Search results for Lava Heron

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Giant Plumose Anemones cover underwater reef, Browning Pass, northern Vancouver Island, Canada
Giant Plumose Anemones cover underwater reef, Browning Pass, northern Vancouver Island, Canada.
Location: British Columbia, Canada
Image ID: 35824  
Giant Plumose Anemones cover underwater reef, Browning Pass, northern Vancouver Island, Canada, Metridium farcimen
Giant Plumose Anemones cover underwater reef, Browning Pass, northern Vancouver Island, Canada.
Species: Giant plumose anemone, Metridium farcimen
Location: British Columbia, Canada
Image ID: 34428  
Giant Plumose Anemones cover underwater reef, Browning Pass, northern Vancouver Island, Canada, Metridium farcimen
Giant Plumose Anemones cover underwater reef, Browning Pass, northern Vancouver Island, Canada.
Species: Giant plumose anemone, Metridium farcimen
Location: British Columbia, Canada
Image ID: 34433  
Giant Plumose Anemones cover underwater reef, Browning Pass, northern Vancouver Island, Canada, Metridium farcimen
Giant Plumose Anemones cover underwater reef, Browning Pass, northern Vancouver Island, Canada.
Species: Giant plumose anemone, Metridium farcimen
Location: British Columbia, Canada
Image ID: 34442  
Giant Plumose Anemones cover underwater reef, Browning Pass, northern Vancouver Island, Canada, Metridium farcimen
Giant Plumose Anemones cover underwater reef, Browning Pass, northern Vancouver Island, Canada.
Species: Giant plumose anemone, Metridium farcimen
Location: British Columbia, Canada
Image ID: 34443  
Giant Plumose Anemones cover underwater reef, Browning Pass, northern Vancouver Island, Canada, Metridium farcimen
Giant Plumose Anemones cover underwater reef, Browning Pass, northern Vancouver Island, Canada.
Species: Giant plumose anemone, Metridium farcimen
Location: British Columbia, Canada
Image ID: 34446  
Giant Plumose Anemones cover underwater reef, Browning Pass, northern Vancouver Island, Canada, Metridium farcimen
Giant Plumose Anemones cover underwater reef, Browning Pass, northern Vancouver Island, Canada.
Species: Giant plumose anemone, Metridium farcimen
Location: British Columbia, Canada
Image ID: 34447  
Red Irish Lord fin detail, Browning Pass, British Columbia, Hemilepidotus hemilepidotus
Red Irish Lord fin detail, Browning Pass, British Columbia.
Species: Red irish lord, Hemilepidotus hemilepidotus
Location: British Columbia, Canada
Image ID: 35445  
Red Irish Lord eye detail, Browning Pass, British Columbia, Hemilepidotus hemilepidotus
Red Irish Lord eye detail, Browning Pass, British Columbia.
Species: Red irish lord, Hemilepidotus hemilepidotus
Location: British Columbia, Canada
Image ID: 35448  
Balaklava Island and Browning Pass, location of the best cold water diving in the world, aerial photo
Balaklava Island and Browning Pass, location of the best cold water diving in the world, aerial photo.
Location: British Columbia, Canada
Image ID: 34485  
Panorama dimensions: 4570 x 12090
Hurst Island, Balaklava Island (left) and Gods Pocket Provincial Park, aerial photo, Vancouver Island, British Columbia, Canada
Hurst Island, Balaklava Island (left) and Gods Pocket Provincial Park, aerial photo.
Location: Gods Pocket Provincial Park, Vancouver Island, British Columbia, Canada
Image ID: 34488  
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  
Volcanic debris, small lava rocks scattered about the Eureka Valley, Death Valley National Park, California
Volcanic debris, small lava rocks scattered about the Eureka Valley.
Location: Eureka Valley, Death Valley National Park, California
Image ID: 25340  
Balaklava Island and Hurst Island, aerial view, Canada
Balaklava Island and Hurst Island, aerial view, Canada.
Location: British Columbia, Canada
Image ID: 35540  
Great Blue Heron Perched in Tree, Ardea herodias, Bolsa Chica State Ecological Reserve, Huntington Beach, California
Great Blue Heron Perched in Tree.
Species: Great Blue Heron, Ardea herodias
Location: Bolsa Chica State Ecological Reserve, Huntington Beach, California
Image ID: 40030  
Great Blue Heron Perched in Tree, Ardea herodias, Bolsa Chica State Ecological Reserve, Huntington Beach, California
Great Blue Heron Perched in Tree.
Species: Great Blue Heron, Ardea herodias
Location: Bolsa Chica State Ecological Reserve, Huntington Beach, California
Image ID: 40031  
Paulet Island, near the Antarctic Peninsula, is a cinder cone flanks by lava flows on which thousands of Adelie Penguins nest
Paulet Island, near the Antarctic Peninsula, is a cinder cone flanks by lava flows on which thousands of Adelie Penguins nest.
Location: Paulet Island, Antarctic Peninsula, Antarctica
Image ID: 26358  
Paulet Island, near the Antarctic Peninsula, is a cinder cone flanks by lava flows on which thousands of Adelie Penguins nest
Paulet Island, near the Antarctic Peninsula, is a cinder cone flanks by lava flows on which thousands of Adelie Penguins nest.
Location: Paulet Island, Antarctic Peninsula, Antarctica
Image ID: 26359  
Great blue heron in flight, Ardea herodias, Batiquitos Lagoon, Carlsbad, California
Great blue heron in flight.
Species: Great blue heron, Ardea herodias
Location: Batiquitos Lagoon, Carlsbad, California
Image ID: 18723  
Paulet Island, near the Antarctic Peninsula, is a cinder cone flanks by lava flows on which thousands of Adelie Penguins nest
Paulet Island, near the Antarctic Peninsula, is a cinder cone flanks by lava flows on which thousands of Adelie Penguins nest.
Location: Paulet Island, Antarctic Peninsula, Antarctica
Image ID: 24824  
Paulet Island, near the Antarctic Peninsula, is a cinder cone flanks by lava flows on which thousands of Adelie Penguins nest
Paulet Island, near the Antarctic Peninsula, is a cinder cone flanks by lava flows on which thousands of Adelie Penguins nest.
Location: Paulet Island, Antarctic Peninsula, Antarctica
Image ID: 26361  
Lava formations, Guadalupe Island, Mexico, Guadalupe Island (Isla Guadalupe)
Lava formations, Guadalupe Island, Mexico.
Location: Guadalupe Island (Isla Guadalupe), Baja California, Mexico
Image ID: 36139  
Paulet Island, near the Antarctic Peninsula, is a cinder cone flanks by lava flows on which thousands of Adelie Penguins nest
Paulet Island, near the Antarctic Peninsula, is a cinder cone flanks by lava flows on which thousands of Adelie Penguins nest.
Location: Paulet Island, Antarctic Peninsula, Antarctica
Image ID: 24891  
Marine iguana, underwater, forages for green algae that grows on the lava reef, Amblyrhynchus cristatus, Bartolome Island
Marine iguana, underwater, forages for green algae that grows on the lava reef.
Species: Marine iguana, Amblyrhynchus cristatus
Location: Bartolome Island, Galapagos Islands, Ecuador
Image ID: 16228  
Encrusting sponges cover the lava reef, Cousins
Encrusting sponges cover the lava reef.
Location: Cousins, Galapagos Islands, Ecuador
Image ID: 16456  
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