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Culture and Ecology of Chaco Canyon and the San Juan Basin

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The Final Years 239most <strong>of</strong>ten with great houses, it never exceeds 1percent <strong>of</strong> <strong>the</strong> ceramic assemblages (H. Toll <strong>and</strong>McKenna 1997:334). The quality <strong>of</strong> its craftsmanship<strong>and</strong> its striking appearance may <strong>of</strong>ten lead to enhancedsignificance; for example, Neitzel <strong>and</strong> Bishop (1990:69) suggested that it may represent an elite possession.<strong>Chaco</strong> McElmo Black-an-white marks not only<strong>the</strong> shift to carbon paint, but also a change in designs<strong>and</strong> <strong>the</strong>ir execution. This introduction <strong>of</strong> carbonpaintedpottery was considered by some investigatorsto be an indication <strong>of</strong> influences entering <strong>Chaco</strong> from<strong>the</strong> north (e.g., Gordon Vivian <strong>and</strong> Ma<strong>the</strong>ws [1965],Who included sherds <strong>of</strong> this type in <strong>the</strong>ir McElmoBlack-on-white category). It is considered similar to<strong>the</strong> McElmo Black-an-white <strong>of</strong> <strong>the</strong> Mesa Verde series,with which it can easily be confused. Dates <strong>of</strong> usespan <strong>the</strong> period from A.D. 1100 to 1150.McElmo Black-on-white sherds from <strong>the</strong> <strong>Chaco</strong>Project were <strong>of</strong>ten classified under <strong>the</strong> Pueblo II­Pueblo III (PH-PIlI) carbon-an-white category (H.Toll <strong>and</strong> McKenna 1997:377), which dates to approximatelyA.D. 1075 through 1300. Tighter datesfor McElmo Black-on-white are A.D. 1125 to 1225(H. Toll et al. 1980:Figure 2).Mesa Verde Black-an-white is a distinct type in<strong>Chaco</strong> <strong>Canyon</strong> that dates from A.D. 1200 through1300. It is not an import from Mesa Verde, however.Temper studies suggest that some vessels (26 percent)were made locally; some (7 percent) in <strong>the</strong> ChuskaMountains; <strong>and</strong> some (SO percent) along <strong>the</strong> <strong>San</strong> <strong>Juan</strong>River (H. Toll <strong>and</strong> McKenna 1997:392).The detailed ceramic analysis from 29SJ633 ledMcKenna <strong>and</strong> Toll (1991) to reaffirm <strong>the</strong>ir placement<strong>of</strong>29SJ633 in a continuum within <strong>the</strong> regionally basedceramic attributes, even though <strong>the</strong>re are some fundamentaldifferences between <strong>the</strong> Mesa Verde Black-onwhite<strong>and</strong> <strong>the</strong> Pueblo II-III carbon-an-white ceramicsfrom <strong>the</strong> earlier period. During <strong>the</strong> later period, decoratingsystems changed; motifs decreased in number;<strong>and</strong> placement <strong>of</strong> b<strong>and</strong>s around <strong>the</strong> rims as parallelframers became prevalent. Temper analysis revealedthat ceramics from 29SJ633 were similar to types ato<strong>the</strong>r sites in <strong>the</strong> canyon with regard to <strong>the</strong> primarypresence <strong>of</strong> s<strong>and</strong>stone or quartz s<strong>and</strong>. Trachyte temperfrom <strong>the</strong> Chuska Mountains was also present, butin a smaller proportion <strong>of</strong> <strong>the</strong> sherds than <strong>the</strong> igneoustempers from <strong>the</strong> <strong>San</strong> <strong>Juan</strong> area, which was <strong>the</strong>predominant nonlocal temper material found in <strong>the</strong>carbon-painted ceramics. Through time <strong>the</strong>re was amarked change in rim form from tapered to flat tobeveled. By <strong>the</strong> late A.D. 1100s <strong>and</strong> early A.D.1200s, <strong>the</strong> presence <strong>of</strong> Socorro Black-on-white bowls,pitchers, <strong>and</strong>jars suggested that specific sets <strong>of</strong>formswere being obtained from <strong>the</strong> south. McKenna <strong>and</strong>Toll (1991) indicate that none <strong>of</strong> <strong>the</strong> ceramicassemblages were exclusively used or deposited assets; a variety <strong>of</strong> vessel forms were imported fromdifferent areas. Although <strong>the</strong>re was a continuum in<strong>the</strong> diversity <strong>of</strong> pottery types, sources 7 <strong>and</strong> forms,<strong>the</strong>re was a decline in <strong>the</strong> variety <strong>of</strong> forms throughtime, which possibly indicates increased seasonal use<strong>of</strong> <strong>the</strong> site during <strong>the</strong> Mesa Verde phase. Bowls <strong>and</strong>personal-service items such as ladles, mugs, <strong>and</strong>cooking jars were <strong>the</strong> only forms found among <strong>the</strong>decorated sherds.This analysis suggested a shift in <strong>the</strong> center <strong>of</strong> aregional system from <strong>Chaco</strong> <strong>Canyon</strong> to <strong>the</strong> <strong>San</strong> <strong>Juan</strong>area instead <strong>of</strong> a distinct migration <strong>of</strong> nor<strong>the</strong>rn peopleinto <strong>Chaco</strong> <strong>Canyon</strong> after an ab<strong>and</strong>onment.... we have shown that considerableamounts <strong>of</strong> pottery were still being movedinto <strong>Chaco</strong> <strong>Canyon</strong> although it is not clearif this was <strong>the</strong> result <strong>of</strong> <strong>the</strong> nature <strong>of</strong> <strong>Chaco</strong><strong>Canyon</strong> or <strong>the</strong> nature <strong>of</strong> pottery as a commodityper se.... The complementary nature<strong>of</strong> decorated <strong>and</strong> utility wares in <strong>the</strong>series that makes up <strong>the</strong> late assemblagesuggests that ceramics were not acquired asr<strong>and</strong>om additions but were selected forspecified functions. The level <strong>of</strong> imports,<strong>the</strong> continuity in sources with past assemblages,<strong>and</strong> <strong>the</strong> technological compensationsundertaken with <strong>the</strong> decline inChuskan grayware all suggest a regionalsystem adjusting to changing conditionsbut enduring. Our view regarding somefusion <strong>of</strong> <strong>Chaco</strong>an <strong>and</strong> <strong>San</strong> <strong>Juan</strong> traditionsfor this assemblage still holds. The assemblageis sufficiently similar to earlier <strong>and</strong>contemporary complexes to suggest thathuman occupation encompassed a variety<strong>of</strong> ceramically related activities thatcontinued for an indeterminate time.(McKenna <strong>and</strong> Toll 1991:205)

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