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Nameless Lake (10709'), surrounded by glacier-sculpted granite peaks of the Cathedral Range, near Vogelsang High Sierra Camp, Yosemite National Park, California Add To Light Table 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 Add To Light Table 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 Add To Light Table
Nameless Lake (10709'), surrounded by glacier-sculpted granite peaks of the Cathedral Range, near Vogelsang High Sierra Camp.
Image ID: 23205  
Location: Yosemite National Park, California, USA
 
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.
Image ID: 23219  
Location: Yosemite National Park, California, USA
 
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.
Image ID: 23225  
Location: Yosemite National Park, California, USA
 
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 Add To Light Table 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 Add To Light Table Nameless Lake (10709'), surrounded by glacier-sculpted granite peaks of the Cathedral Range, near Vogelsang High Sierra Camp, Yosemite National Park, California Add To Light Table
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.
Image ID: 23228  
Location: Yosemite National Park, California, USA
 
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.
Image ID: 23244  
Location: Yosemite National Park, California, USA
 
Nameless Lake (10709'), surrounded by glacier-sculpted granite peaks of the Cathedral Range, near Vogelsang High Sierra Camp.
Image ID: 23245  
Location: Yosemite National Park, California, USA
 
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 Add To Light Table 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 Add To Light Table Nameless Lake, surrounded by glacier-sculpted granite peaks of the Cathedral Range, near Vogelsang High Sierra Camp, Yosemite National Park, California Add To Light Table
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.
Image ID: 23252  
Location: Yosemite National Park, California, USA
 
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.
Image ID: 23254  
Location: Yosemite National Park, California, USA
 
Nameless Lake, surrounded by glacier-sculpted granite peaks of the Cathedral Range, near Vogelsang High Sierra Camp.
Image ID: 23255  
Location: Yosemite National Park, California, USA
 
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 Add To Light Table 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 Add To Light Table 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 Add To Light Table
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.
Image ID: 23256  
Location: Yosemite National Park, California, USA
 
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.
Image ID: 23265  
Location: Yosemite National Park, California, USA
 
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.
Image ID: 23279  
Location: Yosemite National Park, California, USA
 
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 Add To Light Table 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 Add To Light Table 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 Add To Light Table
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.
Image ID: 23280  
Location: Yosemite National Park, California, USA
 
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.
Image ID: 23281  
Location: Devils Postpile National Monument, California, USA
 
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.
Image ID: 23282  
Location: Devils Postpile National Monument, California, USA
 
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 Add To Light Table 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 Add To Light Table 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 Add To Light Table
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.
Image ID: 23283  
Location: Devils Postpile National Monument, California, USA
 
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.
Image ID: 23284  
Location: Devils Postpile National Monument, California, USA
 
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.
Image ID: 23286  
Location: Devils Postpile National Monument, California, USA
 
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 Add To Light Table Drygalski Fjord, packed with brash ice which has broken away from Risting Glacier at the end of the narrow fjord Add To Light Table M/V Polar Star approaches Jenkins Glacier (left), Risting Glacier (center) and a third glacier (right) at the end of Drygalski Fjord Add To Light Table
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.
Image ID: 23287  
Location: Devils Postpile National Monument, California, USA
 
Drygalski Fjord, packed with brash ice which has broken away from Risting Glacier at the end of the narrow fjord.
Image ID: 24687  
Location: Drygalski Fjord, South Georgia Island
 
M/V Polar Star approaches Jenkins Glacier (left), Risting Glacier (center) and a third glacier (right) at the end of Drygalski Fjord.
Image ID: 24688  
Location: Drygalski Fjord, South Georgia Island
 
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 Add To Light Table 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 Add To Light Table Drygalski Fjord, passengers on icebreak M/V Polar Star.  The water is packed with brash ice which has broken away from Risting Glacier at the end of the narrow fjord Add To Light Table
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.
Image ID: 25531  
Location: Cierva Cove, Antarctic Peninsula, Antarctica
 
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.
Image ID: 24321  
Location: South Georgia Island
 
Drygalski Fjord, passengers on icebreak M/V Polar Star. The water is packed with brash ice which has broken away from Risting Glacier at the end of the narrow fjord.
Image ID: 24684  
Location: Drygalski Fjord, South Georgia Island
 
Drygalski Fjord, packed with brash ice which has broken away from Risting Glacier at the end of the narrow fjord Add To Light Table Grassy windy highlands and rocks, overlooking alluvial floodplain formed by glacier runoff near Stromness Bay, Stromness Harbour Add To Light Table Reindeer on South Georgia Island.  Reindeer (known as caribou when wild) were introduced to South Georgia Island by Norway in the early 20th Century.  There are now two distinct herds which are permanently separated by glaciers, Rangifer tarandus, Fortuna Bay Add To Light Table
Drygalski Fjord, packed with brash ice which has broken away from Risting Glacier at the end of the narrow fjord.
Image ID: 24697  
Location: Drygalski Fjord, South Georgia Island
 
Grassy windy highlands and rocks, overlooking alluvial floodplain formed by glacier runoff near Stromness Bay.
Image ID: 24584  
Location: Stromness Harbour, South Georgia Island
 
Reindeer on South Georgia Island. Reindeer (known as caribou when wild) were introduced to South Georgia Island by Norway in the early 20th Century. There are now two distinct herds which are permanently separated by glaciers.
Image ID: 24592  
Species: Reindeer, Rangifer tarandus
Location: Fortuna Bay, South Georgia Island
 
Drygalski Fjord, packed with brash ice which has broken away from the glacier at the end of the narrow fjord Add To Light Table M/V Polar Star approaches Jenkins Glacier (left), Risting Glacier (center) and a third glacier (right) at the end of Drygalski Fjord Add To Light Table A glacier fractures and cracks, as the leading of a glacier fractures and cracks as it reaches the ocean.  The pieces will float away to become icebergs, Neko Harbor Add To Light Table
Drygalski Fjord, packed with brash ice which has broken away from the glacier at the end of the narrow fjord.
Image ID: 24698  
Location: Drygalski Fjord, South Georgia Island
 
M/V Polar Star approaches Jenkins Glacier (left), Risting Glacier (center) and a third glacier (right) at the end of Drygalski Fjord.
Image ID: 24699  
Location: Drygalski Fjord, South Georgia Island
 
A glacier fractures and cracks, as the leading of a glacier fractures and cracks as it reaches the ocean. The pieces will float away to become icebergs.
Image ID: 25654  
Location: Neko Harbor, Antarctic Peninsula, Antarctica
 


Natural History Photography Blog posts (20) related to Glacier



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Species Appearing Among These Images:
Rangifer tarandus

Natural History Photography Blog posts (20) related to Glacier
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Natural History Photography - Best Photos of 2015
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New Work - September 2013
Perseid Meteor Shower, Milky Way, Half Dome and Yosemite National Park
Zodiacal Light, Milky Way and Jupiter over Yosemite National Park
Stars Over Half Dome and Glacier Point, Yosemite National Park
Sunrise over Half Dome from Glacier Point, Yosemite National Park
Neko Harbor, Antarctica
Cierva Cove, Antarctica
A Return to Vogelsang High Sierra Camp
Brown Bluff, Antarctica
Coronation Island, South Orkney Islands
Drygalski Fjord, South Georgia Island
Salisbury Plain, South Georgia Island
Grytviken, South Georgia Island
Stromness Harbour and Shackleton Hike, South Georgia Island
Right Whale Bay, South Georgia Island
Approaching South Georgia Island
Ushuaia, Tierra del Fuego, Argentina

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Updated: June 5, 2020