Fracture Photos

Milky Way over Sandstone Fins. Sandstone fins stand on edge. Vertical fractures separate standing plates of sandstone that are eroded into freestanding fins, that may one day further erode into arches, Arches National Park, Utah
Milky Way over Sandstone Fins. Sandstone fins stand on edge. Vertical fractures separate standing plates of sandstone that are eroded into freestanding fins, that may one day further erode into arches.
Location: Arches National Park, Utah
Image ID: 29254  
Sunrise light touches the Fins. Sandstone fins stand on edge. Vertical fractures separate standing plates of sandstone that are eroded into freestanding fins, that may one day further erode into arches, Arches National Park, Utah
Sunrise light touches the Fins. Sandstone fins stand on edge. Vertical fractures separate standing plates of sandstone that are eroded into freestanding fins, that may one day further erode into arches.
Location: Arches National Park, Utah
Image ID: 29255  
Milky Way over Sandstone Fins. Sandstone fins stand on edge. Vertical fractures separate standing plates of sandstone that are eroded into freestanding fins, that may one day further erode into arches, Arches National Park, Utah
Milky Way over Sandstone Fins. Sandstone fins stand on edge. Vertical fractures separate standing plates of sandstone that are eroded into freestanding fins, that may one day further erode into arches.
Location: Arches National Park, Utah
Image ID: 29253  
Panorama dimensions: 7791 x 15529
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: 23266  
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  
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  
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
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.
Location: Neko Harbor, Antarctic Peninsula, Antarctica
Image ID: 25654  
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
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.
Location: Neko Harbor, Antarctic Peninsula, Antarctica
Image ID: 25741  
Sandstone fins stand on edge. Vertical fractures separate standing plates of sandstone that are eroded into freestanding fins, that may one day further erode into arches, Arches National Park, Utah
Sandstone fins stand on edge. Vertical fractures separate standing plates of sandstone that are eroded into freestanding fins, that may one day further erode into arches.
Location: Arches National Park, Utah
Image ID: 29256  
Panorama dimensions: 6933 x 11514
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
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.
Location: Neko Harbor, Antarctic Peninsula, Antarctica
Image ID: 25671  
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
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.
Location: Neko Harbor, Antarctic Peninsula, Antarctica
Image ID: 25738  
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
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.
Location: Neko Harbor, Antarctic Peninsula, Antarctica
Image ID: 25655  
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
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.
Location: Neko Harbor, Antarctic Peninsula, Antarctica
Image ID: 25672  
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
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.
Location: Neko Harbor, Antarctic Peninsula, Antarctica
Image ID: 25740  
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
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.
Location: Neko Harbor, Antarctic Peninsula, Antarctica
Image ID: 25742  
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
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.
Location: Neko Harbor, Antarctic Peninsula, Antarctica
Image ID: 25743  
A glacier fractures and cracks, as the leading edge reaches the ocean. The pieces will float away to become icebergs, Neko Harbor
A glacier fractures and cracks, as the leading edge reaches the ocean. The pieces will float away to become icebergs.
Location: Neko Harbor, Antarctic Peninsula, Antarctica
Image ID: 25739  
All photographs copyright © Phillip Colla / Oceanlight.com, all rights reserved worldwide.