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The Navajo Sandstone is a geological formation in the Glen Canyon Group that is spread across the U.S ... and other inherent rock properties of the sandstone, varying ...
Thin ridges created by the erosion of differentially cemented, large-scale eolian cross bedding within Navajo sandstone. The Wave is a sandstone rock formation located in Arizona, US, near its northern border with Utah. The formation is situated on the slopes of the Coyote Buttes in the Paria Canyon-Vermilion Cliffs Wilderness of the Colorado ...
The Navajo Sandstone has body fossils of the theropod Segisaurus and an Ammosaurus-like prosauropod, and tracks. [5] The following summarizes vertebrate fossils and tracks reported in the Glen Canyon Group: Navajo Sandstone: Body fossils Tritylodontidae indet. [26] Protosuchidae indet. [26] Segisaurus hallii Camp [26] Ammosaurus [26] Trace fossils
View of Monument Valley in Utah, looking south on U.S. Route 163 from 13 miles (21 km) north of the Utah–Arizona state line Mitchell Mesa from the View Hotel.. Monument Valley (Navajo: Tsé Biiʼ Ndzisgaii, pronounced [tsʰépìːʔ ǹtsɪ̀skɑ̀ìː], meaning "valley of the rocks") is a region of the Colorado Plateau characterized by a cluster of sandstone buttes, with the largest reaching ...
Kolob Canyons from the end of Kolob Canyons Road. Stream erosion has incised the Kolob Plateau to form canyons that expose the red-orange colored Navajo Sandstone and other formations. The geology of the Zion and Kolob canyons area includes nine known exposed formations, all visible in Zion National Park in the U.S. state of Utah.
Cross bedded sand dunes accumulated to great thickness, especially in the nearby Zion and Kolob canyons area (see geology of the Zion and Kolob canyons area), forming the buff to pale orange Navajo Sandstone. Navajo outcrops form cliffs, temples, and under certain conditions natural arches (such as Millard Canyon Arch) in the area.
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The Navajo, Wingate, and Kayenta sandstones are distinguished by the cross-bedding of the Kayenta Sandstone across the Colorado Plateau, which tends to be more characteristic of a stream environment than the sand dune deposits that make up the Wingate Sandstone. The Navajo Sandstone began to form in the late Triassic but is mainly a Jurassic ...