Tag Archive for: Navajo Sandstone
Gooseberry Mesa, Washington County, Utah
Photographer: J. Lucy Jordan; © 2016
Sunset on Gooseberry Mesa shines golden light on cliffs of Triassic-age Shinarump Conglomerate and the underlying slope-forming Moenkopi Formation. White cliffs and peaks in the distance are thrones and temples of Zion National Park, formed of Jurassic-age Navajo Sandstone.
Zion National Park, Washington County, Utah
Photographer: Adam McKean; © 2015
Towering 1,488 feet above the canyon floor, Angels Landing is a joint-controlled resistant fin of Jurassic-age Navajo Sandstone, carved out by the incised North Fork Virgin River. A popular, but steep and exposed, hiking trail guides park visitors along the sheer fin to inspiring views of Zion Canyon.
Zion National Park, Washington County, Utah
Photographer: Adam McKean; © 2015
The setting sun illuminates the Jurassic-age Navajo Sandstone cliffs of Cougar Mountain (right) and South Guardian Angel (left) as viewed from Kolob Reservoir Road. Here, the road travels on top of the 220,000- to 310,000-year-old Grapevine Wash lava flow (dark rocks in middle ground).
The mornings are becoming a little crisper, and night comes a little quicker. It won’t belong before we see this scene!
Zion National Park, Kane County, Utah
Photographer: Adam Hiscock; © 2015
Snow highlights cross-bedding on the sides of buttes and mesas along the Clear Creek drainage on the east side of Zion National Park. Cross-beds in the nearly 2,000-foot-thick Jurassic-age Navajo Sandstone formed in ancient sand dunes and reflect changing wind directions as the sand was being deposited.
Zion National Park, Washington County, Utah
Photographer: Tyler Knudsen; © 2014
One of numerous slot canyons carved into Jurassic-age Navajo Sandstone in Zion National Park, Bear Trap Canyon is particularly dark and narrow. With little sunlight penetrating to the canyon floor, snow and ice often linger well into spring.
San Rafael Swell, Emery County, Utah
Photographer: Robert Ressetar; © 2013
Window Blind Peak rises to an elevation of 7,030 feet in the interior of the San Rafael Swell. The resistant Triassic to Jurassic-age Wingate and Navajo Sandstones form, respectively, the massive lower cliffs and the upper pinnacle.
livescience.com
Hikers rambling through Utah’s candy-striped canyons sometimes come across a strange-looking sight. Where the Navajo Sandstone loses its iconic peach, orange and red stripes, hundreds of round, iron-coated stones often litter the ground.