 |
 |
  |
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 and Stars at Night, Milky Way galaxy.
Image ID: 28519
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.
Image ID: 26968
Location: Mono Lake, California, USA
Pano dimensions: 5331 x 14966 |
 |
 |
  |
Tufa and Stars at Night, Milky Way galaxy.
Image ID: 28509
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 | Mono Lake sunset, tufa and clouds reflected in the still waters of Mono Lake.
Image ID: 27005
Location: Mono Lake, California, USA |
 |
  |
 |
Mono Lake Tufa at Sunset.
Image ID: 31072
Location: Mono Lake, California, USA | Tufa and Stars at Night, Milky Way galaxy.
Image ID: 28517
Location: Mono Lake, California, USA | Tufa and Stars at Night, Milky Way galaxy.
Image ID: 28507
Location: Mono Lake, California, USA |
 |
 |
 |
Tufa and Stars at Night, Milky Way galaxy.
Image ID: 28508
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.
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.
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 | Lee Vining Canyon and the Sierra Nevada mountain range, with storm clouds and sun beams, viewed from Mono Lake.
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.
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.
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.
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.
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.
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.
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.
Image ID: 09934
Location: Mono Lake, California, USA |