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The Wave, an area of fantastic eroded sandstone featuring beautiful swirls, wild colors, countless striations, and bizarre shapes set amidst the dramatic surrounding North Coyote Buttes of Arizona and Utah. The sandstone formations of the North Coyote Buttes, including the Wave, date from the Jurassic period. Managed by the Bureau of Land Management, the Wave is located in the Paria Canyon-Vermilion Cliffs Wilderness and is accessible on foot by permit only.
Image ID: 20605
Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA | The Second Wave at sunset. The Second Wave, a curiously-shaped sandstone swirl, takes on rich warm tones and dramatic shadowed textures at sunset. Set in the North Coyote Buttes of Arizona and Utah, the Second Wave is characterized by striations revealing layers of sedimentary deposits, a visible historical record depicting eons of submarine geology.
Image ID: 20606
Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA | The Wave, an area of fantastic eroded sandstone featuring beautiful swirls, wild colors, countless striations, and bizarre shapes set amidst the dramatic surrounding North Coyote Buttes of Arizona and Utah. The sandstone formations of the North Coyote Buttes, including the Wave, date from the Jurassic period. Managed by the Bureau of Land Management, the Wave is located in the Paria Canyon-Vermilion Cliffs Wilderness and is accessible on foot by permit only.
Image ID: 20607
Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA |
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The Wave, an area of fantastic eroded sandstone featuring beautiful swirls, wild colors, countless striations, and bizarre shapes set amidst the dramatic surrounding North Coyote Buttes of Arizona and Utah. The sandstone formations of the North Coyote Buttes, including the Wave, date from the Jurassic period. Managed by the Bureau of Land Management, the Wave is located in the Paria Canyon-Vermilion Cliffs Wilderness and is accessible on foot by permit only.
Image ID: 20608
Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA | Zabriskie Point, sunrise. Manly Beacon rises in the center of an eroded, curiously banded area of sedimentary rock, with the Panamint Mountains visible in the distance.
Image ID: 15585
Location: Zabriskie Point, Death Valley National Park, California, USA | The Wave, an area of fantastic eroded sandstone featuring beautiful swirls, wild colors, countless striations, and bizarre shapes set amidst the dramatic surrounding North Coyote Buttes of Arizona and Utah. The sandstone formations of the North Coyote Buttes, including the Wave, date from the Jurassic period. Managed by the Bureau of Land Management, the Wave is located in the Paria Canyon-Vermilion Cliffs Wilderness and is accessible on foot by permit only.
Image ID: 20609
Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA |
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Panorama of the Wave. The Wave is a sweeping, dramatic display of eroded sandstone, forged by eons of water and wind erosion, laying bare striations formed from compacted sand dunes over millenia. This panoramic picture is formed from thirteen individual photographs.
Image ID: 20700
Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA
Pano dimensions: 4661 x 25458 |
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Panorama of the Wave. The Wave is a sweeping, dramatic display of eroded sandstone, forged by eons of water and wind erosion, laying bare striations formed from compacted sand dunes over millenia. This panoramic picture is formed from thirteen individual photographs.
Image ID: 20702
Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA
Pano dimensions: 4617 x 17432 |
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Hiker in Buckskin Gulch. A hiker considers the towering walls and narrow passageway of Buckskin Gulch, a dramatic slot canyon forged by centuries of erosion through sandstone. Buckskin Gulch is the worlds longest accessible slot canyon, running from the Paria River toward the Colorado River. Flash flooding is a serious danger in the narrows where there is no escape.
Image ID: 20716
Location: Buckskin Gulch, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA | Brain rocks. Sandstone is curiously eroded through the forces water and wind acting over eons. Cracks and joints arise when water freezes and expands repeatedly, braking apart the soft sandstone.
Image ID: 20747
Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA | Zabriskie Point, sunrise. Manly Beacon rises in the center of an eroded, curiously banded area of sedimentary rock, with the Panamint Mountains visible in the distance.
Image ID: 15575
Location: Zabriskie Point, Death Valley National Park, California, USA |
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Buckskin Gulch hiker. A hiker moves through the deep narrow passages of Buckskin Gulch, a slot canyon cut deep into sandstone by years of river-induced erosion. In some places the Buckskin Gulch narrows are only about 15 feet wide but several hundred feet high, blocking sunlight. Flash floods are dangerous as there is no escape once into the Buckskin Gulch slot canyons. This is a panorama made of sixteen individual photos.
Image ID: 20699
Location: Buckskin Gulch, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA
Pano dimensions: 4771 x 15311 |
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Geometric joints and cracks form in eroding sandstone.
Image ID: 20610
Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA | Brain rocks, curious sandstone formations in the North Coyote Buttes.
Image ID: 20611
Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA | Striations in sandstone tell of eons of sedimentary deposits, a visible geologic record of the time when this region was under the sea.
Image ID: 20612
Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA |
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The Second Wave at sunset. The Second Wave, a curiously-shaped sandstone swirl, takes on rich warm tones and dramatic shadowed textures at sunset. Set in the North Coyote Buttes of Arizona and Utah, the Second Wave is characterized by striations revealing layers of sedimentary deposits, a visible historical record depicting eons of submarine geology.
Image ID: 20613
Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA | The Wave, an area of fantastic eroded sandstone featuring beautiful swirls, wild colors, countless striations, and bizarre shapes set amidst the dramatic surrounding North Coyote Buttes of Arizona and Utah. The sandstone formations of the North Coyote Buttes, including the Wave, date from the Jurassic period. Managed by the Bureau of Land Management, the Wave is located in the Paria Canyon-Vermilion Cliffs Wilderness and is accessible on foot by permit only.
Image ID: 20614
Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA | The Wave, an area of fantastic eroded sandstone featuring beautiful swirls, wild colors, countless striations, and bizarre shapes set amidst the dramatic surrounding North Coyote Buttes of Arizona and Utah. The sandstone formations of the North Coyote Buttes, including the Wave, date from the Jurassic period. Managed by the Bureau of Land Management, the Wave is located in the Paria Canyon-Vermilion Cliffs Wilderness and is accessible on foot by permit only.
Image ID: 20623
Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA |
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Wire Pass narrows opens into the Buckskin Gulch. These narrow slot canyons are formed by water erosion which cuts slots deep into the surrounding sandstone plateau. This is a panorama created from ten individual photographs.
Image ID: 20705
Location: Wire Pass, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA
Pano dimensions: 4366 x 16390 |
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Hiker in Buckskin Gulch. A hiker considers the towering walls and narrow passageway of Buckskin Gulch, a dramatic slot canyon forged by centuries of erosion through sandstone. Buckskin Gulch is the worlds longest accessible slot canyon, running from the Paria River toward the Colorado River. Flash flooding is a serious danger in the narrows where there is no escape.
Image ID: 20710
Location: Buckskin Gulch, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA | A hiker walking through the Wire Pass narrows. This exceedingly narrow slot canyon, in some places only two feet wide, is formed by water erosion which cuts slots deep into the surrounding sandstone plateau.
Image ID: 20715
Location: Wire Pass, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA | Suspended log in Buckskin Gulch. A hiker considers a heavy log stuck between the narrow walls of Buckskin Gulch, placed there by a flash flood some time in the past. Buckskin Gulch is the world's longest accessible slot canyon, forged by centuries of erosion through sandstone. Flash flooding is a serious danger in the narrows where there is no escape.
Image ID: 20717
Location: Buckskin Gulch, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA |
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The Wire Pass narrows. This exceedingly narrow slot canyon, in some places only two feet wide, is formed by water erosion which cuts slots deep into the surrounding sandstone plateau.
Image ID: 20720
Location: Wire Pass, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA | Sandstone formations. Layers of sandstone are revealed by erosion in the Wire Pass narrows.
Image ID: 20731
Location: Wire Pass, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA | The Wave. The main corridor of the Wave, a famous and curiously shaped sandstone bowl.
Image ID: 20732
Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA |
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Sandstone striations. Prehistoric sand dunes, compressed into sandstone, are now revealed in sandstone layers subject to the carving erosive forces of wind and water.
Image ID: 20733
Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA | Sandstone striations. Prehistoric sand dunes, compressed into sandstone, are now revealed in sandstone layers subject to the carving erosive forces of wind and water.
Image ID: 20735
Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA | Sandstone striations. Prehistoric sand dunes, compressed into sandstone, are now revealed in sandstone layers subject to the carving erosive forces of wind and water.
Image ID: 20742
Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA |
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Sandstone joints. These cracks and joints are formed in the sandstone by water that seeps into spaces and is then frozen at night, expanding and cracking the sandstone into geometric forms.
Image ID: 20748
Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA | Brain rocks. Sandstone is curiously eroded through the forces water and wind acting over eons. Cracks and joints arise when water freezes and expands repeatedly, braking apart the soft sandstone.
Image ID: 20750
Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA |
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