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Wave and backwash spray, La Jolla, California Add To Light Table Ugly wave, the Wedge, The Wedge, Newport Beach, California Add To Light Table Breaking wave, Moonlight Beach, Encinitas, California Add To Light Table
Wave and backwash spray.
Image ID: 18286  
Location: La Jolla, California, USA
 
Ugly wave, the Wedge.
Image ID: 18712  
Location: The Wedge, Newport Beach, California, USA
 
Breaking wave.
Image ID: 19131  
Location: Moonlight Beach, Encinitas, California, USA
 
Breaking wave, Moonlight Beach, Encinitas, California Add To Light Table Breaking wave, Moonlight Beach, Encinitas, California Add To Light Table Breaking wave, South Carlsbad State Beach, Ponto, morning, winter Add To Light Table
Breaking wave.
Image ID: 19132  
Location: Moonlight Beach, Encinitas, California, USA
 
Breaking wave.
Image ID: 19133  
Location: Moonlight Beach, Encinitas, California, USA
 
Breaking wave, South Carlsbad State Beach, Ponto, morning, winter.
Image ID: 14789  
Location: Ponto, Carlsbad, California, USA
 
Breaking wave, South Carlsbad State Beach, Ponto, morning, winter Add To Light Table The Wedge, overcast day, Newport Beach, California Add To Light Table Breaking wave, the Wedge, The Wedge, Newport Beach, California Add To Light Table
Breaking wave, South Carlsbad State Beach, Ponto, morning, winter.
Image ID: 14790  
Location: Ponto, Carlsbad, California, USA
 
The Wedge, overcast day.
Image ID: 16930  
Location: The Wedge, Newport Beach, California, USA
 
Breaking wave, the Wedge.
Image ID: 17023  
Location: The Wedge, Newport Beach, 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
 


Natural History Photography Blog posts (20) related to Beach Spring



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Categories Appearing Among These Images:
Animal  >  Bird  >  Eagle (Accipitridae)  >  Bald Eagle
Gallery  >  California
Gallery  >  Carlsbad
Gallery  >  Icon
Gallery  >  Landscape
Gallery  >  Man And Ocean
Gallery  >  Ocean And Light
Gallery  >  Ocean And Motion
Gallery  >  San Diego
Gallery  >  Sierra Nevada
Gallery  >  Waves
Location  >  Protected Threatened and Significant Places  >  Ecological Reserves  >  Bolsa Chica State Ecological Reserve
Location  >  Protected Threatened and Significant Places  >  National Parks  >  Yellowstone National Park (Wyoming)  >  Geothermal Features  >  Spring  >  Beach Spring
Location  >  Protected Threatened and Significant Places  >  World Heritage Sites  >  Yellowstone National Park (USA)
Location  >  USA  >  Alaska  >  Homer
Location  >  USA  >  California  >  Carlsbad
Location  >  USA  >  California  >  Huntington Beach
Location  >  USA  >  California  >  Mono Lake
Location  >  USA  >  California  >  Newport Beach  >  The Wedge
Location  >  USA  >  Wyoming  >  Yellowstone National Park
Natural World  >  Geothermal Features  >  Spring
Natural World  >  Habitat  >  Saline Lake
Natural World  >  Wave
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Species Appearing Among These Images:
Haliaeetus leucocephalus
Haliaeetus leucocephalus washingtoniensis
Pandion haliaetus

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Updated: August 15, 2020