Waterpocket Fold in southern Utah is a 100-mile geologic wrinkle in the earth, renowned for its sculpted canyons, colorful rock layers, and remote desert solitude.
Waterpocket Fold is a monocline, a step-like fold in the earth's crust that formed roughly 65 million years ago as tectonic forces buckled the Colorado Plateau. The result is a nearly continuous ridge of upturned rock layers running from Thousand Lake Mountain south to Lake Powell, forming the backbone of Capitol Reef National Park in Utah.
Visitors can explore the fold through a network of scenic drives, day hikes, and rugged backcountry routes. The Capitol Gorge trail winds through a narrow sandstone canyon past pioneer inscriptions and natural water pockets carved into the rock. The Cathedral Valley loop takes hardy travelers through remote badlands studded with towering monoliths of Entrada sandstone.
The Fremont River cuts directly through the fold, creating a fertile riparian corridor where cottonwoods and willows line the banks. Historic orchards planted by Mormon settlers still produce fruit each summer, and visitors are welcome to pick what is in season.
Few places in the American Southwest offer such a concentrated sense of geologic time and desert quiet. Waterpocket Fold rewards patience and curiosity in equal measure, making it a destination that stays with you long after you leave.
Visit in spring or fall when temperatures are mild and the desert light is especially warm and clear.
Carry more water than you think you need, as reliable water sources in the backcountry are scarce and seasonal.
Explore Strike Valley Overlook for a panoramic view of the full length of the fold stretching into the distance.
Bring a detailed topographic map, as cell service is essentially nonexistent throughout most of Capitol Reef National Park.
Start any canyon hike early in the morning to avoid midday heat and to catch the best angled light on the rock walls.