By Timothy A. Kohler
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Extra resources for Emergence and Collapse of Early Villages: Models of Central Mesa Verde Archæology
11B translates our total momentary population estimates into population growth rates for each period. 007). Although we recognize this is a conservative limit (see Kirch 2010:138; Richerson et al. 2001:396–397), we follow Cowgill (1975) in interpreting values above or below this threshold as indicating movement of people into or out of the study area. By this criterion, settlement in the region included several periods of in-migration and out-migration. , Berry 1982; Cameron 1995; Clark 2001; Lyons 2003; Naranjo 1995; Ortman 2009, 2010; Ortman and Cameron 2011; Stone 2003; Wilshusen and Ortman 1999).
Highway 491, which skirts the heads of numerous canyons as it travels northwest from Cortez to Dove Creek, Colorado. The area north and east of the diagonal is of generally higher elevation, receives more annual precipitation, is relatively undissected by canyons, and possesses more continuous expanses of deep loess soils. The Dolores River also ﬂows through the northeast corner, but because of cold-air drainage out of the high mountains to the east, the river valley itself has rarely been suitable for agriculture (Peterson and Clay 1987).
Martin was drawn to southwestern Colorado because relatively little research had been done despite the dense concentration of sites. He selected Lowry because he thought the site would contain deep, stratiﬁed middens that would allow him to establish a pottery sequence. Martin was also interested in understanding the site’s Chacoan architectural traits, which he believed were locally adopted and modiﬁed attributes. Martin’s work at Lowry demonstrated that the site occupation was dynamic, with multiple building episodes and periods of short-term abandonment, reoccupation, and widespread remodeling.