Search results for Mono Lake

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Mono Lake sunset, tufa and clouds reflected in the still waters of Mono Lake
Mono Lake sunset, tufa and clouds reflected in the still waters of Mono Lake.
Location: Mono Lake, California
Image ID: 26977  
Sun pillar rises over the Sierra Nevada and this Mono Lake sunset, Sierra Nevada mountain range and tufas, clouds reflected in the still waters of Mono Lake
Sun pillar rises over the Sierra Nevada and this Mono Lake sunset, Sierra Nevada mountain range and tufas, clouds reflected in the still waters of Mono Lake.
Location: Mono Lake, California
Image ID: 26968  
Panorama dimensions: 5331 x 14966
Mono Lake sunset, Sierra Nevada mountain range and tufas, clouds reflected in the still waters of Mono Lake
Mono Lake sunset, Sierra Nevada mountain range and tufas, clouds reflected in the still waters of Mono Lake.
Location: Mono Lake, California
Image ID: 26978  
Tufa and Stars at Night, Milky Way galaxy, Mono Lake, California
Tufa and Stars at Night, Milky Way galaxy.
Location: Mono Lake, California
Image ID: 28519  
Tufa and Stars at Night, Milky Way galaxy, Mono Lake, California
Tufa and Stars at Night, Milky Way galaxy.
Location: Mono Lake, California
Image ID: 28509  
Vogelsang Peak reflected in spectacular Vogelsang Lake, in Yosemite's high country near the John Muir Trial and Vogelsang High Sierra Camp. Vogelsang Peak (11516') was sculpted by glaciers from monolithic granite, Yosemite National Park, California
Vogelsang Peak reflected in spectacular Vogelsang Lake, in Yosemite's high country near the John Muir Trial and Vogelsang High Sierra Camp. Vogelsang Peak (11516') was sculpted by glaciers from monolithic granite.
Location: Yosemite National Park, California
Image ID: 23225  
Tufa towers rise from Mono Lake, with the Eastern Sierra visible in the distance. Tufa towers are formed when underwater springs rich in calcium mix with lakewater rich in carbonates, forming calcium carbonate (limestone) structures below the surface of the lake. The towers were eventually revealed when the water level in the lake was lowered starting in 1941
Tufa towers rise from Mono Lake, with the Eastern Sierra visible in the distance. Tufa towers are formed when underwater springs rich in calcium mix with lakewater rich in carbonates, forming calcium carbonate (limestone) structures below the surface of the lake. The towers were eventually revealed when the water level in the lake was lowered starting in 1941.
Location: Mono Lake, California
Image ID: 26983  
Mono Lake sunset, tufa and clouds reflected in the still waters of Mono Lake
Mono Lake sunset, tufa and clouds reflected in the still waters of Mono Lake.
Location: Mono Lake, California
Image ID: 27005  
Mono Lake Tufa at Sunset
Mono Lake Tufa at Sunset.
Location: Mono Lake, California
Image ID: 31072  
Tufa and Stars at Night, Milky Way galaxy, Mono Lake, California
Tufa and Stars at Night, Milky Way galaxy.
Location: Mono Lake, California
Image ID: 28517  
Tufa and Stars at Night, Milky Way galaxy, Mono Lake, California
Tufa and Stars at Night, Milky Way galaxy.
Location: Mono Lake, California
Image ID: 28518  
Tufa and Stars at Night, Milky Way galaxy, Mono Lake, California
Tufa and Stars at Night, Milky Way galaxy.
Location: Mono Lake, California
Image ID: 28520  
Tufa and Stars at Night, Milky Way galaxy, Mono Lake, California
Tufa and Stars at Night, Milky Way galaxy.
Location: Mono Lake, California
Image ID: 28507  
Tufa and Stars at Night, Milky Way galaxy, Mono Lake, California
Tufa and Stars at Night, Milky Way galaxy.
Location: Mono Lake, California
Image ID: 28508  
Mono Lake sunset, Sierra Nevada mountain range and tufas, clouds reflected in the still waters of Mono Lake
Mono Lake sunset, Sierra Nevada mountain range and tufas, clouds reflected in the still waters of Mono Lake.
Location: Mono Lake, California
Image ID: 26967  
Panorama dimensions: 4835 x 12178
Mono Lake sunset, Sierra Nevada mountain range and tufas, clouds reflected in the still waters of Mono Lake
Mono Lake sunset, Sierra Nevada mountain range and tufas, clouds reflected in the still waters of Mono Lake.
Location: Mono Lake, California
Image ID: 26969  
Panorama dimensions: 5348 x 9435
Tufa towers rise from Mono Lake, with the Eastern Sierra visible in the distance. Tufa towers are formed when underwater springs rich in calcium mix with lakewater rich in carbonates, forming calcium carbonate (limestone) structures below the surface of the lake. The towers were eventually revealed when the water level in the lake was lowered starting in 1941
Tufa towers rise from Mono Lake, with the Eastern Sierra visible in the distance. Tufa towers are formed when underwater springs rich in calcium mix with lakewater rich in carbonates, forming calcium carbonate (limestone) structures below the surface of the lake. The towers were eventually revealed when the water level in the lake was lowered starting in 1941.
Location: Mono Lake, California
Image ID: 26991  
Tufa towers rise from Mono Lake, with the Eastern Sierra visible in the distance. Tufa towers are formed when underwater springs rich in calcium mix with lakewater rich in carbonates, forming calcium carbonate (limestone) structures below the surface of the lake. The towers were eventually revealed when the water level in the lake was lowered starting in 1941
Tufa towers rise from Mono Lake, with the Eastern Sierra visible in the distance. Tufa towers are formed when underwater springs rich in calcium mix with lakewater rich in carbonates, forming calcium carbonate (limestone) structures below the surface of the lake. The towers were eventually revealed when the water level in the lake was lowered starting in 1941.
Location: Mono Lake, California
Image ID: 26992  
Tufa towers rise from Mono Lake, with the Eastern Sierra visible in the distance. Tufa towers are formed when underwater springs rich in calcium mix with lakewater rich in carbonates, forming calcium carbonate (limestone) structures below the surface of the lake. The towers were eventually revealed when the water level in the lake was lowered starting in 1941
Tufa towers rise from Mono Lake, with the Eastern Sierra visible in the distance. Tufa towers are formed when underwater springs rich in calcium mix with lakewater rich in carbonates, forming calcium carbonate (limestone) structures below the surface of the lake. The towers were eventually revealed when the water level in the lake was lowered starting in 1941.
Location: Mono Lake, California
Image ID: 26993  
Lee Vining Canyon and the Sierra Nevada mountain range, with storm clouds and sun beams, viewed from Mono Lake
Lee Vining Canyon and the Sierra Nevada mountain range, with storm clouds and sun beams, viewed from Mono Lake.
Location: Mono Lake, California
Image ID: 27002  
Tufa towers rise from Mono Lake, with the Eastern Sierra visible in the distance. Tufa towers are formed when underwater springs rich in calcium mix with lakewater rich in carbonates, forming calcium carbonate (limestone) structures below the surface of the lake. The towers were eventually revealed when the water level in the lake was lowered starting in 1941
Tufa towers rise from Mono Lake, with the Eastern Sierra visible in the distance. Tufa towers are formed when underwater springs rich in calcium mix with lakewater rich in carbonates, forming calcium carbonate (limestone) structures below the surface of the lake. The towers were eventually revealed when the water level in the lake was lowered starting in 1941.
Location: Mono Lake, California
Image ID: 27003  
Mono Lake sunset, tufa and clouds reflected in the still waters of Mono Lake
Mono Lake sunset, tufa and clouds reflected in the still waters of Mono Lake.
Location: Mono Lake, California
Image ID: 27004  
Tufa towers rise from Mono Lake. Tufa towers are formed when underwater springs rich in calcium mix with lakewater rich in carbonates, forming calcium carbonate (limestone) structures below the surface of the lake. The towers were eventually revealed when the water level in the lake was lowered starting in 1941. South tufa grove, Navy Beach
Tufa towers rise from Mono Lake. Tufa towers are formed when underwater springs rich in calcium mix with lakewater rich in carbonates, forming calcium carbonate (limestone) structures below the surface of the lake. The towers were eventually revealed when the water level in the lake was lowered starting in 1941. South tufa grove, Navy Beach.
Location: Mono Lake, California
Image ID: 09929  
Tufa towers rise from Mono Lake with the Eastern Sierra visible in the distance. Tufa towers are formed when underwater springs rich in calcium mix with lakewater rich in carbonates, forming calcium carbonate (limestone) structures below the surface of the lake. The towers were eventually revealed when the water level in the lake was lowered starting in 1941. South tufa grove, Navy Beach
Tufa towers rise from Mono Lake with the Eastern Sierra visible in the distance. Tufa towers are formed when underwater springs rich in calcium mix with lakewater rich in carbonates, forming calcium carbonate (limestone) structures below the surface of the lake. The towers were eventually revealed when the water level in the lake was lowered starting in 1941. South tufa grove, Navy Beach.
Location: Mono Lake, California
Image ID: 09932  
Tufa towers rise from Mono Lake with the Eastern Sierra visible in the distance. Tufa towers are formed when underwater springs rich in calcium mix with lakewater rich in carbonates, forming calcium carbonate (limestone) structures below the surface of the lake. The towers were eventually revealed when the water level in the lake was lowered starting in 1941. South tufa grove, Navy Beach
Tufa towers rise from Mono Lake with the Eastern Sierra visible in the distance. Tufa towers are formed when underwater springs rich in calcium mix with lakewater rich in carbonates, forming calcium carbonate (limestone) structures below the surface of the lake. The towers were eventually revealed when the water level in the lake was lowered starting in 1941. South tufa grove, Navy Beach.
Location: Mono Lake, California
Image ID: 09937  
Tufa towers rise from Mono Lake. Tufa towers are formed when underwater springs rich in calcium mix with lakewater rich in carbonates, forming calcium carbonate (limestone) structures below the surface of the lake. The towers were eventually revealed when the water level in the lake was lowered starting in 1941. South tufa grove, Navy Beach
Tufa towers rise from Mono Lake. Tufa towers are formed when underwater springs rich in calcium mix with lakewater rich in carbonates, forming calcium carbonate (limestone) structures below the surface of the lake. The towers were eventually revealed when the water level in the lake was lowered starting in 1941. South tufa grove, Navy Beach.
Location: Mono Lake, California
Image ID: 23173  
Tufa towers rise from Mono Lake. Tufa towers are formed when underwater springs rich in calcium mix with lakewater rich in carbonates, forming calcium carbonate (limestone) structures below the surface of the lake. The towers were eventually revealed when the water level in the lake was lowered starting in 1941. South tufa grove, Navy Beach
Tufa towers rise from Mono Lake. Tufa towers are formed when underwater springs rich in calcium mix with lakewater rich in carbonates, forming calcium carbonate (limestone) structures below the surface of the lake. The towers were eventually revealed when the water level in the lake was lowered starting in 1941. South tufa grove, Navy Beach.
Location: Mono Lake, California
Image ID: 23174  
Tufa towers rise from Mono Lake. Tufa towers are formed when underwater springs rich in calcium mix with lakewater rich in carbonates, forming calcium carbonate (limestone) structures below the surface of the lake. The towers were eventually revealed when the water level in the lake was lowered starting in 1941. South tufa grove, Navy Beach
Tufa towers rise from Mono Lake. Tufa towers are formed when underwater springs rich in calcium mix with lakewater rich in carbonates, forming calcium carbonate (limestone) structures below the surface of the lake. The towers were eventually revealed when the water level in the lake was lowered starting in 1941. South tufa grove, Navy Beach.
Location: Mono Lake, California
Image ID: 09926  
Tufa towers rise from Mono Lake. Tufa towers are formed when underwater springs rich in calcium mix with lakewater rich in carbonates, forming calcium carbonate (limestone) structures below the surface of the lake. The towers were eventually revealed when the water level in the lake was lowered starting in 1941. South tufa grove, Navy Beach
Tufa towers rise from Mono Lake. Tufa towers are formed when underwater springs rich in calcium mix with lakewater rich in carbonates, forming calcium carbonate (limestone) structures below the surface of the lake. The towers were eventually revealed when the water level in the lake was lowered starting in 1941. South tufa grove, Navy Beach.
Location: Mono Lake, California
Image ID: 09927  
Tufa towers rise from Mono Lake. Tufa towers are formed when underwater springs rich in calcium mix with lakewater rich in carbonates, forming calcium carbonate (limestone) structures below the surface of the lake. The towers were eventually revealed when the water level in the lake was lowered starting in 1941. South tufa grove, Navy Beach
Tufa towers rise from Mono Lake. Tufa towers are formed when underwater springs rich in calcium mix with lakewater rich in carbonates, forming calcium carbonate (limestone) structures below the surface of the lake. The towers were eventually revealed when the water level in the lake was lowered starting in 1941. South tufa grove, Navy Beach.
Location: Mono Lake, California
Image ID: 09928  
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