The Escalante Desert Watershed (HUC 16030006) covers an area of 3,703 square miles in south-central Utah. The hydrology of the area is dominated by the Escalante River, which flows through a wide, steep-walled canyon and is fed by several tributaries. The watershed is characterized by a high-elevation mountain range, which contributes to a significant snowpack in the winter months. The snowmelt is the primary source of surface water for the region, and is critical for agricultural and domestic use. There are several reservoirs in the watershed that store water for irrigation and municipal purposes. The area is known for its extreme climate, with hot summers and cold winters, and is prone to drought conditions. In recent years, there has been a downward trend in snowpack and precipitation, which has led to concerns about water availability in the future.