Abstract
Previous studies of obsidian sources in the western Great Basin have identified a similar pattern of use through time, though varying somewhat in scope, methodology, and conclusions. A distributional or "non-site" archaeological survey strategy was adopted to investigate the Mt. Hicks obsidian source. Spatial associations of artifacts were recorded and samples collected for analysis. In addition to techno-morphological assessment, select obsidian artifacts were subjected to obsidian hydration analysis. Results of these analyses indicate that the Mt. Hicks production curve broadly resembles that of other western Great Basin obsidian sources, but when examined in detail all differ from one another in significant ways. Results also suggest that some explanations presented to explain the shape of production curves seem inadequate, and that general trends in flaked stone use through time meet theoretical expectations.