Search results for Bachelor And Three Graces

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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, 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  
North Lake lit by alpenglow before sunrise, a three frame panorama, with groves of yellow and orange aspen trees on the side of Paiute Peak, Bishop Creek Canyon, Sierra Nevada Mountains
North Lake lit by alpenglow before sunrise, a three frame panorama, with groves of yellow and orange aspen trees on the side of Paiute Peak.
Location: Bishop Creek Canyon, Sierra Nevada Mountains, California
Image ID: 23336  
Panorama dimensions: 2991 x 8972
Stars over the Three Gossips, Arches National Park, Courthouse Towers
Stars over the Three Gossips, Arches National Park.
Location: Courthouse Towers, Arches National Park, Utah
Image ID: 29270  
Yoga Pelican performing Warrior Three Pose Virabhadrasana, Pelecanus occidentalis, Pelecanus occidentalis californicus, La Jolla, California
Yoga Pelican performing Warrior Three Pose Virabhadrasana.
Species: Brown Pelican, Pelecanus occidentalis, Pelecanus occidentalis californicus
Location: La Jolla, California
Image ID: 37634  
Yoga Pelican performing Warrior Three Pose Virabhadrasana, Pelecanus occidentalis, Pelecanus occidentalis californicus, La Jolla, California
Yoga Pelican performing Warrior Three Pose Virabhadrasana.
Species: Brown Pelican, Pelecanus occidentalis, Pelecanus occidentalis californicus
Location: La Jolla, California
Image ID: 37690  
Three brown pelicans gossiping, meeting on cliffs over the sea to discuss the days fishing news, La Jolla, California
Three brown pelicans gossiping, meeting on cliffs over the sea to discuss the days fishing news.
Location: La Jolla, California
Image ID: 38697  
Three California sea lions bodysurf together, suspended in the face of a big wave, Boomer Beach, La Jolla
Three California sea lions bodysurf together, suspended in the face of a big wave, Boomer Beach, La Jolla.
Location: La Jolla, California
Image ID: 39015  
Three bald eagles stand together on wooden perch, Haliaeetus leucocephalus, Haliaeetus leucocephalus washingtoniensis, Kachemak Bay, Homer, Alaska
Three bald eagles stand together on wooden perch.
Species: Bald eagle, Haliaeetus leucocephalus, Haliaeetus leucocephalus washingtoniensis
Location: Kachemak Bay, Homer, Alaska
Image ID: 22671  
Immature bald eagle (center) raises wings and vocalizes as another eagle (left) lands on a wooden perch. Three bald eagles on a perch. Immature plumage coloration. Note immature coloration showing white speckling on feathers, Haliaeetus leucocephalus, Haliaeetus leucocephalus washingtoniensis, Kachemak Bay, Homer, Alaska
Immature bald eagle (center) raises wings and vocalizes as another eagle (left) lands on a wooden perch. Three bald eagles on a perch. Immature plumage coloration. Note immature coloration showing white speckling on feathers.
Species: Bald eagle, Haliaeetus leucocephalus, Haliaeetus leucocephalus washingtoniensis
Location: Kachemak Bay, Homer, Alaska
Image ID: 22702  
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  
Three Brothers, Yosemite Valley, Yosemite National Park, California
Three Brothers, Yosemite Valley.
Location: Yosemite National Park, California
Image ID: 07040  
Pacific Harbor Seal Pup in La Jolla About Three Weeks Old, hauled out on a white sand beach along the coast of San Diego. This young seal will be weaned off its mothers milk and care when it is about four to six weeks old, and before that time it must learn how to forage for food on its own, a very difficult time for a young seal, Phoca vitulina richardsi
Pacific Harbor Seal Pup in La Jolla About Three Weeks Old, hauled out on a white sand beach along the coast of San Diego. This young seal will be weaned off its mothers milk and care when it is about four to six weeks old, and before that time it must learn how to forage for food on its own, a very difficult time for a young seal.
Species: Pacific harbor seal, Phoca vitulina richardsi
Location: La Jolla, California
Image ID: 39128  
Pacific Harbor Seal Pup in La Jolla About Three Weeks Old, hauled out on a white sand beach along the coast of San Diego. This young seal will be weaned off its mothers milk and care when it is about four to six weeks old, and before that time it must learn how to forage for food on its own, a very difficult time for a young seal, Phoca vitulina richardsi
Pacific Harbor Seal Pup in La Jolla About Three Weeks Old, hauled out on a white sand beach along the coast of San Diego. This young seal will be weaned off its mothers milk and care when it is about four to six weeks old, and before that time it must learn how to forage for food on its own, a very difficult time for a young seal.
Species: Pacific harbor seal, Phoca vitulina richardsi
Location: La Jolla, California
Image ID: 39131  
Piedras Blancas lighthouse. Completed in 1875, the 115-foot-tall Piedras Blancas lighthouse is one of the few tall-style lighthouses on the West Coast of the United States. Piedras Blancas, named for a group of three white rocks just offshore, is north of San Simeon, California very close to Hearst Castle
Piedras Blancas lighthouse. Completed in 1875, the 115-foot-tall Piedras Blancas lighthouse is one of the few tall-style lighthouses on the West Coast of the United States. Piedras Blancas, named for a group of three white rocks just offshore, is north of San Simeon, California very close to Hearst Castle.
Location: Piedras Blancas, San Simeon, California
Image ID: 20348  
Large group of bachelor adult male California sea lions, underwater view, at Isla Las Animas near La Paz, Sea of Cortez, Baja California, Zalophus californianus
Large group of bachelor adult male California sea lions, underwater view, at Isla Las Animas near La Paz, Sea of Cortez, Baja California.
Species: California sea lion, Zalophus californianus
Location: Sea of Cortez, Baja California, Mexico
Image ID: 27463  
Light patterns on a Florida manatees wide tail, Trichechus manatus, Three Sisters Springs, Crystal River
Light patterns on a Florida manatees wide tail.
Species: West indian manatee, Trichechus manatus
Location: Three Sisters Springs, Crystal River, Florida
Image ID: 36322  
Florida Manatees at Three Sisters Springs, Crystal River, Florida, Trichechus manatus
Florida Manatees at Three Sisters Springs, Crystal River, Florida.
Species: West indian manatee, Trichechus manatus
Location: Three Sisters Springs, Crystal River, Florida
Image ID: 36324  
A Florida manatee surfaces to breathe, at Three Sisters Springs, Crystal River, Florida, Trichechus manatus
A Florida manatee surfaces to breathe, at Three Sisters Springs, Crystal River, Florida.
Species: West indian manatee, Trichechus manatus
Location: Three Sisters Springs, Crystal River, Florida
Image ID: 36331  
A Florida manatee surfaces to breathe, at Three Sisters Springs, Crystal River, Florida, Trichechus manatus
A Florida manatee surfaces to breathe, at Three Sisters Springs, Crystal River, Florida.
Species: West indian manatee, Trichechus manatus
Location: Three Sisters Springs, Crystal River, Florida
Image ID: 36333  
A Florida manatee surfaces to breathe, at Three Sisters Springs, Crystal River, Florida, Trichechus manatus
A Florida manatee surfaces to breathe, at Three Sisters Springs, Crystal River, Florida.
Species: West indian manatee, Trichechus manatus
Location: Three Sisters Springs, Crystal River, Florida
Image ID: 36334  
The Morro Bay Power Plant, with its distinctive three stacks, rises above fishing boats in Morro Bay harbor. Morro Bay
The Morro Bay Power Plant, with its distinctive three stacks, rises above fishing boats in Morro Bay harbor. Morro Bay.
Location: Morro Bay, California
Image ID: 14900  
Florida Manatee at Three Sisters Springs, Crystal River, Florida, Trichechus manatus
Florida Manatee at Three Sisters Springs, Crystal River, Florida.
Species: West indian manatee, Trichechus manatus
Location: Three Sisters Springs, Crystal River, Florida
Image ID: 36323  
Florida Manatee at Three Sisters Springs, Crystal River, Florida, Trichechus manatus
Florida Manatee at Three Sisters Springs, Crystal River, Florida.
Species: West indian manatee, Trichechus manatus
Location: Three Sisters Springs, Crystal River, Florida
Image ID: 36325  
A Florida manatee surfaces to breathe, at Three Sisters Springs, Crystal River, Florida, Trichechus manatus
A Florida manatee surfaces to breathe, at Three Sisters Springs, Crystal River, Florida.
Species: West indian manatee, Trichechus manatus
Location: Three Sisters Springs, Crystal River, Florida
Image ID: 36326  
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