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Culture and Ecology of Chaco Canyon and the San Juan Basin

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Basketmaker III to Pueblo I 99In summary, at <strong>the</strong> start <strong>of</strong> <strong>the</strong> <strong>Chaco</strong> Project,<strong>the</strong>re were several issues that deserved attention.Among <strong>the</strong>m were <strong>the</strong> difficulty in estimating <strong>the</strong>number <strong>of</strong> pit structures buried under several feet <strong>of</strong>alluvium along <strong>the</strong> main <strong>Chaco</strong> Wash or under latersite components, in assigning dates to components, ininterpreting <strong>the</strong> variability in architectural features forcontemporary sites, <strong>the</strong> settlement pattern, <strong>and</strong> <strong>the</strong>possibility that more than one group lived within <strong>the</strong>area. It would be difficult to underst<strong>and</strong> <strong>the</strong> transitionsfrom horticulture to agriculture <strong>and</strong> from pitstructures to above-ground houses without better datedexcavations.This chapter will focus on information ga<strong>the</strong>redduring surveys <strong>and</strong> excavations in order to address<strong>the</strong>se issues. The final report on Basketmaker III­Pueblo I excavations (windes 2006a) will providegreater detail. Here, I have relied heavily onMcKenna's (1986) synopsis <strong>of</strong> small-site excavations<strong>and</strong> Truell's (1986) syn<strong>the</strong>sis <strong>of</strong> small-site architecture,which provide careful analyses <strong>of</strong> changes inpit structures <strong>and</strong> above-ground structures throughtime. Their information is combined with artifactanalyses <strong>and</strong> o<strong>the</strong>r studies to provide a picture <strong>of</strong> <strong>the</strong>foundations for later developments in <strong>Chaco</strong> <strong>Canyon</strong><strong>and</strong> <strong>the</strong> <strong>San</strong> <strong>Juan</strong> <strong>Basin</strong>.<strong>Chaco</strong> Project StudiesThe <strong>Chaco</strong> Prospectus (NPS 1969) recommendedthat ceramic <strong>and</strong> architectural sequences be reevaluated<strong>and</strong> populations be estimated in order tobetter underst<strong>and</strong> <strong>the</strong> shift <strong>of</strong> Basketmaker sites typical<strong>of</strong> <strong>the</strong> sou<strong>the</strong>rn half <strong>of</strong> <strong>the</strong> <strong>San</strong> <strong>Juan</strong> <strong>Basin</strong> into <strong>the</strong><strong>Chaco</strong> area <strong>and</strong> <strong>the</strong> shift from mesa top locations tovalley bottom locations. Changes in <strong>the</strong> environmentthat related to <strong>the</strong> discovery <strong>of</strong> pithouses beneath <strong>the</strong>present surface along <strong>the</strong> <strong>Chaco</strong> Wash neededclarification.Survey DataJudge's transect survey crew identified 43Basketmaker III sites based on <strong>the</strong> presence <strong>of</strong>depressions, indicating pithouses, <strong>and</strong> a dominance <strong>of</strong>Lino Gray pottery. An absence <strong>of</strong> surface structureswas a major factor in distinguishing <strong>the</strong>se sites fromlater Pueblo I sites (Judge 1972:31-32). Although <strong>the</strong>Basketmaker III sites were found at similar mean siteelevations as earlier Preceramic sites, <strong>the</strong>ir location onMenafee Shale 66 percent <strong>of</strong> <strong>the</strong> time <strong>and</strong> on s<strong>and</strong>stone24 percent <strong>of</strong> <strong>the</strong> time was exactly opposite from <strong>the</strong>earlier site distributions with regard to geologicalsubstrate. The mesa <strong>and</strong> canyon edge locations <strong>of</strong>many <strong>of</strong> <strong>the</strong> open-air Preceramic sites would havebeen unsuitable for <strong>the</strong> construction <strong>of</strong> pithouses.Judge also attributed this difference to an association<strong>of</strong> Basket maker III sites with a low average distance to<strong>the</strong> nearest stream, especially when compared withsites assigned to different periods. Basketmaker IIIsites were generally found on hills, ridges, or activedunes in upl<strong>and</strong> areas south <strong>of</strong> Chacra Mesa, as wellas on <strong>the</strong> elevated Menafee Shale outcroppings foundat mesa bases in close association with tributariesra<strong>the</strong>r than major streams.Hayes's (1981) inventory survey assigned datesfor <strong>the</strong> Basketmaker III period from A.D. 400 or 500to A.D. 725 or 750. Subcircular subterranean pithouseswith antechambers or large ventilator shaftshad oval or bean-shaped cists located behind <strong>the</strong>m.Characteristic artifacts included two major ceramictypes (Lino Gray <strong>and</strong> La Plata Black-on-white);imported ceramics from <strong>the</strong> Mogollon region (darkredwith black smudged interiors); bows <strong>and</strong> arrowsinstead <strong>of</strong> atlatls; <strong>and</strong> deep trough metates.Using<strong>the</strong>se criteria, <strong>the</strong> survey crews identified a total <strong>of</strong>188 Basketmaker III sites located on mesas (n=60),on plains (n = 40), <strong>and</strong> in bottoml<strong>and</strong>s (n = 88) (Hayes1981:Figure 13).Because 15 Basketmaker III sites were found incutbanks <strong>of</strong> canyon bottom arroyos, Hayes (1981:24)was concerned about site visibility for <strong>the</strong>se pitstructures. Windblown s<strong>and</strong> quickly covers pitstructures on mesa tops (e.g., Roberts's [1929] needto trench to uncover pithouses at Shabik'eshcheeVillage), <strong>and</strong> exposures in arroyo cuts indicatedconsiderable aggradation <strong>of</strong> <strong>the</strong> <strong>Chaco</strong> Wash overtime. Hayes estimated a rate <strong>of</strong> deposition <strong>of</strong> about3.9 m (13 ft) in 500 years, <strong>and</strong> suspected that 150 sitesmay have been buried in <strong>the</strong> floodplain <strong>and</strong> notrecorded. If Hayes's estimate is correct, approximatelytwo-thirds <strong>of</strong> <strong>the</strong> Basketmaker III sites wouldhave been located in <strong>the</strong> bottoml<strong>and</strong>s, closer tointermittent streams.Two great kivas were recorded, one atShabik'eshchee Village <strong>and</strong> <strong>the</strong> o<strong>the</strong>r at 29SJ423 on

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