Search results for Salt

-1- 2 3 4 5
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes, Death Valley National Park, California
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes.
Location: Badwater, Death Valley National Park, California
Image ID: 25242  
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes, Death Valley National Park, California
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes.
Location: Badwater, Death Valley National Park, California
Image ID: 27631  
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes, Death Valley National Park, California
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes.
Location: Badwater, Death Valley National Park, California
Image ID: 25254  
A river of salt flows across Death Valley, toward the lowest point in the United States at Badwater, Death Valley National Park, California
A river of salt flows across Death Valley, toward the lowest point in the United States at Badwater.
Location: Badwater, Death Valley National Park, California
Image ID: 25260  
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes, Death Valley National Park, California
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes.
Location: Badwater, Death Valley National Park, California
Image ID: 25262  
Salt Creek surf, pretty big day, winter, morning, Laguna Niguel, California
Salt Creek surf, pretty big day, winter, morning.
Location: Salt Creek, Laguna Niguel, California
Image ID: 14851  
Salt Creek surf, pretty big day, winter, morning, Laguna Niguel, California
Salt Creek surf, pretty big day, winter, morning.
Location: Salt Creek, Laguna Niguel, California
Image ID: 14852  
Panorama of the Minarets at sunrise, near Mammoth Mountain. The Minarets are a series of seventeen jagged peaks in the Ritter Range, west of Mammoth Mountain in the Ansel Adams Wilderness. These basalt peaks were carved by glaciers on both sides of the range. The highest of the Minarets stands 12,281 feet above sea level, Mammoth Lakes, California
Panorama of the Minarets at sunrise, near Mammoth Mountain. The Minarets are a series of seventeen jagged peaks in the Ritter Range, west of Mammoth Mountain in the Ansel Adams Wilderness. These basalt peaks were carved by glaciers on both sides of the range. The highest of the Minarets stands 12,281 feet above sea level.
Location: Mammoth Lakes, California
Image ID: 19126  
Panorama dimensions: 3249 x 29914
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes, Death Valley National Park, California
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes.
Location: Badwater, Death Valley National Park, California
Image ID: 25259  
Natural Salt Lake on Isla San Jose, Aerial View, Sea of Cortez
Natural Salt Lake on Isla San Jose, Aerial View, Sea of Cortez.
Location: Isla San Jose, Baja California, Mexico
Image ID: 33620  
Panorama dimensions: 5379 x 12529
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  
Erosion in the salt patterns of Badwater Playa, Death Valley National Park
Erosion in the salt patterns of Badwater Playa, Death Valley National Park.
Location: Badwater, Death Valley National Park, California
Image ID: 30472  
Erosion in the salt patterns of Badwater Playa, Death Valley National Park
Erosion in the salt patterns of Badwater Playa, Death Valley National Park.
Location: Badwater, Death Valley National Park, California
Image ID: 30473  
Erosion in the salt patterns of Badwater Playa, Death Valley National Park
Erosion in the salt patterns of Badwater Playa, Death Valley National Park.
Location: Badwater, Death Valley National Park, California
Image ID: 30474  
Erosion in the salt patterns of Badwater Playa, Death Valley National Park
Erosion in the salt patterns of Badwater Playa, Death Valley National Park.
Location: Badwater, Death Valley National Park, California
Image ID: 30475  
Natural Salt Lake on Isla San Jose, Aerial View, Sea of Cortez
Natural Salt Lake on Isla San Jose, Aerial View, Sea of Cortez.
Location: Isla San Jose, Baja California, Mexico
Image ID: 33621  
Panorama dimensions: 3966 x 10878
Salt Lake on Isla Espiritu Santo, Baja California, aerial view
Salt Lake on Isla Espiritu Santo, Baja California, aerial view.
Location: Isla Espiritu Santo, Baja California, Mexico
Image ID: 33821  
Panorama dimensions: 4761 x 17704
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  
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes, Death Valley National Park, California
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes.
Location: Badwater, Death Valley National Park, California
Image ID: 25293  
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes, Death Valley National Park, California
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes.
Location: Badwater, Death Valley National Park, California
Image ID: 25294  
A river of salt flows across Death Valley, toward the lowest point in the United States at Badwater, Death Valley National Park, California
A river of salt flows across Death Valley, toward the lowest point in the United States at Badwater.
Location: Badwater, Death Valley National Park, California
Image ID: 25300  
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes, Death Valley National Park, California
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes.
Location: Badwater, Death Valley National Park, California
Image ID: 25303  
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes, Death Valley National Park, California
Salt polygons. After winter flooding, the salt on the Badwater Basin playa dries into geometric polygonal shapes.
Location: Badwater, Death Valley National Park, California
Image ID: 25304  
-1- 2 3 4 5
Permalink: Salt photos

All photographs copyright © Phillip Colla / Oceanlight.com, all rights reserved worldwide.