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Culture and Ecology of Chaco Canyon and the San Juan Basin

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-------------- ._----------88 <strong>Chaco</strong> Project Syn<strong>the</strong>sisTable 3.6.Comparison <strong>of</strong> chipped stone materials recovered from Atlatl Cave <strong>and</strong> <strong>the</strong> two dune siteslocated in <strong>the</strong> same rincon. All numbers are percentages.·Material TypeAtlatl CaveSleeping DuneAnt Hill Dune1052 Clear translucent chalcedony661053 Chalcedony with black inclusions 101091 Chert, chaldeconic (Pedernal chert) 101112 Dark silicified wood (nonchalcedonic)1113 Light-colored silicified wood1120 Red-colored silicified wood 271140 Light-colored to white chalcedonic silicified wood1142 Light-colored silicified wood, chalccdonic, undifferentiated 181151 Yellow-brown silicified (jasperized) wood 94000 Quartzite, undifferentiated 6O<strong>the</strong>rTotal percent 10014318516201001426681914-1.100a Taken from Neller (1976b:Tablc 4), with Warren's descriptions for lithic codes added.that <strong>the</strong> shelter represented limited use. The surfacecollections at <strong>the</strong> open sites also were larger.Neller (1976b) also compared <strong>the</strong> chipped stonefrom Atlatl Cave <strong>and</strong> Sleeping Dune with Judge'ssurvey data from Folsom sites along <strong>the</strong> Rio Gr<strong>and</strong>e.He concluded that <strong>the</strong> Archaic-Basketmaker II siteswere different from Folsom <strong>and</strong> that <strong>the</strong> <strong>Chaco</strong> sitesdid not represent base camps, processing sites, orarmament sites. He also compared <strong>the</strong>se three siteswith Preceramic site-location data from Judge's transectsurvey; <strong>the</strong>re was a negative correlation for dunes<strong>and</strong> rincons, thus indicating that <strong>the</strong>se sites were nottypical.Comparative DataThe <strong>Chaco</strong> <strong>Canyon</strong> AreaBesides Atlatl Cave, two o<strong>the</strong>r rockshelters wereexcavated as part <strong>of</strong> <strong>the</strong> <strong>Chaco</strong> Shelters Project(Simmons 1984a) in order to increase knowledge <strong>of</strong><strong>the</strong> Archaic use <strong>of</strong> rockshelters <strong>and</strong> to evaluateSimmons's hypo<strong>the</strong>sis that <strong>the</strong> <strong>Chaco</strong> area may havebeen <strong>the</strong> winter location <strong>of</strong> Archaic peoples whowould be more protected in <strong>the</strong>se rockshelters than inopen areas. Simmons wanted to establish an absolutechronology for <strong>the</strong> <strong>San</strong> <strong>Juan</strong> <strong>Basin</strong> Archaic (which heconsidered a possible variant <strong>of</strong> <strong>the</strong> Oshara tradition[Irwin-Williams 1973,1979; Simmons 1984d: 10)) <strong>and</strong>to improve <strong>the</strong> database available for use inreconstructing <strong>the</strong> paleoenvironment. This projectcontributed more toward <strong>the</strong> latter goal, but data from<strong>the</strong> excavations at Sheep Camp Shelter (29SJ178), <strong>and</strong>Ashislepah Shelter (CAP PB AH 15), <strong>and</strong> surveys in<strong>the</strong> surrounding areas also improved our underst<strong>and</strong>ing<strong>of</strong> <strong>the</strong> Archaic period in this area.Gillespie (1984a) described Sheep Camp Shelter,which is located on <strong>the</strong> north side <strong>of</strong> <strong>Chaco</strong> <strong>Canyon</strong>just east <strong>of</strong> <strong>Chaco</strong> <strong>Culture</strong> National Historical Park<strong>and</strong> 1.5 km west <strong>of</strong> Sheep Camp <strong>Canyon</strong>. It isapproximately 600 m north <strong>of</strong> <strong>the</strong> floodplain at <strong>the</strong>bottom <strong>of</strong> <strong>the</strong> canyon, 60 m above <strong>the</strong> canyon floor (at

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