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

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Strong eruption at Mount Sinabung generating large pyroclastic flow, August 02, 2017Strong eruption at Mount Sinabung generating large pyroclastic flow, August 02, 2017Strong eruption at Mount Sinabung generating large pyroclastic flow, August 02, 2017© Franck Gueffier / BiosphotoJPG - RM

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Strong eruption at Mount Sinabung generating large pyroclastic

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Strong eruption at Mount Sinabung generating large pyroclastic flow, August 02, 2017Strong eruption at Mount Sinabung generating large pyroclastic flow, August 02, 2017Strong eruption at Mount Sinabung generating large pyroclastic flow, August 02, 2017© Franck Gueffier / BiosphotoJPG - RM

2134953

Strong eruption at Mount Sinabung generating large pyroclastic

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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

1987861

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

1852519

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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1781060

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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1752023

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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1258959

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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1250654

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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1250653

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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2103216

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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1933459

Emperor penguin - Antarctica Southern Ocean ; Emperor penguins in

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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

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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

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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

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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

2436987

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

2436986

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

2434459

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

2434458

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

2434426

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

2434424

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

2432396

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

2431608

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

2431607

"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

2431606

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

2431593

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

2431557

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

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Musk Ox (Ovibos moschatus), in snowstorm, winter, Dovrefjell-Sunndalsfjella-Nationalpark, NorwayMusk Ox (Ovibos moschatus), in snowstorm, winter, Dovrefjell-Sunndalsfjella-Nationalpark, NorwayMusk Ox (Ovibos moschatus), in snowstorm, winter, Dovrefjell-Sunndalsfjella-Nationalpark, Norway© Robert Haasmann / BiosphotoJPG - RMNon exclusive sale

2427119

Musk Ox (Ovibos moschatus), in snowstorm, winter,

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Musk Ox (Ovibos moschatus), bulls in snowstorm, winter, Dovrefjell-Sunndalsfjella-Nationalpark, NorwayMusk Ox (Ovibos moschatus), bulls in snowstorm, winter, Dovrefjell-Sunndalsfjella-Nationalpark, NorwayMusk Ox (Ovibos moschatus), bulls in snowstorm, winter, Dovrefjell-Sunndalsfjella-Nationalpark, Norway© Robert Haasmann / BiosphotoJPG - RMNon exclusive sale

2427118

Musk Ox (Ovibos moschatus), bulls in snowstorm, winter,

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Plantation avalanche protection in Oisans, Ferrand Valley, Ecrins NP, Oisans, Northern Alps, FrancePlantation avalanche protection in Oisans, Ferrand Valley, Ecrins NP, Oisans, Northern Alps, FrancePlantation avalanche protection in Oisans, Ferrand Valley, Ecrins NP, Oisans, Northern Alps, France© Jean-Philippe Delobelle / BiosphotoJPG - RM

2425945

Plantation avalanche protection in Oisans, Ferrand Valley, Ecrins

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Plantation avalanche protection in Oisans, Ferrand Valley, Ecrins NP, Oisans, Northern Alps, FrancePlantation avalanche protection in Oisans, Ferrand Valley, Ecrins NP, Oisans, Northern Alps, FrancePlantation avalanche protection in Oisans, Ferrand Valley, Ecrins NP, Oisans, Northern Alps, France© Jean-Philippe Delobelle / BiosphotoJPG - RM

2425944

Plantation avalanche protection in Oisans, Ferrand Valley, Ecrins

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Rough seas off North Norfolk in winterRough seas off North Norfolk in winterRough seas off North Norfolk in winter© David Tipling / BiosphotoJPG - RMSale prohibited in UK
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2425695

Rough seas off North Norfolk in winter

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Rough seas off North Norfolk in winterRough seas off North Norfolk in winterRough seas off North Norfolk in winter© David Tipling / BiosphotoJPG - RMSale prohibited in UK
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Rough seas off North Norfolk in winter

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Black-headed Gull (Chroicocephalus ridibundus), adults on the shore with rough sea the background, Campania, ItalyBlack-headed Gull (Chroicocephalus ridibundus), adults on the shore with rough sea the background, Campania, ItalyBlack-headed Gull (Chroicocephalus ridibundus), adults on the shore with rough sea the background, Campania, Italy© Saverio Gatto / BiosphotoJPG - RM

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Black-headed Gull (Chroicocephalus ridibundus), adults on the

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Storm on Deception Volcanic Island in South Shetland, AntarcticaStorm on Deception Volcanic Island in South Shetland, AntarcticaStorm on Deception Volcanic Island in South Shetland, Antarctica© Raphaël Sané / BiosphotoJPG - RMUse for the promotion of hunting prohibited

2420966

Storm on Deception Volcanic Island in South Shetland, Antarctica

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Bobcat (Lynx rufus) under snowstorm at Yellowstone NP. USABobcat (Lynx rufus) under snowstorm at Yellowstone NP. USABobcat (Lynx rufus) under snowstorm at Yellowstone NP. USA© Manon Moulis / BiosphotoJPG - RM

2420293

Bobcat (Lynx rufus) under snowstorm at Yellowstone NP. USA

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Black grouse (Lyrurus tetrix) in lek in a snowy bog during a snowstormBlack grouse (Lyrurus tetrix) in lek in a snowy bog during a snowstormBlack grouse (Lyrurus tetrix) in lek in a snowy bog during a snowstorm© Christophe Perelle / BiosphotoJPG - RM

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Black grouse (Lyrurus tetrix) in lek in a snowy bog during a

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Alpine Chamois (Rupicapra rupicapra) in a snowstorm, Jura, Switzerland.Alpine Chamois (Rupicapra rupicapra) in a snowstorm, Jura, Switzerland.Alpine Chamois (Rupicapra rupicapra) in a snowstorm, Jura, Switzerland.© Olivier Born / BiosphotoJPG - RM

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Alpine Chamois (Rupicapra rupicapra) in a snowstorm, Jura,

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Mountain Hare (Lepus timidus) at winter white coat in snow, Alps, Switzerland.Mountain Hare (Lepus timidus) at winter white coat in snow, Alps, Switzerland.Mountain Hare (Lepus timidus) at winter white coat in snow, Alps, Switzerland.© Olivier Born / BiosphotoJPG - RM

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Mountain Hare (Lepus timidus) at winter white coat in snow, Alps,

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Lowering of the water level of Lake Annecy in October 2018 following a major drought in Haute Savoie, FranceLowering of the water level of Lake Annecy in October 2018 following a major drought in Haute Savoie, FranceLowering of the water level of Lake Annecy in October 2018 following a major drought in Haute Savoie, France© Jean-Luc & Françoise Ziegler / BiosphotoJPG - RM

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Lowering of the water level of Lake Annecy in October 2018

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Lowering of the water level of Lake Annecy in October 2018 following a major drought in Haute Savoie, FranceLowering of the water level of Lake Annecy in October 2018 following a major drought in Haute Savoie, FranceLowering of the water level of Lake Annecy in October 2018 following a major drought in Haute Savoie, France© Jean-Luc & Françoise Ziegler / BiosphotoJPG - RM

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Lowering of the water level of Lake Annecy in October 2018

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Lowering of the water level of Lake Annecy in October 2018 following a major drought in Haute Savoie, FranceLowering of the water level of Lake Annecy in October 2018 following a major drought in Haute Savoie, FranceLowering of the water level of Lake Annecy in October 2018 following a major drought in Haute Savoie, France© Jean-Luc & Françoise Ziegler / BiosphotoJPG - RM

2411124

Lowering of the water level of Lake Annecy in October 2018

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Baisse du niveau d'eau du lac de Vouglans en octobre 2018 suite à une sécheresse importante dans le Jura, FranceBaisse du niveau d'eau du lac de Vouglans en octobre 2018 suite à une sécheresse importante dans le Jura, FranceBaisse du niveau d'eau du lac de Vouglans en octobre 2018 suite à une sécheresse importante dans le Jura, France© Jean-Luc & Françoise Ziegler / BiosphotoJPG - RM

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Baisse du niveau d'eau du lac de Vouglans en octobre 2018 suite

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Grey Seal (Halichoerus grypus). A Grey Seal changes angle to avoid the incoming sandstorm off the coast of Lincolnshire in the UK.Grey Seal (Halichoerus grypus). A Grey Seal changes angle to avoid the incoming sandstorm off the coast of Lincolnshire in the UK.Grey Seal (Halichoerus grypus). A Grey Seal changes angle to avoid the incoming sandstorm off the coast of Lincolnshire in the UK.© Tesni Ward / BiosphotoJPG - RM

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Grey Seal (Halichoerus grypus). A Grey Seal changes angle to

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Grey Seal (Halichoerus grypus). A Grey Seal tolerates an ongoing sandstorm off the coast of Lincolnshire in the UK.Grey Seal (Halichoerus grypus). A Grey Seal tolerates an ongoing sandstorm off the coast of Lincolnshire in the UK.Grey Seal (Halichoerus grypus). A Grey Seal tolerates an ongoing sandstorm off the coast of Lincolnshire in the UK.© Tesni Ward / BiosphotoJPG - RM

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Grey Seal (Halichoerus grypus). A Grey Seal tolerates an ongoing

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Dry Ain River Source, Conte, Jura, FranceDry Ain River Source, Conte, Jura, FranceDry Ain River Source, Conte, Jura, France© Frédéric Tournay / BiosphotoJPG - RM

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Dry Ain River Source, Conte, Jura, France

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Dry Ain River Source, Conte, Jura, FranceDry Ain River Source, Conte, Jura, FranceDry Ain River Source, Conte, Jura, France© Frédéric Tournay / BiosphotoJPG - RM

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Dry Ain River Source, Conte, Jura, France

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Norway spruce (Picea abies) grazed by cattle, Mont d'Or, Métabief, Doubs, FranceNorway spruce (Picea abies) grazed by cattle, Mont d'Or, Métabief, Doubs, FranceNorway spruce (Picea abies) grazed by cattle, Mont d'Or, Métabief, Doubs, France© Frédéric Tournay / BiosphotoJPG - RM

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Norway spruce (Picea abies) grazed by cattle, Mont d'Or,

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Avalanche barrier, Mont d'Or, Métabief, Doubs, FranceAvalanche barrier, Mont d'Or, Métabief, Doubs, FranceAvalanche barrier, Mont d'Or, Métabief, Doubs, France© Frédéric Tournay / BiosphotoJPG - RM

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Avalanche barrier, Mont d'Or, Métabief, Doubs, France

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Emperor Penguins (Aptenodytes forsteri), young huddling together to form a creche to keep warm, during storm, Dawson Lambton Glacier, Weddell Sea, AntarcticaEmperor Penguins (Aptenodytes forsteri), young huddling together to form a creche to keep warm, during storm, Dawson Lambton Glacier, Weddell Sea, AntarcticaEmperor Penguins (Aptenodytes forsteri), young huddling together to form a creche to keep warm, during storm, Dawson Lambton Glacier, Weddell Sea, Antarctica© David Tipling / BiosphotoJPG - RMSale prohibited in UK
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Emperor Penguins (Aptenodytes forsteri), young huddling together

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View towards Weybourne from Salthouse North Norfolk of rough seas during gale force northerly winds OctoberView towards Weybourne from Salthouse North Norfolk of rough seas during gale force northerly winds OctoberView towards Weybourne from Salthouse North Norfolk of rough seas during gale force northerly winds October© David Tipling / BiosphotoJPG - RMSale prohibited in UK
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View towards Weybourne from Salthouse North Norfolk of rough seas

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Avalanche in AntarcticaAvalanche in AntarcticaAvalanche in Antarctica© Raphaël Sané / BiosphotoJPG - RMUse for the promotion of hunting prohibited

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Avalanche in Antarctica

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Tsunami Evacuation Road, Near Homer Harbor, Kenai Peninsula, Alaska,Tsunami Evacuation Road, Near Homer Harbor, Kenai Peninsula, Alaska,Tsunami Evacuation Road, Near Homer Harbor, Kenai Peninsula, Alaska,© Robert Valarcher / BiosphotoJPG - RM

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Tsunami Evacuation Road, Near Homer Harbor, Kenai Peninsula,

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