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volcanologist on Piton de la Fournaise in activity, Volcano eruption 16 of september 2016, Reunionvolcanologist on Piton de la Fournaise in activity, Volcano eruption 16 of september 2016, Reunionvolcanologist on Piton de la Fournaise in activity, Volcano eruption 16 of september 2016, Reunion© Gabriel Barathieu / BiosphotoJPG - RM

2090991

volcanologist on Piton de la Fournaise in activity, Volcano

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Piton de la Fournaise in activity, Volcano eruption 13 of september 2016, ReunionPiton de la Fournaise in activity, Volcano eruption 13 of september 2016, ReunionPiton de la Fournaise in activity, Volcano eruption 13 of september 2016, Reunion© Gabriel Barathieu / BiosphotoJPG - RM

2090985

Piton de la Fournaise in activity, Volcano eruption 13 of

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Piton de la Fournaise in activity under the milky way, Volcano eruption 11 of september 2016, ReunionPiton de la Fournaise in activity under the milky way, Volcano eruption 11 of september 2016, ReunionPiton de la Fournaise in activity under the milky way, Volcano eruption 11 of september 2016, Reunion© Gabriel Barathieu / BiosphotoJPG - RM

2090973

Piton de la Fournaise in activity under the milky way, Volcano

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Piton de la Fournaise in activity, Volcano eruption of July 31, 2015, ReunionPiton de la Fournaise in activity, Volcano eruption of July 31, 2015, ReunionPiton de la Fournaise in activity, Volcano eruption of July 31, 2015, Reunion© Gabriel Barathieu / BiosphotoJPG - RM

2090962

Piton de la Fournaise in activity, Volcano eruption of July 31,

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Recent corded lavas on the island of El Herrio, in the Canaries. Pahoehoe type basalts (fluids) - El Lajial - Restinga region - El Herrio is a recent volcanic island and part of the network of European Geoparks - Canary IslandsRecent corded lavas on the island of El Herrio, in the Canaries. Pahoehoe type basalts (fluids) - El Lajial - Restinga region - El Herrio is a recent volcanic island and part of the network of European Geoparks - Canary IslandsRecent corded lavas on the island of El Herrio, in the Canaries. Pahoehoe type basalts (fluids) - El Lajial - Restinga region - El Herrio is a recent volcanic island and part of the network of European Geoparks - Canary Islands© Jean-Philippe Delobelle / BiosphotoJPG - RM

2447425

Recent corded lavas on the island of El Herrio, in the Canaries.

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Recent corded lavas on the island of El Herrio, in the Canaries. Pahoehoe type basalts (fluids) - El Lajial - Restinga region - El Herrio is a recent volcanic island and part of the network of European Geoparks - Canary IslandsRecent corded lavas on the island of El Herrio, in the Canaries. Pahoehoe type basalts (fluids) - El Lajial - Restinga region - El Herrio is a recent volcanic island and part of the network of European Geoparks - Canary IslandsRecent corded lavas on the island of El Herrio, in the Canaries. Pahoehoe type basalts (fluids) - El Lajial - Restinga region - El Herrio is a recent volcanic island and part of the network of European Geoparks - Canary Islands© Jean-Philippe Delobelle / BiosphotoJPG - RM

2447424

Recent corded lavas on the island of El Herrio, in the Canaries.

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Recent corded lavas on the island of El Herrio, in the Canaries. Pahoehoe type basalts (fluids) - El Lajial - Restinga region - El Herrio is a recent volcanic island and part of the network of European Geoparks - Canary IslandsRecent corded lavas on the island of El Herrio, in the Canaries. Pahoehoe type basalts (fluids) - El Lajial - Restinga region - El Herrio is a recent volcanic island and part of the network of European Geoparks - Canary IslandsRecent corded lavas on the island of El Herrio, in the Canaries. Pahoehoe type basalts (fluids) - El Lajial - Restinga region - El Herrio is a recent volcanic island and part of the network of European Geoparks - Canary Islands© Jean-Philippe Delobelle / BiosphotoJPG - RM

2447418

Recent corded lavas on the island of El Herrio, in the Canaries.

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Bejeques (Aeonium aureum) on the island of El Herrio in the Canaries. Aeonium aureum, spectacular species colonizing the humid, cool and not very sunny cliffs of the Canary Islands, in association with lichens (stereocaulon) and ferns.Bejeques (Aeonium aureum) on the island of El Herrio in the Canaries. Aeonium aureum, spectacular species colonizing the humid, cool and not very sunny cliffs of the Canary Islands, in association with lichens (stereocaulon) and ferns.Bejeques (Aeonium aureum) on the island of El Herrio in the Canaries. Aeonium aureum, spectacular species colonizing the humid, cool and not very sunny cliffs of the Canary Islands, in association with lichens (stereocaulon) and ferns.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2447413

Bejeques (Aeonium aureum) on the island of El Herrio in the

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Bejeques (Aeonium aureum) on the island of El Herrio in the Canaries. Aeonium aureum, spectacular species colonizing the humid, cool and not very sunny cliffs of the Canary Islands, in association with lichens (stereocaulon) and ferns.Bejeques (Aeonium aureum) on the island of El Herrio in the Canaries. Aeonium aureum, spectacular species colonizing the humid, cool and not very sunny cliffs of the Canary Islands, in association with lichens (stereocaulon) and ferns.Bejeques (Aeonium aureum) on the island of El Herrio in the Canaries. Aeonium aureum, spectacular species colonizing the humid, cool and not very sunny cliffs of the Canary Islands, in association with lichens (stereocaulon) and ferns.© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Bejeques (Aeonium aureum) on the island of El Herrio in the

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Canary pines and sea of clouds on the island of Tenerife. Canary Island pine (Pinus canariensis) is a magnificent endemic species of the archipelago, very resistant to fire and colonizing bare volcanic soils, like here basalt flows of the Teide - The northeast trade winds regularly cause the formation of a dense sea of cloud on the slopes of Teide, strato volcano on the island of Tenerife, in the Canary Islands.Canary pines and sea of clouds on the island of Tenerife. Canary Island pine (Pinus canariensis) is a magnificent endemic species of the archipelago, very resistant to fire and colonizing bare volcanic soils, like here basalt flows of the Teide - The northeast trade winds regularly cause the formation of a dense sea of cloud on the slopes of Teide, strato volcano on the island of Tenerife, in the Canary Islands.Canary pines and sea of clouds on the island of Tenerife. Canary Island pine (Pinus canariensis) is a magnificent endemic species of the archipelago, very resistant to fire and colonizing bare volcanic soils, like here basalt flows of the Teide - The northeast trade winds regularly cause the formation of a dense sea of cloud on the slopes of Teide, strato volcano on the island of Tenerife, in the Canary Islands.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2447349

Canary pines and sea of clouds on the island of Tenerife. Canary

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Washed strings in the caldera of las Cañadas del Teide. Teide is a huge volcano strato on the island of Tenerife, in the Canary Islands. It measures 3718 m above the ocean, but almost 7000 m from its base on the ocean floor, making it the 3rd known volcanic structure. It comes from the activity of a hot spot that formed the Canary archipelago during the displacement of the African plate.Washed strings in the caldera of las Cañadas del Teide. Teide is a huge volcano strato on the island of Tenerife, in the Canary Islands. It measures 3718 m above the ocean, but almost 7000 m from its base on the ocean floor, making it the 3rd known volcanic structure. It comes from the activity of a hot spot that formed the Canary archipelago during the displacement of the African plate.Washed strings in the caldera of las Cañadas del Teide. Teide is a huge volcano strato on the island of Tenerife, in the Canary Islands. It measures 3718 m above the ocean, but almost 7000 m from its base on the ocean floor, making it the 3rd known volcanic structure. It comes from the activity of a hot spot that formed the Canary archipelago during the displacement of the African plate.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2447348

Washed strings in the caldera of las Cañadas del Teide. Teide is

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Washed strings in the caldera of las Cañadas del Teide. Teide is a huge volcano strato on the island of Tenerife, in the Canary Islands. It measures 3718 m above the ocean, but almost 7000 m from its base on the ocean floor, making it the 3rd known volcanic structure. It comes from the activity of a hot spot that formed the Canary archipelago during the displacement of the African plate.Washed strings in the caldera of las Cañadas del Teide. Teide is a huge volcano strato on the island of Tenerife, in the Canary Islands. It measures 3718 m above the ocean, but almost 7000 m from its base on the ocean floor, making it the 3rd known volcanic structure. It comes from the activity of a hot spot that formed the Canary archipelago during the displacement of the African plate.Washed strings in the caldera of las Cañadas del Teide. Teide is a huge volcano strato on the island of Tenerife, in the Canary Islands. It measures 3718 m above the ocean, but almost 7000 m from its base on the ocean floor, making it the 3rd known volcanic structure. It comes from the activity of a hot spot that formed the Canary archipelago during the displacement of the African plate.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2447347

Washed strings in the caldera of las Cañadas del Teide. Teide is

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Washed strings in the caldera of las Cañadas del Teide. Teide is a huge volcano strato on the island of Tenerife, in the Canary Islands. It measures 3718 m above the ocean, but almost 7000 m from its base on the ocean floor, making it the 3rd known volcanic structure. It comes from the activity of a hot spot that formed the Canary archipelago during the displacement of the African plate.Washed strings in the caldera of las Cañadas del Teide. Teide is a huge volcano strato on the island of Tenerife, in the Canary Islands. It measures 3718 m above the ocean, but almost 7000 m from its base on the ocean floor, making it the 3rd known volcanic structure. It comes from the activity of a hot spot that formed the Canary archipelago during the displacement of the African plate.Washed strings in the caldera of las Cañadas del Teide. Teide is a huge volcano strato on the island of Tenerife, in the Canary Islands. It measures 3718 m above the ocean, but almost 7000 m from its base on the ocean floor, making it the 3rd known volcanic structure. It comes from the activity of a hot spot that formed the Canary archipelago during the displacement of the African plate.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2447346

Washed strings in the caldera of las Cañadas del Teide. Teide is

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Black lavas rich in obsidian on the sides of Teide. Teide is a huge volcano strato on the island of Tenerife, in the Canary Islands. It measures 3718 m above the ocean, but almost 7000 m from its base on the ocean floor, making it the 3rd known volcanic structure. It comes from the activity of a hot spot that formed the Canary archipelago during the displacement of the African plate.Black lavas rich in obsidian on the sides of Teide. Teide is a huge volcano strato on the island of Tenerife, in the Canary Islands. It measures 3718 m above the ocean, but almost 7000 m from its base on the ocean floor, making it the 3rd known volcanic structure. It comes from the activity of a hot spot that formed the Canary archipelago during the displacement of the African plate.Black lavas rich in obsidian on the sides of Teide. Teide is a huge volcano strato on the island of Tenerife, in the Canary Islands. It measures 3718 m above the ocean, but almost 7000 m from its base on the ocean floor, making it the 3rd known volcanic structure. It comes from the activity of a hot spot that formed the Canary archipelago during the displacement of the African plate.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2447344

Black lavas rich in obsidian on the sides of Teide. Teide is a

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Canary pines and sea of clouds on the island of Tenerife. Canary Island pine (Pinus canariensis) is a magnificent endemic species of the archipelago, very resistant to fire and colonizing bare volcanic soils, like here basalt flows of the Teide - The northeast trade winds regularly cause the formation of a dense sea of cloud on the slopes of Teide, strato volcano on the island of Tenerife, in the Canary Islands.Canary pines and sea of clouds on the island of Tenerife. Canary Island pine (Pinus canariensis) is a magnificent endemic species of the archipelago, very resistant to fire and colonizing bare volcanic soils, like here basalt flows of the Teide - The northeast trade winds regularly cause the formation of a dense sea of cloud on the slopes of Teide, strato volcano on the island of Tenerife, in the Canary Islands.Canary pines and sea of clouds on the island of Tenerife. Canary Island pine (Pinus canariensis) is a magnificent endemic species of the archipelago, very resistant to fire and colonizing bare volcanic soils, like here basalt flows of the Teide - The northeast trade winds regularly cause the formation of a dense sea of cloud on the slopes of Teide, strato volcano on the island of Tenerife, in the Canary Islands.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2447337

Canary pines and sea of clouds on the island of Tenerife. Canary

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Canary pines and sea of clouds on the island of Tenerife. Canary Island pine (Pinus canariensis) is a magnificent endemic species of the archipelago, very resistant to fire and colonizing bare volcanic soils, like here basalt flows of the Teide - The northeast trade winds regularly cause the formation of a dense sea of cloud on the slopes of Teide, strato volcano on the island of Tenerife, in the Canary Islands.Canary pines and sea of clouds on the island of Tenerife. Canary Island pine (Pinus canariensis) is a magnificent endemic species of the archipelago, very resistant to fire and colonizing bare volcanic soils, like here basalt flows of the Teide - The northeast trade winds regularly cause the formation of a dense sea of cloud on the slopes of Teide, strato volcano on the island of Tenerife, in the Canary Islands.Canary pines and sea of clouds on the island of Tenerife. Canary Island pine (Pinus canariensis) is a magnificent endemic species of the archipelago, very resistant to fire and colonizing bare volcanic soils, like here basalt flows of the Teide - The northeast trade winds regularly cause the formation of a dense sea of cloud on the slopes of Teide, strato volcano on the island of Tenerife, in the Canary Islands.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2447336

Canary pines and sea of clouds on the island of Tenerife. Canary

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Canary pines on the island of Tenerife (Canary Islands). Canary Island pine (Pinus canariensis) is a magnificent endemic species of the archipelago, very resistant to fire and colonizing bare volcanic soils, like here basalt flowsof Teide, on island of tenerifeCanary pines on the island of Tenerife (Canary Islands). Canary Island pine (Pinus canariensis) is a magnificent endemic species of the archipelago, very resistant to fire and colonizing bare volcanic soils, like here basalt flowsof Teide, on island of tenerifeCanary pines on the island of Tenerife (Canary Islands). Canary Island pine (Pinus canariensis) is a magnificent endemic species of the archipelago, very resistant to fire and colonizing bare volcanic soils, like here basalt flowsof Teide, on island of tenerife© Jean-Philippe Delobelle / BiosphotoJPG - RM

2447335

Canary pines on the island of Tenerife (Canary Islands). Canary

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Canary pines on the island of Tenerife (Canary Islands). Canary Island pine (Pinus canariensis) is a magnificent endemic species of the archipelago, very resistant to fire and colonizing bare volcanic soils, like here basalt flowsof Teide, on island of tenerifeCanary pines on the island of Tenerife (Canary Islands). Canary Island pine (Pinus canariensis) is a magnificent endemic species of the archipelago, very resistant to fire and colonizing bare volcanic soils, like here basalt flowsof Teide, on island of tenerifeCanary pines on the island of Tenerife (Canary Islands). Canary Island pine (Pinus canariensis) is a magnificent endemic species of the archipelago, very resistant to fire and colonizing bare volcanic soils, like here basalt flowsof Teide, on island of tenerife© Jean-Philippe Delobelle / BiosphotoJPG - RM

2447334

Canary pines on the island of Tenerife (Canary Islands). Canary

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Canary pines on the island of Tenerife (Canary Islands). Canary Island pine (Pinus canariensis) is a magnificent endemic species of the archipelago, very resistant to fire and colonizing bare volcanic soils, like here basalt flowsof Teide, on island of tenerifeCanary pines on the island of Tenerife (Canary Islands). Canary Island pine (Pinus canariensis) is a magnificent endemic species of the archipelago, very resistant to fire and colonizing bare volcanic soils, like here basalt flowsof Teide, on island of tenerifeCanary pines on the island of Tenerife (Canary Islands). Canary Island pine (Pinus canariensis) is a magnificent endemic species of the archipelago, very resistant to fire and colonizing bare volcanic soils, like here basalt flowsof Teide, on island of tenerife© Jean-Philippe Delobelle / BiosphotoJPG - RM

2447333

Canary pines on the island of Tenerife (Canary Islands). Canary

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Lichens on recent basalts on the island of Tenerife (Canary Islands). Lavender lichen (Stereocaulon vulcani): pioneer lichen running on recent basalts - Basaltic flows of Chinyero, dating from 1909, on the slopes of Teide, on the island of TenerifeLichens on recent basalts on the island of Tenerife (Canary Islands). Lavender lichen (Stereocaulon vulcani): pioneer lichen running on recent basalts - Basaltic flows of Chinyero, dating from 1909, on the slopes of Teide, on the island of TenerifeLichens on recent basalts on the island of Tenerife (Canary Islands). Lavender lichen (Stereocaulon vulcani): pioneer lichen running on recent basalts - Basaltic flows of Chinyero, dating from 1909, on the slopes of Teide, on the island of Tenerife© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Lichens on recent basalts on the island of Tenerife (Canary

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Lichens on recent basalts on the island of Tenerife (Canary Islands). Lavender lichen (Stereocaulon vulcani): pioneer lichen running on recent basalts - Basaltic flows of Chinyero, dating from 1909, on the slopes of Teide, on the island of TenerifeLichens on recent basalts on the island of Tenerife (Canary Islands). Lavender lichen (Stereocaulon vulcani): pioneer lichen running on recent basalts - Basaltic flows of Chinyero, dating from 1909, on the slopes of Teide, on the island of TenerifeLichens on recent basalts on the island of Tenerife (Canary Islands). Lavender lichen (Stereocaulon vulcani): pioneer lichen running on recent basalts - Basaltic flows of Chinyero, dating from 1909, on the slopes of Teide, on the island of Tenerife© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Lichens on recent basalts on the island of Tenerife (Canary

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Canary pines on the island of Tenerife (Canary Islands). Canary Island pine (Pinus canariensis) is a magnificent endemic species of the archipelago, very resistant to fire and colonizing bare volcanic soils, like here basalt flows from Chinyero, dating from 1909, on the slopes of Teide, on island of tenerifeCanary pines on the island of Tenerife (Canary Islands). Canary Island pine (Pinus canariensis) is a magnificent endemic species of the archipelago, very resistant to fire and colonizing bare volcanic soils, like here basalt flows from Chinyero, dating from 1909, on the slopes of Teide, on island of tenerifeCanary pines on the island of Tenerife (Canary Islands). Canary Island pine (Pinus canariensis) is a magnificent endemic species of the archipelago, very resistant to fire and colonizing bare volcanic soils, like here basalt flows from Chinyero, dating from 1909, on the slopes of Teide, on island of tenerife© Jean-Philippe Delobelle / BiosphotoJPG - RM

2447330

Canary pines on the island of Tenerife (Canary Islands). Canary

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Canary pines on the island of Tenerife (Canary Islands). Canary Island pine (Pinus canariensis) is a magnificent endemic species of the archipelago, very resistant to fire and colonizing bare volcanic soils, like here basalt flows from Chinyero, dating from 1909, on the slopes of Teide, on island of tenerifeCanary pines on the island of Tenerife (Canary Islands). Canary Island pine (Pinus canariensis) is a magnificent endemic species of the archipelago, very resistant to fire and colonizing bare volcanic soils, like here basalt flows from Chinyero, dating from 1909, on the slopes of Teide, on island of tenerifeCanary pines on the island of Tenerife (Canary Islands). Canary Island pine (Pinus canariensis) is a magnificent endemic species of the archipelago, very resistant to fire and colonizing bare volcanic soils, like here basalt flows from Chinyero, dating from 1909, on the slopes of Teide, on island of tenerife© Jean-Philippe Delobelle / BiosphotoJPG - RM

2447329

Canary pines on the island of Tenerife (Canary Islands). Canary

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Black lavas rich in obsidian on the sides of Teide. Teide is a huge volcano strato on the island of Tenerife, in the Canary Islands. It measures 3718 m above the ocean, but almost 7000 m from its base on the ocean floor, making it the 3rd known volcanic structure. It comes from the activity of a hot spot that formed the Canary archipelago during the displacement of the African plate.Black lavas rich in obsidian on the sides of Teide. Teide is a huge volcano strato on the island of Tenerife, in the Canary Islands. It measures 3718 m above the ocean, but almost 7000 m from its base on the ocean floor, making it the 3rd known volcanic structure. It comes from the activity of a hot spot that formed the Canary archipelago during the displacement of the African plate.Black lavas rich in obsidian on the sides of Teide. Teide is a huge volcano strato on the island of Tenerife, in the Canary Islands. It measures 3718 m above the ocean, but almost 7000 m from its base on the ocean floor, making it the 3rd known volcanic structure. It comes from the activity of a hot spot that formed the Canary archipelago during the displacement of the African plate.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2447322

Black lavas rich in obsidian on the sides of Teide. Teide is a

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Black lavas rich in obsidian on the sides of Teide. Teide is a huge volcano strato on the island of Tenerife, in the Canary Islands. It measures 3718 m above the ocean, but almost 7000 m from its base on the ocean floor, making it the 3rd known volcanic structure. It comes from the activity of a hot spot that formed the Canary archipelago during the displacement of the African plate.Black lavas rich in obsidian on the sides of Teide. Teide is a huge volcano strato on the island of Tenerife, in the Canary Islands. It measures 3718 m above the ocean, but almost 7000 m from its base on the ocean floor, making it the 3rd known volcanic structure. It comes from the activity of a hot spot that formed the Canary archipelago during the displacement of the African plate.Black lavas rich in obsidian on the sides of Teide. Teide is a huge volcano strato on the island of Tenerife, in the Canary Islands. It measures 3718 m above the ocean, but almost 7000 m from its base on the ocean floor, making it the 3rd known volcanic structure. It comes from the activity of a hot spot that formed the Canary archipelago during the displacement of the African plate.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2447319

Black lavas rich in obsidian on the sides of Teide. Teide is a

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Teide volcano, Tenerife island, Canary IslandTeide volcano, Tenerife island, Canary IslandTeide volcano, Tenerife island, Canary Island© Marc Le Fèvre / BiosphotoJPG - RM

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Teide volcano, Tenerife island, Canary Island

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Kupukupu Fern (Nephrolepis cordifolia), Big Island, Hawaii. This fern is noted for being a pioneer species along with lichens on new lava fields.Kupukupu Fern (Nephrolepis cordifolia), Big Island, Hawaii. This fern is noted for being a pioneer species along with lichens on new lava fields.Kupukupu Fern (Nephrolepis cordifolia), Big Island, Hawaii. This fern is noted for being a pioneer species along with lichens on new lava fields.© Stuart Wilson / BiosphotoJPG - RMNon exclusive sale

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Kupukupu Fern (Nephrolepis cordifolia), Big Island, Hawaii. This

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Cascade Sainte-Anne, pillow basalt Pillow Lava, impassable natural barrier for Atlantic salmon These underwater volcanic rocks were created during the formation of the Chics-Chocs Mountains, Haute-Gaspésie National Park, Gaspésie , Quebec, CanadaCascade Sainte-Anne, pillow basalt Pillow Lava, impassable natural barrier for Atlantic salmon These underwater volcanic rocks were created during the formation of the Chics-Chocs Mountains, Haute-Gaspésie National Park, Gaspésie , Quebec, CanadaCascade Sainte-Anne, pillow basalt Pillow Lava, impassable natural barrier for Atlantic salmon These underwater volcanic rocks were created during the formation of the Chics-Chocs Mountains, Haute-Gaspésie National Park, Gaspésie , Quebec, Canada© Jean-Paul Chatagnon / BiosphotoJPG - RM

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Cascade Sainte-Anne, pillow basalt Pillow Lava, impassable

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Coulée de lave cordée. Isla Santiago Isla Galapagos EquateurCoulée de lave cordée. Isla Santiago Isla Galapagos EquateurCoulée de lave cordée. Isla Santiago Isla Galapagos Equateur© Michel Gunther / BiosphotoJPG - RM

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Coulée de lave cordée. Isla Santiago Isla Galapagos Equateur

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Coulée de lave cordée. Isla Santiago Isla Galapagos EquateurCoulée de lave cordée. Isla Santiago Isla Galapagos EquateurCoulée de lave cordée. Isla Santiago Isla Galapagos Equateur© Michel Gunther / BiosphotoJPG - RM

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Coulée de lave cordée. Isla Santiago Isla Galapagos Equateur

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Ribbed lava flow, Isla Santiago, Galapagos IslandsRibbed lava flow, Isla Santiago, Galapagos IslandsRibbed lava flow, Isla Santiago, Galapagos Islands© Michel Gunther / BiosphotoJPG - RM

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Ribbed lava flow, Isla Santiago, Galapagos Islands

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Lava flow in the Tsingy fossil coral reef of Ankarana, 18 220 ha NP over 35 km, North-West MadagascarLava flow in the Tsingy fossil coral reef of Ankarana, 18 220 ha NP over 35 km, North-West MadagascarLava flow in the Tsingy fossil coral reef of Ankarana, 18 220 ha NP over 35 km, North-West Madagascar© Jean Mayet / BiosphotoJPG - RM

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Lava flow in the Tsingy fossil coral reef of Ankarana, 18 220 ha

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Barter's Anubias (Anubias barteri) on lava rockBarter's Anubias (Anubias barteri) on lava rockBarter's Anubias (Anubias barteri) on lava rock© Aqua Press / BiosphotoJPG - RMNon exclusive sale

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Barter's Anubias (Anubias barteri) on lava rock

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Peters' Lava Lizard (Tropidurus hispidus)Peters' Lava Lizard (Tropidurus hispidus)Peters' Lava Lizard (Tropidurus hispidus)© Matthijs Kuijpers / BiosphotoJPG - RMNon exclusive sale
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Peters' Lava Lizard (Tropidurus hispidus)

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Collared tree lizard (Plica plica)Collared tree lizard (Plica plica)Collared tree lizard (Plica plica)© Matthijs Kuijpers / BiosphotoJPG - RMNon exclusive sale
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2428475

Collared tree lizard (Plica plica)

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Lava gull (Leucophaeus fuliginosus) on rock, GalapagosLava gull (Leucophaeus fuliginosus) on rock, GalapagosLava gull (Leucophaeus fuliginosus) on rock, Galapagos© Jean-Paul Chatagnon / BiosphotoJPG - RM

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Lava gull (Leucophaeus fuliginosus) on rock, Galapagos

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Galapagos Lava Lizard (Microlophus albemarlensis) on rock, GalapagosGalapagos Lava Lizard (Microlophus albemarlensis) on rock, GalapagosGalapagos Lava Lizard (Microlophus albemarlensis) on rock, Galapagos© Jean-Paul Chatagnon / BiosphotoJPG - RM

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Galapagos Lava Lizard (Microlophus albemarlensis) on rock,

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Tara Oceans Expeditions - May 2011. Marine Iguana (Amblyrhynchus cristatus) on lava rock, Isabela Island, Galapagos, EcuadorTara Oceans Expeditions - May 2011. Marine Iguana (Amblyrhynchus cristatus) on lava rock, Isabela Island, Galapagos, EcuadorTara Oceans Expeditions - May 2011. Marine Iguana (Amblyrhynchus cristatus) on lava rock, Isabela Island, Galapagos, Ecuador© Christoph Gerigk / BiosphotoJPG - RM

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Tara Oceans Expeditions - May 2011. Marine Iguana (Amblyrhynchus

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Tara Pacific expedition - november 2017 Ancient lava flow, small Cauliflower corals, D: 3 m, Anne Sophie’s Reef, Kimbe Bay, Papua New GuineaTara Pacific expedition - november 2017 Ancient lava flow, small Cauliflower corals, D: 3 m, Anne Sophie’s Reef, Kimbe Bay, Papua New GuineaTara Pacific expedition - november 2017 Ancient lava flow, small Cauliflower corals, D: 3 m, Anne Sophie’s Reef, Kimbe Bay, Papua New Guinea© Christoph Gerigk / BiosphotoJPG - RM

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Tara Pacific expedition - november 2017 Ancient lava flow, small

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Pāhoehoe lava, Reunion IslandPāhoehoe lava, Reunion IslandPāhoehoe lava, Reunion Island© Régis Cavignaux / BiosphotoJPG - RM

2412083

Pāhoehoe lava, Reunion Island

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Vegetal colonization of a lava flow, Reunion IslandVegetal colonization of a lava flow, Reunion IslandVegetal colonization of a lava flow, Reunion Island© Régis Cavignaux / BiosphotoJPG - RM

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Vegetal colonization of a lava flow, Reunion Island

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Pāhoehoe lava, Reunion IslandPāhoehoe lava, Reunion IslandPāhoehoe lava, Reunion Island© Régis Cavignaux / BiosphotoJPG - RM

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Pāhoehoe lava, Reunion Island

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Lava lichen (Stereocaulon vulcani) on lava, Reunion IslandLava lichen (Stereocaulon vulcani) on lava, Reunion IslandLava lichen (Stereocaulon vulcani) on lava, Reunion Island© Régis Cavignaux / BiosphotoJPG - RM

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Lava lichen (Stereocaulon vulcani) on lava, Reunion Island

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Fern (Nephrolepis abrupta) and Lava lichen (Stereocaulon vulcani) on lava, Reunion IslandFern (Nephrolepis abrupta) and Lava lichen (Stereocaulon vulcani) on lava, Reunion IslandFern (Nephrolepis abrupta) and Lava lichen (Stereocaulon vulcani) on lava, Reunion Island© Régis Cavignaux / BiosphotoJPG - RM

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Fern (Nephrolepis abrupta) and Lava lichen (Stereocaulon vulcani)

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Fern (Nephrolepis abrupta) and Lava lichen (Stereocaulon vulcani) on lava, Reunion IslandFern (Nephrolepis abrupta) and Lava lichen (Stereocaulon vulcani) on lava, Reunion IslandFern (Nephrolepis abrupta) and Lava lichen (Stereocaulon vulcani) on lava, Reunion Island© Régis Cavignaux / BiosphotoJPG - RM

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Fern (Nephrolepis abrupta) and Lava lichen (Stereocaulon vulcani)

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Lava Flow, Le grand brulé, Reunion IslandLava Flow, Le grand brulé, Reunion IslandLava Flow, Le grand brulé, Reunion Island© Régis Cavignaux / BiosphotoJPG - RM

2412077

Lava Flow, Le grand brulé, Reunion Island

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Colonization of lavas by lichens and ferns, Lava Flow, Le grand brulé, Reunion IslandColonization of lavas by lichens and ferns, Lava Flow, Le grand brulé, Reunion IslandColonization of lavas by lichens and ferns, Lava Flow, Le grand brulé, Reunion Island© Régis Cavignaux / BiosphotoJPG - RM

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Colonization of lavas by lichens and ferns, Lava Flow, Le grand

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Rocky shore, Saint Philippe, Reunion IslandRocky shore, Saint Philippe, Reunion IslandRocky shore, Saint Philippe, Reunion Island© Régis Cavignaux / BiosphotoJPG - RM

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Rocky shore, Saint Philippe, Reunion Island

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Piton de la Fournaise, Reunion IslandPiton de la Fournaise, Reunion IslandPiton de la Fournaise, Reunion Island© Régis Cavignaux / BiosphotoJPG - RM

2412021

Piton de la Fournaise, Reunion Island

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Piton de la Fournaise, Reunion IslandPiton de la Fournaise, Reunion IslandPiton de la Fournaise, Reunion Island© Régis Cavignaux / BiosphotoJPG - RM

2412020

Piton de la Fournaise, Reunion Island

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