In north-central New Mexico, between Albuquerque and Santa Fe, lies the unique geological area known as Kasha-Katuwe Tent Rocks. Kasha-Katuwe or "white cliffs" in Keresan, the traditional language for the Pueblo de Cochiti, is an area that features large, tent-shaped rocks that hug the steep cliffs of Peralta Canyon. These rocks were created by the powerful forces of vulcanism and erosion, which have built up and then torn down this landscape.During the last million years, a tremendous volcanic explosion northwest of Kasha-Katuwe Tent Rocks spewed rock and ash for hundreds of square miles, leaving volcanic debris up to 400 feet thick. Over time, water cut into these deposits, creating canyons, arroyos and other area features. The cone-shaped rock formations are wind- and water-eroded pumice and tuff deposits. Their hard, erosion-resistant caprocks protect the softer tents below. While uniform in shape, the tent rock formations vary in height from a few feet to 90 feet.
Map + Directions
Kasha-Katuwe Tent Rocks is located 40 miles southwest of Santa Fe and 50 miles north of Albuquerque, New Mexico, with the most direct access from Interstate 25. Take the Cochiti Reservoir exit from I-25 to NM Route 22 and follow the signs to Cochiti Pueblo. Turn right at the pueblo water tower (painted like a drum) onto Tribal Route 92 (connects to Forest Service Road 266). Travel 5 miles on a dirt road to the Tent Rocks parking area, which is marked with a sign. This is the only parking area for Kasha-Katuwe Tent Rocks.