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Salt polygons.  After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes, Death Valley National Park, California Add To Light Table Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes, Death Valley National Park, California Add To Light Table Salt polygons.  After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes, Death Valley National Park, California Add To Light Table
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes.
Image ID: 25242  
Location: Badwater, Death Valley National Park, California, USA
 
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes.
Image ID: 27631  
Location: Badwater, Death Valley National Park, California, USA
 
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes.
Image ID: 25254  
Location: Badwater, Death Valley National Park, California, USA
 
Salt polygons.  After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes, Death Valley National Park, California Add To Light Table Salt polygons.  After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes, Death Valley 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
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes.
Image ID: 25262  
Location: Badwater, Death Valley National Park, California, USA
 
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes.
Image ID: 25259  
Location: Badwater, Death Valley 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: 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, 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: 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.
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.
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, 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: 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.
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, 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 Salt polygons.  After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes, Death Valley 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.
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.
Image ID: 23287  
Location: Devils Postpile National Monument, California, USA
 
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes.
Image ID: 25293  
Location: Badwater, Death Valley National Park, California, USA
 
Salt polygons.  After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes, Death Valley National Park, California Add To Light Table Salt polygons.  After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes, Death Valley National Park, California Add To Light Table Salt polygons.  After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes, Death Valley National Park, California Add To Light Table
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes.
Image ID: 25294  
Location: Badwater, Death Valley National Park, California, USA
 
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes.
Image ID: 25303  
Location: Badwater, Death Valley National Park, California, USA
 
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes.
Image ID: 25304  
Location: Badwater, Death Valley National Park, California, USA
 
Salt polygons.  After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes, Death Valley National Park, California Add To Light Table Devils Golf Course, California.  Evaporated salt has formed into gnarled, complex crystalline shapes in on the salt pan of Death Valley National Park, one of the largest salt pans in the world.  The shapes are constantly evolving as occasional floods submerge the salt concretions before receding and depositing more salt Add To Light Table Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes, Death Valley National Park, California Add To Light Table
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes.
Image ID: 25305  
Location: Badwater, Death Valley National Park, California, USA
 
Devils Golf Course, California. Evaporated salt has formed into gnarled, complex crystalline shapes in on the salt pan of Death Valley National Park, one of the largest salt pans in the world. The shapes are constantly evolving as occasional floods submerge the salt concretions before receding and depositing more salt.
Image ID: 15582  
Location: Devils Golf Course, Death Valley National Park, California, USA
 
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes.
Image ID: 27635  
Location: Badwater, Death Valley National Park, California, USA
 
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes, Death Valley National Park, California Add To Light Table Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes, Death Valley National Park, California Add To Light Table Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes, Death Valley National Park, California Add To Light Table
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes.
Image ID: 27632  
Location: Badwater, Death Valley National Park, California, USA
 
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes.
Image ID: 27633  
Location: Badwater, Death Valley National Park, California, USA
 
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes.
Image ID: 27634  
Location: Badwater, Death Valley National Park, California, USA
 
Devils Golf Course, California.  Evaporated salt has formed into gnarled, complex crystalline shapes in on the salt pan of Death Valley National Park, one of the largest salt pans in the world.  The shapes are constantly evolving as occasional floods submerge the salt concretions before receding and depositing more salt Add To Light Table Devils Golf Course, California.  Evaporated salt has formed into gnarled, complex crystalline shapes in on the salt pan of Death Valley National Park, one of the largest salt pans in the world.  The shapes are constantly evolving as occasional floods submerge the salt concretions before receding and depositing more salt Add To Light Table Salt polygons.  After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes, Death Valley National Park, California Add To Light Table
Devils Golf Course, California. Evaporated salt has formed into gnarled, complex crystalline shapes in on the salt pan of Death Valley National Park, one of the largest salt pans in the world. The shapes are constantly evolving as occasional floods submerge the salt concretions before receding and depositing more salt.
Image ID: 15583  
Location: Devils Golf Course, Death Valley National Park, California, USA
 
Devils Golf Course, California. Evaporated salt has formed into gnarled, complex crystalline shapes in on the salt pan of Death Valley National Park, one of the largest salt pans in the world. The shapes are constantly evolving as occasional floods submerge the salt concretions before receding and depositing more salt.
Image ID: 15597  
Location: Devils Golf Course, Death Valley National Park, California, USA
 
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes.
Image ID: 25299  
Location: Badwater, Death Valley National Park, California, USA
 
Devils Golf Course, California.  Evaporated salt has formed into gnarled, complex crystalline shapes in on the salt pan of Death Valley National Park, one of the largest salt pans in the world.  The shapes are constantly evolving as occasional floods submerge the salt concretions before receding and depositing more salt Add To Light Table Devils Golf Course, California.  Evaporated salt has formed into gnarled, complex crystalline shapes in on the salt pan of Death Valley National Park, one of the largest salt pans in the world.  The shapes are constantly evolving as occasional floods submerge the salt concretions before receding and depositing more salt Add To Light Table Devils Golf Course, California.  Evaporated salt has formed into gnarled, complex crystalline shapes in on the salt pan of Death Valley National Park, one of the largest salt pans in the world.  The shapes are constantly evolving as occasional floods submerge the salt concretions before receding and depositing more salt Add To Light Table
Devils Golf Course, California. Evaporated salt has formed into gnarled, complex crystalline shapes in on the salt pan of Death Valley National Park, one of the largest salt pans in the world. The shapes are constantly evolving as occasional floods submerge the salt concretions before receding and depositing more salt.
Image ID: 15615  
Location: Devils Golf Course, Death Valley National Park, California, USA
 
Devils Golf Course, California. Evaporated salt has formed into gnarled, complex crystalline shapes in on the salt pan of Death Valley National Park, one of the largest salt pans in the world. The shapes are constantly evolving as occasional floods submerge the salt concretions before receding and depositing more salt.
Image ID: 15616  
Location: Devils Golf Course, Death Valley National Park, California, USA
 
Devils Golf Course, California. Evaporated salt has formed into gnarled, complex crystalline shapes in on the salt pan of Death Valley National Park, one of the largest salt pans in the world. The shapes are constantly evolving as occasional floods submerge the salt concretions before receding and depositing more salt.
Image ID: 15627  
Location: Devils Golf Course, Death Valley National Park, California, USA
 


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Updated: October 1, 2020