Eagle Lake was once part of a large lake on the
Modoc Plateau millions of years ago. The modern lake is long by wide and is highly alkaline (pH 8-9). The lake consists of three basins, two of them averaging deep, the third averaging and reaching a depth of nearly . The tributaries of Eagle Lake (beginning in the lake's north end and going clockwise) are Cleghorn Creek, Papoose Creek, Merrill Creek, and
Pine Creek. Pine Creek is the main tributary of Eagle Lake and is long. Now an intermittent stream; only the upper of Pine Creek has perennial flow. In 1923 the Leon Bly Tunnel was constructed to export lake water to the Honey Lake Valley via Willow Creek, a tributary of the
Susan River. The long tunnel was cut through old lava flows but falling lake levels rendered it useless and a landslide partially blocked the tunnel entrance. However, a 1990 study found that lake water still flows through the tunnel although tunnel fish are from the Willow Creek assemblage. Image:Eagle Lake Shoreline 1.jpg|The lake just before dusk. Image:Eagle Lake Shoreline 2.jpg|The lake in the afternoon. ==See also==