Capote Springs, Texas: Where Warm Waters Feed the Tallest Waterfall in the State

Capote Springs lies in a remote section of western Presidio County, about eleven miles northeast of the small border community of Candelaria. The springs are situated in rugged desert country within the Sierra Vieja Mountains, a range known for its dramatic cliffs and volcanic formations. The landscape around the springs is defined by rocky outcroppings, sparse vegetation, and wide, open skies that highlight the region’s striking natural beauty. The isolation of Capote Springs has helped preserve its quiet, untouched atmosphere, making it one of the most secluded natural features in Texas.

The Springs and Waterfall

The springs at Capote are a group of natural warm-water sources that feed Capote Creek. This creek flows over a steep rhyolite cliff to form Capote Falls, which stands at approximately 175 feet and is recognized as the tallest waterfall in Texas. The cliff face is part of the Sierra Vieja volcanic formation, composed primarily of rhyolite and tuff from ancient volcanic activity. The combination of the desert terrain, volcanic rock, and flowing water creates an unexpected oasis amid the arid surroundings.

Temperature and Flow

Capote Springs maintains a steady temperature of about 99 degrees Fahrenheit throughout the year. The warmth comes from geothermal activity beneath the surface, giving the water a pleasant and stable temperature even in cooler months. Historical measurements recorded a steady flow of roughly two gallons per second, showing that the springs produce a consistent water supply despite the dry conditions of the Chihuahuan Desert region.

Access and Conservation

Although the area is well known among geologists and nature enthusiasts, Capote Springs and Capote Falls are located on private property. Access is limited and requires landowner permission, which has helped preserve the site’s pristine condition. The surrounding environment supports a range of desert flora and fauna, and the springs themselves play an important role as a rare water source for local wildlife. The remoteness and restricted access have made the springs a largely undisturbed natural landmark.

Geological and Natural Significance

Capote Springs and Capote Falls highlight the geological diversity of far West Texas. The rhyolite cliffs of the Sierra Vieja are remnants of volcanic activity dating back millions of years, and the presence of thermal springs indicates continued geothermal movement beneath the surface. This combination of features makes Capote Springs both a geological and ecological point of interest, offering insight into the processes that shaped the Trans-Pecos region.