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Mono Lake sunset, tufa and clouds reflected in the still waters of Mono Lake Add To Light Table Mono Lake sunset, Sierra Nevada mountain range and tufas, clouds reflected in the still waters of Mono Lake Add To Light Table 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 Add To Light Table
Mono Lake sunset, tufa and clouds reflected in the still waters of Mono Lake.
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.
Image ID: 26978  
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.
Image ID: 26983  
Location: Mono Lake, California, USA
 
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 Add To Light Table
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.
Image ID: 26968  
Location: Mono Lake, California, USA
Pano dimensions: 5331 x 14966
 
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.Add To Light Table 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 Add To Light Table 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 Add To Light Table
Mono Lake sunset, tufa and clouds reflected in the still waters of Mono Lake.
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.
Image ID: 26991  
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.
Image ID: 26992  
Location: Mono Lake, California, USA
 
Mono Lake sunset, Sierra Nevada mountain range and tufas, clouds reflected in the still waters of Mono Lake Add To Light Table
Mono Lake sunset, Sierra Nevada mountain range and tufas, clouds reflected in the still waters of Mono Lake.
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 Add To Light Table 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 Add To Light Table 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 Add To Light Table
Mono Lake sunset, Sierra Nevada mountain range and tufas, clouds reflected in the still waters of Mono Lake.
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.
Image ID: 26993  
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.
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 Add To Light Table 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 Add To Light Table 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 Add To Light Table
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.
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.
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.
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 Add To Light Table 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 Add To Light Table 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 Add To Light Table
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.
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.
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.
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 Add To Light Table 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 Add To Light Table 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 Add To Light Table
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.
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.
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.
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 Add To Light Table 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 Add To Light Table 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 Add To Light Table
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.
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.
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.
Image ID: 09936  
Location: Mono Lake, California, USA
 

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Updated: March 30, 2020