While we were staying in Santa Fe New Mexico, our gracious host took us out hiking to an amazing place called Kasha-Katuwe Tent Rocks National Monument.
Extracts from official website: “…The cone-shaped tent rock formations are the products of volcanic eruptions that occurred 6 to 7 million years ago and left pumice, ash and tuff deposits over 1,000 feet thick. Tremendous explosions from the Jemez volcanic field spewed pyroclasts (rock fragments), while searing hot gases blasted down slopes in an incandescent avalanche called a “pyroclastic flow.” …
Precariously perched on many of the tapering hoodoos are boulder caps that protect the softer pumice and tuff below. Some tents have lost their hard, resistant caprocks and are disintegrating. While fairly uniform in shape, the tent rock formations vary in height from a few feet to 90 feet…
…The complex landscape and spectacular geologic scenery of the national monument has been a focal point for visitors for centuries. Before nearby Cochiti Reservoir was built, surveys recorded numerous archaeological sites reflecting human occupations spanning 4,000 years. During the 14th and 15th centuries, several large ancestral pueblos were established and their descendants, the Pueblo de Cochiti, still inhabit the surrounding area. Kasha-Katuwe means “white cliffs” in the traditional Keresan language of the Pueblo….
…A portion of the five-mile access road to the national monument crosses Pueblo de Cochiti tribal land. Along with the pueblo, neighbors in the vicinity include the Santo Domingo Indians, the Jemez Indians, private landowners, the Santa Fe National Forest and State of New Mexico. Please respect these landowners and their property.”
The rock formations are indeed stunning! Keep scrolling down for photos!
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