Speleothems are used as paleoclimate indicators because of their lengthy recording of time and general availability throughout the. Because of the direct relationship with precipitation, speleothems of calcium carbonate (CaCO3) composition, show levels of oxygen content in precipitation and, therefore, glaciation of the earth. Bermuda is a "classic" study area for determining global sea-level variation due to glaciations because its carbonate caves and its speleothems are useful for analysis and the stability of the Bermuda reef platform (subsidence rates of 1m/100ka). 206 samples were drilled for 18 O stable isotopes and U series techniques were used to find three dates on four flowstone samples from Bermuda. From the 18 O data, we would like to find dates at both the high and low peaks. This data can be used to further constrain the timing of glacial terminations, specifically Termination II. Future work consists of collecting more dates to test certainty of peak sea-level variation at MIS 9 and then compare to known speleothem records around the world.