Search results for Salt Creek

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Kanarra Creek Falls in Kanarra Canyon, Utah, Kanarraville
Kanarra Creek Falls in Kanarra Canyon, Utah.
Location: Kanarra Creek, Kanarraville, Utah
Image ID: 32638  
Kanarra Creek Falls in Kanarra Canyon, Utah, Kanarraville
Kanarra Creek Falls in Kanarra Canyon, Utah.
Location: Kanarra Creek, Kanarraville, Utah
Image ID: 32643  
Kanarra Creek Falls in Kanarra Canyon, Utah, Kanarraville
Kanarra Creek Falls in Kanarra Canyon, Utah.
Location: Kanarra Creek, Kanarraville, Utah
Image ID: 32645  
Fall Colors in Kanarra Creek Canyon, Utah, Kanarraville
Fall Colors in Kanarra Creek Canyon, Utah.
Location: Kanarra Creek, Kanarraville, Utah
Image ID: 32646  
Kanarra Creek Canyon, Utah, Kanarraville
Kanarra Creek Canyon, Utah.
Location: Kanarra Creek, Kanarraville, Utah
Image ID: 32648  
Panorama dimensions: 5304 x 9938
Natural Salt Lake on Isla San Jose, Aerial View, Sea of Cortez
Natural Salt Lake on Isla San Jose, Aerial View, Sea of Cortez.
Location: Isla San Jose, Baja California, Mexico
Image ID: 33621  
Panorama dimensions: 3966 x 10878
Salt Lake on Isla Espiritu Santo, Baja California, aerial view
Salt Lake on Isla Espiritu Santo, Baja California, aerial view.
Location: Isla Espiritu Santo, Baja California, Mexico
Image ID: 33821  
Panorama dimensions: 4761 x 17704
Fletcher Peak (11407') at sunset, viewed from Vogelsang High Sierra Camp in Yosemite's high country, Yosemite National Park, California
Fletcher Peak (11407') at sunset, viewed from Vogelsang High Sierra Camp in Yosemite's high country.
Location: Yosemite National Park, California
Image ID: 23203  
Vogelsang Peak (11516') at sunset, reflected in a small creek near Vogelsang High Sierra Camp in Yosemite's high country, Yosemite National Park, California
Vogelsang Peak (11516') at sunset, reflected in a small creek near Vogelsang High Sierra Camp in Yosemite's high country.
Location: Yosemite National Park, California
Image ID: 23220  
Vogelsang Peak (11516') in Yosemite's High Sierra, reflected in small creek, morning, summer, Yosemite National Park, California
Vogelsang Peak (11516') in Yosemite's High Sierra, reflected in small creek, morning, summer.
Location: Yosemite National Park, California
Image ID: 23229  
Rafferty Creek along the John Muir Trail, on approach to Vogelsang High Sierra Camp in Yosemite's high country, Yosemite National Park, California
Rafferty Creek along the John Muir Trail, on approach to Vogelsang High Sierra Camp in Yosemite's high country.
Location: Yosemite National Park, California
Image ID: 23242  
Rafferty Creek, flows under blue skies, on approach to Vogelsang High Sierra Camp. Vogelsang Peak is seen in the distance, Yosemite National Park, California
Rafferty Creek, flows under blue skies, on approach to Vogelsang High Sierra Camp. Vogelsang Peak is seen in the distance.
Location: Yosemite National Park, California
Image ID: 23247  
Vogelsang Peak (11516') at sunset, reflected in a small creek near Vogelsang High Sierra Camp in Yosemite's high country, Yosemite National Park, California
Vogelsang Peak (11516') at sunset, reflected in a small creek near Vogelsang High Sierra Camp in Yosemite's high country.
Location: Yosemite National Park, California
Image ID: 23251  
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  
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes, Death Valley National Park, California
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes.
Location: Badwater, Death Valley National Park, California
Image ID: 25293  
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes, Death Valley National Park, California
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes.
Location: Badwater, Death Valley National Park, California
Image ID: 25294  
A river of salt flows across Death Valley, toward the lowest point in the United States at Badwater, Death Valley National Park, California
A river of salt flows across Death Valley, toward the lowest point in the United States at Badwater.
Location: Badwater, Death Valley National Park, California
Image ID: 25300  
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes, Death Valley National Park, California
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes.
Location: Badwater, Death Valley National Park, California
Image ID: 25303  
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes, Death Valley National Park, California
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes.
Location: Badwater, Death Valley National Park, California
Image ID: 25304  
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes, Death Valley National Park, California
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes.
Location: Badwater, Death Valley National Park, California
Image ID: 25305  
Small waterfalls and autumn trees, along the left fork in North Creek Canyon, with maple and cottonwood trees turning fall colors, Zion National Park, Utah
Small waterfalls and autumn trees, along the left fork in North Creek Canyon, with maple and cottonwood trees turning fall colors.
Location: Zion National Park, Utah
Image ID: 26133  
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, Athene cunicularia, Athene cunicularia hypugaea, Salton Sea, Imperial County, California
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.
Species: Burrowing owl, Athene cunicularia, Athene cunicularia hypugaea
Location: Salton Sea, Imperial County, California
Image ID: 22477  
Aspen trees, fall colors, reflected in the still waters of North Lake, Populus tremuloides, Bishop Creek Canyon Sierra Nevada Mountains
Aspen trees, fall colors, reflected in the still waters of North Lake.
Species: Aspen, Populus tremuloides
Location: Bishop Creek Canyon Sierra Nevada Mountains, California
Image ID: 26063  
Sage brush and aspen trees, autumn, in the shade of Bishop Creek Canyon in the Sierra Nevada, Populus tremuloides, Bishop Creek Canyon Sierra Nevada Mountains
Sage brush and aspen trees, autumn, in the shade of Bishop Creek Canyon in the Sierra Nevada.
Species: Aspen, Populus tremuloides
Location: Bishop Creek Canyon Sierra Nevada Mountains, California
Image ID: 26060  
Sierra Nevada mountains and aspen trees, fall colors reflected in the still waters of North Lake, Populus tremuloides, Bishop Creek Canyon Sierra Nevada Mountains
Sierra Nevada mountains and aspen trees, fall colors reflected in the still waters of North Lake.
Species: Aspen, Populus tremuloides
Location: Bishop Creek Canyon Sierra Nevada Mountains, California
Image ID: 26061  
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