Search results for Devil Postpile

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Sapphire devil (blue damselfish), female/juvenile coloration, Chrysiptera cyanea
Sapphire devil (blue damselfish), female/juvenile coloration.
Species: Sapphire devil, Chrysiptera cyanea
Image ID: 11834  
Pine Tree Arch on the Devil's Garden Trail in Arches National Park
Pine Tree Arch on the Devil's Garden Trail in Arches National Park.
Location: Pine Tree Arch, Arches National Park, Utah
Image ID: 18186  
Galapagos sea lion, Devils Crown, Zalophus californianus wollebacki, Zalophus californianus wollebaeki, Floreana Island
Galapagos sea lion, Devils Crown.
Species: Galapagos sea lion, Zalophus californianus wollebacki, Zalophus californianus wollebaeki
Location: Floreana Island, Galapagos Islands, Ecuador
Image ID: 01707  
Adelie penguin colony, panoramic photograph, Pygoscelis adeliae, Devil Island
Adelie penguin colony, panoramic photograph.
Species: Adelie penguin, Pygoscelis adeliae
Location: Devil Island, Antarctic Peninsula, Antarctica
Image ID: 26313  
Panorama dimensions: 3564 x 28099
Devil's Postpile, a spectacular example of columnar basalt. Once molten and under great pressure underground, the lava that makes up Devil's Postpile cooled evenly and slowly, contracting and fracturing into polygonal-sided columns. The age of the formation is estimated between 100 and 700 thousand years old. Sometime after the basalt columns formed, a glacier passed over the formation, cutting and polishing the tops of the columns. The columns have from three to seven sides, varying because of differences in how quickly portions of the lava cooled, Devils Postpile National Monument, California
Devil's Postpile, a spectacular example of columnar basalt. Once molten and under great pressure underground, the lava that makes up Devil's Postpile cooled evenly and slowly, contracting and fracturing into polygonal-sided columns. The age of the formation is estimated between 100 and 700 thousand years old. Sometime after the basalt columns formed, a glacier passed over the formation, cutting and polishing the tops of the columns. The columns have from three to seven sides, varying because of differences in how quickly portions of the lava cooled.
Location: Devils Postpile National Monument, California
Image ID: 23266  
Devil's Postpile, a spectacular example of columnar basalt. Once molten and under great pressure underground, the lava that makes up Devil's Postpile cooled evenly and slowly, contracting and fracturing into polygonal-sided columns. The age of the formation is estimated between 100 and 700 thousand years old. Sometime after the basalt columns formed, a glacier passed over the formation, cutting and polishing the tops of the columns. The columns have from three to seven sides, varying because of differences in how quickly portions of the lava cooled, Devils Postpile National Monument, California
Devil's Postpile, a spectacular example of columnar basalt. Once molten and under great pressure underground, the lava that makes up Devil's Postpile cooled evenly and slowly, contracting and fracturing into polygonal-sided columns. The age of the formation is estimated between 100 and 700 thousand years old. Sometime after the basalt columns formed, a glacier passed over the formation, cutting and polishing the tops of the columns. The columns have from three to seven sides, varying because of differences in how quickly portions of the lava cooled.
Location: Devils Postpile National Monument, California
Image ID: 23267  
Devil's Postpile, a spectacular example of columnar basalt. Once molten and under great pressure underground, the lava that makes up Devil's Postpile cooled evenly and slowly, contracting and fracturing into polygonal-sided columns. The age of the formation is estimated between 100 and 700 thousand years old. Sometime after the basalt columns formed, a glacier passed over the formation, cutting and polishing the tops of the columns. The columns have from three to seven sides, varying because of differences in how quickly portions of the lava cooled, Devils Postpile National Monument, California
Devil's Postpile, a spectacular example of columnar basalt. Once molten and under great pressure underground, the lava that makes up Devil's Postpile cooled evenly and slowly, contracting and fracturing into polygonal-sided columns. The age of the formation is estimated between 100 and 700 thousand years old. Sometime after the basalt columns formed, a glacier passed over the formation, cutting and polishing the tops of the columns. The columns have from three to seven sides, varying because of differences in how quickly portions of the lava cooled.
Location: Devils Postpile National Monument, California
Image ID: 23285  
Devil's Postpile, a spectacular example of columnar basalt. Once molten and under great pressure underground, the lava that makes up Devil's Postpile cooled evenly and slowly, contracting and fracturing into polygonal-sided columns. The age of the formation is estimated between 100 and 700 thousand years old. Sometime after the basalt columns formed, a glacier passed over the formation, cutting and polishing the tops of the columns. The columns have from three to seven sides, varying because of differences in how quickly portions of the lava cooled, Devils Postpile National Monument, California
Devil's Postpile, a spectacular example of columnar basalt. Once molten and under great pressure underground, the lava that makes up Devil's Postpile cooled evenly and slowly, contracting and fracturing into polygonal-sided columns. The age of the formation is estimated between 100 and 700 thousand years old. Sometime after the basalt columns formed, a glacier passed over the formation, cutting and polishing the tops of the columns. The columns have from three to seven sides, varying because of differences in how quickly portions of the lava cooled.
Location: Devils Postpile National Monument, California
Image ID: 23281  
Devil's Postpile, a spectacular example of columnar basalt. Once molten and under great pressure underground, the lava that makes up Devil's Postpile cooled evenly and slowly, contracting and fracturing into polygonal-sided columns. The age of the formation is estimated between 100 and 700 thousand years old. Sometime after the basalt columns formed, a glacier passed over the formation, cutting and polishing the tops of the columns. The columns have from three to seven sides, varying because of differences in how quickly portions of the lava cooled, Devils Postpile National Monument, California
Devil's Postpile, a spectacular example of columnar basalt. Once molten and under great pressure underground, the lava that makes up Devil's Postpile cooled evenly and slowly, contracting and fracturing into polygonal-sided columns. The age of the formation is estimated between 100 and 700 thousand years old. Sometime after the basalt columns formed, a glacier passed over the formation, cutting and polishing the tops of the columns. The columns have from three to seven sides, varying because of differences in how quickly portions of the lava cooled.
Location: Devils Postpile National Monument, California
Image ID: 23282  
Devil's Postpile, a spectacular example of columnar basalt. Once molten and under great pressure underground, the lava that makes up Devil's Postpile cooled evenly and slowly, contracting and fracturing into polygonal-sided columns. The age of the formation is estimated between 100 and 700 thousand years old. Sometime after the basalt columns formed, a glacier passed over the formation, cutting and polishing the tops of the columns. The columns have from three to seven sides, varying because of differences in how quickly portions of the lava cooled, Devils Postpile National Monument, California
Devil's Postpile, a spectacular example of columnar basalt. Once molten and under great pressure underground, the lava that makes up Devil's Postpile cooled evenly and slowly, contracting and fracturing into polygonal-sided columns. The age of the formation is estimated between 100 and 700 thousand years old. Sometime after the basalt columns formed, a glacier passed over the formation, cutting and polishing the tops of the columns. The columns have from three to seven sides, varying because of differences in how quickly portions of the lava cooled.
Location: Devils Postpile National Monument, California
Image ID: 23283  
Devil's Postpile, a spectacular example of columnar basalt. Once molten and under great pressure underground, the lava that makes up Devil's Postpile cooled evenly and slowly, contracting and fracturing into polygonal-sided columns. The age of the formation is estimated between 100 and 700 thousand years old. Sometime after the basalt columns formed, a glacier passed over the formation, cutting and polishing the tops of the columns. The columns have from three to seven sides, varying because of differences in how quickly portions of the lava cooled, Devils Postpile National Monument, California
Devil's Postpile, a spectacular example of columnar basalt. Once molten and under great pressure underground, the lava that makes up Devil's Postpile cooled evenly and slowly, contracting and fracturing into polygonal-sided columns. The age of the formation is estimated between 100 and 700 thousand years old. Sometime after the basalt columns formed, a glacier passed over the formation, cutting and polishing the tops of the columns. The columns have from three to seven sides, varying because of differences in how quickly portions of the lava cooled.
Location: Devils Postpile National Monument, California
Image ID: 23284  
Devil's Postpile, a spectacular example of columnar basalt. Once molten and under great pressure underground, the lava that makes up Devil's Postpile cooled evenly and slowly, contracting and fracturing into polygonal-sided columns. The age of the formation is estimated between 100 and 700 thousand years old. Sometime after the basalt columns formed, a glacier passed over the formation, cutting and polishing the tops of the columns. The columns have from three to seven sides, varying because of differences in how quickly portions of the lava cooled, Devils Postpile National Monument, California
Devil's Postpile, a spectacular example of columnar basalt. Once molten and under great pressure underground, the lava that makes up Devil's Postpile cooled evenly and slowly, contracting and fracturing into polygonal-sided columns. The age of the formation is estimated between 100 and 700 thousand years old. Sometime after the basalt columns formed, a glacier passed over the formation, cutting and polishing the tops of the columns. The columns have from three to seven sides, varying because of differences in how quickly portions of the lava cooled.
Location: Devils Postpile National Monument, California
Image ID: 23286  
Devil's Postpile, a spectacular example of columnar basalt. Once molten and under great pressure underground, the lava that makes up Devil's Postpile cooled evenly and slowly, contracting and fracturing into polygonal-sided columns. The age of the formation is estimated between 100 and 700 thousand years old. Sometime after the basalt columns formed, a glacier passed over the formation, cutting and polishing the tops of the columns. The columns have from three to seven sides, varying because of differences in how quickly portions of the lava cooled, Devils Postpile National Monument, California
Devil's Postpile, a spectacular example of columnar basalt. Once molten and under great pressure underground, the lava that makes up Devil's Postpile cooled evenly and slowly, contracting and fracturing into polygonal-sided columns. The age of the formation is estimated between 100 and 700 thousand years old. Sometime after the basalt columns formed, a glacier passed over the formation, cutting and polishing the tops of the columns. The columns have from three to seven sides, varying because of differences in how quickly portions of the lava cooled.
Location: Devils Postpile National Monument, California
Image ID: 23287  
Adelie penguins at the nest, part of the large nesting colony of penguins that resides along the lower slopes of Devil Island, Pygoscelis adeliae
Adelie penguins at the nest, part of the large nesting colony of penguins that resides along the lower slopes of Devil Island.
Species: Adelie penguin, Pygoscelis adeliae
Location: Devil Island, Antarctic Peninsula, Antarctica
Image ID: 25013  
Adelie penguin, Pygoscelis adeliae, Devil Island
Adelie penguin.
Species: Adelie penguin, Pygoscelis adeliae
Location: Devil Island, Antarctic Peninsula, Antarctica
Image ID: 25044  
Panorama of Devil Island in Antarctica
Panorama of Devil Island in Antarctica.
Location: Devil Island, Antarctic Peninsula, Antarctica
Image ID: 26303  
Panorama dimensions: 3325 x 26885
Adelie penguins, adults and chicks, Pygoscelis adeliae, Devil Island
Adelie penguins, adults and chicks.
Species: Adelie penguin, Pygoscelis adeliae
Location: Devil Island, Antarctic Peninsula, Antarctica
Image ID: 25102  
Photographer making pictures as M/V Polar Star approaches Devil Island
Photographer making pictures as M/V Polar Star approaches Devil Island.
Location: Devil Island, Antarctic Peninsula, Antarctica
Image ID: 26372  
Summit of Devil Island, with Vega Island in the distance
Summit of Devil Island, with Vega Island in the distance.
Location: Devil Island, Antarctic Peninsula, Antarctica
Image ID: 24786  
Crested snow patterns along the slopes of Devil Island
Crested snow patterns along the slopes of Devil Island.
Location: Devil Island, Antarctic Peninsula, Antarctica
Image ID: 24879  
Adelie penguin, adults feeding chicks, part of the large nesting colony of penguins that resides along the lower slopes of Devil Island, Pygoscelis adeliae
Adelie penguin, adults feeding chicks, part of the large nesting colony of penguins that resides along the lower slopes of Devil Island.
Species: Adelie penguin, Pygoscelis adeliae
Location: Devil Island, Antarctic Peninsula, Antarctica
Image ID: 25042  
Devil Island, Antarctica Peninsula
Devil Island, Antarctica Peninsula.
Location: Devil Island, Antarctic Peninsula, Antarctica
Image ID: 26373  
The Giraffe Traps, or what is officially known as Two Running Violet V Forms, was the second piece in the Stuart Collection at University of California San Diego (UCSD). Commissioned in 1983 and produced by Robert Irwin, the odd fence resides in the eucalyptus grove between Mandeville Auditorium and Central Library, University of California, San Diego, La Jolla
The Giraffe Traps, or what is officially known as Two Running Violet V Forms, was the second piece in the Stuart Collection at University of California San Diego (UCSD). Commissioned in 1983 and produced by Robert Irwin, the odd fence resides in the eucalyptus grove between Mandeville Auditorium and Central Library.
Location: University of California, San Diego, La Jolla
Image ID: 12842  
Devils Golf Course, California. Evaporated salt has formed into gnarled, complex crystalline shapes in on the salt pan of Death Valley National Park, one of the largest salt pans in the world. The shapes are constantly evolving as occasional floods submerge the salt concretions before receding and depositing more salt
Devils Golf Course, California. Evaporated salt has formed into gnarled, complex crystalline shapes in on the salt pan of Death Valley National Park, one of the largest salt pans in the world. The shapes are constantly evolving as occasional floods submerge the salt concretions before receding and depositing more salt.
Location: Devils Golf Course, Death Valley National Park, California
Image ID: 15582  
Icebreaker M/V Polar Star near Devil Island, sunrise
Icebreaker M/V Polar Star near Devil Island, sunrise.
Location: Devil Island, Antarctic Peninsula, Antarctica
Image ID: 24819  
Crested snow patterns along the slopes of Devil Island
Crested snow patterns along the slopes of Devil Island.
Location: Devil Island, Antarctic Peninsula, Antarctica
Image ID: 24787  
Summit of Devil Island with portions of the Erebus and Terror Gulf region of the Weddell Sea in the background
Summit of Devil Island with portions of the Erebus and Terror Gulf region of the Weddell Sea in the background.
Location: Devil Island, Antarctic Peninsula, Antarctica
Image ID: 24816  
Enjoying a sunny warm day on the summit of Devil Island, with the cliffs of Vega Island in the distance
Enjoying a sunny warm day on the summit of Devil Island, with the cliffs of Vega Island in the distance.
Location: Devil Island, Antarctic Peninsula, Antarctica
Image ID: 24817  
Crested snow patterns along the slopes of Devil Island
Crested snow patterns along the slopes of Devil Island.
Location: Devil Island, Antarctic Peninsula, Antarctica
Image ID: 24818  
Adelie penguins at the nest, part of the large nesting colony of penguins that resides along the lower slopes of Devil Island, Pygoscelis adeliae
Adelie penguins at the nest, part of the large nesting colony of penguins that resides along the lower slopes of Devil Island.
Species: Adelie penguin, Pygoscelis adeliae
Location: Devil Island, Antarctic Peninsula, Antarctica
Image ID: 25043  
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