Search results for Exit Glacier

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Half Dome at sunrise, viewed from Glacier Point, Yosemite National Park, California
Half Dome at sunrise, viewed from Glacier Point.
Location: Yosemite National Park, California
Image ID: 27737  
Half Dome and pre-dawn light, sunrise, viewed from Glacier Point, Yosemite National Park, California
Half Dome and pre-dawn light, sunrise, viewed from Glacier Point.
Location: Yosemite National Park, California
Image ID: 27739  
Glacier, Skaftafell / Vatnajokull National Park, Southern Iceland
Glacier, Skaftafell / Vatnajokull National Park, Southern Iceland.
Location: Iceland
Image ID: 35735  
Pacific Harbor Seal Young Young Pup, only days old, exiting the ocean, beside its mother on the beach at the Children's Pool in La Jolla, Phoca vitulina richardsi
Pacific Harbor Seal Young Young Pup, only days old, exiting the ocean, beside its mother on the beach at the Children's Pool in La Jolla.
Species: Pacific harbor seal, Phoca vitulina richardsi
Location: La Jolla, California
Image ID: 39056  
Nameless Lake (10709'), surrounded by glacier-sculpted granite peaks of the Cathedral Range, near Vogelsang High Sierra Camp, Yosemite National Park, California
Nameless Lake (10709'), surrounded by glacier-sculpted granite peaks of the Cathedral Range, near Vogelsang High Sierra Camp.
Location: Yosemite National Park, California
Image ID: 23205  
Townsley Lake (10396'), a beautiful alpine lake sitting below blue sky, clouds and Fletcher Peak (right), lies amid the Cathedral Range of glacier-sculpted granite peaks in Yosemite's high country, near Vogelsang High Sierra Camp, Yosemite National Park, California
Townsley Lake (10396'), a beautiful alpine lake sitting below blue sky, clouds and Fletcher Peak (right), lies amid the Cathedral Range of glacier-sculpted granite peaks in Yosemite's high country, near Vogelsang High Sierra Camp.
Location: Yosemite National Park, California
Image ID: 23219  
Vogelsang Peak reflected in spectacular Vogelsang Lake, in Yosemite's high country near the John Muir Trial and Vogelsang High Sierra Camp. Vogelsang Peak (11516') was sculpted by glaciers from monolithic granite, Yosemite National Park, California
Vogelsang Peak reflected in spectacular Vogelsang Lake, in Yosemite's high country near the John Muir Trial and Vogelsang High Sierra Camp. Vogelsang Peak (11516') was sculpted by glaciers from monolithic granite.
Location: Yosemite National Park, California
Image ID: 23225  
Townsley Lake (10396'), a beautiful alpine lake sitting below blue sky, clouds and Fletcher Peak (right), lies amid the Cathedral Range of glacier-sculpted granite peaks in Yosemite's high country, near Vogelsang High Sierra Camp, Yosemite National Park, California
Townsley Lake (10396'), a beautiful alpine lake sitting below blue sky, clouds and Fletcher Peak (right), lies amid the Cathedral Range of glacier-sculpted granite peaks in Yosemite's high country, near Vogelsang High Sierra Camp.
Location: Yosemite National Park, California
Image ID: 23228  
Parson's Peak and Gallison Lake, part of the Cathedral Range of glacier-sculpted granite mountains, viewed from Vogelsang Pass in Yosemite's High Sierra, Yosemite National Park, California
Parson's Peak and Gallison Lake, part of the Cathedral Range of glacier-sculpted granite mountains, viewed from Vogelsang Pass in Yosemite's High Sierra.
Location: Yosemite National Park, California
Image ID: 23244  
Nameless Lake (10709'), surrounded by glacier-sculpted granite peaks of the Cathedral Range, near Vogelsang High Sierra Camp, Yosemite National Park, California
Nameless Lake (10709'), surrounded by glacier-sculpted granite peaks of the Cathedral Range, near Vogelsang High Sierra Camp.
Location: Yosemite National Park, California
Image ID: 23245  
Townsley Lake, a beautiful alpine lake sitting below blue sky, clouds and Fletcher Peak (right), lies amid the Cathedral Range of glacier-sculpted granite peaks in Yosemite's high country, near Vogelsang High Sierra Camp, Yosemite National Park, California
Townsley Lake, a beautiful alpine lake sitting below blue sky, clouds and Fletcher Peak (right), lies amid the Cathedral Range of glacier-sculpted granite peaks in Yosemite's high country, near Vogelsang High Sierra Camp.
Location: Yosemite National Park, California
Image ID: 23252  
Townsley Lake, a beautiful alpine lake sitting below blue sky, clouds and Fletcher Peak (right), lies amid the Cathedral Range of glacier-sculpted granite peaks in Yosemite's high country, near Vogelsang High Sierra Camp, Yosemite National Park, California
Townsley Lake, a beautiful alpine lake sitting below blue sky, clouds and Fletcher Peak (right), lies amid the Cathedral Range of glacier-sculpted granite peaks in Yosemite's high country, near Vogelsang High Sierra Camp.
Location: Yosemite National Park, California
Image ID: 23254  
Nameless Lake, surrounded by glacier-sculpted granite peaks of the Cathedral Range, near Vogelsang High Sierra Camp, Yosemite National Park, California
Nameless Lake, surrounded by glacier-sculpted granite peaks of the Cathedral Range, near Vogelsang High Sierra Camp.
Location: Yosemite National Park, California
Image ID: 23255  
Townsley Lake, a beautiful alpine lake sitting below blue sky, clouds and Fletcher Peak (right), lies amid the Cathedral Range of glacier-sculpted granite peaks in Yosemite's high country, near Vogelsang High Sierra Camp, Yosemite National Park, California
Townsley Lake, a beautiful alpine lake sitting below blue sky, clouds and Fletcher Peak (right), lies amid the Cathedral Range of glacier-sculpted granite peaks in Yosemite's high country, near Vogelsang High Sierra Camp.
Location: Yosemite National Park, California
Image ID: 23256  
Glacial erratic boulders atop Olmsted Point. Erratics are huge boulders left behind by the passing of glaciers which carved the granite surroundings into their present-day form. When the glaciers melt, any boulders and other geologic material that it was carrying are left in place, sometimes many miles from their original location, Yosemite National Park, California
Glacial erratic boulders atop Olmsted Point. Erratics are huge boulders left behind by the passing of glaciers which carved the granite surroundings into their present-day form. When the glaciers melt, any boulders and other geologic material that it was carrying are left in place, sometimes many miles from their original location.
Location: Yosemite National Park, California
Image ID: 23265  
Glacial erratic boulders atop Olmsted Point. Erratics are huge boulders left behind by the passing of glaciers which carved the granite surroundings into their present-day form. When the glaciers melt, any boulders and other geologic material that it was carrying are left in place, sometimes many miles from their original location, Yosemite National Park, California
Glacial erratic boulders atop Olmsted Point. Erratics are huge boulders left behind by the passing of glaciers which carved the granite surroundings into their present-day form. When the glaciers melt, any boulders and other geologic material that it was carrying are left in place, sometimes many miles from their original location.
Location: Yosemite National Park, California
Image ID: 23279  
Glacial erratic boulder atop Olmsted Point, with the massive granite monoliths Half Dome and Clouds Rest in the background. Erratics are huge boulders left behind by the passing of glaciers which carved the granite surroundings into their present-day form. When the glaciers melt, any boulders and other geologic material that it was carrying are left in place, sometimes many miles from their original location, Yosemite National Park, California
Glacial erratic boulder atop Olmsted Point, with the massive granite monoliths Half Dome and Clouds Rest in the background. Erratics are huge boulders left behind by the passing of glaciers which carved the granite surroundings into their present-day form. When the glaciers melt, any boulders and other geologic material that it was carrying are left in place, sometimes many miles from their original location.
Location: Yosemite National Park, California
Image ID: 23280  
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  
Drygalski Fjord, packed with brash ice which has broken away from Risting Glacier at the end of the narrow fjord
Drygalski Fjord, packed with brash ice which has broken away from Risting Glacier at the end of the narrow fjord.
Location: Drygalski Fjord, South Georgia Island
Image ID: 24687  
M/V Polar Star approaches Jenkins Glacier (left), Risting Glacier (center) and a third glacier (right) at the end of Drygalski Fjord
M/V Polar Star approaches Jenkins Glacier (left), Risting Glacier (center) and a third glacier (right) at the end of Drygalski Fjord.
Location: Drygalski Fjord, South Georgia Island
Image ID: 24688  
Chinstrap penguins at Bailey Head, Deception Island. Chinstrap penguins enter and exit the surf on the black sand beach at Bailey Head on Deception Island. Bailey Head is home to one of the largest colonies of chinstrap penguins in the world, Pygoscelis antarcticus
Chinstrap penguins at Bailey Head, Deception Island. Chinstrap penguins enter and exit the surf on the black sand beach at Bailey Head on Deception Island. Bailey Head is home to one of the largest colonies of chinstrap penguins in the world.
Species: Chinstrap penguin, Pygoscelis antarcticus
Location: Deception Island, Antarctic Peninsula, Antarctica
Image ID: 25456  
Brash ice and pack ice in Antarctica. Brash ices fills the ocean waters of Cierva Cove on the Antarctic Peninsula. The ice is a mix of sea ice that has floated near shore on the tide and chunks of ice that have fallen into the water from nearby land-bound glaciers
Brash ice and pack ice in Antarctica. Brash ices fills the ocean waters of Cierva Cove on the Antarctic Peninsula. The ice is a mix of sea ice that has floated near shore on the tide and chunks of ice that have fallen into the water from nearby land-bound glaciers.
Location: Cierva Cove, Antarctic Peninsula, Antarctica
Image ID: 25531  
Half Dome and the Glacier Point Road, Yosemite National Park
Half Dome and the Glacier Point Road, Yosemite National Park.
Location: Yosemite National Park, California
Image ID: 36379  
North Peak (12,242') over Conness Lake, water colored by glacier runoff, Hoover Wilderness, Conness Lakes Basin
North Peak (12,242') over Conness Lake, water colored by glacier runoff, Hoover Wilderness.
Location: Conness Lakes Basin, Hoover Wilderness, California
Image ID: 36425  
Panorama dimensions: 7198 x 16405
South Georgia Island coastline, showing the island's characteristic rugged topography. 56% of the island is covered by 161 glaciers, which have created numerous large bays and inlets that provide excellent habitat for marine animals and seabirds. Mountains meet the sea in steep-sided seacliffs covered with sparse vegetation. The highest point on South Georgia Island is Mt. Paget at 2,915m
South Georgia Island coastline, showing the island's characteristic rugged topography. 56% of the island is covered by 161 glaciers, which have created numerous large bays and inlets that provide excellent habitat for marine animals and seabirds. Mountains meet the sea in steep-sided seacliffs covered with sparse vegetation. The highest point on South Georgia Island is Mt. Paget at 2,915m.
Location: South Georgia Island
Image ID: 24321  
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