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Culture and Ecology of Chaco Canyon and the San Juan Basin

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- - ----- -------------------------- --12 <strong>Chaco</strong> Project Syn<strong>the</strong>sisfeatures allowed investigators to measure volumes <strong>and</strong>wall thicknesses, to add <strong>and</strong> subtract walls to createmaps <strong>of</strong> different construction stages, <strong>and</strong> to printmaps at any point during <strong>the</strong>se manipulations (Drager<strong>and</strong> Lyons 1985; Pouls et aI. 1976).Are <strong>the</strong>se methods cost-effective? Irel<strong>and</strong> (1980)reported that for small sites <strong>the</strong> traditional methods areuseful <strong>and</strong> cost-effective, but when a site is large ormore than one site is to be mapped, photogrammetricor photo-interpretive mapping should be considered.O<strong>the</strong>r /11Ulgery <strong>and</strong> Sensors. Experimentswith o<strong>the</strong>r imagery obtained above ground werecarried out. Loose (1976a) found that airborne taperecording provided excellent color imagery, but thatfilm resolution was not as good as that obtained fromaerial photographs. Data from a Bendix M 2 S multiscannerflown approximately 457 m (1,500 ft) aboveground over five pueblos in <strong>Chaco</strong> <strong>Canyon</strong> showedpromise in detecting agricultural fields, structures, <strong>and</strong>linear alignments (Morain et aI. 1981). Satelliteimagery (ERTS <strong>and</strong> LANDSAT) provided repeatedbeam video <strong>and</strong> multispectral scans at several scales,including 1:250,OOO--<strong>the</strong> size <strong>of</strong> USGS topographicmaps. Depending on <strong>the</strong> scans combined into a composite,false color infrared or black-<strong>and</strong>-white imagescould be obtained <strong>and</strong> computer enhanced (Drager1983b). Schalk <strong>and</strong> Lyons (1976) stratified <strong>the</strong> <strong>San</strong><strong>Juan</strong> <strong>Basin</strong> into gross ecological zones, <strong>and</strong> determinedthat a clear division between <strong>the</strong> nor<strong>the</strong>astern <strong>and</strong>southwestern parts <strong>of</strong> <strong>the</strong> basin existed. <strong>Chaco</strong><strong>Canyon</strong> is an erosional feature situated on <strong>the</strong> contact<strong>of</strong> two ecotones; <strong>the</strong> resources in each one suggestedenvironmental determinants <strong>of</strong> settlement patterns thatmight be observed from such imagery. Vegetativecover type for <strong>the</strong> <strong>San</strong> <strong>Juan</strong> <strong>Basin</strong> (Camilli 1983;Drager 1983a) was plotted (Drager <strong>and</strong> Livingston1983) <strong>and</strong> compared with geology <strong>and</strong> precipitationmaps (Irel<strong>and</strong> 1983), <strong>and</strong> soils (Irel<strong>and</strong> <strong>and</strong> Drager1983) at <strong>the</strong> same scales as aides in predictingarchaeological site densities for unsurveyed areaswithin a study area (Drager 1983b; Drager <strong>and</strong> Irel<strong>and</strong>1983).One ethnographic study by Fanale (1982) usedboth LANDSAT <strong>and</strong> aerial photography to facilitateresearch on late-nineteenth- <strong>and</strong> early-twentiethcenturyNavajo l<strong>and</strong> use in <strong>the</strong> <strong>San</strong> <strong>Juan</strong> <strong>Basin</strong>.Acetate overlays <strong>of</strong> 31 areas were prepared usingLANDSAT imagery. Cover type, l<strong>and</strong> formations,vegetative associations, soil types, <strong>and</strong> rainfallpatterns were noted. This method quickly provideduseful information about <strong>the</strong> environment <strong>of</strong> each <strong>of</strong><strong>the</strong> study areas (Fanale 1982:75-79). Armed withmaps depicting settlement features, legal l<strong>and</strong> tenureinformation, <strong>and</strong> o<strong>the</strong>r information, as well as aerialphotographs, Fanale was able to quickly locatehousehold units <strong>and</strong> preplan routes to sites that were<strong>of</strong>ten difficult to find in open areas <strong>of</strong> <strong>the</strong> basin.During interviews, informants could mark places <strong>the</strong>yhad lived, zones used for herds, <strong>and</strong> mobility routes(Fanale 1982: 84-85).Three sensors that detect anomalies under groundwere evaluated. Refractive seismology was used toprobe <strong>the</strong> surface beneath <strong>the</strong> canyon floor todetermine depth to bedrock (Lewis <strong>and</strong> Shipman 1972;Ross 1978). However, transects across site 29SJ633by Phil B<strong>and</strong>y (1980) were disappointing. Jacobson(1979; in Mathien 1991a:351) found that none <strong>of</strong> <strong>the</strong>patterns could be interpreted as features. Protonmagnetometer measurements at 29SJ633 <strong>and</strong> PuebloAlto did detect a number <strong>of</strong> features (Bennett <strong>and</strong>Weymouth 1981, 1987:MF-29; Jacobson 1979; inMathien 1991a:353). Tests with subsurface radardetected masonry walls but not adobe walls (Vickers<strong>and</strong> Dolphin 1975; Vickers et al. 1976). Since <strong>the</strong>seexperiments were conducted, many improvementshave been made in equipment to provide better results.In conclusion, as Giardino <strong>and</strong> Thomas (2002)indicate that "By <strong>the</strong> early 1980's, <strong>the</strong>re weresufficient accomplishments in <strong>the</strong> application <strong>of</strong>remote sensing to anthropology <strong>and</strong> archaeology thata chapter on <strong>the</strong> subject was included in fundamentalremote sensing references (Ebert <strong>and</strong> Lyons 1983)."Many <strong>of</strong> <strong>the</strong>se techniques have been fur<strong>the</strong>r refined<strong>and</strong> are now accepted practices in North America <strong>and</strong>Europe (Kvamme 2003). The remote sensing stafffulfilled <strong>the</strong> goals set forth in <strong>the</strong> <strong>Chaco</strong> Prospectus totest this new suite <strong>of</strong> sensors, as well as contributed to<strong>the</strong> cultural research program (contributions areincluded in <strong>the</strong> remaining chapters as appropriate).Survey TechniquesPrevious site surveys ei<strong>the</strong>r focused on Pueblosi tes along <strong>the</strong> bottom <strong>of</strong> <strong>the</strong> canyon (Pierson 1949) orwere limited to a specific area that included l<strong>and</strong>

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