Coyote Spring
Coyote Spring in Beaver County emerges at 68°F near Milford at 5,020 feet elevation, delivering relatively fresh water with only 558 mg/L TDS and balanced mineral chemistry.
Located in the high desert landscape of southwestern Utah's Escalante Desert, the spring sits in terrain characterized by sagebrush flats, scattered juniper, and distant mountain ranges. The Mineral Mountains rise to the east while the San Francisco Mountains define the western horizon. This semi-arid setting receives only 9.5 inches of annual precipitation with 29.2 inches of snow, creating sparse vegetation adapted to moisture stress. The spring requires a 517-meter walk from the nearest road access through open desert terrain.
The moderately warm temperature and remote location make this spring primarily of interest for hydrogeological study rather than recreation. Water quality is relatively good but flow and accessibility should be verified before visiting. The high desert setting requires appropriate preparation for temperature extremes and limited shade. No nearby campgrounds are listed. Spring and fall offer the most moderate temperatures in this exposed desert environment.
The Coyote Spring name reflects common wildlife nomenclature in Utah's desert regions, where coyotes remain abundant. Historical documentation for this specific spring is sparse, though the Milford area saw mining and ranching activity from the late 1800s onward. Whether the spring served as a water source for early travelers or ranchers is not clearly documented in available records.
The water at Coyote Spring is slightly alkaline (pH 7.5) with 558 mg/L total dissolved solids. It is notably rich in chloride (natural antiseptic with skin health benefits).
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Coyote Spring is road-accessible, so you can bring more gear.
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