Search results for Calcium Carbonate

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Dendronephthya soft coral detail including polyps and calcium carbonate spicules, Fiji, Dendronephthya, Namena Marine Reserve, Namena Island
Dendronephthya soft coral detail including polyps and calcium carbonate spicules, Fiji.
Species: Dendronephthya soft coral, Dendronephthya
Location: Namena Marine Reserve, Namena Island, Fiji
Image ID: 35008  
Dendronephthya soft coral detail including polyps and calcium carbonate spicules, Fiji, Dendronephthya, Namena Marine Reserve, Namena Island
Dendronephthya soft coral detail including polyps and calcium carbonate spicules, Fiji.
Species: Dendronephthya soft coral, Dendronephthya
Location: Namena Marine Reserve, Namena Island, Fiji
Image ID: 35009  
Coral reefscape in Fiji. Stony corals, such as the various species in this image, grow a calcium carbonate skeleton which they leave behind when they die. Over years, this deposit of calcium carbonate builds up the foundation of the coral reef. Fiji, Vatu I Ra Passage, Bligh Waters, Viti Levu  Island
Coral reefscape in Fiji. Stony corals, such as the various species in this image, grow a calcium carbonate skeleton which they leave behind when they die. Over years, this deposit of calcium carbonate builds up the foundation of the coral reef. Fiji.
Location: Vatu I Ra Passage, Bligh Waters, Viti Levu Island, Fiji
Image ID: 31706  
Coral reefscape in Fiji. Stony corals, such as the various species in this image, grow a calcium carbonate skeleton which they leave behind when they die. Over years, this deposit of calcium carbonate builds up the foundation of the coral reef. Fiji, Vatu I Ra Passage, Bligh Waters, Viti Levu  Island
Coral reefscape in Fiji. Stony corals, such as the various species in this image, grow a calcium carbonate skeleton which they leave behind when they die. Over years, this deposit of calcium carbonate builds up the foundation of the coral reef. Fiji.
Location: Vatu I Ra Passage, Bligh Waters, Viti Levu Island, Fiji
Image ID: 31707  
Dendronephthya soft coral detail including polyps and calcium carbonate spicules, Fiji, Dendronephthya, Makogai Island, Lomaiviti Archipelago
Dendronephthya soft coral detail including polyps and calcium carbonate spicules, Fiji.
Species: Dendronephthya soft coral, Dendronephthya
Location: Makogai Island, Lomaiviti Archipelago, Fiji
Image ID: 31782  
Dendronephthya soft coral detail including polyps and calcium carbonate spicules, Fiji, Dendronephthya, Makogai Island, Lomaiviti Archipelago
Dendronephthya soft coral detail including polyps and calcium carbonate spicules, Fiji.
Species: Dendronephthya soft coral, Dendronephthya
Location: Makogai Island, Lomaiviti Archipelago, Fiji
Image ID: 31784  
Dendronephthya soft coral detail including polyps and calcium carbonate spicules, Fiji, Dendronephthya, Makogai Island, Lomaiviti Archipelago
Dendronephthya soft coral detail including polyps and calcium carbonate spicules, Fiji.
Species: Dendronephthya soft coral, Dendronephthya
Location: Makogai Island, Lomaiviti Archipelago, Fiji
Image ID: 31788  
Dendronephthya soft coral detail including polyps and calcium carbonate spicules, Fiji, Dendronephthya, Makogai Island, Lomaiviti Archipelago
Dendronephthya soft coral detail including polyps and calcium carbonate spicules, Fiji.
Species: Dendronephthya soft coral, Dendronephthya
Location: Makogai Island, Lomaiviti Archipelago, Fiji
Image ID: 31789  
Dendronephthya soft coral detail including polyps and calcium carbonate spicules, Fiji, Dendronephthya, Makogai Island, Lomaiviti Archipelago
Dendronephthya soft coral detail including polyps and calcium carbonate spicules, Fiji.
Species: Dendronephthya soft coral, Dendronephthya
Location: Makogai Island, Lomaiviti Archipelago, Fiji
Image ID: 31790  
Dendronephthya soft coral detail including polyps and calcium carbonate spicules, Fiji, Dendronephthya, Makogai Island, Lomaiviti Archipelago
Dendronephthya soft coral detail including polyps and calcium carbonate spicules, Fiji.
Species: Dendronephthya soft coral, Dendronephthya
Location: Makogai Island, Lomaiviti Archipelago, Fiji
Image ID: 31797  
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.
Location: Mono Lake, California
Image ID: 26983  
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.
Location: Mono Lake, California
Image ID: 26991  
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.
Location: Mono Lake, California
Image ID: 26992  
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.
Location: Mono Lake, California
Image ID: 26993  
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.
Location: Mono Lake, California
Image ID: 27003  
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: 09929  
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: 09932  
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: 09937  
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: 23173  
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: 23174  
Soda Butte. This travertine (calcium carbonate) mound was formed more than a century ago by a hot spring. Only small amounts of hydrothermal water and hydrogen sulfide gas currently flow from this once more prolific spring, Yellowstone National Park, Wyoming
Soda Butte. This travertine (calcium carbonate) mound was formed more than a century ago by a hot spring. Only small amounts of hydrothermal water and hydrogen sulfide gas currently flow from this once more prolific spring.
Location: Yellowstone National Park, Wyoming
Image ID: 13642  
Soda Butte. This travertine (calcium carbonate) mound was formed more than a century ago by a hot spring. Only small amounts of hydrothermal water and hydrogen sulfide gas currently flow from this once more prolific spring, Yellowstone National Park, Wyoming
Soda Butte. This travertine (calcium carbonate) mound was formed more than a century ago by a hot spring. Only small amounts of hydrothermal water and hydrogen sulfide gas currently flow from this once more prolific spring.
Location: Yellowstone National Park, Wyoming
Image ID: 13643  
Soda Butte. This travertine (calcium carbonate) mound was formed more than a century ago by a hot spring. Only small amounts of hydrothermal water and hydrogen sulfide gas currently flow from this once more prolific spring, Yellowstone National Park, Wyoming
Soda Butte. This travertine (calcium carbonate) mound was formed more than a century ago by a hot spring. Only small amounts of hydrothermal water and hydrogen sulfide gas currently flow from this once more prolific spring.
Location: Yellowstone National Park, Wyoming
Image ID: 13644  
Soda Butte. This travertine (calcium carbonate) mound was formed more than a century ago by a hot spring. Only small amounts of hydrothermal water and hydrogen sulfide gas currently flow from this once more prolific spring, Yellowstone National Park, Wyoming
Soda Butte. This travertine (calcium carbonate) mound was formed more than a century ago by a hot spring. Only small amounts of hydrothermal water and hydrogen sulfide gas currently flow from this once more prolific spring.
Location: Yellowstone National Park, Wyoming
Image ID: 13645  
Soda Butte. This travertine (calcium carbonate) mound was formed more than a century ago by a hot spring. Only small amounts of hydrothermal water and hydrogen sulfide gas currently flow from this once more prolific spring, Yellowstone National Park, Wyoming
Soda Butte. This travertine (calcium carbonate) mound was formed more than a century ago by a hot spring. Only small amounts of hydrothermal water and hydrogen sulfide gas currently flow from this once more prolific spring.
Location: Yellowstone National Park, Wyoming
Image ID: 13646  
Dead trees embedded in calcium carbonate deposits in the travertine terraces of Mammoth Hot Springs, near Minerva terrace .  Over two tons of calcium carbonate (in solution) is deposited each day on the terraces, gradually killing any vegetation that had managed to be growing, Yellowstone National Park, Wyoming
Dead trees embedded in calcium carbonate deposits in the travertine terraces of Mammoth Hot Springs, near Minerva terrace . Over two tons of calcium carbonate (in solution) is deposited each day on the terraces, gradually killing any vegetation that had managed to be growing.
Location: Mammoth Hot Springs, Yellowstone National Park, Wyoming
Image ID: 19795  
Dead trees embedded in calcium carbonate deposits in the travertine terraces of Mammoth Hot Springs, near Minerva terrace .  Over two tons of calcium carbonate (in solution) is deposited each day on the terraces, gradually killing any vegetation that had managed to be growing, Yellowstone National Park, Wyoming
Dead trees embedded in calcium carbonate deposits in the travertine terraces of Mammoth Hot Springs, near Minerva terrace . Over two tons of calcium carbonate (in solution) is deposited each day on the terraces, gradually killing any vegetation that had managed to be growing.
Location: Mammoth Hot Springs, Yellowstone National Park, Wyoming
Image ID: 19796  
Dead trees embedded in calcium carbonate deposits in the travertine terraces of Mammoth Hot Springs, near Minerva terrace .  Over two tons of calcium carbonate (in solution) is deposited each day on the terraces, gradually killing any vegetation that had managed to be growing, Yellowstone National Park, Wyoming
Dead trees embedded in calcium carbonate deposits in the travertine terraces of Mammoth Hot Springs, near Minerva terrace . Over two tons of calcium carbonate (in solution) is deposited each day on the terraces, gradually killing any vegetation that had managed to be growing.
Location: Mammoth Hot Springs, Yellowstone National Park, Wyoming
Image ID: 19797  
Dead trees embedded in calcium carbonate deposits in the travertine terraces of Mammoth Hot Springs, near Minerva terrace .  Over two tons of calcium carbonate (in solution) is deposited each day on the terraces, gradually killing any vegetation that had managed to be growing, Yellowstone National Park, Wyoming
Dead trees embedded in calcium carbonate deposits in the travertine terraces of Mammoth Hot Springs, near Minerva terrace . Over two tons of calcium carbonate (in solution) is deposited each day on the terraces, gradually killing any vegetation that had managed to be growing.
Location: Mammoth Hot Springs, Yellowstone National Park, Wyoming
Image ID: 19798  
Travertine terrace detail, calcium carbonate, Minerva's terraces, Mammoth Hot Springs, Yellowstone National Park, Wyoming
Travertine terrace detail, calcium carbonate, Minerva's terraces.
Location: Mammoth Hot Springs, Yellowstone National Park, Wyoming
Image ID: 19799  
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