Perforated plates were apparently used as base molds for ceramics and as potters' turntables (Christenson 1994 Lyons and Lindsay 2006), and petrographic analysis indicates this household implement was produced locally at Las Colinas (Elizabeth J. Las Colinas has yielded more perforated plates than any site in southern Arizona except for Reeve Ruin and the Davis Ranch site, in the San Pedro Valley, both of which are widely accepted by archaeologists as Kayenta enclaves (Clark and Lyons 2012 Lindsay 1987). Another three fragments were found during the 1982-1984 excavations (Arizona State Museum collections). Patricia Crown (1981:165) reported fragments of 69 different perforated plates recovered as a result of the 1968 excavations at Las Colinas. Las Colinas and Los Muertos, however, at the distal ends of their canal systems, have yielded the most abundant traces of people practicing northern traditions. Perforated plates, Kayenta pottery-making tools (Lyons and Lindsay 2006), have been recovered from Los Muertos and Los Hornos, in Canal System 1 (Haury 1945:111-112, 180) Pueblo Grande, La Ciudad, and Las Colinas, in Canal System 2 (Crown 1981 Haury 1945:186 Wilcox 1987:203) and South Pueblo Blanco, in the Scottsdale Canal System (McDonnell et al. The presence of descendants of ancestral Puebloan groups from the Kayenta region of northeastern Arizona and southeastern Utah frequently has been posited (Abbott 2003 Haury 1945 Lyons 2003a Lyons and Lindsay 2006). Pre-Classic ceramic assemblages from Las Colinas indicate the presence of a Yuman "barrio" at Las Colinas (Beckwith 1988 Teague 1989a:122-123) and co-residence of Hohokam and Patayan groups has been documented downstream on the lower Salt (Watkins and Rice 2010). Newcomers to the lower Salt included immigrants from Hohokam hinterlands, perhaps including the lower San Pedro River Valley, Tonto Basin, and Verde Valley.
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