A trace fossil exposure located at Dougherty Gap, Walker County, Georgia, provides an excellent opportunity to evaluate existing physical information, and compare a uniformitarian interpretation and a young-earth Flood interpretation for that site. This examination reveals that a turbidity current depositional environment better explains the stratigraphic record found at this site than does the proposed uniformitarian prograding delta model. Additionally, a turbidity current depositional environment fits within both the expected depositional environment and the timeframes of the young-earth Flood model.