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Aerial View, Geological Landscape, Lastras de las Heras, Valle de Losa, Junta de Traslaloma, Las Merindades, Burgos, Castilla y Leon, Spain, EuropeAerial View, Geological Landscape, Lastras de las Heras, Valle de Losa, Junta de Traslaloma, Las Merindades, Burgos, Castilla y Leon, Spain, EuropeAerial View, Geological Landscape, Lastras de las Heras, Valle de Losa, Junta de Traslaloma, Las Merindades, Burgos, Castilla y Leon, Spain, Europe© Juan-Carlos Muñoz / BiosphotoJPG - RMNon exclusive sale, exclusive sale possible in France

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Aerial View, Geological Landscape, Lastras de las Heras, Valle de

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Pattern, Texture, Landscape in Tolar Grande, La Puna, Argentina, South America, AmericaPattern, Texture, Landscape in Tolar Grande, La Puna, Argentina, South America, AmericaPattern, Texture, Landscape in Tolar Grande, La Puna, Argentina, South America, America© Juan-Carlos Muñoz / BiosphotoJPG - RMNon exclusive sale, exclusive sale possible in France

2452584

Pattern, Texture, Landscape in Tolar Grande, La Puna, Argentina,

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Pattern, Texture, Landscape in Tolar Grande, La Puna, Argentina, South America, AmericaPattern, Texture, Landscape in Tolar Grande, La Puna, Argentina, South America, AmericaPattern, Texture, Landscape in Tolar Grande, La Puna, Argentina, South America, America© Juan-Carlos Muñoz / BiosphotoJPG - RMNon exclusive sale, exclusive sale possible in France

2452583

Pattern, Texture, Landscape in Tolar Grande, La Puna, Argentina,

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Pattern, Texture, Landscape in Tolar Grande, La Puna, Argentina, South America, AmericaPattern, Texture, Landscape in Tolar Grande, La Puna, Argentina, South America, AmericaPattern, Texture, Landscape in Tolar Grande, La Puna, Argentina, South America, America© Juan-Carlos Muñoz / BiosphotoJPG - RMNon exclusive sale, exclusive sale possible in France

2452582

Pattern, Texture, Landscape in Tolar Grande, La Puna, Argentina,

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Pattern, Texture, Landscape in Tolar Grande, La Puna, Argentina, South America, AmericaPattern, Texture, Landscape in Tolar Grande, La Puna, Argentina, South America, AmericaPattern, Texture, Landscape in Tolar Grande, La Puna, Argentina, South America, America© Juan-Carlos Muñoz / BiosphotoJPG - RMNon exclusive sale, exclusive sale possible in France

2452581

Pattern, Texture, Landscape in Tolar Grande, La Puna, Argentina,

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Geological formation of Cordillera Huayhuash, Andes, PeruGeological formation of Cordillera Huayhuash, Andes, PeruGeological formation of Cordillera Huayhuash, Andes, Peru© Raphaël Sané / BiosphotoJPG - RMUse for the promotion of hunting prohibited

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Geological formation of Cordillera Huayhuash, Andes, Peru

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Calanques de Piana: Geological formation of pink porphyry carved by the wind, Corsica, FranceCalanques de Piana: Geological formation of pink porphyry carved by the wind, Corsica, FranceCalanques de Piana: Geological formation of pink porphyry carved by the wind, Corsica, France© Georges Lopez / BiosphotoJPG - RM

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Calanques de Piana: Geological formation of pink porphyry carved

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Calanques de Piana: Geological formation of plutonic rocks sculpted by marine winds: (pink porphyry), Sector of Porto, Corsica, FranceCalanques de Piana: Geological formation of plutonic rocks sculpted by marine winds: (pink porphyry), Sector of Porto, Corsica, FranceCalanques de Piana: Geological formation of plutonic rocks sculpted by marine winds: (pink porphyry), Sector of Porto, Corsica, France© Georges Lopez / BiosphotoJPG - RM

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Calanques de Piana: Geological formation of plutonic rocks

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Geological reserve, La Désirade, GuadeloupeGeological reserve, La Désirade, GuadeloupeGeological reserve, La Désirade, Guadeloupe© Jean-Philippe Vantighem / BiosphotoJPG - RM

2150969

Geological reserve, La Désirade, Guadeloupe

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Geological reserve, La Désirade, GuadeloupeGeological reserve, La Désirade, GuadeloupeGeological reserve, La Désirade, Guadeloupe© Jean-Philippe Vantighem / BiosphotoJPG - RM

2150968

Geological reserve, La Désirade, Guadeloupe

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Pillow Lava, Geological Reserve, La Désirade, GuadeloupePillow Lava, Geological Reserve, La Désirade, GuadeloupePillow Lava, Geological Reserve, La Désirade, Guadeloupe© Jean-Philippe Vantighem / BiosphotoJPG - RM

2150960

Pillow Lava, Geological Reserve, La Désirade, Guadeloupe

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Geological cirque of Creux du Van, Jura, SwitzerlandGeological cirque of Creux du Van, Jura, SwitzerlandGeological cirque of Creux du Van, Jura, Switzerland© Christian Cabron / BiosphotoJPG - RMNon exclusive sale, exclusive sale possible in France

2125492

Geological cirque of Creux du Van, Jura, Switzerland

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Geological cirque of Creux du Van, Jura, SwitzerlandGeological cirque of Creux du Van, Jura, SwitzerlandGeological cirque of Creux du Van, Jura, Switzerland© Jean-Philippe Vantighem / BiosphotoJPG - RM

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Geological cirque of Creux du Van, Jura, Switzerland

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The Spearfish Formation along the Belle Fourche River in the area of Devils Tower, Wyoming, USAThe Spearfish Formation along the Belle Fourche River in the area of Devils Tower, Wyoming, USAThe Spearfish Formation along the Belle Fourche River in the area of Devils Tower, Wyoming, USA© Marc Le Fèvre / BiosphotoJPG - RM

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The Spearfish Formation along the Belle Fourche River in the area

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Las Aquarales: geological formation caused by the filtering of water through the clay in the course of 25 million years, Valpalmas, Aragon, SpainLas Aquarales: geological formation caused by the filtering of water through the clay in the course of 25 million years, Valpalmas, Aragon, SpainLas Aquarales: geological formation caused by the filtering of water through the clay in the course of 25 million years, Valpalmas, Aragon, Spain© Georges Lopez / BiosphotoJPG - RM

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Las Aquarales: geological formation caused by the filtering of

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Las Aquarales: geological formation caused by the filtering of water through the clay in the course of 25 million years, Valpalmas, Aragon, SpainLas Aquarales: geological formation caused by the filtering of water through the clay in the course of 25 million years, Valpalmas, Aragon, SpainLas Aquarales: geological formation caused by the filtering of water through the clay in the course of 25 million years, Valpalmas, Aragon, Spain© Georges Lopez / BiosphotoJPG - RM

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Las Aquarales: geological formation caused by the filtering of

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La Serre de l'Ane downstream of La Charce - Diois France ; Classified geological site "Unesco world reference." A mix of clay and limestone marl beds, stratotype world reference transition Valanginien Hauterivien (secondary era) La Serre de l'Ane downstream of La Charce - Diois FranceLa Serre de l'Ane downstream of La Charce - Diois France ; Classified geological site "Unesco world reference." A mix of clay and limestone marl beds, stratotype world reference transition Valanginien Hauterivien (secondary era) © Jean-Philippe Delobelle / BiosphotoJPG - RM

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La Serre de l'Ane downstream of La Charce - Diois France ;

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La Serre de l'Ane downstream of La Charce - Diois France ; Classified geological site "Unesco world reference." A mix of clay and limestone marl beds, stratotype world reference transition Valanginien Hauterivien (secondary era) La Serre de l'Ane downstream of La Charce - Diois FranceLa Serre de l'Ane downstream of La Charce - Diois France ; Classified geological site "Unesco world reference." A mix of clay and limestone marl beds, stratotype world reference transition Valanginien Hauterivien (secondary era) © Jean-Philippe Delobelle / BiosphotoJPG - RM

2036292

La Serre de l'Ane downstream of La Charce - Diois France ;

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Geological landscape - Zion NP Utah USA  ; These domes are Navajo sandstone, from wind (petrified dunes), and from the early Jurassic (desert on the west side of Pangaea)strata are cut by fractures created by the alternating freezing and extreme heat over millions of yearsGeological landscape - Zion NP Utah USA Geological landscape - Zion NP Utah USA ; These domes are Navajo sandstone, from wind (petrified dunes), and from the early Jurassic (desert on the west side of Pangaea)strata are cut by fractures created by the alternating freezing and extreme heat over millions of years© Jean-Philippe Delobelle / BiosphotoJPG - RM

2033244

Geological landscape - Zion NP Utah USA ; These domes are Navajo

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Geological landscape - Zion NP Utah USA  ; These domes are Navajo sandstone, from wind (petrified dunes), and from the early Jurassic (desert on the west side of Pangaea)strata are cut by fractures created by the alternating freezing and extreme heat over millions of yearsGeological landscape - Zion NP Utah USA Geological landscape - Zion NP Utah USA ; These domes are Navajo sandstone, from wind (petrified dunes), and from the early Jurassic (desert on the west side of Pangaea)strata are cut by fractures created by the alternating freezing and extreme heat over millions of years© Jean-Philippe Delobelle / BiosphotoJPG - RM

2033243

Geological landscape - Zion NP Utah USA ; These domes are Navajo

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Geological landscape - Zion NP Utah USA  ; These domes are Navajo sandstone, from wind (petrified dunes), and from the early Jurassic (desert on the west side of Pangaea)strata are cut by fractures created by the alternating freezing and extreme heat over millions of yearsGeological landscape - Zion NP Utah USA Geological landscape - Zion NP Utah USA ; These domes are Navajo sandstone, from wind (petrified dunes), and from the early Jurassic (desert on the west side of Pangaea)strata are cut by fractures created by the alternating freezing and extreme heat over millions of years© Jean-Philippe Delobelle / BiosphotoJPG - RM

2033242

Geological landscape - Zion NP Utah USA ; These domes are Navajo

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Geological landscape - Zion NP Utah USA  ; These domes are Navajo sandstone, from wind (petrified dunes), and from the early Jurassic (desert on the west side of Pangaea)strata are cut by fractures created by the alternating freezing and extreme heat over millions of yearsGeological landscape - Zion NP Utah USA Geological landscape - Zion NP Utah USA ; These domes are Navajo sandstone, from wind (petrified dunes), and from the early Jurassic (desert on the west side of Pangaea)strata are cut by fractures created by the alternating freezing and extreme heat over millions of years© Jean-Philippe Delobelle / BiosphotoJPG - RM

2033241

Geological landscape - Zion NP Utah USA ; These domes are Navajo

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Geological landscape - Cedar Breaks NM Utah USA ; Amphitheater<br>Deltaic sediments of Jurassic age (Claron Formation) of sandstone, dolomite and marl colored by iron oxides and carved by erosion into a vast amphitheater of hoodoos (pinnacles) richly colored with oxides of iron and manganeseGeological landscape - Cedar Breaks NM Utah USAGeological landscape - Cedar Breaks NM Utah USA ; Amphitheater
Deltaic sediments of Jurassic age (Claron Formation) of sandstone, dolomite and marl colored by iron oxides and carved by erosion into a vast amphitheater of hoodoos (pinnacles) richly colored with oxides of iron and manganese
© Jean-Philippe Delobelle / BiosphotoJPG - RM

2033237

Geological landscape - Cedar Breaks NM Utah USA ;

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Geological landscape - Cedar Breaks NM Utah USA ; Amphitheater<br>Deltaic sediments of Jurassic age (Claron Formation) of sandstone, dolomite and marl colored by iron oxides and carved by erosion into a vast amphitheater of hoodoos (pinnacles) richly colored with oxides of iron and manganeseGeological landscape - Cedar Breaks NM Utah USAGeological landscape - Cedar Breaks NM Utah USA ; Amphitheater
Deltaic sediments of Jurassic age (Claron Formation) of sandstone, dolomite and marl colored by iron oxides and carved by erosion into a vast amphitheater of hoodoos (pinnacles) richly colored with oxides of iron and manganese
© Jean-Philippe Delobelle / BiosphotoJPG - RM

2033236

Geological landscape - Cedar Breaks NM Utah USA ;

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Geological landscape - 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 metersGeological landscape - Bryce Canyon NP Utah USAGeological landscape - 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

2033216

Geological landscape - Bryce Canyon NP Utah USA ;

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Geological landscape - 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 metersGeological landscape - Bryce Canyon NP Utah USAGeological landscape - 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

2033215

Geological landscape - Bryce Canyon NP Utah USA ;

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Geological landscape - 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 metersGeological landscape - Bryce Canyon NP Utah USAGeological landscape - 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

2033214

Geological landscape - Bryce Canyon NP Utah USA ;

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Geological landscape - 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 metersGeological landscape - Bryce Canyon NP Utah USAGeological landscape - 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

2033213

Geological landscape - Bryce Canyon NP Utah USA ;

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Geological landscape - 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 metersGeological landscape - Bryce Canyon NP Utah USAGeological landscape - 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

2033212

Geological landscape - Bryce Canyon NP Utah USA ;

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Geological landscape - 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 metersGeological landscape - Bryce Canyon NP Utah USAGeological landscape - 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

2033211

Geological landscape - Bryce Canyon NP Utah USA ;

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Geological landscape - Bryce Canyon NP Utah USA ; Amphitheatre<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 metersGeological landscape - Bryce Canyon NP Utah USAGeological landscape - Bryce Canyon NP Utah USA ; Amphitheatre
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

2033210

Geological landscape - Bryce Canyon NP Utah USA ;

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Geological landscape - Blurr trail Capitol Reff Utah USA ; The colorful marl belong to the Chinle formation, while the massive sandstones forming the cliff are the Wingate training Geological landscape - Blurr trail Capitol Reff Utah USAGeological landscape - Blurr trail Capitol Reff Utah USA ; The colorful marl belong to the Chinle formation, while the massive sandstones forming the cliff are the Wingate training © Jean-Philippe Delobelle / BiosphotoJPG - RM

2033200

Geological landscape - Blurr trail Capitol Reff Utah USA ; The

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A mix of clay and limestone beds of marl - France ; Geological site ranked "global benchmark Unesco." Stratotype global benchmark Hauterivian Valanginian transition (secondary era) A mix of clay and limestone beds of marl - FranceA mix of clay and limestone beds of marl - France ; Geological site ranked "global benchmark Unesco." Stratotype global benchmark Hauterivian Valanginian transition (secondary era) © Jean-Philippe Delobelle / BiosphotoJPG - RM

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A mix of clay and limestone beds of marl - France ; Geological

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Geological formation - Spitsbergen SvalbardGeological formation - Spitsbergen SvalbardGeological formation - Spitsbergen Svalbard© Juan-Carlos Muñoz / BiosphotoJPG - RMNon exclusive sale, exclusive sale possible in France

1993570

Geological formation - Spitsbergen Svalbard

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Landscape of the Waterberg Plateau - Namibia ; Geological base of 850 million years Landscape of the Waterberg Plateau - NamibiaLandscape of the Waterberg Plateau - Namibia ; Geological base of 850 million years © Claude Thouvenin / BiosphotoJPG - RM

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Landscape of the Waterberg Plateau - Namibia ; Geological base of

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Marl - Geological Reserve of Haute Provence France Marl - Geological Reserve of Haute Provence France Marl - Geological Reserve of Haute Provence France © Jean-Philippe Delobelle / BiosphotoJPG - RM

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Marl - Geological Reserve of Haute Provence France

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Erosion in limestone marl - Geological Reserve France Erosion in limestone marl - Geological Reserve France Erosion in limestone marl - Geological Reserve France © Jean-Philippe Delobelle / BiosphotoJPG - RM

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Erosion in limestone marl - Geological Reserve France

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Sector Roubine on Galabre - Geological Reserve France ; Black Earth formed Oxfordian marl, of Jurassic age (deep marine sediments)Sector Roubine on Galabre - Geological Reserve FranceSector Roubine on Galabre - Geological Reserve France ; Black Earth formed Oxfordian marl, of Jurassic age (deep marine sediments)© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Sector Roubine on Galabre - Geological Reserve France ; Black

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Sector Roubine on Galabre - Geological Reserve France ; Black Earth formed Oxfordian marl, of Jurassic age (deep marine sediments)Sector Roubine on Galabre - Geological Reserve FranceSector Roubine on Galabre - Geological Reserve France ; Black Earth formed Oxfordian marl, of Jurassic age (deep marine sediments)© Jean-Philippe Delobelle / BiosphotoJPG - RM

1925145

Sector Roubine on Galabre - Geological Reserve France ; Black

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Sector Roubine on Galabre - Geological Reserve France ; Black Earth formed Oxfordian marl, of Jurassic age (deep marine sediments)Sector Roubine on Galabre - Geological Reserve FranceSector Roubine on Galabre - Geological Reserve France ; Black Earth formed Oxfordian marl, of Jurassic age (deep marine sediments)© Jean-Philippe Delobelle / BiosphotoJPG - RM

1925144

Sector Roubine on Galabre - Geological Reserve France ; Black

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Sector Roubine on Galabre - Geological Reserve France ; Black Earth formed Oxfordian marl, of Jurassic age (deep marine sediments)Sector Roubine on Galabre - Geological Reserve FranceSector Roubine on Galabre - Geological Reserve France ; Black Earth formed Oxfordian marl, of Jurassic age (deep marine sediments)© Jean-Philippe Delobelle / BiosphotoJPG - RM

1925143

Sector Roubine on Galabre - Geological Reserve France ; Black

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Sector Roubine on Galabre - Geological Reserve France ; Black Earth formed Oxfordian marl, of Jurassic age (deep marine sediments)Sector Roubine on Galabre - Geological Reserve FranceSector Roubine on Galabre - Geological Reserve France ; Black Earth formed Oxfordian marl, of Jurassic age (deep marine sediments)© Jean-Philippe Delobelle / BiosphotoJPG - RM

1925142

Sector Roubine on Galabre - Geological Reserve France ; Black

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Sector Roubine on Galabre - Geological Reserve France ; Black Earth formed Oxfordian marl, of Jurassic age (deep marine sediments)Sector Roubine on Galabre - Geological Reserve FranceSector Roubine on Galabre - Geological Reserve France ; Black Earth formed Oxfordian marl, of Jurassic age (deep marine sediments)© Jean-Philippe Delobelle / BiosphotoJPG - RM

1925141

Sector Roubine on Galabre - Geological Reserve France ; Black

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Sector Roubine on Galabre - Geological Reserve France ; Black Earth formed Oxfordian marl, of Jurassic age (deep marine sediments)Sector Roubine on Galabre - Geological Reserve FranceSector Roubine on Galabre - Geological Reserve France ; Black Earth formed Oxfordian marl, of Jurassic age (deep marine sediments)© Jean-Philippe Delobelle / BiosphotoJPG - RM

1925140

Sector Roubine on Galabre - Geological Reserve France ; Black

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Man on hard geological strata - Badlands Alberta Canada ; This erosion resulted in the discovery of many dinosaur skeletons, making this region one of the world's largest fossil sites of these speciesMan on hard geological strata - Badlands Alberta CanadaMan on hard geological strata - Badlands Alberta Canada ; This erosion resulted in the discovery of many dinosaur skeletons, making this region one of the world's largest fossil sites of these species© Alain Mafart-Renodier / BiosphotoJPG - RMNon exclusive sale

1921803

Man on hard geological strata - Badlands Alberta Canada ; This

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Yuanmou Clay Forest - Yunnan China ; Soil forest , Wumao Earth Forest, Badlands in YuanMou of Yunnan, China, also named as YuanMou Mud-forest, showing forces of erosion over millions of years. The Earth Forest in Yuanmou is a provincial class scenic spot covering an area of 50 sq km. It was formed by geological movement and soil erosion one or two million years ago. It is named for its shape like immense forest and the main composition of the expansion earth. The whole landscape is mainly castle, screen, curtain and column, including the highest about 40 meters and very grand.Yuanmou Clay Forest - Yunnan ChinaYuanmou Clay Forest - Yunnan China ; Soil forest , Wumao Earth Forest, Badlands in YuanMou of Yunnan, China, also named as YuanMou Mud-forest, showing forces of erosion over millions of years. The Earth Forest in Yuanmou is a provincial class scenic spot covering an area of 50 sq km. It was formed by geological movement and soil erosion one or two million years ago. It is named for its shape like immense forest and the main composition of the expansion earth. The whole landscape is mainly castle, screen, curtain and column, including the highest about 40 meters and very grand.© Sylvain Cordier / BiosphotoJPG - RMNon exclusive sale

1920327

Yuanmou Clay Forest - Yunnan China ; Soil forest , Wumao Earth

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Yuanmou Clay Forest - Yunnan China ; Soil forest , Wumao Earth Forest, Badlands in YuanMou of Yunnan, China, also named as YuanMou Mud-forest, showing forces of erosion over millions of years. The Earth Forest in Yuanmou is a provincial class scenic spot covering an area of 50 sq km. It was formed by geological movement and soil erosion one or two million years ago. It is named for its shape like immense forest and the main composition of the expansion earth. The whole landscape is mainly castle, screen, curtain and column, including the highest about 40 meters and very grand.Yuanmou Clay Forest - Yunnan ChinaYuanmou Clay Forest - Yunnan China ; Soil forest , Wumao Earth Forest, Badlands in YuanMou of Yunnan, China, also named as YuanMou Mud-forest, showing forces of erosion over millions of years. The Earth Forest in Yuanmou is a provincial class scenic spot covering an area of 50 sq km. It was formed by geological movement and soil erosion one or two million years ago. It is named for its shape like immense forest and the main composition of the expansion earth. The whole landscape is mainly castle, screen, curtain and column, including the highest about 40 meters and very grand.© Sylvain Cordier / BiosphotoJPG - RMNon exclusive sale

1920326

Yuanmou Clay Forest - Yunnan China ; Soil forest , Wumao Earth

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Yuanmou Clay Forest - Yunnan China ; Soil forest , Wumao Earth Forest, Badlands in YuanMou of Yunnan, China, also named as YuanMou Mud-forest, showing forces of erosion over millions of years. The Earth Forest in Yuanmou is a provincial class scenic spot covering an area of 50 sq km. It was formed by geological movement and soil erosion one or two million years ago. It is named for its shape like immense forest and the main composition of the expansion earth. The whole landscape is mainly castle, screen, curtain and column, including the highest about 40 meters and very grand.Yuanmou Clay Forest - Yunnan ChinaYuanmou Clay Forest - Yunnan China ; Soil forest , Wumao Earth Forest, Badlands in YuanMou of Yunnan, China, also named as YuanMou Mud-forest, showing forces of erosion over millions of years. The Earth Forest in Yuanmou is a provincial class scenic spot covering an area of 50 sq km. It was formed by geological movement and soil erosion one or two million years ago. It is named for its shape like immense forest and the main composition of the expansion earth. The whole landscape is mainly castle, screen, curtain and column, including the highest about 40 meters and very grand.© Sylvain Cordier / BiosphotoJPG - RMNon exclusive sale

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Yuanmou Clay Forest - Yunnan China ; Soil forest , Wumao Earth

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Yuanmou Clay Forest - Yunnan China ; Soil forest , Wumao Earth Forest, Badlands in YuanMou of Yunnan, China, also named as YuanMou Mud-forest, showing forces of erosion over millions of years. The Earth Forest in Yuanmou is a provincial class scenic spot covering an area of 50 sq km. It was formed by geological movement and soil erosion one or two million years ago. It is named for its shape like immense forest and the main composition of the expansion earth. The whole landscape is mainly castle, screen, curtain and column, including the highest about 40 meters and very grand.Yuanmou Clay Forest - Yunnan ChinaYuanmou Clay Forest - Yunnan China ; Soil forest , Wumao Earth Forest, Badlands in YuanMou of Yunnan, China, also named as YuanMou Mud-forest, showing forces of erosion over millions of years. The Earth Forest in Yuanmou is a provincial class scenic spot covering an area of 50 sq km. It was formed by geological movement and soil erosion one or two million years ago. It is named for its shape like immense forest and the main composition of the expansion earth. The whole landscape is mainly castle, screen, curtain and column, including the highest about 40 meters and very grand.© Sylvain Cordier / BiosphotoJPG - RMNon exclusive sale

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Yuanmou Clay Forest - Yunnan China ; Soil forest , Wumao Earth

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Waterfall in the Geological Reserve of Haute-Provence FranceWaterfall in the Geological Reserve of Haute-Provence FranceWaterfall in the Geological Reserve of Haute-Provence France© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Waterfall in the Geological Reserve of Haute-Provence France

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