Lake Mono Photo
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Mono Lake sunset, tufa and 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 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
Mono Lake sunset, tufa and clouds reflected in the still waters of Mono Lake. Lake Mono Photo.
Image ID: 26977  
Location: Mono Lake, California, USA
 		 Mono Lake sunset, Sierra Nevada mountain range and tufas, clouds reflected in the still waters of Mono Lake. Lake Mono Picture.
Image ID: 26978  
Location: Mono Lake, California, USA
 		 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. Stock Photography of Lake Mono.
Image ID: 23225  
Location: Yosemite National Park, California, USA
 
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. Photograph of Lake Mono.
Image ID: 26968  
Location: Mono Lake, California, USA
Pano dimensions: 5331 x 14966
 
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 Mono Lake sunset, tufa and clouds reflected in the still waters of Mono Lake This photo is the top of a stack of similar images, click to see them all. 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 Lake Mono Photos.
Image ID: 26983  
Location: Mono Lake, California, USA
 		 Mono Lake sunset, tufa and clouds reflected in the still waters of Mono Lake. Lake Mono Image.
Image ID: 27005  
Location: Mono Lake, California, USA
 		 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 Professional stock photos of Lake Mono.
Image ID: 26991  
Location: Mono Lake, California, USA
 
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. Pictures of Lake Mono.
Image ID: 26967  
Location: Mono Lake, California, USA
Pano dimensions: 4835 x 12178
 
Mono Lake sunset, Sierra Nevada mountain range and tufas, clouds reflected in the still waters of Mono Lake 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
Mono Lake sunset, Sierra Nevada mountain range and tufas, clouds reflected in the still waters of Mono Lake. Lake Mono Photo.
Image ID: 26969  
Location: Mono Lake, California, USA
Pano 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 Lake Mono Picture.
Image ID: 26992  
Location: Mono Lake, California, USA
 		 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 Stock Photography of Lake Mono.
Image ID: 26993  
Location: Mono Lake, California, USA
 
Lee Vining Canyon and the Sierra Nevada mountain range, with storm clouds and sun beams, viewed from Mono Lake 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. 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
Lee Vining Canyon and the Sierra Nevada mountain range, with storm clouds and sun beams, viewed from Mono Lake. Photograph of Lake Mono.
Image ID: 27002  
Location: Mono Lake, California, USA
 		 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 Lake Mono Photos.
Image ID: 27003  
Location: Mono Lake, California, USA
 		 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. Lake Mono Image.
Image ID: 09929  
Location: Mono Lake, California, USA
 
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 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 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. Professional stock photos of Lake Mono.
Image ID: 09932  
Location: Mono Lake, California, USA
 		 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. Pictures of Lake Mono.
Image ID: 09937  
Location: Mono Lake, California, USA
 		 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. Lake Mono Photo.
Image ID: 23173  
Location: Mono Lake, California, USA
 
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 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. Lake Mono Picture.
Image ID: 23174  
Location: Mono Lake, California, USA
 		 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. Stock Photography of Lake Mono.
Image ID: 09926  
Location: Mono Lake, California, USA
 		 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. Photograph of Lake Mono.
Image ID: 09927  
Location: Mono Lake, California, USA
 
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 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. Lake Mono Photos.
Image ID: 09928  
Location: Mono Lake, California, USA
 		 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. Lake Mono Image.
Image ID: 09930  
Location: Mono Lake, California, USA
 		 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. Professional stock photos of Lake Mono.
Image ID: 09931  
Location: Mono Lake, California, USA
 
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 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. Pictures of Lake Mono.
Image ID: 09933  
Location: Mono Lake, California, USA
 		 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. Lake Mono Photo.
Image ID: 09934  
Location: Mono Lake, California, USA
 		 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. Lake Mono Picture.
Image ID: 09935  
Location: Mono Lake, California, USA
 
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. Stock Photography of Lake Mono.
Image ID: 09936  
Location: Mono Lake, California, USA
 

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Updated: February 10, 2012