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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 Add To Light Table 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 Add To Light Table 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 Add To Light Table
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.
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.
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.
Image ID: 14894  
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 Add To Light Table 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 Add To Light Table 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 Add To Light Table
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.
Image ID: 14895  
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.
Image ID: 14896  
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.
Image ID: 14897  
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 Add To Light Table 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 Add To Light Table 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, Death Valley National Park, California Add To Light Table
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.
Image ID: 14898  
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.
Image ID: 14899  
Location: Gaviota State Beach, Santa Barbara, California, 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: 15586  
Location: Zabriskie Point, Death Valley National Park, California, USA
 
Zabriskie Point, sunrise.  Curiously banded area of sedimentary rock lies in the foreground with the Panamint Mountains visible in the distance, Death Valley National Park, California Add To Light Table 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, Death Valley National Park, California Add To Light Table 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, Death Valley National Park, California Add To Light Table
Zabriskie Point, sunrise. Curiously banded area of sedimentary rock lies in the foreground with the Panamint Mountains visible in the distance.
Image ID: 15601  
Location: Zabriskie Point, Death Valley National Park, California, 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: 15602  
Location: Zabriskie Point, Death Valley National Park, California, 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: 15618  
Location: Zabriskie Point, Death Valley National Park, California, 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, Death Valley National Park, California Add To Light Table 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 Add To Light Table 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 Add To Light Table
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: 15619  
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: 20615  
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: 20616  
Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA
 
Brain rocks, curious sandstone formations in the North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona Add To Light Table 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 Add To Light Table 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 Add To Light Table
Brain rocks, curious sandstone formations in the North Coyote Buttes.
Image ID: 20617  
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: 20618  
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: 20619  
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 Add To Light Table 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 Add To Light Table 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 Add To Light Table
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: 20620  
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: 20621  
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: 20622  
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, Paria Canyon-Vermilion Cliffs Wilderness Add To Light Table 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 Add To Light Table 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 Add To Light Table
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: 20624  
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: 20625  
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: 20626  
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, North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona Add To Light Table 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 Add To Light Table 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 Add To Light Table
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: 20627  
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: 20628  
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: 20629  
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 Add To Light Table 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 Add To Light Table 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 Add To Light Table
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: 20630  
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: 20631  
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: 20632  
Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA
 


Natural History Photography Blog posts (5) related to Sedimentary



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Natural History Photography Blog posts (5) related to Sedimentary
Photo of the Second Wave
Photo of Diagenetic Coloration in Sandstone, North Coyote Buttes
Photo of Badwater, Death Valley National Park
Photo of Zabriskie Point, Death Valley National Park
Photo of Badwater, Death Valley National Park

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Updated: December 4, 2021