Biosphoto : Agence Photographique spécialisée dans la Nature et l'Environnement

Kelp 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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African 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 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 Monolith on Quiraing - Isle of Skye Trotternish UK ; Mini Storr© Nicolas Orillard-Demaire / BiosphotoJPG - RMSale prohibited by Agents
Sale prohibited for poster and Fine art print worlwide
Use for calendar prohibited

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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 SkyeTree on escarpment and Quiraing - Trotternish Isle of Skye ; Not the one© Nicolas Orillard-Demaire / BiosphotoJPG - RMSale prohibited by Agents
Sale prohibited for poster and Fine art print worlwide
Use for calendar prohibited

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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 centuries

Bristlecone 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 meters

Blackjack 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 - RMUse for calendar cover in France prohibited 31-12-2019

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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 opening© Brandon Cole / BiosphotoJPG - RMSale prohibited by some Agents
Sale prohibited by Agents in the U.S.A., in United Kingdom and in Japan
Sale possible by Agents : Argus Photoland, Auscape, Diomedia, East news, Euro créan, Lineair, Mak Media, Okapia, Other images and Tips

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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 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, 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 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 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, Australia© Cyril Ruoso / BiosphotoJPG - RMNon exclusive sale
Use for exhibitions prohibited

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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 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 Emirates© Xavier Eichaker / BiosphotoJPG - RMSale prohibited in United Arab Emirates
Non exclusive sale, exclusive sale possible in France

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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, Europe© Alfred & Annaliese Trunk / imageBROKER / BiosphotoJPG - RMNon exclusive sale
Sale prohibited by Agents

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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, Europe© Alessandra Sarti / imageBROKER / BiosphotoJPG - RMNon exclusive sale
Sale prohibited by Agents

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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, Africa© Stefan Espenhahn / imageBROKER / BiosphotoJPG - RMNon exclusive sale
Sale prohibited by Agents

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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 Switzerland© Olivier Born / BiosphotoJPG - RMNon exclusive sale

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Ptarmigan moulting on rock - Swiss Alps Switzerland

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Reflection 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, 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, 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, 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, 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, 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, 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, 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, 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, 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, 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, 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, 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, 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, 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, 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, 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 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 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 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 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 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 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 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 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 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 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 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 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 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.© 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 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 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 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.© 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.© Jean-Philippe Delobelle / BiosphotoJPG - RM

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

Right Managed

JPG

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

2437372

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

Right Managed

JPG