom, aswell as on ridges or mesa ledges in o<strong>the</strong>r areas <strong>of</strong> <strong>the</strong>park (Hayes 1981).There is limited evidence for <strong>the</strong> use <strong>of</strong> <strong>the</strong> areaaround <strong>Chaco</strong> <strong>Canyon</strong> from Paleoindian through LateArchaic. The Paleoindian evidence consl' ..... "t".c\ -- ..... ""'. f on ....... Iv Jfive diagnostic projectile points. The more robustArchaic evidence indicates that approximately 28 sites,plus two isolated points (Figure 3.2), are locatedwithin <strong>the</strong> current park boundaries. The greatestnumber <strong>of</strong> Preceramic sites were occupied during <strong>the</strong>Middle <strong>and</strong> Late Archaic; points from <strong>the</strong> additionall<strong>and</strong>s survey peaked in Late Jay <strong>and</strong> Middle Archaic.Gillespie (1985) thought that <strong>the</strong> Late Jay <strong>and</strong> Bajadaperiods represented moist summers with an increase inplants <strong>and</strong> animals, <strong>the</strong> availability <strong>of</strong> pinon nuts, <strong>and</strong>probably <strong>the</strong> peak abundance <strong>of</strong> bison, followed by aless mesic but cooler period (<strong>San</strong> Jose-Armijo) duringwhich <strong>the</strong>re would have been less abundance <strong>of</strong>resources. Thus, <strong>the</strong> low numbers <strong>of</strong> sites/points(which mayor may not be truly representative <strong>of</strong> <strong>the</strong>use <strong>of</strong> <strong>the</strong> area) indicate larger populations during<strong>the</strong>se moister periods. Whe<strong>the</strong>r <strong>the</strong>se sites representseasonal use by mobile groups or use by a limitednumber <strong>of</strong> people living in <strong>the</strong> <strong>Chaco</strong> area was notascertained. The documentation <strong>of</strong> nonlocal materials(obsidian <strong>and</strong> basalt) indicates ei<strong>the</strong>r large territoriesfor mobile groups or trade among Archaic people.ExcavationsInitially, Thomas W. Ma<strong>the</strong>ws was responsiblefor <strong>the</strong> preceramic site excavations. Sites with culturalhorizons such as <strong>the</strong> Paleoindian, Archaic, <strong>and</strong>Basketmaker II horizons, were considered "on <strong>the</strong>basis <strong>of</strong> single phase occupations where no earlier orlater manifestations would be likely to complicate <strong>the</strong>,.Figure 3.2. Examples <strong>of</strong> Archaic <strong>and</strong> BasketmakerII dart points <strong>and</strong> preforms.(Taken from Cameron <strong>and</strong> Young2005.)excavations <strong>and</strong> confuse <strong>the</strong> picture" (Ma<strong>the</strong>ws 1979).One goal was to reassess <strong>the</strong> existence <strong>of</strong> BasketmakerII sites; which were thought to resemble <strong>the</strong> LateArchaic sites, with <strong>the</strong> addition <strong>of</strong> cultigens. Toobtain necessary data, rockshelters <strong>and</strong> cave loci, aswell as open sites without ceramics, were considered.Fur<strong>the</strong>r considerations were Archaic flaked stoneforms, open site configuration <strong>and</strong> location, presence<strong>of</strong> "figure-eight"-shaped surface depressions surroundedby broken cobble or o<strong>the</strong>r stone paving, <strong>and</strong>location near or on dunes.Five sites, considered to be Archaic, wereselected for excavation. All were on <strong>the</strong> north side <strong>of</strong><strong>the</strong> <strong>Chaco</strong> Wash, ei<strong>the</strong>r around Cly's <strong>Canyon</strong>(29S1126, 29S1116, <strong>and</strong> 29S11118)(Figure 3.3) or <strong>the</strong>next canyon to <strong>the</strong> west (29S11156 <strong>and</strong> 29S11157)(Figure 3.4); none were on Chacra Mesa. Once excavationswere under way, 29SJ1118, a lithic site with

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