Flaked Stone and Social Interaction in the Casas Grandes Region, Chihuahua, Mexico

Abstract

This analysis uses flaked stone artifacts to gain insight into the social and economic structure of the Casas Grandes region, northern Chihuahua, Mexico. It begins by considering the intrasite variation in flaked stone reduction at Galeana, a large site near the modern town of Galeana. The analysis of debitage and cores from Galeana indicates that the assemblage is primarily the product of hard hammer, generalized reduction of locally available materials. Differences within the assemblage indicate the presence of spatially distinct reduction areas, with initial core reduction occurring in open areas, and then continuing in room blocks. We then compare the Galeana assemblage with the flaked stone assemblage from the site of Paquimé (Casas Grandes), Chihuahua. The analysis indicates that the reduction technique employed at both sites is similar, but that the Paquimé assemblage is characterized by a greater proportion of cryptocrystaline silicates and obsidian than the Galeana assemblage. Furthermore, much of the raw material from Paquimé does not appear to be locally available. We conclude that the prehistoric inhabitants of Paquimé had greater access to cryptocrystaline silicates and obsidian acquired through trade than did the inhabitants of Galeana. This evidence indicates that the economic pattern evident at Paquimé did not extend to Galeana and supports the idea that Paquimé's economic and political influence over other Casas Grandes sites was limited beyond a 30-km radius.