Search results for Mammoth Mountain

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Mammoth Peak over Tuolumne Meadows, Tioga Pass, Yosemite National Park
Mammoth Peak over Tuolumne Meadows, Tioga Pass, Yosemite National Park.
Location: Yosemite National Park, California
Image ID: 28514  
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
Mammoth Peak (12,117') reflected in small tarn pond at sunrise, viewed from meadows near Tioga Pass, Yosemite National Park, California
Mammoth Peak (12,117') reflected in small tarn pond at sunrise, viewed from meadows near Tioga Pass.
Location: Yosemite National Park, California
Image ID: 25758  
Mammoth Peak (12,117') reflected in small tarn pond at sunrise, viewed from meadows near Tioga Pass, Yosemite National Park, California
Mammoth Peak (12,117') reflected in small tarn pond at sunrise, viewed from meadows near Tioga Pass.
Location: Yosemite National Park, California
Image ID: 25759  
Mammoth Peak and alpine meadows in the High Sierra are reflected in Tioga Lake at sunrise. This spectacular location is just a short walk from the Tioga Pass road. Near Tuolumne Meadows and Yosemite National Park
Mammoth Peak and alpine meadows in the High Sierra are reflected in Tioga Lake at sunrise. This spectacular location is just a short walk from the Tioga Pass road. Near Tuolumne Meadows and Yosemite National Park.
Location: Tioga Lake, Yosemite National Park, California
Image ID: 09949  
Mammoth Peak in the High Sierra range is reflected in Tioga Lake at sunrise. This spectacular location is just a short walk from the Tioga Pass road. Near Tuolumne Meadows and Yosemite National Park
Mammoth Peak in the High Sierra range is reflected in Tioga Lake at sunrise. This spectacular location is just a short walk from the Tioga Pass road. Near Tuolumne Meadows and Yosemite National Park.
Location: Tioga Lake, Yosemite National Park, California
Image ID: 09948  
Mammoth Peak over Tuolumne Meadows, Tioga Pass, Yosemite National Park
Mammoth Peak over Tuolumne Meadows, Tioga Pass, Yosemite National Park.
Location: Yosemite National Park, California
Image ID: 28510  
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  
Mammoth Peak rises above a placid Tioga Lake, at sunrise, Yosemite National Park, California
Mammoth Peak rises above a placid Tioga Lake, at sunrise.
Location: Tioga Lake, Yosemite National Park, California
Image ID: 23291  
Mammoth Peak (12,117') rises above grassy meadows and granite boulders near Tioga Pass, Yosemite National Park, California
Mammoth Peak (12,117') rises above grassy meadows and granite boulders near Tioga Pass.
Location: Yosemite National Park, California
Image ID: 25766  
Mammoth Peak over Tuolumne Meadows, Tioga Pass, Yosemite National Park
Mammoth Peak over Tuolumne Meadows, Tioga Pass, Yosemite National Park.
Location: Yosemite National Park, California
Image ID: 28511  
Panoramic Photo of Crystal Lake, Mammoth Lakes, Inyo National Forest
Panoramic Photo of Crystal Lake, Mammoth Lakes, Inyo National Forest.
Location: Mammoth Lakes, Inyo National Forest, California
Image ID: 31188  
Panorama dimensions: 5659 x 19050
Panoramic Photo of Lake George, Mammoth Lakes, Inyo National Forest
Panoramic Photo of Lake George, Mammoth Lakes, Inyo National Forest.
Location: Mammoth Lakes, Inyo National Forest, California
Image ID: 31189  
Panorama dimensions: 5772 x 15775
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  
Mammoth Peak rises above a placid Tioga Lake, at sunrise, Yosemite National Park, California
Mammoth Peak rises above a placid Tioga Lake, at sunrise.
Location: Tioga Lake, Yosemite National Park, California
Image ID: 23268  
Mammoth Peak rises above a placid Tioga Lake, at sunrise, Yosemite National Park, California
Mammoth Peak rises above a placid Tioga Lake, at sunrise.
Location: Tioga Lake, Yosemite National Park, California
Image ID: 23290  
Mammoth Peak (12,117') reflected in small tarn pond at sunrise, viewed from meadows near Tioga Pass, Yosemite National Park, California
Mammoth Peak (12,117') reflected in small tarn pond at sunrise, viewed from meadows near Tioga Pass.
Location: Yosemite National Park, California
Image ID: 25773  
Mammoth Peak over Tuolumne Meadows, Tioga Pass, Yosemite National Park
Mammoth Peak over Tuolumne Meadows, Tioga Pass, Yosemite National Park.
Location: Yosemite National Park, California
Image ID: 28512  
Mammoth Peak, reflected in a small alpine tarn (pond) at Tioga Pass, with meadow grasses and trees, Yosemite National Park, California
Mammoth Peak, reflected in a small alpine tarn (pond) at Tioga Pass, with meadow grasses and trees.
Location: Yosemite National Park, California
Image ID: 23269  
Mammoth Peak over Tuolumne Meadows, Tioga Pass, Yosemite National Park
Mammoth Peak over Tuolumne Meadows, Tioga Pass, Yosemite National Park.
Location: Yosemite National Park, California
Image ID: 28513  
Mammoth Peak over Tuolumne Meadows, Tioga Pass, Yosemite National Park
Mammoth Peak over Tuolumne Meadows, Tioga Pass, Yosemite National Park.
Location: Yosemite National Park, California
Image ID: 28515  
Mammoth Peak over Tuolumne Meadows, Tioga Pass, Yosemite National Park
Mammoth Peak over Tuolumne Meadows, Tioga Pass, Yosemite National Park.
Location: Yosemite National Park, California
Image ID: 28516  
Mammoth Peak (12,117') reflected in small tarn pond at sunrise, viewed from meadows near Tioga Pass, Yosemite National Park, California
Mammoth Peak (12,117') reflected in small tarn pond at sunrise, viewed from meadows near Tioga Pass.
Location: Yosemite National Park, California
Image ID: 25792  
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