A total of 17 samples were collected for OSL dating from a Swift Creek archaeological site, known as Harrison Ring, which lies on the Tyndall Air force peninsula in northwest Florida. High-resolution vertical sampling conducted at 10 cm intervals from the surface was performed in order to determine the timing of occupation at the site, and to look for patterns in radiation dosimetry and post-depositional disturbance that can compromise OSL results. We find OSL ages determined using both 0.5 mm aliquots and single grains at the archaeological levels (approximately 1751 ± 339 years ago) to be consistent with the timing of early Swift Creek cultures on the Florida Gulf Coast. The ages we report are both consistent with radiocarbon dates taken at Harrison Ring, and those taken at other Swift Creek sites on the Gulf Coast. In general, we find OSL equivalent doses that show high overdispersion and skewness that we attribute to beta-microdosimetry and possible bioturbation in the profiles. We also present results from a test with a novel dosimetric technique employing Al2O3:C chips. By using Al2O3:C dosimeters, we find that large variability in beta dose rates exist in the sedimentary profile at Harrison Ring. By testing a combination of dosimetric techniques in a site with a well-constrained age, we find that the best agreement with independent age control exists when calculating ages using a beta dose rate from NAA/DNC and gamma dose rate from Al2O3:C dosimetry. / Thesis / Master of Science (MSc)