Lower Bear-Malad

Watershed Hydrology

The Lower Bear Malad Watershed (HUC 16010204) is located in southeastern Idaho and covers an area of approximately 2,500 square miles. The watershed is characterized by a semi-arid climate with hot summers and cold winters. Snowpack is an important component of the hydrology of the watershed, providing a significant amount of the surface water and contributing to the recharge of groundwater. Surface water in the watershed is primarily provided by the Bear River and its tributaries, including the Malad River. The Bear River is also used for irrigation and is regulated by a number of reservoirs, including the Bear Lake Reservoir and the Oneida Narrows Reservoir. Interesting climatic facts and trends in the watershed include a decline in snowpack and an increase in temperatures, which may lead to water scarcity issues in the future. Additionally, the area experiences frequent droughts, which exacerbate water supply issues.


Surface Flows

Lower Bear-Malad Watershed

Snowpack Depths

Lower Bear-Malad Watershed

Dams & Reservoirs

Lower Bear-Malad Watershed

Groundwater Levels

Lower Bear-Malad Watershed

Lower Bear-Malad Rivers

Rivers of the Watershed