Bisti/De-Na-Zin Wilderness, New Mexico
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Bisti Badlands, De-Na-Zin Wilderness, New Mexico
by muha04
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The Bisti Badlands, New Mexico...
These surreal rock formations are some of New Mexico's greatest treasures. The Bisti/De-Na-Zin Wilderness is a 45,000-acre (18,000 ha) wilderness area located in San Juan County in the U.S. state of New Mexico. Sediments that created them were deposited 75 million years ago, as the dinosaurs still roamed the Earth. Then, millions of years of erosion formed these residual formations. Once covered in swamps and deltas of the Western Interior Seaway, the area was filled with sediments and organic materials in prehistoric times. This particular image shows a formation called the "cracked eggs", which are the result of differential erosion between hard and soft sediments.
Credit: John Fowler via Flickr https://buff.ly/3PdivAn
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Rock formations called “hoodoos” fill the Bisti De-Na-Zin Wilderness in northern New Mexico. The desert area is rich with fossils from dinosaurs and animals that lived here in ancient times.
PHOTOGRAPH BY EFRAIN PADRO, ALAMY STOCK
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This particular page has 3 different places being represented. Bisti/ De-na-zin wildlife area, White Sands, and Carlsbad Caverns.
Bisti was a very interesting place, challenged my navigating skills. Saw these really cool wind-weathered vaguely egg shaped stones of mid-thigh height. Some almost looked like stone boats. The rock formation I decided to draw though was a hoodoo that looked really cool.
The tree I drew at white sands was practically the only one I found with any significant height.
Carlsbad was a surprise as far as how much I enjoyed it. I liked being able to go at my own speed through the cave. When I went to Mammoth caves, you always have to have a guide and there’s just so many people along with.
Image ID: Traditional drawings done in pencil and some with watercolor. From the top: a flat hoodoo atop a skinny fin-like formation in a slight v shape (if viewed from above).
a tree with roots exposed and going fun directions, holding it above a pale sand. The canopy shading the viewer. Occasional grasses and bushes surrounding it.
A blue, gray, and black mess that looks vaguely like the entrance outside from inside a cavern.
A yellow and orange mess that looks like the deposits left behind from the dripping and flowing water inside caverns.
A dead cave swallow; it is laying on its side with wings folded, no visible decay.
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The Bisti/De-Na-Zin Wilderness encompasses 41,170 acres of rock formations that would seem more natural on Mars. It is one of several protected badlands in the Four Corners area. Ah-She-Sle-Pah Wilderness is a few miles south. Angel Peak badlands is about 20 miles northeast.
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The geological diversity of the badlands in the Bisti/De-Na-Zin Wilderness is astounding.
New Mexico
By Jason Coward
📆 Mar 30, 2024
📷 1/1000 s at f/14, ISO 640, 400mm
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Bob Miller
Mammatus Monster - Bisti De-Na-Zin, New
Mexico
(single exposure)
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Bisticeratops froeseorum Dalman et al., 2022 (new genus and species)
(Type skull of Bisticeratops froeseorum, from Dalman et al., 2022)
Meaning of name: Bisticeratops = Bisti/De-na-zin Wilderness Area horned face [in Greek]; froeseorum = for Edgar Froese [the late founder of the band Tangerine Dream] and Jerome Froese [former member of Tangerine Dream and founder of the band Loom]
Age: Late Cretaceous (Campanian), about 74 million years ago
Where found: Kirtland Formation, New Mexico, U.S.A.
How much is known: Nearly complete skull of one individual.
Notes: Bisticeratops was a chasmosaurine ceratopsian, making it a fairly close relative of Triceratops. The holotype skull of Bisticeratops was originally considered a specimen of Pentaceratops, another chasmosaurine from the Campanian of New Mexico. However, a new study identifies several distinguishing features that suggest it is a separate species. In addition, Bisticeratops is approximately 2 million years younger than Pentaceratops proper. Along with several other recently named ceratopsians, such as Sierraceratops, Navajoceratops, and Terminocavus, Bisticeratops shows that chasmosaurine diversity was very high in the Campanian of southwestern North America.
The Bisticeratops type specimen is also noteworthy in that it preserves multiple bite marks that were likely made by tyrannosaurids. One of these bite marks shows signs of healing, indicating that this individual had survived at least one attack from a predator.
Reference: Dalman, S.G., S.E. Jasinski, and S.G. Lucas. 2022. A new chasmosaurine ceratopsid from the Upper Cretaceous (Campanian) Farmington Member of the Kirtland Formation, New Mexico. New Mexico Museum of Natural History and Science Bulletin 90: 127–153.
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Bisti/ De-Na-Zin Wilderness, New Mexico, USA
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Bisti/De-Na-Zin Wilderness, New Mexico, US [OC] [4023 x 3018]
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Bisti / De-Na-Zin wilderness area, New Mexico
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