Fracture Photo

Home > Natural History Photography Blog > Search > Fracture

$Devil's Postpile, a spectacular example of columnar basalt. Once molten and under great pressure underground, the lava that makes up Devil's Postpile cooled evenly and slowly, contracting and fracturing into polygonal-sided columns. The age of the formation is estimated between 100 and 700 thousand years old. Sometime after the basalt columns formed, a glacier passed over the formation, cutting and polishing the tops of the columns. The columns have from three to seven sides, varying because of differences in how quickly portions of the lava cooled, Devils Postpile National Monument, California$	$Devil's Postpile, a spectacular example of columnar basalt. Once molten and under great pressure underground, the lava that makes up Devil's Postpile cooled evenly and slowly, contracting and fracturing into polygonal-sided columns. The age of the formation is estimated between 100 and 700 thousand years old. Sometime after the basalt columns formed, a glacier passed over the formation, cutting and polishing the tops of the columns. The columns have from three to seven sides, varying because of differences in how quickly portions of the lava cooled, Devils Postpile National Monument, California$	$Devil's Postpile, a spectacular example of columnar basalt. Once molten and under great pressure underground, the lava that makes up Devil's Postpile cooled evenly and slowly, contracting and fracturing into polygonal-sided columns. The age of the formation is estimated between 100 and 700 thousand years old. Sometime after the basalt columns formed, a glacier passed over the formation, cutting and polishing the tops of the columns. The columns have from three to seven sides, varying because of differences in how quickly portions of the lava cooled, Devils Postpile National Monument, California$
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. Fracture Photo. Image ID: 23266 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. Fracture Picture. Image ID: 23267 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. Stock Photography of Fracture. Image ID: 23285 Location: Devils Postpile National Monument, California, USA
$Devil's Postpile, a spectacular example of columnar basalt. Once molten and under great pressure underground, the lava that makes up Devil's Postpile cooled evenly and slowly, contracting and fracturing into polygonal-sided columns. The age of the formation is estimated between 100 and 700 thousand years old. Sometime after the basalt columns formed, a glacier passed over the formation, cutting and polishing the tops of the columns. The columns have from three to seven sides, varying because of differences in how quickly portions of the lava cooled, Devils Postpile National Monument, California$	$Devil's Postpile, a spectacular example of columnar basalt. Once molten and under great pressure underground, the lava that makes up Devil's Postpile cooled evenly and slowly, contracting and fracturing into polygonal-sided columns. The age of the formation is estimated between 100 and 700 thousand years old. Sometime after the basalt columns formed, a glacier passed over the formation, cutting and polishing the tops of the columns. The columns have from three to seven sides, varying because of differences in how quickly portions of the lava cooled, Devils Postpile National Monument, California$	$Devil's Postpile, a spectacular example of columnar basalt. Once molten and under great pressure underground, the lava that makes up Devil's Postpile cooled evenly and slowly, contracting and fracturing into polygonal-sided columns. The age of the formation is estimated between 100 and 700 thousand years old. Sometime after the basalt columns formed, a glacier passed over the formation, cutting and polishing the tops of the columns. The columns have from three to seven sides, varying because of differences in how quickly portions of the lava cooled, Devils Postpile National Monument, California$
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. Photograph of Fracture. 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. Fracture Photos. 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. Fracture Image. Image ID: 23283 Location: Devils Postpile National Monument, California, USA
$Devil's Postpile, a spectacular example of columnar basalt. Once molten and under great pressure underground, the lava that makes up Devil's Postpile cooled evenly and slowly, contracting and fracturing into polygonal-sided columns. The age of the formation is estimated between 100 and 700 thousand years old. Sometime after the basalt columns formed, a glacier passed over the formation, cutting and polishing the tops of the columns. The columns have from three to seven sides, varying because of differences in how quickly portions of the lava cooled, Devils Postpile National Monument, California$	$Devil's Postpile, a spectacular example of columnar basalt. Once molten and under great pressure underground, the lava that makes up Devil's Postpile cooled evenly and slowly, contracting and fracturing into polygonal-sided columns. The age of the formation is estimated between 100 and 700 thousand years old. Sometime after the basalt columns formed, a glacier passed over the formation, cutting and polishing the tops of the columns. The columns have from three to seven sides, varying because of differences in how quickly portions of the lava cooled, Devils Postpile National Monument, California$	$Devil's Postpile, a spectacular example of columnar basalt. Once molten and under great pressure underground, the lava that makes up Devil's Postpile cooled evenly and slowly, contracting and fracturing into polygonal-sided columns. The age of the formation is estimated between 100 and 700 thousand years old. Sometime after the basalt columns formed, a glacier passed over the formation, cutting and polishing the tops of the columns. The columns have from three to seven sides, varying because of differences in how quickly portions of the lava cooled, Devils Postpile National Monument, California$
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. Professional stock photos of Fracture. 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. Pictures of Fracture. 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. Fracture Photo. Image ID: 23287 Location: Devils Postpile National Monument, California, USA
$A glacier fractures and cracks, as the leading of a glacier fractures and cracks as it reaches the ocean. The pieces will float away to become icebergs, Neko Harbor$	$A glacier fractures and cracks, as the leading of a glacier fractures and cracks as it reaches the ocean. The pieces will float away to become icebergs, Neko Harbor$	$A glacier fractures and cracks, as the leading of a glacier fractures and cracks as it reaches the ocean. The pieces will float away to become icebergs, Neko Harbor$
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. Fracture Picture. Image ID: 25654 Location: Neko Harbor, Antarctic Peninsula, Antarctica	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. Stock Photography of Fracture. Image ID: 25741 Location: Neko Harbor, Antarctic Peninsula, Antarctica	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. Photograph of Fracture. Image ID: 25671 Location: Neko Harbor, Antarctic Peninsula, Antarctica
$A glacier fractures and cracks, as the leading of a glacier fractures and cracks as it reaches the ocean. The pieces will float away to become icebergs, Neko Harbor$	$A glacier fractures and cracks, as the leading of a glacier fractures and cracks as it reaches the ocean. The pieces will float away to become icebergs, Neko Harbor$	$A glacier fractures and cracks, as the leading of a glacier fractures and cracks as it reaches the ocean. The pieces will float away to become icebergs, Neko Harbor$
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. Fracture Photos. Image ID: 25738 Location: Neko Harbor, Antarctic Peninsula, Antarctica	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. Fracture Image. Image ID: 25655 Location: Neko Harbor, Antarctic Peninsula, Antarctica	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. Professional stock photos of Fracture. Image ID: 25672 Location: Neko Harbor, Antarctic Peninsula, Antarctica
$A glacier fractures and cracks, as the leading of a glacier fractures and cracks as it reaches the ocean. The pieces will float away to become icebergs, Neko Harbor$	$A glacier fractures and cracks, as the leading of a glacier fractures and cracks as it reaches the ocean. The pieces will float away to become icebergs, Neko Harbor$	$A glacier fractures and cracks, as the leading of a glacier fractures and cracks as it reaches the ocean. The pieces will float away to become icebergs, Neko Harbor$
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. Pictures of Fracture. Image ID: 25740 Location: Neko Harbor, Antarctic Peninsula, Antarctica	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. Fracture Photo. Image ID: 25742 Location: Neko Harbor, Antarctic Peninsula, Antarctica	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. Fracture Picture. Image ID: 25743 Location: Neko Harbor, Antarctic Peninsula, Antarctica
$A glacier fractures and cracks, as the leading edge reaches the ocean. The pieces will float away to become icebergs, Neko Harbor$
A glacier fractures and cracks, as the leading edge reaches the ocean. The pieces will float away to become icebergs. Stock Photography of Fracture. Image ID: 25739 Location: Neko Harbor, Antarctic Peninsula, Antarctica