Search results for Owl

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Purple owls clover, Rancho La Costa, Carlsbad
Purple owls clover, Rancho La Costa, Carlsbad.
Location: Rancho La Costa, Carlsbad, California
Image ID: 39362  
Guineafowl puffer fish, black phase, Isla San Diego, Baja California, Mexico
Guineafowl puffer fish, black phase.
Location: Isla San Diego, Baja California, Mexico
Image ID: 33541  
Guineafowl puffer fish, black phase, Isla San Diego, Baja California, Mexico
Guineafowl puffer fish, black phase.
Location: Isla San Diego, Baja California, Mexico
Image ID: 33542  
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  
Delicate Arch, dusted with snow, at sunset, with the snow-covered La Sal mountains in the distance. Delicate Arch stands 45 feet high, with a span of 33 feet, atop of bowl of slickrock sandstone, Arches National Park, Utah
Delicate Arch, dusted with snow, at sunset, with the snow-covered La Sal mountains in the distance. Delicate Arch stands 45 feet high, with a span of 33 feet, atop of bowl of slickrock sandstone.
Location: Delicate Arch, Arches National Park, Utah
Image ID: 18106  
Lowlying plants grow where a forest fire has cleared the forest floor of debris, allowing seeds of small shrubs and trees to take root. The charred and burnt trees remain behind, some of them still alive in spite of their blackened appearance, Mariposa Grove, Yosemite National Park, California
Lowlying plants grow where a forest fire has cleared the forest floor of debris, allowing seeds of small shrubs and trees to take root. The charred and burnt trees remain behind, some of them still alive in spite of their blackened appearance.
Location: Mariposa Grove, Yosemite National Park, California
Image ID: 23262  
Lowlying plants grow where a forest fire has cleared the forest floor of debris, allowing seeds of small shrubs and trees to take root. The charred and burnt trees remain behind, some of them still alive in spite of their blackened appearance, Mariposa Grove, Yosemite National Park, California
Lowlying plants grow where a forest fire has cleared the forest floor of debris, allowing seeds of small shrubs and trees to take root. The charred and burnt trees remain behind, some of them still alive in spite of their blackened appearance.
Location: Mariposa Grove, Yosemite National Park, California
Image ID: 23277  
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  
The leafy seadragon (Phycodurus eques) is found on the southern and western coasts of Australia. Its extravagent appendages serve only for camoflage, since it has a nearly-invisible dorsal fin that propels it slowly through the water. The leafy sea dragon is the marine emblem of South Australia, Phycodurus eques, Rapid Bay Jetty
The leafy seadragon (Phycodurus eques) is found on the southern and western coasts of Australia. Its extravagent appendages serve only for camoflage, since it has a nearly-invisible dorsal fin that propels it slowly through the water. The leafy sea dragon is the marine emblem of South Australia.
Species: Leafy seadragon, Phycodurus eques
Location: Rapid Bay Jetty, South Australia
Image ID: 39133  
The leafy seadragon (Phycodurus eques) is found on the southern and western coasts of Australia. Its extravagent appendages serve only for camoflage, since it has a nearly-invisible dorsal fin that propels it slowly through the water. The leafy sea dragon is the marine emblem of South Australia, Phycodurus eques, Rapid Bay Jetty
The leafy seadragon (Phycodurus eques) is found on the southern and western coasts of Australia. Its extravagent appendages serve only for camoflage, since it has a nearly-invisible dorsal fin that propels it slowly through the water. The leafy sea dragon is the marine emblem of South Australia.
Species: Leafy seadragon, Phycodurus eques
Location: Rapid Bay Jetty, South Australia
Image ID: 39136  
Fallen coast redwood tree. This tree will slowly decompose, providing a substrate and nutrition for new plants to grow and structure for small animals to use. Nurse log, Sequoia sempervirens, Redwood National Park, California
Fallen coast redwood tree. This tree will slowly decompose, providing a substrate and nutrition for new plants to grow and structure for small animals to use. Nurse log.
Species: California redwood, Coast redwood, Giant redwood, Sequoia sempervirens
Location: Redwood National Park, California
Image ID: 25803  
Fallen coast redwood tree. This tree will slowly decompose, providing a substrate and nutrition for new plants to grow and structure for small animals to use. Nurse log, Sequoia sempervirens, Redwood National Park, California
Fallen coast redwood tree. This tree will slowly decompose, providing a substrate and nutrition for new plants to grow and structure for small animals to use. Nurse log.
Species: California redwood, Coast redwood, Giant redwood, Sequoia sempervirens
Location: Redwood National Park, California
Image ID: 25820  
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: 22478  
Limestone and marble underground formations in Oregon Caves National Monument. Eons of acidified groundwater have slowly etched away at marble, creating the extensive and intricate cave formations in Oregon Caves National Monument
Limestone and marble underground formations in Oregon Caves National Monument. Eons of acidified groundwater have slowly etched away at marble, creating the extensive and intricate cave formations in Oregon Caves National Monument.
Location: Oregon Caves National Monument
Image ID: 25861  
Limestone and marble underground formations in Oregon Caves National Monument. Eons of acidified groundwater have slowly etched away at marble, creating the extensive and intricate cave formations in Oregon Caves National Monument
Limestone and marble underground formations in Oregon Caves National Monument. Eons of acidified groundwater have slowly etched away at marble, creating the extensive and intricate cave formations in Oregon Caves National Monument.
Location: Oregon Caves National Monument
Image ID: 25862  
Limestone and marble underground formations, Miller's Chapel grotto in Oregon Caves National Monument. Eons of acidified groundwater have slowly etched away at marble, creating the extensive and intricate cave formations in Oregon Caves National Monument
Limestone and marble underground formations, Miller's Chapel grotto in Oregon Caves National Monument. Eons of acidified groundwater have slowly etched away at marble, creating the extensive and intricate cave formations in Oregon Caves National Monument.
Location: Oregon Caves National Monument
Image ID: 25863  
Limestone and marble underground formations, Miller's Chapel grotto in Oregon Caves National Monument. Eons of acidified groundwater have slowly etched away at marble, creating the extensive and intricate cave formations in Oregon Caves National Monument
Limestone and marble underground formations, Miller's Chapel grotto in Oregon Caves National Monument. Eons of acidified groundwater have slowly etched away at marble, creating the extensive and intricate cave formations in Oregon Caves National Monument.
Location: Oregon Caves National Monument
Image ID: 25864  
Paradise Lost formation in Oregon Caves National Monument. Eons of acidified groundwater have slowly etched away at marble, creating the extensive and intricate cave formations in Oregon Caves National Monument
Paradise Lost formation in Oregon Caves National Monument. Eons of acidified groundwater have slowly etched away at marble, creating the extensive and intricate cave formations in Oregon Caves National Monument.
Location: Oregon Caves National Monument
Image ID: 25865  
The Wave. The main corridor of the Wave, a famous and curiously shaped sandstone bowl, North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona
The Wave. The main corridor of the Wave, a famous and curiously shaped sandstone bowl.
Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona
Image ID: 20732  
Bombay Beach, lies alongside and below the flood level of the Salton Sea, so that it floods occasionally when the Salton Sea rises. A part of Bombay Beach is composed of derelict old trailer homes, shacks and wharfs, slowly sinking in the mud and salt, Imperial County, California
Bombay Beach, lies alongside and below the flood level of the Salton Sea, so that it floods occasionally when the Salton Sea rises. A part of Bombay Beach is composed of derelict old trailer homes, shacks and wharfs, slowly sinking in the mud and salt.
Location: Salton Sea, Imperial County, California
Image ID: 22487  
Bombay Beach, lies alongside and below the flood level of the Salton Sea, so that it floods occasionally when the Salton Sea rises. A part of Bombay Beach is composed of derelict old trailer homes, shacks and wharfs, slowly sinking in the mud and salt, Imperial County, California
Bombay Beach, lies alongside and below the flood level of the Salton Sea, so that it floods occasionally when the Salton Sea rises. A part of Bombay Beach is composed of derelict old trailer homes, shacks and wharfs, slowly sinking in the mud and salt.
Location: Salton Sea, Imperial County, California
Image ID: 22488  
Bombay Beach, lies alongside and below the flood level of the Salton Sea, so that it floods occasionally when the Salton Sea rises. A part of Bombay Beach is composed of derelict old trailer homes, shacks and wharfs, slowly sinking in the mud and salt, Imperial County, California
Bombay Beach, lies alongside and below the flood level of the Salton Sea, so that it floods occasionally when the Salton Sea rises. A part of Bombay Beach is composed of derelict old trailer homes, shacks and wharfs, slowly sinking in the mud and salt.
Location: Salton Sea, Imperial County, California
Image ID: 22489  
Bombay Beach, lies alongside and below the flood level of the Salton Sea, so that it floods occasionally when the Salton Sea rises. A part of Bombay Beach is composed of derelict old trailer homes, shacks and wharfs, slowly sinking in the mud and salt, Imperial County, California
Bombay Beach, lies alongside and below the flood level of the Salton Sea, so that it floods occasionally when the Salton Sea rises. A part of Bombay Beach is composed of derelict old trailer homes, shacks and wharfs, slowly sinking in the mud and salt.
Location: Salton Sea, Imperial County, California
Image ID: 22490  
Bombay Beach, lies alongside and below the flood level of the Salton Sea, so that it floods occasionally when the Salton Sea rises. A part of Bombay Beach is composed of derelict old trailer homes, shacks and wharfs, slowly sinking in the mud and salt, Imperial County, California
Bombay Beach, lies alongside and below the flood level of the Salton Sea, so that it floods occasionally when the Salton Sea rises. A part of Bombay Beach is composed of derelict old trailer homes, shacks and wharfs, slowly sinking in the mud and salt.
Location: Salton Sea, Imperial County, California
Image ID: 22491  
Bombay Beach, lies alongside and below the flood level of the Salton Sea, so that it floods occasionally when the Salton Sea rises. A part of Bombay Beach is composed of derelict old trailer homes, shacks and wharfs, slowly sinking in the mud and salt, Imperial County, California
Bombay Beach, lies alongside and below the flood level of the Salton Sea, so that it floods occasionally when the Salton Sea rises. A part of Bombay Beach is composed of derelict old trailer homes, shacks and wharfs, slowly sinking in the mud and salt.
Location: Salton Sea, Imperial County, California
Image ID: 22492  
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