Dear Readers, I drove another piece of Route 66 in 2017, from Santa Fe, New Mexico, to Tulsa, Oklahoma. We will continue our tour of the Mother Road with a short return hike in the amazing Kasha-Katuwe Tent Rocks National Monument. Archaeologists have documented evidence of 4000 years of human habitation in the region. This implies a dependable water supply throughout the year. The Peublo de Cochiti people still inhabit the surrounding area. My trip was in July, the "monsoon" season in New Mexico, and the skies were amazing with towering thunderheads. Also, this time, I used black and white film instead of digital.
The Slot Canyon Trail is an easy way to get the feel of the desert, rock formations, and views. From a parking at about 5,200 ft altitude, you gradually ascend across dusty desert and enter a narrow slot canyon. You wind your way through the narrow canyon with vertical walls, and then ascend to the plateau at about 6,300 ft. The last part is steep but well-marked. The trail ends at an overlook of the Monument’s teepee (or tent) shaped rock formations.
As I wrote before, these teepees remind me of the cones of tuffa in Cappadocia, in central Anatolia (Turkey). Read more about the geology at the New Mexico Bureau of Geology & Mineral Resources.
The bent-over and weathered trees are especially interesting.
Late afternoon, and the lightning crackles in the distance, and the thunders rumbles. The signs warn you about flash floods. But the tourists were still coming in and heading to the slot canyon.
I took these photographs with my Yashica Electro 35CC camera (with 35mm f/1.8 Color-Yashinon lens) using Kodak BW400CN film. I scanned the negatives with a Plustek 7600i scanner. Note, in the 1970s, the word "color" was applied to all sorts of optics to demonstrate that they were so superior, you could use them for color film. Brilliant. Today, the marketers would use the word "digital" instead. Or maybe they would use "nano."
This blog documents what remains when we abandon our buildings, homes, schools, and factories. These decaying structures represent our impact on the world: where we lived, worked, and built. The blog also shows examples of where decay was averted or reversed with hard work and imagination.
Showing posts with label Kasha-Katuwe Tent Rocks National Monument. Show all posts
Showing posts with label Kasha-Katuwe Tent Rocks National Monument. Show all posts
Monday, October 16, 2017
Thursday, May 18, 2017
Travels on the Mother Road, Route 66: Part 10, the Kasha-Katuwe Tent Rocks National Monument
At one time, Route 66 extended between Santa Fe and Albuquerque. As far as I can tell, today there are few 66 remains between the two cities. But my Santa Fe friends told me about a spectacular geological place to visit. A short distance northwest of I-25 (which gobbled up much of Route 66) is the Kasha-Katuwe Tent Rocks National Monument, an terrain of rock pinnacles, cones, and narrow canyons. President Bill Clinton established the Monument in January, 2001. It is operated by the Bureau of Land Management (BLM), and if you have a National Parks pass, you can access the rocks without additional fee. According to Wikipedia, "Kasha-Katuwe means "white cliffs" in the Pueblo language."
This rugged terrain of weathered spires and pinnacles was created by layers of volcanic rock and ash deposited by pyroclastic flow ("a dense, destructive mass of very hot ash, lava fragments, and gases ejected explosively from a volcano and typically flowing downslope at great speed") from an explosion about 6 or 7 million years ago from the Jemez volcanic field. Since then, weathering (chemical or mechanical deterioration of rock material) and erosion (movement of rock material by water, wind, or ice) of these relatively soft layers has created the canyons and tent rocks. The tent rocks are cones of pumice or tuff upon which a cap of harder rock has remained, almost looking like some giant hand must have balanced it on the cone below.
There are a number of hiking trails. They are not too rugged: you can do them with running shoes. But better not use flip-flops, as some tourists demonstrate (hint: there are rattlesnakes). Wear a wide-brimmed hat and take water. The Slot Canyon trail makes for a nice 3 or 4 hour outing.
The only other place I know of with similar cones and spires of volcanic tuff and ash is in Cappadocia, in central Anatolia, Turkey. The Goreme area of Cappadocia was settled by early Christians, who carved homes, churches, and entire towns into the soft rock. First visit Kasha-Katuwe, then go to Cappadocia (but I will admit, I did it in the opposite order). Both are astonishing scenic and cultural wonders.
This rugged terrain of weathered spires and pinnacles was created by layers of volcanic rock and ash deposited by pyroclastic flow ("a dense, destructive mass of very hot ash, lava fragments, and gases ejected explosively from a volcano and typically flowing downslope at great speed") from an explosion about 6 or 7 million years ago from the Jemez volcanic field. Since then, weathering (chemical or mechanical deterioration of rock material) and erosion (movement of rock material by water, wind, or ice) of these relatively soft layers has created the canyons and tent rocks. The tent rocks are cones of pumice or tuff upon which a cap of harder rock has remained, almost looking like some giant hand must have balanced it on the cone below.
The pines cling to the rocks with roots reaching down into cracks to find water. |
Yes, the Slot Canyon trail goes through this slot. |
Uchisar, Cappadocia, Turkey (Rolleiflex 3.5E film photograph) |
Dear Readers, this is the last of my 2016 Route 66 posts. Thank you for riding along.
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