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Kelp gull (Larus dominicanus) on streaked iceberg, AntarcticaKelp gull (Larus dominicanus) on streaked iceberg, AntarcticaKelp gull (Larus dominicanus) on streaked iceberg, Antarctica© Raphaël Sané / BiosphotoJPG - RMUse for the promotion of hunting prohibited

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Kelp gull (Larus dominicanus) on streaked iceberg, Antarctica

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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

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

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African Fish Eagle (Haliaeetus vocifer) on cliff at Victoria FallsAfrican Fish Eagle (Haliaeetus vocifer) on cliff at Victoria FallsAfrican Fish Eagle (Haliaeetus vocifer) on cliff at Victoria Falls© Juan-Carlos Muñoz / BiosphotoJPG - RMNon exclusive sale, exclusive sale possible in France

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African Fish Eagle (Haliaeetus vocifer) on cliff at Victoria Falls

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The Old Man of Storr - Isle of Skye Hebrides ScotlandThe Old Man of Storr - Isle of Skye Hebrides ScotlandThe Old Man of Storr - Isle of Skye Hebrides Scotland© Duncan MacArthur / BiosphotoJPG - RM

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The Old Man of Storr - Isle of Skye Hebrides Scotland

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Monolith on Quiraing - Isle of Skye Trotternish UK ; Mini StorrMonolith on Quiraing - Isle of Skye Trotternish UK Monolith on Quiraing - Isle of Skye Trotternish UK ; Mini Storr© Nicolas Orillard-Demaire / BiosphotoJPG - RMSale prohibited by Agents
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Monolith on Quiraing - Isle of Skye Trotternish UK ; Mini Storr

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Tree on escarpment and Quiraing - Trotternish Isle of Skye ; Not the oneTree on escarpment and Quiraing - Trotternish Isle of SkyeTree on escarpment and Quiraing - Trotternish Isle of Skye ; Not the one© Nicolas Orillard-Demaire / BiosphotoJPG - RMSale prohibited by Agents
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2035705

Tree on escarpment and Quiraing - Trotternish Isle of Skye ; Not

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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

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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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Diver into the light shining down through a cenote opening

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Alpine Ibex female and young - Alps Valais Switzerland ; YearlingAlpine Ibex female and young - Alps Valais SwitzerlandAlpine Ibex female and young - Alps Valais Switzerland ; Yearling© Olivier Born / BiosphotoJPG - RMNon exclusive sale

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Alpine Ibex female and young - Alps Valais Switzerland ; Yearling

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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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Morelet's crocodile in a cenote Yucatan MexicoMorelet's crocodile in a cenote Yucatan MexicoMorelet's crocodile in a cenote Yucatan Mexico© Bruno Guénard / BiosphotoJPG - RM

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Morelet's crocodile in a cenote Yucatan Mexico

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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

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Eroded sandstone massif Jaizkibel Basque Country Spain

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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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The 12 Apostles Port Campbell National Park, Australia

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Pair of Chinstrap penguins Antarctic PeninsulaPair of Chinstrap penguins Antarctic PeninsulaPair of Chinstrap penguins Antarctic Peninsula© Sylvain Cordier / BiosphotoJPG - RMNon exclusive sale

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Pair of Chinstrap penguins Antarctic Peninsula

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Run of sand in the dunes United Arab EmiratesRun of sand in the dunes United Arab EmiratesRun of sand in the dunes United Arab Emirates© Xavier Eichaker / BiosphotoJPG - RMSale prohibited in United Arab Emirates
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Run of sand in the dunes United Arab Emirates

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Taugl, Tauglbach flows through gorge, Tauglbachklamm, autumn, Tennengau, Bad Vigaun, Salzburger Land, Austria, EuropeTaugl, Tauglbach flows through gorge, Tauglbachklamm, autumn, Tennengau, Bad Vigaun, Salzburger Land, Austria, EuropeTaugl, Tauglbach flows through gorge, Tauglbachklamm, autumn, Tennengau, Bad Vigaun, Salzburger Land, Austria, Europe© Alfred & Annaliese Trunk / imageBROKER / BiosphotoJPG - RMNon exclusive sale
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Taugl, Tauglbach flows through gorge, Tauglbachklamm, autumn,

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Gorges du Verdon, Verdon Gorge, Parc Naturel Regional du Verdon, Verdon Natural Regional Park, Provence, Provence-Alpes-Cote d'Azur, France, EuropeGorges du Verdon, Verdon Gorge, Parc Naturel Regional du Verdon, Verdon Natural Regional Park, Provence, Provence-Alpes-Cote d'Azur, France, EuropeGorges du Verdon, Verdon Gorge, Parc Naturel Regional du Verdon, Verdon Natural Regional Park, Provence, Provence-Alpes-Cote d'Azur, France, Europe© Alessandra Sarti / imageBROKER / BiosphotoJPG - RMNon exclusive sale
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Gorges du Verdon, Verdon Gorge, Parc Naturel Regional du Verdon,

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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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Mushroom-shaped limestone rock formation, White Desert, Farafra

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Ptarmigan moulting on rock - Swiss Alps SwitzerlandPtarmigan moulting on rock - Swiss Alps SwitzerlandPtarmigan moulting on rock - Swiss Alps Switzerland© Olivier Born / BiosphotoJPG - RMNon exclusive sale

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Ptarmigan moulting on rock - Swiss Alps Switzerland

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Under the islands. Raja Ampat's islands are like Swiss cheese. They are dotted with holes of various shapes. The limestone nature of the islands make them brittle and vulnerable to time which gives strange shapes as illustrated by this panorama. IndonesiaUnder the islands. Raja Ampat's islands are like Swiss cheese. They are dotted with holes of various shapes. The limestone nature of the islands make them brittle and vulnerable to time which gives strange shapes as illustrated by this panorama. IndonesiaUnder the islands. Raja Ampat's islands are like Swiss cheese. They are dotted with holes of various shapes. The limestone nature of the islands make them brittle and vulnerable to time which gives strange shapes as illustrated by this panorama. Indonesia© Gabriel Barathieu / BiosphotoJPG - RM

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Under the islands. Raja Ampat's islands are like Swiss cheese.

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Marine erosion on Las Terrenas beach. Coconut palm roots can no longer hold sand. Samana. Dominican RepublicMarine erosion on Las Terrenas beach. Coconut palm roots can no longer hold sand. Samana. Dominican RepublicMarine erosion on Las Terrenas beach. Coconut palm roots can no longer hold sand. Samana. Dominican Republic© Antoine Lorgnier / BiosphotoJPG - RM

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Marine erosion on Las Terrenas beach. Coconut palm roots can no

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Cliffs of Cap Blanc-nez in winter, Pas de Calais, France. Cliff composed of chalk and marl, constantly receding, because of the incessant assaults of the sea but also as we can see in the foreground of the infiltrations of fresh water which weaken it.Cliffs of Cap Blanc-nez in winter, Pas de Calais, France. Cliff composed of chalk and marl, constantly receding, because of the incessant assaults of the sea but also as we can see in the foreground of the infiltrations of fresh water which weaken it.Cliffs of Cap Blanc-nez in winter, Pas de Calais, France. Cliff composed of chalk and marl, constantly receding, because of the incessant assaults of the sea but also as we can see in the foreground of the infiltrations of fresh water which weaken it.© Yann Avril / BiosphotoJPG - RM

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Cliffs of Cap Blanc-nez in winter, Pas de Calais, France. Cliff

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Meneham Beach, Kerlouan, Pays Pagan, Finistère, Brittany, FranceMeneham Beach, Kerlouan, Pays Pagan, Finistère, Brittany, FranceMeneham Beach, Kerlouan, Pays Pagan, Finistère, Brittany, France© Dominique Delfino / BiosphotoJPG - RM

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Meneham Beach, Kerlouan, Pays Pagan, Finistère, Brittany, France

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Meneham Beach, Kerlouan, Pays Pagan, Finistère, Brittany, FranceMeneham Beach, Kerlouan, Pays Pagan, Finistère, Brittany, FranceMeneham Beach, Kerlouan, Pays Pagan, Finistère, Brittany, France© Dominique Delfino / BiosphotoJPG - RM

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Meneham Beach, Kerlouan, Pays Pagan, Finistère, Brittany, France

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Meneham Beach, Kerlouan, Pays Pagan, Finistère, Brittany, FranceMeneham Beach, Kerlouan, Pays Pagan, Finistère, Brittany, FranceMeneham Beach, Kerlouan, Pays Pagan, Finistère, Brittany, France© Dominique Delfino / BiosphotoJPG - RM

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Meneham Beach, Kerlouan, Pays Pagan, Finistère, Brittany, France

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Meneham Beach, Kerlouan, Pays Pagan, Finistère, Brittany, FranceMeneham Beach, Kerlouan, Pays Pagan, Finistère, Brittany, FranceMeneham Beach, Kerlouan, Pays Pagan, Finistère, Brittany, France© Dominique Delfino / BiosphotoJPG - RM

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Meneham Beach, Kerlouan, Pays Pagan, Finistère, Brittany, France

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Vivant 's Gesse (Lathyrus vivantii), rare species from rocky places, endemic to the western Pyrenees, Pyrenees, FranceVivant 's Gesse (Lathyrus vivantii), rare species from rocky places, endemic to the western Pyrenees, Pyrenees, FranceVivant 's Gesse (Lathyrus vivantii), rare species from rocky places, endemic to the western Pyrenees, Pyrenees, France© Georges Lopez / BiosphotoJPG - RM

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Vivant 's Gesse (Lathyrus vivantii), rare species from rocky

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Pyrenean groundsel (Senecio pyrenaicus) endemic to the Pyrenees, habitat: subalpine lawns on limestone facing the scree of the Pic du Midi d'Ossau, Pyrenees, FrancePyrenean groundsel (Senecio pyrenaicus) endemic to the Pyrenees, habitat: subalpine lawns on limestone facing the scree of the Pic du Midi d'Ossau, Pyrenees, FrancePyrenean groundsel (Senecio pyrenaicus) endemic to the Pyrenees, habitat: subalpine lawns on limestone facing the scree of the Pic du Midi d'Ossau, Pyrenees, France© Georges Lopez / BiosphotoJPG - RM

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Pyrenean groundsel (Senecio pyrenaicus) endemic to the Pyrenees,

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Large-flowered Leopard's Bane (Doronicum grandiflorum), Habitat: large block scree, Subalpine stage, Pyrénées, FranceLarge-flowered Leopard's Bane (Doronicum grandiflorum), Habitat: large block scree, Subalpine stage, Pyrénées, FranceLarge-flowered Leopard's Bane (Doronicum grandiflorum), Habitat: large block scree, Subalpine stage, Pyrénées, France© Georges Lopez / BiosphotoJPG - RM

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Large-flowered Leopard's Bane (Doronicum grandiflorum), Habitat:

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Large-flowered Leopard's Bane (Doronicum grandiflorum), Habitat: large block scree, Subalpine stage, Pyrénées, FranceLarge-flowered Leopard's Bane (Doronicum grandiflorum), Habitat: large block scree, Subalpine stage, Pyrénées, FranceLarge-flowered Leopard's Bane (Doronicum grandiflorum), Habitat: large block scree, Subalpine stage, Pyrénées, France© Georges Lopez / BiosphotoJPG - RM

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Large-flowered Leopard's Bane (Doronicum grandiflorum), Habitat:

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Vierge island, Crozon Peninsula, Brittany, FranceVierge island, Crozon Peninsula, Brittany, FranceVierge island, Crozon Peninsula, Brittany, France© Georges Lopez / BiosphotoJPG - RM

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Vierge island, Crozon Peninsula, Brittany, France

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Vierge island, Crozon Peninsula, Brittany, FranceVierge island, Crozon Peninsula, Brittany, FranceVierge island, Crozon Peninsula, Brittany, France© Georges Lopez / BiosphotoJPG - RM

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Vierge island, Crozon Peninsula, Brittany, France

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Glacier-polished columnar basalt viewed from above, Devils Postpile National Monument, California.Glacier-polished columnar basalt viewed from above, Devils Postpile National Monument, California.Glacier-polished columnar basalt viewed from above, Devils Postpile National Monument, California.© Stuart Wilson / BiosphotoJPG - RMNon exclusive sale

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Glacier-polished columnar basalt viewed from above, Devils

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Pink granite boulders on the coastal path of Olméto, Nature Reserve of the mouths of Bonifacio, Corsica, FrancePink granite boulders on the coastal path of Olméto, Nature Reserve of the mouths of Bonifacio, Corsica, FrancePink granite boulders on the coastal path of Olméto, Nature Reserve of the mouths of Bonifacio, Corsica, France© Georges Lopez / BiosphotoJPG - RM

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Pink granite boulders on the coastal path of Olméto, Nature

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Tafoni along the coastal path of the Gulf of Ventilegne, Natural Reserve of the mouths of Bonifacio, Corsica, FranceTafoni along the coastal path of the Gulf of Ventilegne, Natural Reserve of the mouths of Bonifacio, Corsica, FranceTafoni along the coastal path of the Gulf of Ventilegne, Natural Reserve of the mouths of Bonifacio, Corsica, France© Georges Lopez / BiosphotoJPG - RM

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Tafoni along the coastal path of the Gulf of Ventilegne, Natural

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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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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

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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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The rock of Quiquillon (1025 m) in Orpierre, regional natural park of Baronnies Provençales, Hautes-Alpes, FranceThe rock of Quiquillon (1025 m) in Orpierre, regional natural park of Baronnies Provençales, Hautes-Alpes, FranceThe rock of Quiquillon (1025 m) in Orpierre, regional natural park of Baronnies Provençales, Hautes-Alpes, France© Michel Cavalier / BiosphotoJPG - RM

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The rock of Quiquillon (1025 m) in Orpierre, regional natural

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Creeping Avens (Geum reptans) in a scree at 2793 m altitude, Natural Reserve of the Cirque du Grand Lac des Estaris, Orcieres Merlette, Écrins National Park, Hautes-Alpes, FranceCreeping Avens (Geum reptans) in a scree at 2793 m altitude, Natural Reserve of the Cirque du Grand Lac des Estaris, Orcieres Merlette, Écrins National Park, Hautes-Alpes, FranceCreeping Avens (Geum reptans) in a scree at 2793 m altitude, Natural Reserve of the Cirque du Grand Lac des Estaris, Orcieres Merlette, Écrins National Park, Hautes-Alpes, France© Michel Cavalier / BiosphotoJPG - RM

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Creeping Avens (Geum reptans) in a scree at 2793 m altitude,

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Creeping Avens (Geum reptans) in a scree at 2793 m altitude, Natural Reserve of the Cirque du Grand Lac des Estaris, Orcieres Merlette, Écrins National Park, Hautes-Alpes, FranceCreeping Avens (Geum reptans) in a scree at 2793 m altitude, Natural Reserve of the Cirque du Grand Lac des Estaris, Orcieres Merlette, Écrins National Park, Hautes-Alpes, FranceCreeping Avens (Geum reptans) in a scree at 2793 m altitude, Natural Reserve of the Cirque du Grand Lac des Estaris, Orcieres Merlette, Écrins National Park, Hautes-Alpes, France© Michel Cavalier / BiosphotoJPG - RM

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Creeping Avens (Geum reptans) in a scree at 2793 m altitude,

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Oscillation Ripples at Low Tide, Praia de Amoreira, PortugalOscillation Ripples at Low Tide, Praia de Amoreira, PortugalOscillation Ripples at Low Tide, Praia de Amoreira, Portugal© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Oscillation Ripples at Low Tide, Praia de Amoreira, Portugal

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Oscillation Ripples at Low Tide, Praia de Amoreira, PortugalOscillation Ripples at Low Tide, Praia de Amoreira, PortugalOscillation Ripples at Low Tide, Praia de Amoreira, Portugal© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Oscillation Ripples at Low Tide, Praia de Amoreira, Portugal

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Las Medulas, former mining site dating back to Roman times. This exploitation over several centuries has left a landscape of eroded red hills and underground galleries (canals). The Las Médulas site has been listed as a UNESCO World Heritage Site, Province of Leon, SpainLas Medulas, former mining site dating back to Roman times. This exploitation over several centuries has left a landscape of eroded red hills and underground galleries (canals). The Las Médulas site has been listed as a UNESCO World Heritage Site, Province of Leon, SpainLas Medulas, former mining site dating back to Roman times. This exploitation over several centuries has left a landscape of eroded red hills and underground galleries (canals). The Las Médulas site has been listed as a UNESCO World Heritage Site, Province of Leon, Spain© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Las Medulas, former mining site dating back to Roman times. This

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Erosion in crust of bread on granite, one of the symbols of the Geopark of Arouca, PortugalErosion in crust of bread on granite, one of the symbols of the Geopark of Arouca, PortugalErosion in crust of bread on granite, one of the symbols of the Geopark of Arouca, Portugal© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Erosion in crust of bread on granite, one of the symbols of the

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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

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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

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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

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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

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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

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Spectacular flysch formations in southern Portugal, The flysch

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Erosion Pots on the Portuguese Coast, Praia de Amoreira, PortugalErosion Pots on the Portuguese Coast, Praia de Amoreira, PortugalErosion Pots on the Portuguese Coast, Praia de Amoreira, Portugal© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Erosion Pots on the Portuguese Coast, Praia de Amoreira, Portugal

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Spectacular marine cave of Algar de Benagil, Algarve, PortugalSpectacular marine cave of Algar de Benagil, Algarve, PortugalSpectacular marine cave of Algar de Benagil, Algarve, Portugal© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Spectacular marine cave of Algar de Benagil, Algarve, Portugal

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Spectacular marine cave of Algar de Benagil, Algarve, PortugalSpectacular marine cave of Algar de Benagil, Algarve, PortugalSpectacular marine cave of Algar de Benagil, Algarve, Portugal© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Spectacular marine cave of Algar de Benagil, Algarve, Portugal

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Ponta da Piedade at rising tide, Jagged ocher cliffs, reference landscape of the Algarve, southern province of PortugalPonta da Piedade at rising tide, Jagged ocher cliffs, reference landscape of the Algarve, southern province of PortugalPonta da Piedade at rising tide, Jagged ocher cliffs, reference landscape of the Algarve, southern province of Portugal© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Ponta da Piedade at rising tide, Jagged ocher cliffs, reference

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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

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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

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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

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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

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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

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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

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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

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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

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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

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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

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Geoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque

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Natural Sculptures (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 then sculpted by erosion - the hollow spheres are probably remnants of paramoudra, concretions around worm burrows.Natural Sculptures (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 then sculpted by erosion - the hollow spheres are probably remnants of paramoudra, concretions around worm burrows.Natural Sculptures (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 then sculpted by erosion - the hollow spheres are probably remnants of paramoudra, concretions around worm burrows.© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Natural Sculptures (Geoforms) in Jaizkibel Sandstone, Jaizkibel

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Paramoudras of Jaizkibel, Coastal Massif of Jaizkibel, Basque Country, Spain. Spectacular fossil sandstone concretions formed around the worm burrows living several hundred meters deep, 45 million years ago (Eocene) - These spheres or tubes have a diameter of 20 to 40 cm in diameter and were flexible originallyParamoudras of Jaizkibel, Coastal Massif of Jaizkibel, Basque Country, Spain. Spectacular fossil sandstone concretions formed around the worm burrows living several hundred meters deep, 45 million years ago (Eocene) - These spheres or tubes have a diameter of 20 to 40 cm in diameter and were flexible originallyParamoudras of Jaizkibel, Coastal Massif of Jaizkibel, Basque Country, Spain. Spectacular fossil sandstone concretions formed around the worm burrows living several hundred meters deep, 45 million years ago (Eocene) - These spheres or tubes have a diameter of 20 to 40 cm in diameter and were flexible originally© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Paramoudras of Jaizkibel, Coastal Massif of Jaizkibel, Basque

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Paramoudras of Jaizkibel, Coastal Massif of Jaizkibel, Basque Country, Spain. Spectacular fossil sandstone concretions formed around the worm burrows living several hundred meters deep, 45 million years ago (Eocene) - These spheres or tubes have a diameter of 20 to 40 cm in diameter and were flexible originallyParamoudras of Jaizkibel, Coastal Massif of Jaizkibel, Basque Country, Spain. Spectacular fossil sandstone concretions formed around the worm burrows living several hundred meters deep, 45 million years ago (Eocene) - These spheres or tubes have a diameter of 20 to 40 cm in diameter and were flexible originallyParamoudras of Jaizkibel, Coastal Massif of Jaizkibel, Basque Country, Spain. Spectacular fossil sandstone concretions formed around the worm burrows living several hundred meters deep, 45 million years ago (Eocene) - These spheres or tubes have a diameter of 20 to 40 cm in diameter and were flexible originally© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437376

Paramoudras of Jaizkibel, Coastal Massif of Jaizkibel, Basque

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Paramoudras of Jaizkibel, Coastal Massif of Jaizkibel, Basque Country, Spain. Spectacular fossil sandstone concretions formed around the worm burrows living several hundred meters deep, 45 million years ago (Eocene) - These spheres or tubes have a diameter of 20 to 40 cm in diameter and were flexible originallyParamoudras of Jaizkibel, Coastal Massif of Jaizkibel, Basque Country, Spain. Spectacular fossil sandstone concretions formed around the worm burrows living several hundred meters deep, 45 million years ago (Eocene) - These spheres or tubes have a diameter of 20 to 40 cm in diameter and were flexible originallyParamoudras of Jaizkibel, Coastal Massif of Jaizkibel, Basque Country, Spain. Spectacular fossil sandstone concretions formed around the worm burrows living several hundred meters deep, 45 million years ago (Eocene) - These spheres or tubes have a diameter of 20 to 40 cm in diameter and were flexible originally© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Paramoudras of Jaizkibel, Coastal Massif of Jaizkibel, Basque

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

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

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

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

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

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

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

2437366

Remarkable flysch formations of Deba, Basque Coast Geopark,

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

2437365

Remarkable flysch formations of Deba, Basque Coast Geopark,

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

2437364

Remarkable flysch formations of Deba, Basque Coast Geopark,

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

2437363

Remarkable flysch formations of Deba, Basque Coast Geopark,

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

2437362

Remarkable flysch formations of Deba, Basque Coast Geopark,

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

2437361

Remarkable flysch formations of Deba, Basque Coast Geopark,

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

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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

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

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Remarkable flysch formations of Deba, Basque Coast Geopark,

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Twilight on the Cantabrian coast. Needles of Liencres, near Santander, SpainTwilight on the Cantabrian coast. Needles of Liencres, near Santander, SpainTwilight on the Cantabrian coast. Needles of Liencres, near Santander, Spain© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Twilight on the Cantabrian coast. Needles of Liencres, near

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Petrified quartzite wave from Playa del Silencio, Asturias, Spain. Spectacular variegated and tortured strata of quartzite, sandstone and schists, deformed by the tectonic and dating from the Paleozoic (Cambrian / Ordovician)Petrified quartzite wave from Playa del Silencio, Asturias, Spain. Spectacular variegated and tortured strata of quartzite, sandstone and schists, deformed by the tectonic and dating from the Paleozoic (Cambrian / Ordovician)Petrified quartzite wave from Playa del Silencio, Asturias, Spain. Spectacular variegated and tortured strata of quartzite, sandstone and schists, deformed by the tectonic and dating from the Paleozoic (Cambrian / Ordovician)© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437332

Petrified quartzite wave from Playa del Silencio, Asturias,

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Petrified quartzite wave from Playa del Silencio, Asturias, Spain. Spectacular variegated and tortured strata of quartzite, sandstone and schists, deformed by the tectonic and dating from the Paleozoic (Cambrian / Ordovician)Petrified quartzite wave from Playa del Silencio, Asturias, Spain. Spectacular variegated and tortured strata of quartzite, sandstone and schists, deformed by the tectonic and dating from the Paleozoic (Cambrian / Ordovician)Petrified quartzite wave from Playa del Silencio, Asturias, Spain. Spectacular variegated and tortured strata of quartzite, sandstone and schists, deformed by the tectonic and dating from the Paleozoic (Cambrian / Ordovician)© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Petrified quartzite wave from Playa del Silencio, Asturias,

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Giant's Causeway, columnar basalt columns, result of an ancient volcanic fissure eruption, Northern Ireland, UK, World Heritage siteGiant's Causeway, columnar basalt columns, result of an ancient volcanic fissure eruption, Northern Ireland, UK, World Heritage siteGiant's Causeway, columnar basalt columns, result of an ancient volcanic fissure eruption, Northern Ireland, UK, World Heritage site© John Cancalosi / BiosphotoJPG - RMSale prohibited in Spain and Portugal
Non exclusive sale, exclusive sale possible in France

2436568

Giant's Causeway, columnar basalt columns, result of an ancient

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Giant's Causeway, columnar basalt columns, result of an ancient volcanic fissure eruption, Northern Ireland, UK, World Heritage siteGiant's Causeway, columnar basalt columns, result of an ancient volcanic fissure eruption, Northern Ireland, UK, World Heritage siteGiant's Causeway, columnar basalt columns, result of an ancient volcanic fissure eruption, Northern Ireland, UK, World Heritage site© John Cancalosi / BiosphotoJPG - RMSale prohibited in Spain and Portugal
Non exclusive sale, exclusive sale possible in France

2436567

Giant's Causeway, columnar basalt columns, result of an ancient

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Giant's Causeway, columnar basalt columns, result of an ancient volcanic fissure eruption, Northern Ireland, UK, World Heritage siteGiant's Causeway, columnar basalt columns, result of an ancient volcanic fissure eruption, Northern Ireland, UK, World Heritage siteGiant's Causeway, columnar basalt columns, result of an ancient volcanic fissure eruption, Northern Ireland, UK, World Heritage site© John Cancalosi / BiosphotoJPG - RMSale prohibited in Spain and Portugal
Non exclusive sale, exclusive sale possible in France

2436563

Giant's Causeway, columnar basalt columns, result of an ancient

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Hiking to the Ecrins refuge, crevasse du Glacier Blanc (2875m), Vallouise valley, Briançonnais region, Ecrins National Park, Hautes-Alpes, FranceHiking to the Ecrins refuge, crevasse du Glacier Blanc (2875m), Vallouise valley, Briançonnais region, Ecrins National Park, Hautes-Alpes, FranceHiking to the Ecrins refuge, crevasse du Glacier Blanc (2875m), Vallouise valley, Briançonnais region, Ecrins National Park, Hautes-Alpes, France© Michel Cavalier / BiosphotoJPG - RM

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Hiking to the Ecrins refuge, crevasse du Glacier Blanc (2875m),

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Hiking to the Ecrins refuge, crevasse du Glacier Blanc (2875m), Vallouise valley, Briançonnais region, Ecrins National Park, Hautes-Alpes, FranceHiking to the Ecrins refuge, crevasse du Glacier Blanc (2875m), Vallouise valley, Briançonnais region, Ecrins National Park, Hautes-Alpes, FranceHiking to the Ecrins refuge, crevasse du Glacier Blanc (2875m), Vallouise valley, Briançonnais region, Ecrins National Park, Hautes-Alpes, France© Michel Cavalier / BiosphotoJPG - RM

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Hiking to the Ecrins refuge, crevasse du Glacier Blanc (2875m),

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