Search results for Mono Lake

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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: 09930  
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: 09931  
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: 09933  
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: 09934  
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: 09935  
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: 09936  
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