Search results for Mammoth Mountain

-1- 2
Mammoth Peak over Tuolumne Meadows, Tioga Pass, Yosemite National Park
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
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, Yosemite National Park, California
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 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 over Tuolumne Meadows, Tioga Pass, Yosemite National Park
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
Mammoth Peak rises above a placid Tioga Lake, at sunrise, Yosemite National Park, California
Mammoth Peak (12,117') rises above grassy meadows and granite boulders near Tioga Pass, Yosemite National Park, California
Mammoth Peak over Tuolumne Meadows, Tioga Pass, Yosemite National Park
Panoramic Photo of Crystal Lake, Mammoth Lakes, Inyo National Forest
Panoramic Photo of Lake George, Mammoth Lakes, Inyo National Forest
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, 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
Mammoth Peak rises above a placid Tioga Lake, at sunrise, Yosemite National Park, California
Mammoth Peak rises above a placid Tioga Lake, at sunrise, Yosemite National Park, California
Mammoth Peak (12,117') reflected in small tarn pond at sunrise, viewed from meadows near Tioga Pass, Yosemite National Park, California
Mammoth Peak over Tuolumne Meadows, Tioga Pass, Yosemite National Park
Mammoth Peak, reflected in a small alpine tarn (pond) at Tioga Pass, with meadow grasses and trees, Yosemite National Park, California
Mammoth Peak over Tuolumne Meadows, Tioga Pass, Yosemite National Park
Mammoth Peak over Tuolumne Meadows, Tioga Pass, Yosemite National Park
Mammoth Peak over Tuolumne Meadows, Tioga Pass, Yosemite National Park
Mammoth Peak (12,117') reflected in small tarn pond at sunrise, viewed from meadows near Tioga Pass, Yosemite National Park, California
-1- 2
Permalink: Mammoth_Mountain photos

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