Kasha-Katuwe Tent Rocks National Monument
The geology of the Tent Rocks is owed to volcanic activity that occurred here millions of years ago.
Nature's work is quite visible at the Kasha-Katuwe Tent Rocks National Monument, situated 40 miles southwest of Santa Fe, New Mexico. Formations here were millions of years in the making and were created by volcanic eruptions. There is a hiking trail perched 5,570 feet to 6,760 feet above sea level on the Pajarito Plateau that provides opportunities for sight-seeing and geological observation.