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Culture and Ecology of Chaco Canyon and the San Juan Basin

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116 <strong>Chaco</strong> Project Syn<strong>the</strong>sisin <strong>the</strong> later stages <strong>of</strong> chipped stone tool manufacture.There could have been a gradual decrease in flintknapping activities or an increase in <strong>the</strong> importation <strong>of</strong>blanks ra<strong>the</strong>r than cores <strong>of</strong> o<strong>the</strong>r materials into <strong>the</strong>canyon so that only finishing touches were needed toprepare <strong>the</strong> tools for use. Cameron's {l997c:652)analysis <strong>of</strong> cores indicated that importation from longdistances was almost nonexistent from A.D. 500through A.D. 920. This would suggest that importedlithic materials came as end products ra<strong>the</strong>r than rawmaterials from which to produce tools or flakes. Forlocally available core materials, however, <strong>the</strong> patternsare varied. The number <strong>of</strong> chert <strong>and</strong> splinterysilicified wood cores does decrease from <strong>the</strong> A.D.500s through <strong>the</strong> A.D. 820 to 920 period. The chertysilicified wood cores, on <strong>the</strong> o<strong>the</strong>r h<strong>and</strong>, increase,while <strong>the</strong> relative percentages <strong>of</strong> chalcedonic silicifiedwood cores peak in <strong>the</strong> A.D. 600s (Cameron 1997b:Table 3C.12).For chipped stone tool use, Cameron (1997b:Table 3.8) indicated that nonlocal materials made up5 percent during <strong>the</strong> A.D. 500s; 10 percent during <strong>the</strong>A.D. 600s; 3 percent during <strong>the</strong> A.D. 700 to 820period; <strong>and</strong> 2 percent during <strong>the</strong> A.D. 820 to 920period. These materials varied by type through time(Cameron 1997b:Table 3.9). Obsidian was always <strong>the</strong>most frequently imported material throughout <strong>the</strong>period. During <strong>the</strong> A.D. 500s <strong>and</strong> 600s, Red Hillobsidian (source in west-central New Mexico;Cameron 1993:Figure 3.2; Cameron <strong>and</strong> Sappington1984) was <strong>the</strong> most frequent obsidian source (69.3percent in <strong>the</strong> A.D. 500s, <strong>and</strong> 43.5 percent in <strong>the</strong> A.D. 600s [Cameron 1997b:Table 3.11]), followed byimports from Polvadero Peak (in north-central NewMexico ), Jemez, <strong>and</strong> Modena (Utah) sources. By <strong>the</strong>A.D. 700 to 820 period, <strong>the</strong> predominant obsidiansource was in <strong>the</strong> Jemez Mountains; <strong>and</strong> by <strong>the</strong> A.D.820 to 920 period, it had shifted back to <strong>the</strong> Polvaderosource. In <strong>the</strong> first three periods, <strong>the</strong>re were alsoobsidian pieces from several o<strong>the</strong>r sources in Arizona,Utah, <strong>and</strong> Colorado.More recent analyses <strong>of</strong> source areas for site29SJ629 (see Windes 1993:304) indicate that <strong>the</strong>remay have been fewer Red Hill specimens at this sitethan was suggested during <strong>the</strong> early studies, when <strong>the</strong>numbers <strong>of</strong> Sources were not as well sampled <strong>and</strong>analyzed. Sources identified by Cameron <strong>and</strong>Sappington (1984) as Polvadera were later identifiedas Grants Ridge; Windes (1993:304) assumed that asource near Grants Ridge was more common <strong>and</strong> that<strong>the</strong> Red Hill may have been rarely used. There wereshifts in percentages obtained between two major areas(to <strong>the</strong> north <strong>and</strong> south), but Windes suggested that wemay not be able to accurately estimate <strong>the</strong> amount <strong>of</strong>material coming from <strong>the</strong>se sources during <strong>the</strong>seperiods.Except for some unusual caches <strong>and</strong> a few gravegoods, formal tools make up only a small percentage<strong>of</strong> <strong>the</strong> chipped stone items (Cameron 1997b; Lekson1997). Formal tools were found more frequently in<strong>the</strong> early periods (A.D. 500s <strong>and</strong> 600s); <strong>and</strong> miscellaneouspoints <strong>and</strong> blades were found mostfrequently in <strong>the</strong> A.D. 500s. The relative proportions<strong>of</strong> materials for finished tools are different from <strong>the</strong>chipped stone material types. Cameron (1997b:564)noted that certain tools (e.g., arrow points) were madefrom imported materials. Obsidian is <strong>the</strong> most frequentmaterial type recorded for <strong>the</strong> A.D. 600 throughA.D. 820 period. Drills <strong>and</strong> scrapers, on <strong>the</strong> o<strong>the</strong>rh<strong>and</strong>, were made primarily from local chalcedonicsilicified wood. Cameron identified a possible chippedstone tool workshop area at 29SJ423. Because <strong>the</strong>cores that would indicate importation from long distancesare almost nonexistent from A.D. 500 throughA.D. 920 (Cameron 1997b:652), it is likely that mostimported lithic materials came as end products ra<strong>the</strong>rthan raw materials from which to produce tools orflakes.Evidence for local manufacture <strong>of</strong> pottery waspresent at three sites (29SJ299, 29MC448, <strong>and</strong>Shabik'eshchee Village) during <strong>the</strong> Basketmaker IIIperiod, <strong>and</strong> at two sites (Half House <strong>and</strong> Judd'sPithouse) during <strong>the</strong> Pueblo I period (H. Toll <strong>and</strong>McKenna 1997:Table 2.67). Evidence includes <strong>the</strong>presence <strong>of</strong> a number <strong>of</strong> different tools, raw or workedclays, possible kilns, <strong>and</strong> some uniformity <strong>of</strong> ceramicswithin specific sites.Changes in ceramic wares, forms, <strong>and</strong> designstyles documented by H. Toll <strong>and</strong> McKenna (1997)parallel those found throughout <strong>the</strong> Anasazi regionduring <strong>the</strong> Basketmaker III <strong>and</strong> Pueblo I periods. Theuse <strong>of</strong> reddish paint increases from 44 percent in <strong>the</strong>A.D. 500s to 70 percent during <strong>the</strong> A.D. 600s, but itdecreases to 6.4 percent between A.D. 700 <strong>and</strong> 820,<strong>and</strong> to 2.2 percent between A.D. 820 <strong>and</strong> 920 (H. Toll

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