Camas

Watershed Hydrology

The Camas Watershed, located in central Idaho, covers an area of approximately 1,360 square miles. It is characterized by a mountainous terrain that is heavily forested, with elevations ranging from 1,500 to 10,000 feet. The watershed is fed by a combination of snowmelt and precipitation, with the snowpack contributing significantly to its hydrology. In particular, the watershed is known for its deep snowpack, which can accumulate up to 10 feet in some areas. Surface water in the watershed is mainly composed of streams and rivers, which provide critical habitat for fish and other aquatic species. There are also several reservoirs located within the watershed, including the Camas Reservoir and the Magic Reservoir. The climate in the Camas Watershed is characterized by cold winters and mild summers, with average temperatures ranging from 20°F in January to 75°F in July. In recent years, the region has experienced increasing temperatures and decreasing snowpack, which has raised concerns about the future of the watershed's hydrology and water availability.


Surface Flows

Camas Watershed

Snowpack Depths

Camas Watershed

Dams & Reservoirs

Camas Watershed

Groundwater Levels

Camas Watershed

Camas Rivers

Rivers of the Watershed