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Culture and Ecology of Chaco Canyon and the San Juan Basin

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The Final Years 243ceramic types, by A.D. 1350 <strong>the</strong> sou<strong>the</strong>rn <strong>San</strong> <strong>Juan</strong><strong>Basin</strong> can be divided into three distinct subdivisions:<strong>the</strong> Western, or Acoma-Laguna, area (Tularosa tradition);<strong>the</strong> Eastern (Mesa Verde tradition); <strong>and</strong> <strong>the</strong>Lower Puerco (Socorro tradition). Along <strong>the</strong> middleRio <strong>San</strong> Jose, <strong>the</strong>re is some overlap <strong>of</strong> <strong>the</strong> Mesa Verdetradition with <strong>the</strong> western tradition, especially in <strong>the</strong>area around Acoma Pueblo. Sherds from <strong>the</strong> Socorrotradition are found in both <strong>the</strong> Tularosa <strong>and</strong> MesaVerde tradition sites. In <strong>the</strong> north, this evolutioncomes to an end at about A.D. 1350, <strong>and</strong> <strong>the</strong> area isab<strong>and</strong>oned, while in <strong>the</strong> south, although <strong>the</strong>re arechanges in settlement pattern, <strong>the</strong>re is continuedoccupation <strong>of</strong> major areas into <strong>the</strong> Historic period.If continued ceramic traditions indicate participationin a long-established group, during <strong>the</strong> periodfrom A.D. 1100 through 1350, a major divisionbetween those using carbon <strong>and</strong> mineral paints tookplace. Roney (1996) suggested that <strong>the</strong> fuzzy ceramicborders at <strong>the</strong> eastern <strong>San</strong> <strong>Juan</strong> <strong>Basin</strong> flow over into<strong>the</strong> Rio Gr<strong>and</strong>e area (<strong>the</strong> close relationship <strong>of</strong>McElmo/Mesa Verde <strong>and</strong> <strong>San</strong>ta Fe types), whichwould suggest ties between <strong>the</strong>se peoples. However,migration, or a slow movement <strong>of</strong> people from <strong>the</strong>Mesa Verde <strong>and</strong> <strong>Chaco</strong> areas through <strong>the</strong> Rio PuercoValley <strong>and</strong> into <strong>the</strong> Rio Gr<strong>and</strong>e, seems unlikelybecause both <strong>the</strong> Mesa Verde <strong>and</strong> Rio Puerco areas areab<strong>and</strong>oned at <strong>the</strong> same time (but see recent commentsby Baker <strong>and</strong> Dur<strong>and</strong> [2003:188-189], who proposemovement downstream to Hummingbird <strong>and</strong> laterpossibly to Pottery Mound, thus indicating possiblecontinuity through time). The presence <strong>of</strong> MesaVerde peoples in both <strong>the</strong> eastern <strong>San</strong> <strong>Juan</strong> <strong>Basin</strong> <strong>and</strong><strong>the</strong> Rio Gr<strong>and</strong>e areas in <strong>the</strong> late 1200s, however, isaccepted.Like Gwinn Vivian (1990) <strong>and</strong> McKenna (1991),Roney (1996) suggested a change in agriculturalpractices; <strong>the</strong> shift led to <strong>the</strong> ab<strong>and</strong>onment <strong>of</strong> dryfarming in lowl<strong>and</strong> areas <strong>and</strong> a movement to lowl<strong>and</strong>areas with slick rock that channeled water to farmingareas or to upl<strong>and</strong> settings that were better watereddue to enhancement by orographic effects. Roney(1996) proposed that local communities retained <strong>the</strong>irorganization. The presence <strong>of</strong> "pre-eminent" sites(those that are larger than o<strong>the</strong>rs in <strong>the</strong> community)suggests some formal organization; <strong>the</strong>se are also <strong>the</strong>last within <strong>the</strong> community to be ab<strong>and</strong>oned. Thesepre-eminent sites vary considerably in layout; somehave plazas, some are in defensive locations, <strong>and</strong> someare walled. The possibility <strong>of</strong> conflict cannot beoverlooked.The period beginning around A.D. 1100 was anunsettled time, when local communities can be easilyassigned to distinct ceramic provinces that <strong>of</strong>ten do notinteract with one ano<strong>the</strong>r (Roney 1996). In <strong>the</strong>Acoma-Laguna area, <strong>the</strong> mixing <strong>of</strong> Mesa Verde <strong>and</strong>Tularosa traditions suggested continued interaction ora melding <strong>of</strong> peoples with different backgrounds <strong>and</strong>outlooks.Roney's ideas are not very different from those<strong>of</strong> Lekson <strong>and</strong> Cameron (1995), who proposed anexpansion <strong>of</strong> <strong>the</strong> <strong>Chaco</strong>an regional system betweenA.D. 1050 <strong>and</strong> 1150, with an early A.D. 1100s shift<strong>of</strong> <strong>the</strong> center from <strong>Chaco</strong> <strong>Canyon</strong> to <strong>the</strong> Totah region<strong>of</strong> <strong>the</strong> <strong>San</strong> <strong>Juan</strong> River. They suggested that aroundA.D. 1150 a balkanization or division <strong>of</strong> <strong>the</strong> regiontook place, but <strong>the</strong> <strong>Chaco</strong> pattern <strong>of</strong> communitycontinued even though it was no longer <strong>the</strong> center.The great houses were still used, but <strong>the</strong>ir functionschanged. Based on similarities between <strong>the</strong> paintedwood recovered from Chetro Ketl (Gwinn Vivian etal. 1978) with that used on contemporary Puebloceremonies, Lekson <strong>and</strong> Cameron suggested thatkatsina dances (associated with <strong>the</strong> use <strong>of</strong> macaws),which <strong>the</strong>y believe originated in <strong>the</strong> Mimbres areaaround A.D. 1050, were introduced. Lekson <strong>and</strong>Cameron (1995) reported ties through oral histories <strong>of</strong><strong>the</strong> Hopi <strong>and</strong> Zuni peoples that point to <strong>Chaco</strong>, whereboth lived toge<strong>the</strong>r <strong>and</strong> where <strong>the</strong>ir ceremonial cyclesbegan; it is still considered <strong>the</strong>ir nor<strong>the</strong>rnmost place(Ferguson <strong>and</strong> Hart 1985). Leksan <strong>and</strong> Cameronprovided a link between Acoma <strong>and</strong> <strong>the</strong> <strong>Chaco</strong> <strong>and</strong>Mesa Verde areas, which are named in migrationaccounts. Lekson (1999) pursued this link fur<strong>the</strong>r; forthis discussion, <strong>the</strong> goal is only to provide a backgroundfor <strong>the</strong> historic pueblos <strong>and</strong> to link <strong>the</strong>m to <strong>the</strong>prehistoric sites <strong>and</strong> possible practices we canreconstruct from <strong>Chaco</strong>an archaeology.Most recent studies by Hill et al. (2004) plot <strong>the</strong>presence <strong>of</strong> sites with 50 rooms or more between A.D.1200 <strong>and</strong> 1600 at 50-year intervals. Their graphicillustration confirms a slow movement out <strong>of</strong> <strong>the</strong> FourComers area to <strong>the</strong> historic Pueblo villages <strong>of</strong> today.They caution, however, that <strong>the</strong>re may have beensmaller sites existing during some <strong>of</strong> <strong>the</strong>se periods so

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