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Winding beech trees after a snow squall, Massif du Grand Colombier, Bugey, Ain, FranceWinding beech trees after a snow squall, Massif du Grand Colombier, Bugey, Ain, FranceWinding beech trees after a snow squall, Massif du Grand Colombier, Bugey, Ain, France© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Winding beech trees after a snow squall, Massif du Grand

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Grey Heron (Ardea cinerea). A adult bird standing on the ice during a snowstorm. Taken on a wintering spot in Sweden.Grey Heron (Ardea cinerea). A adult bird standing on the ice during a snowstorm. Taken on a wintering spot in Sweden.Grey Heron (Ardea cinerea). A adult bird standing on the ice during a snowstorm. Taken on a wintering spot in Sweden.© Ivan Sjögren / BiosphotoJPG - RMNon exclusive sale

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Grey Heron (Ardea cinerea). A adult bird standing on the ice

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Barn owl (Tyto alba) perched on a fence post while snowing, AnglandBarn owl (Tyto alba) perched on a fence post while snowing, AnglandBarn owl (Tyto alba) perched on a fence post while snowing, Angland© Frédéric Desmette / BiosphotoJPG - RMNon exclusive sale
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2194109

Barn owl (Tyto alba) perched on a fence post while snowing,

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Gull (Larus sp) flying over the ocean unleashed, IcelandGull (Larus sp) flying over the ocean unleashed, IcelandGull (Larus sp) flying over the ocean unleashed, Iceland© Philippe Moës / BiosphotoJPG - RMNon exclusive sale, exclusive sale possible in France
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2087854

Gull (Larus sp) flying over the ocean unleashed, Iceland

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Gentoo penguins in a sandstorm - Falkland Islands Gentoo penguins in a sandstorm - Falkland Islands Gentoo penguins in a sandstorm - Falkland Islands © Alain Mafart-Renodier / BiosphotoJPG - RMNon exclusive sale

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Gentoo penguins in a sandstorm - Falkland Islands

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Dead acacia trees at Dead Vlei - Sossusvlei Namib Namibia Dead acacia trees at Dead Vlei - Sossusvlei Namib Namibia Dead acacia trees at Dead Vlei - Sossusvlei Namib Namibia © Juan-Carlos Muñoz / BiosphotoJPG - RMNon exclusive sale, exclusive sale possible in France

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Dead acacia trees at Dead Vlei - Sossusvlei Namib Namibia

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Dead acacia trees at Dead Vlei - Sossusvlei Namib Namibia Dead acacia trees at Dead Vlei - Sossusvlei Namib Namibia Dead acacia trees at Dead Vlei - Sossusvlei Namib Namibia © Juan-Carlos Muñoz / BiosphotoJPG - RMNon exclusive sale, exclusive sale possible in France

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Dead acacia trees at Dead Vlei - Sossusvlei Namib Namibia

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Barn Owl perched on a post in a snow storm Winter GBBarn Owl perched on a post in a snow storm Winter GBBarn Owl perched on a post in a snow storm Winter GB© Frédéric Desmette / BiosphotoJPG - RMNon exclusive sale
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Barn Owl perched on a post in a snow storm Winter GB

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Sandstorm at sunset Sahara Morocco Sandstorm at sunset Sahara Morocco Sandstorm at sunset Sahara Morocco © Laurent Rebelle / BiosphotoJPG - RM

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Sandstorm at sunset Sahara Morocco

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King Penguin (Aptenodytes patagonicus) colony, huddled together during snowstorm, Right Whale Bay, South Georgia, novemberKing Penguin (Aptenodytes patagonicus) colony, huddled together during snowstorm, Right Whale Bay, South Georgia, novemberKing Penguin (Aptenodytes patagonicus) colony, huddled together during snowstorm, Right Whale Bay, South Georgia, november© David Tipling / BiosphotoJPG - RMSale prohibited in UK
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King Penguin (Aptenodytes patagonicus) colony, huddled together

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Dead Vlei Sossusvlei dead acacia Namib Desert Namibia  ; Dead Vlei is an old saltpan named for its eery dead appearance. Water was cut off when the flow of the Tsauchab River changed its course approximately 500 years ago. This now provides visitor with the most spectacular sceneryDead Vlei Sossusvlei dead acacia Namib Desert Namibia Dead Vlei Sossusvlei dead acacia Namib Desert Namibia ; Dead Vlei is an old saltpan named for its eery dead appearance. Water was cut off when the flow of the Tsauchab River changed its course approximately 500 years ago. This now provides visitor with the most spectacular scenery© Martin Harvey / BiosphotoJPG - RMSale prohibited in Germany and UK
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Dead Vlei Sossusvlei dead acacia Namib Desert Namibia ; Dead

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Dead Acacias Dead Vlei Sossusvlei Namib Desert Namibia  ; Water was cut off when the flow of the Tsauchab River changed its course approximately 500 years ago.Dead Acacias Dead Vlei Sossusvlei Namib Desert Namibia Dead Acacias Dead Vlei Sossusvlei Namib Desert Namibia  ; Water was cut off when the flow of the Tsauchab River changed its course approximately 500 years ago.© Martin Harvey / BiosphotoJPG - RMSale prohibited in Germany and UK
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Dead Acacias Dead Vlei Sossusvlei Namib Desert Namibia  ; Water

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King Penguins huddled together during storm South GeorgiaKing Penguins huddled together during storm South GeorgiaKing Penguins huddled together during storm South Georgia© David Tipling / BiosphotoJPG - RMSale prohibited in UK
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King Penguins huddled together during storm South Georgia

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King Penguins huddled together during storm South GeorgiaKing Penguins huddled together during storm South GeorgiaKing Penguins huddled together during storm South Georgia© David Tipling / BiosphotoJPG - RMSale prohibited in UK
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King Penguins huddled together during storm South Georgia

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Red kite on a tree in snow storm GBRed kite on a tree in snow storm GBRed kite on a tree in snow storm GB© Frédéric Desmette / BiosphotoJPG - RMNon exclusive sale
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Red kite on a tree in snow storm GB

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Sea bird landed on a sailboat before the thunderstormSea bird landed on a sailboat before the thunderstormSea bird landed on a sailboat before the thunderstorm© Didier Brandelet / BiosphotoJPG - RM

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Sea bird landed on a sailboat before the thunderstorm

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Young Locust posed on a dry Pea field Switzerland ; During a dryness in a cultivated Pea field, in edge of the natural reserve.<br>The farmer decided not to mow his production because of the weak one<br>output due to the dryness.<br>The identification of the species is not possible because it's about a youthful individual: the characteristics of the species are not apparent enough.Young Locust posed on a dry Pea field SwitzerlandYoung Locust posed on a dry Pea field Switzerland ; During a dryness in a cultivated Pea field, in edge of the natural reserve.
The farmer decided not to mow his production because of the weak one
output due to the dryness.
The identification of the species is not possible because it's about a youthful individual: the characteristics of the species are not apparent enough.
© André Maurer / BiosphotoJPG - RM

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Young Locust posed on a dry Pea field Switzerland ; During a

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White-backed Vulture (Gyps africanus) standing with wings outstretched covered in dustWhite-backed Vulture (Gyps africanus) standing with wings outstretched covered in dustWhite-backed Vulture (Gyps africanus) standing with wings outstretched covered in dust© Peter Delaney / imageBROKER / BiosphotoJPG - RMNon exclusive sale
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White-backed Vulture (Gyps africanus) standing with wings

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Emperor penguin - Antarctica Southern Ocean ; Emperor penguins in blizzard, Aptenodytes forsteri, Weddell Sea, AntarcticaEmperor penguin - Antarctica Southern OceanEmperor penguin - Antarctica Southern Ocean ; Emperor penguins in blizzard, Aptenodytes forsteri, Weddell Sea, Antarctica© Frans Lanting / Mint Images / BiosphotoJPG - RMNon exclusive sale
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Emperor penguin - Antarctica Southern Ocean ; Emperor penguins in

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Cracked clay in a depression of the Teide caldera in the Canaries. Teide is a huge strato volcano (3,718 m) on the island of Tenerife, in the Canary Islands.Cracked clay in a depression of the Teide caldera in the Canaries. Teide is a huge strato volcano (3,718 m) on the island of Tenerife, in the Canary Islands.Cracked clay in a depression of the Teide caldera in the Canaries. Teide is a huge strato volcano (3,718 m) on the island of Tenerife, in the Canary Islands.© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Cracked clay in a depression of the Teide caldera in the

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Winter atmosphere in the Jura mountains, Massif du Grand Colombier, Bugey, Ain, FranceWinter atmosphere in the Jura mountains, Massif du Grand Colombier, Bugey, Ain, FranceWinter atmosphere in the Jura mountains, Massif du Grand Colombier, Bugey, Ain, France© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Winter atmosphere in the Jura mountains, Massif du Grand

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Winter atmosphere in the Jura mountains, Massif du Grand Colombier, Bugey, Ain, FranceWinter atmosphere in the Jura mountains, Massif du Grand Colombier, Bugey, Ain, FranceWinter atmosphere in the Jura mountains, Massif du Grand Colombier, Bugey, Ain, France© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Winter atmosphere in the Jura mountains, Massif du Grand

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Winding beech trees after a snow squall, Massif du Grand Colombier, Bugey, Ain, FranceWinding beech trees after a snow squall, Massif du Grand Colombier, Bugey, Ain, FranceWinding beech trees after a snow squall, Massif du Grand Colombier, Bugey, Ain, France© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Winding beech trees after a snow squall, Massif du Grand

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Solitary Service-tree after a snow squall on the ridges, Massif du Grand Colombier, Bugey, Ain, FranceSolitary Service-tree after a snow squall on the ridges, Massif du Grand Colombier, Bugey, Ain, FranceSolitary Service-tree after a snow squall on the ridges, Massif du Grand Colombier, Bugey, Ain, France© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Solitary Service-tree after a snow squall on the ridges, Massif

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Solitary Service-tree after a snow squall on the ridges, Massif du Grand Colombier, Bugey, Ain, FranceSolitary Service-tree after a snow squall on the ridges, Massif du Grand Colombier, Bugey, Ain, FranceSolitary Service-tree after a snow squall on the ridges, Massif du Grand Colombier, Bugey, Ain, France© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Solitary Service-tree after a snow squall on the ridges, Massif

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Beech forest after a snow squall, Massif du Grand Colombier, Bugey, Ain, FranceBeech forest after a snow squall, Massif du Grand Colombier, Bugey, Ain, FranceBeech forest after a snow squall, Massif du Grand Colombier, Bugey, Ain, France© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Beech forest after a snow squall, Massif du Grand Colombier,

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Beech forest after a snow squall, Massif du Grand Colombier, Bugey, Ain, FranceBeech forest after a snow squall, Massif du Grand Colombier, Bugey, Ain, FranceBeech forest after a snow squall, Massif du Grand Colombier, Bugey, Ain, France© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Beech forest after a snow squall, Massif du Grand Colombier,

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Massif du Grand Colombier - Bugey (Ain)Massif du Grand Colombier - Bugey (Ain)Massif du Grand Colombier - Bugey (Ain)© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Massif du Grand Colombier - Bugey (Ain)

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Dog rose (Rosa sp) after a snow squall, Massif du Grand Colombier, Bugey, Ain, FranceDog rose (Rosa sp) after a snow squall, Massif du Grand Colombier, Bugey, Ain, FranceDog rose (Rosa sp) after a snow squall, Massif du Grand Colombier, Bugey, Ain, France© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Dog rose (Rosa sp) after a snow squall, Massif du Grand

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Dog rose (Rosa sp) after a snow squall, Massif du Grand Colombier, Bugey, Ain, FranceDog rose (Rosa sp) after a snow squall, Massif du Grand Colombier, Bugey, Ain, FranceDog rose (Rosa sp) after a snow squall, Massif du Grand Colombier, Bugey, Ain, France© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Dog rose (Rosa sp) after a snow squall, Massif du Grand

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Snowstorm in a tall-stem orchard, Vosges du Nord Regional Natural Park, FranceSnowstorm in a tall-stem orchard, Vosges du Nord Regional Natural Park, FranceSnowstorm in a tall-stem orchard, Vosges du Nord Regional Natural Park, France© Michel Rauch / BiosphotoJPG - RM

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Snowstorm in a tall-stem orchard, Vosges du Nord Regional Natural

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Genseikaen station in a snowstorm in Abashiri, Hokkaido, JapanGenseikaen station in a snowstorm in Abashiri, Hokkaido, JapanGenseikaen station in a snowstorm in Abashiri, Hokkaido, Japan© Antoine Boureau / BiosphotoJPG - RM

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Genseikaen station in a snowstorm in Abashiri, Hokkaido, Japan

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Single file of Giraffes walking in drough riverbed in Kruger National park, South Africa ; Specie Giraffa camelopardalis family of GiraffidaeSingle file of Giraffes walking in drough riverbed in Kruger National park, South Africa ; Specie Giraffa camelopardalis family of GiraffidaeSingle file of Giraffes walking in drough riverbed in Kruger National park, South Africa ; Specie Giraffa camelopardalis family of Giraffidae© Patrice Correia / BiosphotoJPG - RMNon exclusive sale

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Single file of Giraffes walking in drough riverbed in Kruger

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Waves hitting the Wimereux embankment during a storm, Hauts de France, FranceWaves hitting the Wimereux embankment during a storm, Hauts de France, FranceWaves hitting the Wimereux embankment during a storm, Hauts de France, France© Yann Avril / BiosphotoJPG - RM

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Waves hitting the Wimereux embankment during a storm, Hauts de

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Pier of Boulogne sur mer during storm Ciara, Hauts de France, FrancePier of Boulogne sur mer during storm Ciara, Hauts de France, FrancePier of Boulogne sur mer during storm Ciara, Hauts de France, France© Yann Avril / BiosphotoJPG - RM

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Pier of Boulogne sur mer during storm Ciara, Hauts de France,

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Exit from the port of Boulogne sur mer during storm Ciara, Hauts de France, FranceExit from the port of Boulogne sur mer during storm Ciara, Hauts de France, FranceExit from the port of Boulogne sur mer during storm Ciara, Hauts de France, France© Yann Avril / BiosphotoJPG - RM

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Exit from the port of Boulogne sur mer during storm Ciara, Hauts

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View of Boulogne sur mer, its beach, its port, and the Carnot dike hit by the waves during the storm Ciara, February 2020, Hauts de France, FranceView of Boulogne sur mer, its beach, its port, and the Carnot dike hit by the waves during the storm Ciara, February 2020, Hauts de France, FranceView of Boulogne sur mer, its beach, its port, and the Carnot dike hit by the waves during the storm Ciara, February 2020, Hauts de France, France© Yann Avril / BiosphotoJPG - RM

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View of Boulogne sur mer, its beach, its port, and the Carnot

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Fort d'Ambleteuse during storm Ciara, February 2020, Hauts de France, FranceFort d'Ambleteuse during storm Ciara, February 2020, Hauts de France, FranceFort d'Ambleteuse during storm Ciara, February 2020, Hauts de France, France© Yann Avril / BiosphotoJPG - RM

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Fort d'Ambleteuse during storm Ciara, February 2020, Hauts de

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Villages of Ambleteuse and Audresselles during the storm Ciara, February 2020, Hauts de France, FranceVillages of Ambleteuse and Audresselles during the storm Ciara, February 2020, Hauts de France, FranceVillages of Ambleteuse and Audresselles during the storm Ciara, February 2020, Hauts de France, France© Yann Avril / BiosphotoJPG - RM

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Villages of Ambleteuse and Audresselles during the storm Ciara,

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Waves hitting the Wimereux embankment during the Ciara storm, February 2020, Hauts de France, FranceWaves hitting the Wimereux embankment during the Ciara storm, February 2020, Hauts de France, FranceWaves hitting the Wimereux embankment during the Ciara storm, February 2020, Hauts de France, France© Yann Avril / BiosphotoJPG - RM

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Waves hitting the Wimereux embankment during the Ciara storm,

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Waves hitting the Wimereux embankment during the Ciara storm, February 2020, Hauts de France, FranceWaves hitting the Wimereux embankment during the Ciara storm, February 2020, Hauts de France, FranceWaves hitting the Wimereux embankment during the Ciara storm, February 2020, Hauts de France, France© Yann Avril / BiosphotoJPG - RM

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Waves hitting the Wimereux embankment during the Ciara storm,

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Waves hitting the lighthouse of the Carnot dike with a rainbow created by reflection of light on the waves, during the storm Ciara, Boulogne sur mer, February 2020, Hauts de France, FranceWaves hitting the lighthouse of the Carnot dike with a rainbow created by reflection of light on the waves, during the storm Ciara, Boulogne sur mer, February 2020, Hauts de France, FranceWaves hitting the lighthouse of the Carnot dike with a rainbow created by reflection of light on the waves, during the storm Ciara, Boulogne sur mer, February 2020, Hauts de France, France© Yann Avril / BiosphotoJPG - RM

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Waves hitting the lighthouse of the Carnot dike with a rainbow

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Ecume de mer sur la plage du Noirda lors de la tempête Ciara, Audreselles, Pas de Calais, Hauts de France, FranceEcume de mer sur la plage du Noirda lors de la tempête Ciara, Audreselles, Pas de Calais, Hauts de France, FranceEcume de mer sur la plage du Noirda lors de la tempête Ciara, Audreselles, Pas de Calais, Hauts de France, France© Yann Avril / BiosphotoJPG - RM

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Ecume de mer sur la plage du Noirda lors de la tempête Ciara,

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Waves hitting the Wimereux embankment during the Ciara storm, February 2020, Hauts de France, FranceWaves hitting the Wimereux embankment during the Ciara storm, February 2020, Hauts de France, FranceWaves hitting the Wimereux embankment during the Ciara storm, February 2020, Hauts de France, France© Yann Avril / BiosphotoJPG - RM

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Waves hitting the Wimereux embankment during the Ciara storm,

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The Carnot dike hit by the waves during the storm Ciara, Boulogne sur mer, February 2020, Hauts de France, FranceThe Carnot dike hit by the waves during the storm Ciara, Boulogne sur mer, February 2020, Hauts de France, FranceThe Carnot dike hit by the waves during the storm Ciara, Boulogne sur mer, February 2020, Hauts de France, France© Yann Avril / BiosphotoJPG - RM

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The Carnot dike hit by the waves during the storm Ciara, Boulogne

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Ruisseau à sec à la fin d'un été très sec, le long d'une pelouse sèche, Vallée du Terroin, environs de Toul, Lorraine, FranceRuisseau à sec à la fin d'un été très sec, le long d'une pelouse sèche, Vallée du Terroin, environs de Toul, Lorraine, FranceRuisseau à sec à la fin d'un été très sec, le long d'une pelouse sèche, Vallée du Terroin, environs de Toul, Lorraine, France© André Simon / BiosphotoJPG - RM

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Ruisseau à sec à la fin d'un été très sec, le long d'une

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Norway spruce uprooted following a gale in winter, Moselle, FranceNorway spruce uprooted following a gale in winter, Moselle, FranceNorway spruce uprooted following a gale in winter, Moselle, France© Yann Avril / BiosphotoJPG - RM

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Norway spruce uprooted following a gale in winter, Moselle, France

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A Mountain Hare (Lepus timidus) settles down after a snowstorm in the Cairngorms National Park, Scotland.A Mountain Hare (Lepus timidus) settles down after a snowstorm in the Cairngorms National Park, Scotland.A Mountain Hare (Lepus timidus) settles down after a snowstorm in the Cairngorms National Park, Scotland.© Tesni Ward / BiosphotoJPG - RM

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A Mountain Hare (Lepus timidus) settles down after a snowstorm in

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Sunrise on the Atlantic coast of Gran Canaria after the storm, Bufadera de la Garita, Gran Canaria, SpainSunrise on the Atlantic coast of Gran Canaria after the storm, Bufadera de la Garita, Gran Canaria, SpainSunrise on the Atlantic coast of Gran Canaria after the storm, Bufadera de la Garita, Gran Canaria, Spain© David Jerez / BiosphotoJPG - RMNon exclusive sale

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Sunrise on the Atlantic coast of Gran Canaria after the storm,

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Gas embolism following a drought, in a beech tree, Autumn, Moselle, FranceGas embolism following a drought, in a beech tree, Autumn, Moselle, FranceGas embolism following a drought, in a beech tree, Autumn, Moselle, France© Yann Avril / BiosphotoJPG - RM

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Gas embolism following a drought, in a beech tree, Autumn,

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Ichnofossils on flysch Deba, Geopark of the Basque Coast, Basque Country, Spain. Ichnofossil: Helminthorhaphe and Paleodictyon on the right - Flysch formed at the end of the Mesozoic era, in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, caused by earthquakes, and producing after compaction and crystallization of very regular layers of sandstone and limestone, here corrected by the Pyrenean orogeny and released by erosion.Ichnofossils on flysch Deba, Geopark of the Basque Coast, Basque Country, Spain. Ichnofossil: Helminthorhaphe and Paleodictyon on the right - Flysch formed at the end of the Mesozoic era, in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, caused by earthquakes, and producing after compaction and crystallization of very regular layers of sandstone and limestone, here corrected by the Pyrenean orogeny and released by erosion.Ichnofossils on flysch Deba, Geopark of the Basque Coast, Basque Country, Spain. Ichnofossil: Helminthorhaphe and Paleodictyon on the right - Flysch formed at the end of the Mesozoic era, in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, caused by earthquakes, and producing after compaction and crystallization of very regular layers of sandstone and limestone, here corrected by the Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Ichnofossils on flysch Deba, Geopark of the Basque Coast, Basque

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Ichnofossils on flysch Deba, Geopark of the Basque Coast, Basque Country, Spain. Ichnofossil: Helminthorhaphe - Flysch formed at the end of the Mesozoic era, in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, caused by earthquakes, and producing after compaction and crystallization of very regular layers of sandstone and limestone, here corrected by the Pyrenean orogeny and released by erosion.Ichnofossils on flysch Deba, Geopark of the Basque Coast, Basque Country, Spain. Ichnofossil: Helminthorhaphe - Flysch formed at the end of the Mesozoic era, in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, caused by earthquakes, and producing after compaction and crystallization of very regular layers of sandstone and limestone, here corrected by the Pyrenean orogeny and released by erosion.Ichnofossils on flysch Deba, Geopark of the Basque Coast, Basque Country, Spain. Ichnofossil: Helminthorhaphe - Flysch formed at the end of the Mesozoic era, in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, caused by earthquakes, and producing after compaction and crystallization of very regular layers of sandstone and limestone, here corrected by the Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Ichnofossils on flysch Deba, Geopark of the Basque Coast, Basque

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Ichnofossils on flysch Deba, Geopark of the Basque Coast, Basque Country, Spain. Ichnofossil: Helminthorhaphe - Flysch formed at the end of the Mesozoic era, in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, caused by earthquakes, and producing after compaction and crystallization of very regular layers of sandstone and limestone, here corrected by the Pyrenean orogeny and released by erosion.Ichnofossils on flysch Deba, Geopark of the Basque Coast, Basque Country, Spain. Ichnofossil: Helminthorhaphe - Flysch formed at the end of the Mesozoic era, in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, caused by earthquakes, and producing after compaction and crystallization of very regular layers of sandstone and limestone, here corrected by the Pyrenean orogeny and released by erosion.Ichnofossils on flysch Deba, Geopark of the Basque Coast, Basque Country, Spain. Ichnofossil: Helminthorhaphe - Flysch formed at the end of the Mesozoic era, in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, caused by earthquakes, and producing after compaction and crystallization of very regular layers of sandstone and limestone, here corrected by the Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Ichnofossils on flysch Deba, Geopark of the Basque Coast, Basque

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Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437366

Remarkable flysch formations of Deba, Basque Coast Geopark,

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Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437365

Remarkable flysch formations of Deba, Basque Coast Geopark,

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Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437364

Remarkable flysch formations of Deba, Basque Coast Geopark,

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Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437363

Remarkable flysch formations of Deba, Basque Coast Geopark,

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Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437362

Remarkable flysch formations of Deba, Basque Coast Geopark,

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Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437361

Remarkable flysch formations of Deba, Basque Coast Geopark,

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Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437360

Remarkable flysch formations of Deba, Basque Coast Geopark,

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Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437359

Remarkable flysch formations of Deba, Basque Coast Geopark,

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Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437358

Remarkable flysch formations of Deba, Basque Coast Geopark,

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Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437357

Remarkable flysch formations of Deba, Basque Coast Geopark,

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Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437356

Remarkable flysch formations of Deba, Basque Coast Geopark,

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Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437355

Remarkable flysch formations of Deba, Basque Coast Geopark,

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Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437354

Remarkable flysch formations of Deba, Basque Coast Geopark,

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Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437353

Remarkable flysch formations of Deba, Basque Coast Geopark,

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Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437352

Remarkable flysch formations of Deba, Basque Coast Geopark,

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Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437351

Remarkable flysch formations of Deba, Basque Coast Geopark,

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Le fort d'Ambleteuse, Hauts de France, FranceLe fort d'Ambleteuse, Hauts de France, FranceLe fort d'Ambleteuse, Hauts de France, France© Yann Avril / BiosphotoJPG - RM

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Le fort d'Ambleteuse, Hauts de France, France

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Recovery of a cardinal buoy stranded on the beach of Calais, Hauts de France, FranceRecovery of a cardinal buoy stranded on the beach of Calais, Hauts de France, FranceRecovery of a cardinal buoy stranded on the beach of Calais, Hauts de France, France© Yann Avril / BiosphotoJPG - RM

2437188

Recovery of a cardinal buoy stranded on the beach of Calais,

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Cardinal buoy stranded on the beach of Calais, Hauts de France, FranceCardinal buoy stranded on the beach of Calais, Hauts de France, FranceCardinal buoy stranded on the beach of Calais, Hauts de France, France© Yann Avril / BiosphotoJPG - RM

2437185

Cardinal buoy stranded on the beach of Calais, Hauts de France,

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Southern Giraffe (Giraffa giraffa). Fighting males in the dry and barren Auob riverbed, raising a lot of dust. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Southern Giraffe (Giraffa giraffa). Fighting males in the dry and barren Auob riverbed, raising a lot of dust. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Southern Giraffe (Giraffa giraffa). Fighting males in the dry and barren Auob riverbed, raising a lot of dust. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.© Thomas Dressler / BiosphotoJPG - RMExclusive sale possible

2437006

Southern Giraffe (Giraffa giraffa). Fighting males in the dry and

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Southern Giraffe (Giraffa giraffa). Fighting males in the dry and barren Auob riverbed, raising a lot of dust. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Southern Giraffe (Giraffa giraffa). Fighting males in the dry and barren Auob riverbed, raising a lot of dust. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Southern Giraffe (Giraffa giraffa). Fighting males in the dry and barren Auob riverbed, raising a lot of dust. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.© Thomas Dressler / BiosphotoJPG - RMExclusive sale possible

2437005

Southern Giraffe (Giraffa giraffa). Fighting males in the dry and

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Southern Giraffe (Giraffa giraffa). Fighting males in the dry and barren Auob riverbed, raising a lot of dust. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Southern Giraffe (Giraffa giraffa). Fighting males in the dry and barren Auob riverbed, raising a lot of dust. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Southern Giraffe (Giraffa giraffa). Fighting males in the dry and barren Auob riverbed, raising a lot of dust. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.© Thomas Dressler / BiosphotoJPG - RMExclusive sale possible

2437004

Southern Giraffe (Giraffa giraffa). Fighting males in the dry and

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Southern Giraffe (Giraffa giraffa). Fighting males in the dry and barren Auob riverbed, raising a lot of dust. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Southern Giraffe (Giraffa giraffa). Fighting males in the dry and barren Auob riverbed, raising a lot of dust. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Southern Giraffe (Giraffa giraffa). Fighting males in the dry and barren Auob riverbed, raising a lot of dust. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.© Thomas Dressler / BiosphotoJPG - RMExclusive sale possible

2437003

Southern Giraffe (Giraffa giraffa). Fighting males in the dry and

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Southern Giraffe (Giraffa giraffa). Fighting males in the dry and barren Auob riverbed, raising a lot of dust. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Southern Giraffe (Giraffa giraffa). Fighting males in the dry and barren Auob riverbed, raising a lot of dust. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Southern Giraffe (Giraffa giraffa). Fighting males in the dry and barren Auob riverbed, raising a lot of dust. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.© Thomas Dressler / BiosphotoJPG - RMExclusive sale possible

2437002

Southern Giraffe (Giraffa giraffa). Fighting males in the dry and

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Cheetah (Acinonyx jubatus). Female walking in front of her two subadult male cubs in the dry and barren Auob riverbed. Behind them a thunderstorm. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Cheetah (Acinonyx jubatus). Female walking in front of her two subadult male cubs in the dry and barren Auob riverbed. Behind them a thunderstorm. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Cheetah (Acinonyx jubatus). Female walking in front of her two subadult male cubs in the dry and barren Auob riverbed. Behind them a thunderstorm. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.© Thomas Dressler / BiosphotoJPG - RMExclusive sale possible

2436999

Cheetah (Acinonyx jubatus). Female walking in front of her two

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Cheetah (Acinonyx jubatus). Female behind her two subadult male cubs. Roaming in the dry and barren Auob riverbed during a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Cheetah (Acinonyx jubatus). Female behind her two subadult male cubs. Roaming in the dry and barren Auob riverbed during a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Cheetah (Acinonyx jubatus). Female behind her two subadult male cubs. Roaming in the dry and barren Auob riverbed during a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.© Thomas Dressler / BiosphotoJPG - RMExclusive sale possible

2436994

Cheetah (Acinonyx jubatus). Female behind her two subadult male

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Cheetah (Acinonyx jubatus). Female. Roaming in the dry and barren Auob riverbed during a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Cheetah (Acinonyx jubatus). Female. Roaming in the dry and barren Auob riverbed during a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Cheetah (Acinonyx jubatus). Female. Roaming in the dry and barren Auob riverbed during a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.© Thomas Dressler / BiosphotoJPG - RMExclusive sale possible

2436993

Cheetah (Acinonyx jubatus). Female. Roaming in the dry and barren

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Cheetah (Acinonyx jubatus). Two playful subadult males in the dry and barren Auob riverbed. During a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Cheetah (Acinonyx jubatus). Two playful subadult males in the dry and barren Auob riverbed. During a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Cheetah (Acinonyx jubatus). Two playful subadult males in the dry and barren Auob riverbed. During a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.© Thomas Dressler / BiosphotoJPG - RMExclusive sale possible

2436992

Cheetah (Acinonyx jubatus). Two playful subadult males in the dry

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Cheetah (Acinonyx jubatus). Two playful subadult males in the dry and barren Auob riverbed. During a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Cheetah (Acinonyx jubatus). Two playful subadult males in the dry and barren Auob riverbed. During a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Cheetah (Acinonyx jubatus). Two playful subadult males in the dry and barren Auob riverbed. During a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.© Thomas Dressler / BiosphotoJPG - RMExclusive sale possible

2436991

Cheetah (Acinonyx jubatus). Two playful subadult males in the dry

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Cheetah (Acinonyx jubatus). Two playful subadult males in the dry and barren Auob riverbed. During a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Cheetah (Acinonyx jubatus). Two playful subadult males in the dry and barren Auob riverbed. During a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Cheetah (Acinonyx jubatus). Two playful subadult males in the dry and barren Auob riverbed. During a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.© Thomas Dressler / BiosphotoJPG - RMExclusive sale possible

2436990

Cheetah (Acinonyx jubatus). Two playful subadult males in the dry

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Cheetah (Acinonyx jubatus). Two playful subadult males in the dry and barren Auob riverbed. During a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Cheetah (Acinonyx jubatus). Two playful subadult males in the dry and barren Auob riverbed. During a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Cheetah (Acinonyx jubatus). Two playful subadult males in the dry and barren Auob riverbed. During a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.© Thomas Dressler / BiosphotoJPG - RMExclusive sale possible

2436989

Cheetah (Acinonyx jubatus). Two playful subadult males in the dry

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Cheetah (Acinonyx jubatus). Two playful subadult males in the dry and barren Auob riverbed. During a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Cheetah (Acinonyx jubatus). Two playful subadult males in the dry and barren Auob riverbed. During a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Cheetah (Acinonyx jubatus). Two playful subadult males in the dry and barren Auob riverbed. During a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.© Thomas Dressler / BiosphotoJPG - RMExclusive sale possible

2436988

Cheetah (Acinonyx jubatus). Two playful subadult males in the dry

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Cheetah (Acinonyx jubatus). Two playful subadult males in the dry and barren Auob riverbed. During a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Cheetah (Acinonyx jubatus). Two playful subadult males in the dry and barren Auob riverbed. During a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Cheetah (Acinonyx jubatus). Two playful subadult males in the dry and barren Auob riverbed. During a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.© Thomas Dressler / BiosphotoJPG - RMExclusive sale possible

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Cheetah (Acinonyx jubatus). Two playful subadult males in the dry

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Cheetah (Acinonyx jubatus). Two playful subadult males in the dry and barren Auob riverbed. During a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Cheetah (Acinonyx jubatus). Two playful subadult males in the dry and barren Auob riverbed. During a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Cheetah (Acinonyx jubatus). Two playful subadult males in the dry and barren Auob riverbed. During a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.© Thomas Dressler / BiosphotoJPG - RMExclusive sale possible

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Cheetah (Acinonyx jubatus). Two playful subadult males in the dry

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A snowstorm hits a tourist watching the landscape in Neko Harbour, Antarctica.A snowstorm hits a tourist watching the landscape in Neko Harbour, Antarctica.A snowstorm hits a tourist watching the landscape in Neko Harbour, Antarctica.© Sergio Pitamitz / BiosphotoJPG - RMNon exclusive sale

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A snowstorm hits a tourist watching the landscape in Neko

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A snowstorm hits two tourists watching the landscape in Neko Harbour, Antarctica.A snowstorm hits two tourists watching the landscape in Neko Harbour, Antarctica.A snowstorm hits two tourists watching the landscape in Neko Harbour, Antarctica.© Sergio Pitamitz / BiosphotoJPG - RMNon exclusive sale

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A snowstorm hits two tourists watching the landscape in Neko

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A tourist hiking in Neko Harbour, Antarctica.A tourist hiking in Neko Harbour, Antarctica.A tourist hiking in Neko Harbour, Antarctica.© Sergio Pitamitz / BiosphotoJPG - RMNon exclusive sale

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A tourist hiking in Neko Harbour, Antarctica.

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A snowstorm hits tourist in Portal Point, Antarctica.A snowstorm hits tourist in Portal Point, Antarctica.A snowstorm hits tourist in Portal Point, Antarctica.© Sergio Pitamitz / BiosphotoJPG - RMNon exclusive sale

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A snowstorm hits tourist in Portal Point, Antarctica.

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A snowstorm hits tourist in Portal Point, Antarctica.A snowstorm hits tourist in Portal Point, Antarctica.A snowstorm hits tourist in Portal Point, Antarctica.© Sergio Pitamitz / BiosphotoJPG - RMNon exclusive sale

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A snowstorm hits tourist in Portal Point, Antarctica.

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A snowstorm hits tourist in Portal Point, Antarctica.A snowstorm hits tourist in Portal Point, Antarctica.A snowstorm hits tourist in Portal Point, Antarctica.© Sergio Pitamitz / BiosphotoJPG - RMNon exclusive sale

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A snowstorm hits tourist in Portal Point, Antarctica.

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Abandoned house following a slip of the cliff in Quiberville, Seine Maritime, Normandy, FranceAbandoned house following a slip of the cliff in Quiberville, Seine Maritime, Normandy, FranceAbandoned house following a slip of the cliff in Quiberville, Seine Maritime, Normandy, France© Jean-Luc & Françoise Ziegler / BiosphotoJPG - RM

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Abandoned house following a slip of the cliff in Quiberville,

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During snow storms, Adélie penguin (Pygoscelis adeliae) chicks, already weakened by lack of food, are even more vulnerable to Skuas predation. Dumont d'Urville Antarctic Base, Adélie Land, AntarcticaDuring snow storms, Adélie penguin (Pygoscelis adeliae) chicks, already weakened by lack of food, are even more vulnerable to Skuas predation. Dumont d'Urville Antarctic Base, Adélie Land, AntarcticaDuring snow storms, Adélie penguin (Pygoscelis adeliae) chicks, already weakened by lack of food, are even more vulnerable to Skuas predation. Dumont d'Urville Antarctic Base, Adélie Land, Antarctica© Thibaut Vergoz / BiosphotoJPG - RMNon exclusive sale

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During snow storms, Adélie penguin (Pygoscelis adeliae) chicks,

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"White-out" snowstorm at the Antarctic Dumont d'Urville base, Adélie Land, Antarctica"White-out" snowstorm at the Antarctic Dumont d'Urville base, Adélie Land, Antarctica"White-out" snowstorm at the Antarctic Dumont d'Urville base, Adélie Land, Antarctica© Thibaut Vergoz / BiosphotoJPG - RMNon exclusive sale

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"White-out" snowstorm at the Antarctic Dumont d'Urville base,

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In Antarctica Adelie penguins (Pygoscelis adeliae) can be covered with snow during storms. Dumont d'Urville Antarctic Base, Adélie Land, AntarcticaIn Antarctica Adelie penguins (Pygoscelis adeliae) can be covered with snow during storms. Dumont d'Urville Antarctic Base, Adélie Land, AntarcticaIn Antarctica Adelie penguins (Pygoscelis adeliae) can be covered with snow during storms. Dumont d'Urville Antarctic Base, Adélie Land, Antarctica© Thibaut Vergoz / BiosphotoJPG - RMNon exclusive sale

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In Antarctica Adelie penguins (Pygoscelis adeliae) can be covered

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Astrolabe bow caught in a storm on the way back from Antarctica, and on the way to Australia 5 days North Sea, Southern OceanAstrolabe bow caught in a storm on the way back from Antarctica, and on the way to Australia 5 days North Sea, Southern OceanAstrolabe bow caught in a storm on the way back from Antarctica, and on the way to Australia 5 days North Sea, Southern Ocean© Thibaut Vergoz / BiosphotoJPG - RMNon exclusive sale

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Astrolabe bow caught in a storm on the way back from Antarctica,

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Snowstorm blown on Dumont D'urville, Adélie Land, AntarcticaSnowstorm blown on Dumont D'urville, Adélie Land, AntarcticaSnowstorm blown on Dumont D'urville, Adélie Land, Antarctica© Thibaut Vergoz / BiosphotoJPG - RMNon exclusive sale

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Snowstorm blown on Dumont D'urville, Adélie Land, Antarctica

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Doubs river flood in Villers le Lac, Doubs high, Doubs, FranceDoubs river flood in Villers le Lac, Doubs high, Doubs, FranceDoubs river flood in Villers le Lac, Doubs high, Doubs, France© Dominique Delfino / BiosphotoJPG - RM

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Doubs river flood in Villers le Lac, Doubs high, Doubs, France

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