research has been undertaken between Late Classic centers of similar size in the Petén Lakes region, such as between Motul de San José and Tayasal. One exception is a ceramic figurine study by Halperin (2014), which indicates that western Petén Lakes region sites (Motul de San José, Nixtun Ch'ich', Tayasal, Flores, Trinidad, Buenavista, and Chäkokot) had political-economic ties with each other. The current study provides evidence for the movement of polychrome pottery and, in some cases the raw materials used to produce such pottery, among the Petén Lakes region centers of Motul de San José, Tayasal, Flores, and Zacpetén, as well as among Petén Lakes centers and the primary capital of Tikal. We suggest that centers along the western shores of Lake Petén Itzá allied or affiliated themselves with one another, serving to strengthen provincial relations. Iron oxides, such as hematite, magnetite, goethite, and lepodicrocite, are minerals commonly found in red slips and red slip-paints decorating Classic period Maya pottery (Beaudry, 1989; Goodall et al., 2009; Smith, 2013). These slips and slip paints were applied to the vessel before it was fired at approximately 550-1000°C. Because these minerals are thermally unstable (e.g. magnetite and goethite convert to hematite when heated ca. 300-400°C, lepodicrocite converts to maghemite between 275-300°C and maghemite to hematite ca. 700°C) (Cornell and Schwertmann, 2003, pp. 365-377; Goodall et al., 2009; Walter et al., 2001), mineral analysis of red slips or slip paints can be problematic for identifying paint recipes. On the other hand, chemical analysis of vessel paints in conjunction with vessel pastes can provide a high-resolution, multi-component perspective of materials composition useful for identifying pottery production recipes and sources.