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The Cheran gorges in autumn, River draining the Bauges massif, to Hery sur Alby, Savoie, Alps, FranceThe Cheran gorges in autumn, River draining the Bauges massif, to Hery sur Alby, Savoie, Alps, FranceThe Cheran gorges in autumn, River draining the Bauges massif, to Hery sur Alby, Savoie, Alps, France© Jean-Philippe Delobelle / BiosphotoJPG - RM

2172561

The Cheran gorges in autumn, River draining the Bauges massif, to

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Bristlecone pine multimillennial - Cedar Breaks NM Utah USA ; Older than 2000 years<br>Pines growing at very high altitude (3000 m) and can survive more than 4500 years;they are generally observed in the combat zone, where no other species can survive extreme conditions, and their roots are slowly exposed by erosion over the centuriesBristlecone pine multimillennial - Cedar Breaks NM Utah USABristlecone pine multimillennial - Cedar Breaks NM Utah USA ; Older than 2000 years
Pines growing at very high altitude (3000 m) and can survive more than 4500 years;they are generally observed in the combat zone, where no other species can survive extreme conditions, and their roots are slowly exposed by erosion over the centuries
© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Bristlecone pine multimillennial - Cedar Breaks NM Utah USA ;

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Blackjack pines and Hoodoos - Bryce Canyon NP Utah USA ; Amphiteatre<br>Deltaic sediments of Jurassic age (Claron Formation) of sandstone, dolomite and marl colored by iron oxides and carved by erosion in an amphitheater of hoodoos (pinnacles) arches and bridgesThe reflected light (spectral) from sunrise sun enriched natural polychrome these high walls sometimes nearly 50 metersBlackjack pines and Hoodoos - Bryce Canyon NP Utah USABlackjack pines and Hoodoos - Bryce Canyon NP Utah USA ; Amphiteatre
Deltaic sediments of Jurassic age (Claron Formation) of sandstone, dolomite and marl colored by iron oxides and carved by erosion in an amphitheater of hoodoos (pinnacles) arches and bridgesThe reflected light (spectral) from sunrise sun enriched natural polychrome these high walls sometimes nearly 50 meters
© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Blackjack pines and Hoodoos - Bryce Canyon NP Utah USA ;

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Dome Navajo sandstone - Grand Staircase-Escalante NM Utah ; Petrified wave<br>The Navajo Sandstone is from wind (petrified dunes) and date from the early Jurassic (desert on the west side of Pangaea)Dome Navajo sandstone - Grand Staircase-Escalante NM UtahDome Navajo sandstone - Grand Staircase-Escalante NM Utah ; Petrified wave
The Navajo Sandstone is from wind (petrified dunes) and date from the early Jurassic (desert on the west side of Pangaea)
© Jean-Philippe Delobelle / BiosphotoJPG - RM

2033183

Dome Navajo sandstone - Grand Staircase-Escalante NM Utah ;

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Diver into the light shining down through a cenote openingDiver into the light shining down through a cenote openingDiver into the light shining down through a cenote opening© Brandon Cole / BiosphotoJPG - RMSale prohibited by some Agents
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2031432

Diver into the light shining down through a cenote opening

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The 12 Apostles Port Campbell National Park, AustraliaThe 12 Apostles Port Campbell National Park, AustraliaThe 12 Apostles Port Campbell National Park, Australia© Edouard Bense / BiosphotoJPG - RM

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The 12 Apostles Port Campbell National Park, Australia

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Eroded sandstone massif Jaizkibel Basque Country SpainEroded sandstone massif Jaizkibel Basque Country SpainEroded sandstone massif Jaizkibel Basque Country Spain© Juan-Carlos Muñoz / BiosphotoJPG - RMNon exclusive sale, exclusive sale possible in France

1871696

Eroded sandstone massif Jaizkibel Basque Country Spain

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Two couple of Bee-eaters perching on branch in loess cliffTwo couple of Bee-eaters perching on branch in loess cliffTwo couple of Bee-eaters perching on branch in loess cliff© Berndt Fischer / BiosphotoJPG - RM

1174171

Two couple of Bee-eaters perching on branch in loess cliff

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The 12 Apostles Port Campbell National Park, AustraliaThe 12 Apostles Port Campbell National Park, AustraliaThe 12 Apostles Port Campbell National Park, Australia© Cyril Ruoso / BiosphotoJPG - RMNon exclusive sale
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521090

The 12 Apostles Port Campbell National Park, Australia

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Mushroom-shaped limestone rock formation, White Desert, Farafra Oasis, Libyan Desert, also known as Western Desert, Sahara, Egypt, AfricaMushroom-shaped limestone rock formation, White Desert, Farafra Oasis, Libyan Desert, also known as Western Desert, Sahara, Egypt, AfricaMushroom-shaped limestone rock formation, White Desert, Farafra Oasis, Libyan Desert, also known as Western Desert, Sahara, Egypt, Africa© Stefan Espenhahn / imageBROKER / BiosphotoJPG - RMNon exclusive sale
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2093801

Mushroom-shaped limestone rock formation, White Desert, Farafra

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Chaos of Nîmes-le-vieux, Causse Méjean, Cévennes, Lozère, FranceChaos of Nîmes-le-vieux, Causse Méjean, Cévennes, Lozère, FranceChaos of Nîmes-le-vieux, Causse Méjean, Cévennes, Lozère, France© Jean-Paul Chatagnon / BiosphotoJPG - RM

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Chaos of Nîmes-le-vieux, Causse Méjean, Cévennes, Lozère,

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Chaos of Nîmes-le-vieux, Causse Méjean, Cévennes, Lozère, FranceChaos of Nîmes-le-vieux, Causse Méjean, Cévennes, Lozère, FranceChaos of Nîmes-le-vieux, Causse Méjean, Cévennes, Lozère, France© Jean-Paul Chatagnon / BiosphotoJPG - RM

2454912

Chaos of Nîmes-le-vieux, Causse Méjean, Cévennes, Lozère,

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Mallos de Riglos, Pyrenees, Aragon, SpainMallos de Riglos, Pyrenees, Aragon, SpainMallos de Riglos, Pyrenees, Aragon, Spain© Georges Lopez / BiosphotoJPG - RM

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Mallos de Riglos, Pyrenees, Aragon, Spain

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Dalle aux Arenaygues = stone flowers witnessing the Devonian 360million years ago. Jean Pierre Dugène discovered it in 2010. Rare circular structures with a radiating shape reminiscent of a cartwheel. In the center of the structure is the opening of a chimney for the escape of water and sand, fossilized. These structures were created during an earthquake in sediments of detrital origin deposited in the shallow sea. These 'Arenaygues' are considered to be the most characteristic and best preserved specimens in the world. Ossau Valley, Pyrenees, FranceDalle aux Arenaygues = stone flowers witnessing the Devonian 360million years ago. Jean Pierre Dugène discovered it in 2010. Rare circular structures with a radiating shape reminiscent of a cartwheel. In the center of the structure is the opening of a chimney for the escape of water and sand, fossilized. These structures were created during an earthquake in sediments of detrital origin deposited in the shallow sea. These 'Arenaygues' are considered to be the most characteristic and best preserved specimens in the world. Ossau Valley, Pyrenees, FranceDalle aux Arenaygues = stone flowers witnessing the Devonian 360million years ago. Jean Pierre Dugène discovered it in 2010. Rare circular structures with a radiating shape reminiscent of a cartwheel. In the center of the structure is the opening of a chimney for the escape of water and sand, fossilized. These structures were created during an earthquake in sediments of detrital origin deposited in the shallow sea. These 'Arenaygues' are considered to be the most characteristic and best preserved specimens in the world. Ossau Valley, Pyrenees, France© Georges Lopez / BiosphotoJPG - RM

2452354

Dalle aux Arenaygues = stone flowers witnessing the Devonian

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Dalle aux Arenaygues = stone flowers witnessing the Devonian 360million years ago. Jean Pierre Dugène discovered it in 2010. Rare circular structures with a radiating shape reminiscent of a cartwheel. In the center of the structure is the opening of a chimney for the escape of water and sand, fossilized. These structures were created during an earthquake in sediments of detrital origin deposited in the shallow sea. These 'Arenaygues' are considered to be the most characteristic and best preserved specimens in the world. Ossau Valley, Pyrenees, FranceDalle aux Arenaygues = stone flowers witnessing the Devonian 360million years ago. Jean Pierre Dugène discovered it in 2010. Rare circular structures with a radiating shape reminiscent of a cartwheel. In the center of the structure is the opening of a chimney for the escape of water and sand, fossilized. These structures were created during an earthquake in sediments of detrital origin deposited in the shallow sea. These 'Arenaygues' are considered to be the most characteristic and best preserved specimens in the world. Ossau Valley, Pyrenees, FranceDalle aux Arenaygues = stone flowers witnessing the Devonian 360million years ago. Jean Pierre Dugène discovered it in 2010. Rare circular structures with a radiating shape reminiscent of a cartwheel. In the center of the structure is the opening of a chimney for the escape of water and sand, fossilized. These structures were created during an earthquake in sediments of detrital origin deposited in the shallow sea. These 'Arenaygues' are considered to be the most characteristic and best preserved specimens in the world. Ossau Valley, Pyrenees, France© Georges Lopez / BiosphotoJPG - RM

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Dalle aux Arenaygues = stone flowers witnessing the Devonian

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Grand Canyon du Verdon viewed from the left bank, Verdon Regional Natural Park, Var, FranceGrand Canyon du Verdon viewed from the left bank, Verdon Regional Natural Park, Var, FranceGrand Canyon du Verdon viewed from the left bank, Verdon Regional Natural Park, Var, France© Michel Cavalier / BiosphotoJPG - RM

2448386

Grand Canyon du Verdon viewed from the left bank, Verdon Regional

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Grand Canyon du Verdon viewed from the left bank, Verdon Regional Natural Park, Var, FranceGrand Canyon du Verdon viewed from the left bank, Verdon Regional Natural Park, Var, FranceGrand Canyon du Verdon viewed from the left bank, Verdon Regional Natural Park, Var, France© Michel Cavalier / BiosphotoJPG - RM

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Grand Canyon du Verdon viewed from the left bank, Verdon Regional

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Grand Canyon du Verdon viewed from the left bank, Verdon Regional Natural Park, Var, FranceGrand Canyon du Verdon viewed from the left bank, Verdon Regional Natural Park, Var, FranceGrand Canyon du Verdon viewed from the left bank, Verdon Regional Natural Park, Var, France© Michel Cavalier / BiosphotoJPG - RM

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Grand Canyon du Verdon viewed from the left bank, Verdon Regional

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Grand Canyon du Verdon, Sainte Croix lake, Verdon regional natural park, Var, FranceGrand Canyon du Verdon, Sainte Croix lake, Verdon regional natural park, Var, FranceGrand Canyon du Verdon, Sainte Croix lake, Verdon regional natural park, Var, France© Michel Cavalier / BiosphotoJPG - RM

2448383

Grand Canyon du Verdon, Sainte Croix lake, Verdon regional

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Grand Canyon du Verdon, Sainte Croix lake, Verdon regional natural park, Var, FranceGrand Canyon du Verdon, Sainte Croix lake, Verdon regional natural park, Var, FranceGrand Canyon du Verdon, Sainte Croix lake, Verdon regional natural park, Var, France© Michel Cavalier / BiosphotoJPG - RM

2448380

Grand Canyon du Verdon, Sainte Croix lake, Verdon regional

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Grand Canyon du Verdon, Sainte Croix lake, Verdon regional natural park, Var, FranceGrand Canyon du Verdon, Sainte Croix lake, Verdon regional natural park, Var, FranceGrand Canyon du Verdon, Sainte Croix lake, Verdon regional natural park, Var, France© Michel Cavalier / BiosphotoJPG - RM

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Grand Canyon du Verdon, Sainte Croix lake, Verdon regional

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Grand Canyon du Verdon, the Verdon river after a snowfall, Verdon regional natural park, Alpes-de-Haute-Provence, FranceGrand Canyon du Verdon, the Verdon river after a snowfall, Verdon regional natural park, Alpes-de-Haute-Provence, FranceGrand Canyon du Verdon, the Verdon river after a snowfall, Verdon regional natural park, Alpes-de-Haute-Provence, France© Michel Cavalier / BiosphotoJPG - RM

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Grand Canyon du Verdon, the Verdon river after a snowfall, Verdon

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Grand Canyon du Verdon, green waters of Verdon, regional natural park of Verdon, Alpes-de-Haute-Provence, FranceGrand Canyon du Verdon, green waters of Verdon, regional natural park of Verdon, Alpes-de-Haute-Provence, FranceGrand Canyon du Verdon, green waters of Verdon, regional natural park of Verdon, Alpes-de-Haute-Provence, France© Michel Cavalier / BiosphotoJPG - RM

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Grand Canyon du Verdon, green waters of Verdon, regional natural

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The Gorges du Loup and the village of Courmes, Préalpes d'Azur Regional Natural Park, Alpes-Maritimes, FranceThe Gorges du Loup and the village of Courmes, Préalpes d'Azur Regional Natural Park, Alpes-Maritimes, FranceThe Gorges du Loup and the village of Courmes, Préalpes d'Azur Regional Natural Park, Alpes-Maritimes, France© Michel Cavalier / BiosphotoJPG - RM

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The Gorges du Loup and the village of Courmes, Préalpes d'Azur

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Meadow with Laburnum, Caussols plateau, Préalpes d'Azur Regional Natural Park, Alpes-Maritimes, FranceMeadow with Laburnum, Caussols plateau, Préalpes d'Azur Regional Natural Park, Alpes-Maritimes, FranceMeadow with Laburnum, Caussols plateau, Préalpes d'Azur Regional Natural Park, Alpes-Maritimes, France© Michel Cavalier / BiosphotoJPG - RM

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Meadow with Laburnum, Caussols plateau, Préalpes d'Azur Regional

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Helminthoid flysch, Traces of fossil activity characteristic of flysch in the Embrun region, Vallon du Rabioux, Ecrins National Park, Hautes Alpes, FranceHelminthoid flysch, Traces of fossil activity characteristic of flysch in the Embrun region, Vallon du Rabioux, Ecrins National Park, Hautes Alpes, FranceHelminthoid flysch, Traces of fossil activity characteristic of flysch in the Embrun region, Vallon du Rabioux, Ecrins National Park, Hautes Alpes, France© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Helminthoid flysch, Traces of fossil activity characteristic of

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Flysch from Pic de Goléon, the Aiguille du Goléon is a pyramid cut entirely in the nummulitic flysch, Ecrins National Park, north of La Grave, Alps, FranceFlysch from Pic de Goléon, the Aiguille du Goléon is a pyramid cut entirely in the nummulitic flysch, Ecrins National Park, north of La Grave, Alps, FranceFlysch from Pic de Goléon, the Aiguille du Goléon is a pyramid cut entirely in the nummulitic flysch, Ecrins National Park, north of La Grave, Alps, France© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Flysch from Pic de Goléon, the Aiguille du Goléon is a pyramid

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Flyschs (clay limestone) erupted by frost and sun, Samoëns, Haute-Savoie, Alps, FranceFlyschs (clay limestone) erupted by frost and sun, Samoëns, Haute-Savoie, Alps, FranceFlyschs (clay limestone) erupted by frost and sun, Samoëns, Haute-Savoie, Alps, France© Michel Rauch / BiosphotoJPG - RM

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Flyschs (clay limestone) erupted by frost and sun, Samoëns,

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Colorado Provencal, Rustrel, Vaucluse, FranceColorado Provencal, Rustrel, Vaucluse, FranceColorado Provencal, Rustrel, Vaucluse, France© Frédéric Tournay / BiosphotoJPG - RM

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Colorado Provencal, Rustrel, Vaucluse, France

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Colorado Provencal, Rustrel, Vaucluse, FranceColorado Provencal, Rustrel, Vaucluse, FranceColorado Provencal, Rustrel, Vaucluse, France© Frédéric Tournay / BiosphotoJPG - RM

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Colorado Provencal, Rustrel, Vaucluse, France

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Colorado Provencal, Rustrel, Vaucluse, FranceColorado Provencal, Rustrel, Vaucluse, FranceColorado Provencal, Rustrel, Vaucluse, France© Frédéric Tournay / BiosphotoJPG - RM

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Colorado Provencal, Rustrel, Vaucluse, France

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Maritime pine (Pinus pinaster), Colorado de Rustrel, Vaucluse, FranceMaritime pine (Pinus pinaster), Colorado de Rustrel, Vaucluse, FranceMaritime pine (Pinus pinaster), Colorado de Rustrel, Vaucluse, France© Frédéric Tournay / BiosphotoJPG - RM

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Maritime pine (Pinus pinaster), Colorado de Rustrel, Vaucluse,

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Aiguier du jas du pin, Luberon, Vaucluse, Provence, FranceAiguier du jas du pin, Luberon, Vaucluse, Provence, FranceAiguier du jas du pin, Luberon, Vaucluse, Provence, France© David Tatin / BiosphotoJPG - RM

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Aiguier du jas du pin, Luberon, Vaucluse, Provence, France

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Reflection of the sand mountains in Bardenas Reales, Navarra, SpainReflection of the sand mountains in Bardenas Reales, Navarra, SpainReflection of the sand mountains in Bardenas Reales, Navarra, Spain© David Jerez / BiosphotoJPG - RMNon exclusive sale

2438482

Reflection of the sand mountains in Bardenas Reales, Navarra,

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Falkenstein alveolate sandstone, autumn, Moselle, FranceFalkenstein alveolate sandstone, autumn, Moselle, FranceFalkenstein alveolate sandstone, autumn, Moselle, France© Yann Avril / BiosphotoJPG - RM

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Falkenstein alveolate sandstone, autumn, Moselle, France

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Spectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, PortugalSpectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, PortugalSpectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, Portugal© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437622

Spectacular flysch formations in southern Portugal, The flysch

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Spectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, PortugalSpectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, PortugalSpectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, Portugal© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437621

Spectacular flysch formations in southern Portugal, The flysch

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Spectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, PortugalSpectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, PortugalSpectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, Portugal© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437620

Spectacular flysch formations in southern Portugal, The flysch

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Spectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, PortugalSpectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, PortugalSpectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, Portugal© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437619

Spectacular flysch formations in southern Portugal, The flysch

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Spectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, PortugalSpectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, PortugalSpectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, Portugal© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437618

Spectacular flysch formations in southern Portugal, The flysch

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Gallery of Las Medulas, old Roman gold mine, Province of Leon, SpainGallery of Las Medulas, old Roman gold mine, Province of Leon, SpainGallery of Las Medulas, old Roman gold mine, Province of Leon, Spain© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Gallery of Las Medulas, old Roman gold mine, Province of Leon,

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Natural Sculptures (Geoforms) in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated then sculpted by erosion - the hollow spheres are probably remains of paramoudra, concretions around worm burrowsNatural Sculptures (Geoforms) in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated then sculpted by erosion - the hollow spheres are probably remains of paramoudra, concretions around worm burrowsNatural Sculptures (Geoforms) in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated then sculpted by erosion - the hollow spheres are probably remains of paramoudra, concretions around worm burrows© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437390

Natural Sculptures (Geoforms) in Jaizkibel Sandstone, Jaizkibel

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Natural Sculptures (Geoforms) in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated then sculpted by erosion - the hollow spheres are probably remains of paramoudra, concretions around worm burrowsNatural Sculptures (Geoforms) in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated then sculpted by erosion - the hollow spheres are probably remains of paramoudra, concretions around worm burrowsNatural Sculptures (Geoforms) in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated then sculpted by erosion - the hollow spheres are probably remains of paramoudra, concretions around worm burrows© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437389

Natural Sculptures (Geoforms) in Jaizkibel Sandstone, Jaizkibel

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Natural Sculptures (Geoforms) in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated then sculpted by erosion - the hollow spheres are probably remains of paramoudra, concretions around worm burrowsNatural Sculptures (Geoforms) in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated then sculpted by erosion - the hollow spheres are probably remains of paramoudra, concretions around worm burrowsNatural Sculptures (Geoforms) in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated then sculpted by erosion - the hollow spheres are probably remains of paramoudra, concretions around worm burrows© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437388

Natural Sculptures (Geoforms) in Jaizkibel Sandstone, Jaizkibel

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Natural Sculptures (Geoforms) in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated then sculpted by erosion - the hollow spheres are probably remains of paramoudra, concretions around worm burrowsNatural Sculptures (Geoforms) in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated then sculpted by erosion - the hollow spheres are probably remains of paramoudra, concretions around worm burrowsNatural Sculptures (Geoforms) in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated then sculpted by erosion - the hollow spheres are probably remains of paramoudra, concretions around worm burrows© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437387

Natural Sculptures (Geoforms) in Jaizkibel Sandstone, Jaizkibel

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Geoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque Country, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated by erosion - the yellow discs are undoubtedly remains of paramoudra, concretions around the worm burrowsGeoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque Country, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated by erosion - the yellow discs are undoubtedly remains of paramoudra, concretions around the worm burrowsGeoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque Country, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated by erosion - the yellow discs are undoubtedly remains of paramoudra, concretions around the worm burrows© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437386

Geoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque

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Geoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque Country, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated by erosion - the yellow discs are undoubtedly remains of paramoudra, concretions around the worm burrowsGeoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque Country, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated by erosion - the yellow discs are undoubtedly remains of paramoudra, concretions around the worm burrowsGeoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque Country, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated by erosion - the yellow discs are undoubtedly remains of paramoudra, concretions around the worm burrows© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437385

Geoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque

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Geoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque Country, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated by erosion - the yellow discs are undoubtedly remains of paramoudra, concretions around the worm burrowsGeoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque Country, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated by erosion - the yellow discs are undoubtedly remains of paramoudra, concretions around the worm burrowsGeoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque Country, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated by erosion - the yellow discs are undoubtedly remains of paramoudra, concretions around the worm burrows© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437384

Geoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque

RMRight Managed

JPG

LightboxDownload low resolution image

Geoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque Country, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated by erosion - the yellow discs are undoubtedly remains of paramoudra, concretions around the worm burrowsGeoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque Country, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated by erosion - the yellow discs are undoubtedly remains of paramoudra, concretions around the worm burrowsGeoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque Country, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated by erosion - the yellow discs are undoubtedly remains of paramoudra, concretions around the worm burrows© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437383

Geoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque

RMRight Managed

JPG

LightboxDownload low resolution image

Geoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque Country, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated by erosion - the yellow discs are undoubtedly remains of paramoudra, concretions around the worm burrowsGeoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque Country, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated by erosion - the yellow discs are undoubtedly remains of paramoudra, concretions around the worm burrowsGeoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque Country, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated by erosion - the yellow discs are undoubtedly remains of paramoudra, concretions around the worm burrows© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437382

Geoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque

RMRight Managed

JPG

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