Bradley River is located on the Kenai Peninsula and flows northwest from Bradley Lake for 7 miles (11 km) to Kachemak Bay, about 25 miles (40 km) northeast of Homer, Alaska. The river is possibly named after John A. Bradley, a local prospector, and the name was first published by the U.S. Geological Survey in 1951.
The Bradley Lake hydroelectric project consists of a concrete-faced, rock-filled dam 125 feet (38 m) high, several diversion structures, and a power tunnel 3.5 miles (5.6 km) long, with a diameter of 11 feet (3.4 m), which transports water from the dam to the powerhouse near the Martin River at the head of Kachemak Bay. The power generation potential of Bradley Lake was first studied by the U.S. Army Corps of Engineers in 1955. The Alaska Power Authority assumed responsibility for the project in 1982 and it was completed in 1991. It now provides relatively inexpensive power to Kachemak Bay communities.
The Nuka Glacier is on Bradley Pass, which is the watershed divide between the Nuka River that flows into Kenai Fjords National Park, and the Bradley River that flows into Kachemak Bay. Prior to 1991, most of Nuka Glacier outflow went into the Nuka River during low-flow periods, but during high discharges, most of the water went into the Bradley River. In order to maximize the flow going into Bradley River, a dike 5 feet (1.5 m) high was built at Bradley Pass to divert the river into Bradley Lake. In 2020, a diversion project of Battle Creek was completed that increased the hydropower output by about 10 percent. The retreat of the Dixon Glacier has created a meltwater stream that could be diverted into the Bradley Lake reservoir and potentially increase the hydropower output by about 50 percent. Read more here and here. Explore more of Bradley River here: