Little

Watershed Hydrology

The Little Watershed (HUC 08040304) covers an area of approximately 654 square kilometers and is located in central Colorado. The watershed is predominantly mountainous, and its hydrology is significantly influenced by the Rocky Mountains. The region experiences a unique climate characterized by cold, snowy winters and warm, dry summers. The watershed's snowpack is typically deep and persistent, which can lead to significant spring runoff and flooding. Surface water in the Little Watershed is primarily sourced from snowmelt and precipitation. The primary reservoir in the watershed is Dillon Reservoir, which is used for municipal and irrigation purposes. Interesting climatic facts include the area's susceptibility to drought and the increasing frequency of extreme weather events, such as heavy rainfall and severe wildfires. Overall, the Little Watershed is an important natural resource for the region and is closely monitored by local water authorities to ensure sustainable water management practices.


Surface Flows

Little Watershed

Snowpack Depths

Little Watershed

Dams & Reservoirs

Little Watershed

Groundwater Levels

Little Watershed

Little Rivers

Rivers of the Watershed