The Escalante Watershed (HUC 14070005) is located in southern Utah and covers an area of approximately 2,360 square kilometers. The watershed is characterized by its complex and rugged topography, which includes steep canyons and high plateaus. The region experiences a semi-arid climate with hot summers and cold winters. The watershed is fed by snowpack, which accumulates in the winter months and melts in the spring, providing surface water for streams and rivers. The region is also home to several reservoirs, which are used for irrigation and drinking water. Interesting climatic facts include the region's susceptibility to flash floods, which occur during intense rainfall events, as well as the impact of climate change on snowpack accumulation and water availability. In recent years, the region has experienced decreased snowpack and earlier snowmelt, leading to concerns about water availability for agriculture and human consumption. Overall, the Escalante Watershed is a critical resource for the region, and efforts to protect and manage its water resources are crucial for future sustainability.