Locust

Watershed Hydrology

The Locust Watershed, located in Western Montana, covers an area of approximately 221 square miles. The watershed is characterized by mountainous terrain and is fed by snowpack and precipitation. The watershed contains several small streams that feed into the Clark Fork River. The snowpack in the watershed is an important source of water for the area, with peak snowpack typically occurring in April. There are several small reservoirs in the watershed that help regulate water flow. The climate in the area is characterized by cold winters and warm summers. Recent trends have shown a decrease in snowpack levels, which can have significant impacts on the availability of water for the region. Additionally, the watershed has experienced an increase in wildfires, which can have negative impacts on water quality and quantity.


Surface Flows

Locust Watershed

Snowpack Depths

Locust Watershed

Dams & Reservoirs

Locust Watershed

Groundwater Levels

Locust Watershed

Locust Rivers

Rivers of the Watershed