The Palouse Falls lies on the Palouse River, about 4 mi (6 km) upstream of the confluence with the Snake River in southeast Washington, United States. The falls are 198 ft (60 m) in height. The falls consists of an upper falls with a drop of ~20 feet (6.1 m) which lies 1,000 feet (305 m) north northwest of the main drop, and a lower falls, with a drop of ~180 feet (55 m). In 1984 the Franklin County Public Utilitity District proposed a 30 m (98 ft) high dam be constructed upstream of the falls, allowing for a significant hydraulic head for hydroelectric power generation. This would have provided over one third of the county's power and would have reduced ratepayer charges substantially. However the majority of the ratepayers declined to approve the investment, preserving this geologically significant feature.