Kasha-Katuwe Tent Rocks National Monument

Kasha-Katuwe Tent Rocks National Monument is located in north-central New Mexico, near the Pueblo of Cochiti. This area is famous for its remarkable geological formations, particularly the conical rock structures that give the monument its name and are formed from volcanic eruptions that occurred over six million years ago. The landscape here is mesmerizing, characterized by layers of volcanic rock and ash that have been sculpted into tent-shaped rock formations known as 'hoodoos.' These formations create a striking setting, inviting visitors to explore its rugged beauty. The monument also supports a range of ecological communities, including piñon-juniper and mixed conifer woodlands that offer habitat to a variety of wildlife. Kasha-Katuwe Tent Rocks National Monument is rich in cultural history, deeply tied to the nearby Cochiti Pueblo. Outdoor activities are abundant, with scenic hikes that meander through narrow canyons and ascend ridges, providing panoramic views of the surrounding landscape. The distinct geological and cultural significance, paired with the area's natural beauty, attracts thousands of visitors who come to experience its unique environment and recreational opportunities.