Stevens Arch

Stevens Arch is a large sandstone formation that towers above the Escalante River and Stevens Canyon. It formed from the Navajo Sandstone layer and shows the power of water erosion working across millions of years.

The arch took millions of years to form through erosion of Navajo Sandstone layers, creating one of the largest natural spans in the country. Its development relied on the constant flow of water through the canyons, steadily shaping the rock.

The arch stands in a landscape used for centuries by Navajo and other tribes who hunted and traveled through these canyons. The area holds traces of this long presence in artifacts and camp sites that visitors may notice while exploring.

The hike to reach this arch is demanding and requires endurance, taking you through steep terrain and across river crossings. Start early in the day since the route needs daylight hours, and bring sturdy footwear plus plenty of water.

This arch ranks among the longest natural spans in America, which often surprises visitors when they see its massive size in person. Its location where Stevens Canyon and Coyote Gulch meet creates an extra dramatic setting with multiple waterways.