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| Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes. Salt Photo. Image ID: 25242 Location: Badwater, Death Valley National Park, California, USA | Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes. Salt Picture. Image ID: 27631 Location: Badwater, Death Valley National Park, California, USA | Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes. Stock Photography of Salt. Image ID: 25254 Location: Badwater, Death Valley National Park, California, USA |
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| A river of salt flows across Death Valley, toward the lowest point in the United States at Badwater. Photograph of Salt. Image ID: 25260 Location: Badwater, Death Valley National Park, California, USA | Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes. Salt Photos. Image ID: 25262 Location: Badwater, Death Valley National Park, California, USA | Salt Creek surf, pretty big day, winter, morning. Salt Image. Image ID: 14851 Session: Salt Creek, Laguna Niguel, California, December 22, 2005 Location: Salt Creek, Laguna Niguel, California, USA |
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| Salt Creek surf, pretty big day, winter, morning. Professional stock photos of Salt. Image ID: 14852 Session: Salt Creek, Laguna Niguel, California, December 22, 2005 Location: Salt Creek, Laguna Niguel, California, USA | Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes. Pictures of Salt. Image ID: 25259 Location: Badwater, Death Valley National Park, California, USA | 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. Salt Photo. Image ID: 23266 Location: Devils Postpile National Monument, California, USA |
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| Panorama of the Minarets at sunrise, near Mammoth Mountain. The Minarets are a series of seventeen jagged peaks in the Ritter Range, west of Mammoth Mountain in the Ansel Adams Wilderness. These basalt peaks were carved by glaciers on both sides of the range. The highest of the Minarets stands 12,281 feet above sea level. Salt Picture. Image ID: 19126 Location: Mammoth Lakes, California, USA Pano dimensions: 3249 x 29914 | ||
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| 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. Stock Photography of Salt. Image ID: 23267 Location: Devils Postpile National Monument, California, USA | 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. Photograph of Salt. Image ID: 23285 Location: Devils Postpile National Monument, California, USA | 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. Salt Photos. Image ID: 23281 Location: Devils Postpile National Monument, California, USA |
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| 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. Salt Image. Image ID: 23282 Location: Devils Postpile National Monument, California, USA | 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. Professional stock photos of Salt. Image ID: 23283 Location: Devils Postpile National Monument, California, USA | 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. Pictures of Salt. Image ID: 23284 Location: Devils Postpile National Monument, California, USA |
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| 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. Salt Photo. Image ID: 23286 Location: Devils Postpile National Monument, California, USA | 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. Salt Picture. Image ID: 23287 Location: Devils Postpile National Monument, California, USA | Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes. Stock Photography of Salt. Image ID: 25293 Location: Badwater, Death Valley National Park, California, USA |
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| Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes. Photograph of Salt. Image ID: 25294 Location: Badwater, Death Valley National Park, California, USA | A river of salt flows across Death Valley, toward the lowest point in the United States at Badwater. Salt Photos. Image ID: 25300 Location: Badwater, Death Valley National Park, California, USA | Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes. Salt Image. Image ID: 25303 Location: Badwater, Death Valley National Park, California, USA |
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| Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes. Professional stock photos of Salt. Image ID: 25304 Location: Badwater, Death Valley National Park, California, USA | Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes. Pictures of Salt. Image ID: 25305 Location: Badwater, Death Valley National Park, California, USA | Burrowing owl (Western North American race hypugaea). This 10-inch-tall burrowing owl is standing besides its burrow. These burrows are usually created by squirrels, prairie dogs, or other rodents and even turtles, and only rarely dug by the owl itself. Salt Photo. Image ID: 22477 Species: Burrowing owl, Athene cunicularia, Athene cunicularia hypugaea Location: Salton Sea, Imperial County, California, USA |
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| Sunrise lights Telescope Peak as it rises over the salt flats of Badwater, Death Valley. At 11,049 feet, Telescope Peak is the highest peak in the Panamint Range as well as the highest point in Death Valley National Park. At 282 feet below sea level, Badwater is the lowest point in North America. Salt Picture. Image ID: 20549 Location: Badwater, Death Valley National Park, California, USA | 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. Stock Photography of Salt. Image ID: 15582 Location: Devils Golf Course, Death Valley National Park, California, USA | Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes. Photograph of Salt. Image ID: 27635 Location: Badwater, Death Valley National Park, California, USA |
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| Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes. Salt Photos. Image ID: 27632 Location: Badwater, Death Valley National Park, California, USA | Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes. Salt Image. Image ID: 27633 Location: Badwater, Death Valley National Park, California, USA | |
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