During the height of the last glaciation, the Puget Lowlands were covered by a large lake, Glacial Lake Russell, which catastrophically emptied sometime between 13,000 and 15,000 years ago through the straights of Juan de Fuca. Three icebergs once suspended in Glacial Lake Russell, became stranded in water-logged sediments in North Seattle. These icebergs deformed the landscape, forming three basins of varying depths that became bogs. The creation of these basins in this manner is a relatively rare geological occurrence. A volcanic ash layer was recovered from one of these peat bogs in North Seattle, Washington. The purpose of this research was to determine the age, volcano of origin, and chemical composition of a volcanic ash sample recovered from a peat bog in North Seattle, as a means to gain a better understanding of significant geologic events in this region. Chemical fingerprinting by Ion Chromatography (IC) provided concentrations of specific ions of interest, and carbon dating analysis allowed for the determination of an approximate age for the ash layer. Inductive Coupled Plasma Mass Spectrometry (ICP-MS), was used to determine metal distribution in the ash layer leading us closer to gaining a clearer understanding of when eruptions occurred and when the region was ice free. The ash layer is not present in the upland sediments, and is theorized to have eroded off seasonal snow-pack and settled in the bog. Large, stranded ice takes a few hundred years to melt out, and the mass of the ice can be approximated from the mass of the sediments displaced from the basin. This could help narrow down when exactly Glacial Lake Russell emptied. Understanding the mechanisms of how this rare form of deformation occurred would advance the geological understanding of the Puget Sound Region.