Located in Franklin, Idaho, the Oxford dam stands as a vital water resource structure with a capacity for storing 315 acre-feet of water. Constructed in 1920, this earth-type dam with stone core rests on rock and soil foundations, spanning 1000 feet in length and reaching a height of 20.7 feet. Serving multiple purposes beyond its primary one, Oxford plays a crucial role in regulating water flow and storage in the region, while also contributing to flood control efforts.

Managed by a private entity, the dam is subject to state regulations, inspections, and enforcement to ensure its integrity and safety. Despite being classified as having a low hazard potential, the condition assessment in 2017 reported Oxford to be in fair condition. The spillway, with a width of 10 feet, is uncontrolled, and the risk assessment for the dam is moderate. With a drainage area of 0.9 square miles and located near Wickiup Creek and Bear Creek, Oxford remains a key component of the local water infrastructure.

As water resource and climate enthusiasts continue to monitor and assess the impact of dams on the environment, Oxford stands out as a significant structure in the region. With its historical significance and ongoing role in water management, the dam serves as a reminder of the delicate balance between harnessing water resources for human needs and safeguarding the environment for future generations. As efforts to mitigate climate change and adapt to its effects intensify, understanding the role of structures like Oxford becomes increasingly crucial in sustainable water resource management.