Abstract
The recovery of obsidian artifacts in radiometrically dated cultural stratigraphic levels at the Maya site of Cahal Pech (Belize) suggests that there was a flake-to-bladelet sequence of development of obsidian technology in the Belize Valley region of the Maya lowlands. Obsidian artifacts within levels dating to the first half of the early Middle Formative period (1000-850 B.C.) at Cahal Pech consist exclusively of flakes. Prismatic blades first occur in late Middle Formative (650-450 B.C.) levels, and remain the predominant artifact type throughout the subsequent Late Formative and Classic periods. This Middle Formative transition in obsidian artifacts has been recorded elsewhere in Mesoamerica, but the Cahal Pech data represent the first explicitly documented case of the developmental sequence in the central Maya lowlands.
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