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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. Layers Photo. 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. Layers Picture. 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. Stock Photography of Layers. Image ID: 20607 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. Photograph of Layers. Image ID: 20608 Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA	Navajo sandstone forms the cliffs and walls of Zion National Park. The sandstone reaches a thickness of 2300 feet and consists of ancient cemented desert sand dunes. Horizontal lines, commonly called crossbedding, represent layers of wind-blown sand that built up into sand dunes. These dunes were then buried, and the sand grains glued together by calcite and iron oxide to form sandstone. Layers Photos. Image ID: 12519 Location: Zion National Park, Utah, 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. Layers Image. Image ID: 20609 Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA

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. Professional stock photos of Layers. Image ID: 20700 Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA Pano dimensions: 4661 x 25458

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. Pictures of Layers. 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. Layers Photo. 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. Layers Picture. Image ID: 20623 Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA

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. Stock Photography of Layers. Image ID: 20702 Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA Pano dimensions: 4617 x 17432

Sandstone formations. Layers of sandstone are revealed by erosion in the Wire Pass narrows. Photograph of Layers. 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. Layers Photos. Image ID: 20732 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. Layers Image. 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. Professional stock photos of Layers. 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. Pictures of Layers. Image ID: 20742 Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA	Navajo sandstone forms the cliffs and walls of Zion National Park. The sandstone reaches a thickness of 2300 feet and consists of ancient cemented desert sand dunes. Horizontal lines, commonly called crossbedding, represent layers of wind-blown sand that built up into sand dunes. These dunes were then buried, and the sand grains glued together by calcite and iron oxide to form sandstone. Layers Photo. Image ID: 12514 Location: Zion National Park, Utah, USA

Navajo sandstone forms the cliffs and walls of Zion National Park. The sandstone reaches a thickness of 2300 feet and consists of ancient cemented desert sand dunes. Horizontal lines, commonly called crossbedding, represent layers of wind-blown sand that built up into sand dunes. These dunes were then buried, and the sand grains glued together by calcite and iron oxide to form sandstone. Layers Picture. Image ID: 12515 Location: Zion National Park, Utah, USA	Navajo sandstone forms the cliffs and walls of Zion National Park. The sandstone reaches a thickness of 2300 feet and consists of ancient cemented desert sand dunes. Horizontal lines, commonly called crossbedding, represent layers of wind-blown sand that built up into sand dunes. These dunes were then buried, and the sand grains glued together by calcite and iron oxide to form sandstone. Stock Photography of Layers. Image ID: 12516 Location: Zion National Park, Utah, USA	Navajo sandstone forms the cliffs and walls of Zion National Park. The sandstone reaches a thickness of 2300 feet and consists of ancient cemented desert sand dunes. Horizontal lines, commonly called crossbedding, represent layers of wind-blown sand that built up into sand dunes. These dunes were then buried, and the sand grains glued together by calcite and iron oxide to form sandstone. Photograph of Layers. Image ID: 12517 Location: Zion National Park, Utah, USA

Navajo sandstone forms the cliffs and walls of Zion National Park. The sandstone reaches a thickness of 2300 feet and consists of ancient cemented desert sand dunes. Horizontal lines, commonly called crossbedding, represent layers of wind-blown sand that built up into sand dunes. These dunes were then buried, and the sand grains glued together by calcite and iron oxide to form sandstone. Layers Photos. Image ID: 12518 Location: Zion National Park, Utah, USA	Navajo sandstone forms the cliffs and walls of Zion National Park. The sandstone reaches a thickness of 2300 feet and consists of ancient cemented desert sand dunes. Horizontal lines, commonly called crossbedding, represent layers of wind-blown sand that built up into sand dunes. These dunes were then buried, and the sand grains glued together by calcite and iron oxide to form sandstone. Layers Image. Image ID: 12520 Location: Zion National Park, Utah, USA	Navajo sandstone forms the cliffs and walls of Zion National Park. The sandstone reaches a thickness of 2300 feet and consists of ancient cemented desert sand dunes. Horizontal lines, commonly called crossbedding, represent layers of wind-blown sand that built up into sand dunes. These dunes were then buried, and the sand grains glued together by calcite and iron oxide to form sandstone. Professional stock photos of Layers. Image ID: 12521 Location: Zion National Park, Utah, USA

Navajo sandstone forms the cliffs and walls of Zion National Park. The sandstone reaches a thickness of 2300 feet and consists of ancient cemented desert sand dunes. Horizontal lines, commonly called crossbedding, represent layers of wind-blown sand that built up into sand dunes. These dunes were then buried, and the sand grains glued together by calcite and iron oxide to form sandstone. Pictures of Layers. Image ID: 12522 Location: Zion National Park, Utah, USA	Navajo sandstone forms the cliffs and walls of Zion National Park. The sandstone reaches a thickness of 2300 feet and consists of ancient cemented desert sand dunes. Horizontal lines, commonly called crossbedding, represent layers of wind-blown sand that built up into sand dunes. These dunes were then buried, and the sand grains glued together by calcite and iron oxide to form sandstone. Layers Photo. Image ID: 12523 Location: Zion National Park, Utah, USA	Navajo sandstone forms the cliffs and walls of Zion National Park. The sandstone reaches a thickness of 2300 feet and consists of ancient cemented desert sand dunes. Horizontal lines, commonly called crossbedding, represent layers of wind-blown sand that built up into sand dunes. These dunes were then buried, and the sand grains glued together by calcite and iron oxide to form sandstone. Layers Picture. Image ID: 12524 Location: Zion National Park, Utah, USA

Checkerboard Mesa, a good example of crossbedding (horizontal lines) and vertical cracks caused by thermal expansion/contraction. Navajo sandstone forms the cliffs and walls of Zion National Park. The sandstone reaches a thickness of 2300 feet and consists of ancient cemented desert sand dunes. Horizontal lines, commonly called crossbedding, represent layers of wind-blown sand that built up into sand dunes. These dunes were then buried, and the sand grains glued together by calcite and iron oxide to form sandstone. Stock Photography of Layers. Image ID: 12526 Location: Zion National Park, Utah, USA	Shale is a fine-grained detrital sedimentary rock formed by the compaction of clay, silt, or mud. Shale is formed when mud is pressed into rock over millions of years and often breaks into big flat pieces. Here layers of shale emerge from the sand and cliffs at Gaviota State Beach north of Santa Barbara. Photograph of Layers. Image ID: 14892 Location: Gaviota State Beach, Santa Barbara, California, USA	Shale is a fine-grained detrital sedimentary rock formed by the compaction of clay, silt, or mud. Shale is formed when mud is pressed into rock over millions of years and often breaks into big flat pieces. Here layers of shale emerge from the sand and cliffs at Gaviota State Beach north of Santa Barbara. Layers Photos. Image ID: 14893 Location: Gaviota State Beach, Santa Barbara, California, USA

Shale is a fine-grained detrital sedimentary rock formed by the compaction of clay, silt, or mud. Shale is formed when mud is pressed into rock over millions of years and often breaks into big flat pieces. Here layers of shale emerge from the sand and cliffs at Gaviota State Beach north of Santa Barbara. Layers Image. Image ID: 14894 Location: Gaviota State Beach, Santa Barbara, California, USA