Chevelon Canyon

Watershed Hydrology

The Chevelon Canyon Watershed is located in northern Arizona and covers an area of approximately 456 square miles. The headwaters of the watershed are located at an elevation of over 8,000 feet, and the main stem of the Chevelon Creek flows for approximately 40 miles before joining the Little Colorado River. The hydrology of the watershed is largely influenced by snowpack accumulation during the winter months, which feeds into the surface water during the spring and summer. Reservoirs within the watershed hold water for irrigation and municipal use. Interesting climatic facts include the fact that the watershed experiences a monsoon season in the summer months, which can lead to flash flooding in the area. In recent years, the watershed has experienced periods of drought, which has impacted both the snowpack and surface water availability. Overall, the Chevelon Canyon Watershed is an important resource for the region, providing valuable water resources for communities and agricultural activities.


Surface Flows

Chevelon Canyon Watershed

Snowpack Depths

Chevelon Canyon Watershed

Dams & Reservoirs

Chevelon Canyon Watershed

Groundwater Levels

Chevelon Canyon Watershed

Chevelon Canyon Rivers

Rivers of the Watershed