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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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2172561

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

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Bristlecone pine multimillennial - Cedar Breaks NM Utah USA ; Older than 2000 years<br>Pines growing at very high altitude (3000 m) and can survive more than 4500 years;they are generally observed in the combat zone, where no other species can survive extreme conditions, and their roots are slowly exposed by erosion over the centuriesBristlecone pine multimillennial - Cedar Breaks NM Utah USABristlecone pine multimillennial - Cedar Breaks NM Utah USA ; Older than 2000 years
Pines growing at very high altitude (3000 m) and can survive more than 4500 years;they are generally observed in the combat zone, where no other species can survive extreme conditions, and their roots are slowly exposed by erosion over the centuries© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2033220

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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2033217

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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2033183

Dome Navajo sandstone - Grand Staircase-Escalante NM Utah ;

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

Diver into the light shining down through a cenote opening

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The 12 Apostles Port Campbell National Park, AustraliaThe 12 Apostles Port Campbell National Park, AustraliaThe 12 Apostles Port Campbell National Park, Australia© Edouard Bense / BiosphotoJPG - RM
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1897272

The 12 Apostles Port Campbell National Park, Australia

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Eroded sandstone massif Jaizkibel Basque Country SpainEroded sandstone massif Jaizkibel Basque Country SpainEroded sandstone massif Jaizkibel Basque Country Spain© Juan-Carlos Muñoz / BiosphotoJPG - RMNon exclusive sale, exclusive sale possible in France
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1871696

Eroded sandstone massif Jaizkibel Basque Country Spain

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Two couple of Bee-eaters perching on branch in loess cliffTwo couple of Bee-eaters perching on branch in loess cliffTwo couple of Bee-eaters perching on branch in loess cliff© Berndt Fischer / BiosphotoJPG - RM
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1174171

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

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

The 12 Apostles Port Campbell National Park, Australia

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

2093801

Mushroom-shaped limestone rock formation, White Desert, Farafra

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Prostrate Rosemary (Rosmarinus officinalis) on coastal limestone rocks, Calanques National Park, Bouches-du-Rhone, FranceProstrate Rosemary (Rosmarinus officinalis) on coastal limestone rocks, Calanques National Park, Bouches-du-Rhone, FranceProstrate Rosemary (Rosmarinus officinalis) on coastal limestone rocks, Calanques National Park, Bouches-du-Rhone, France© Marie Aymerez / BiosphotoJPG - RM
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2511760

Prostrate Rosemary (Rosmarinus officinalis) on coastal limestone

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Patch of prostrate vegetation, including Sage-leaved rock-rose (Cistus salviifolius), Rosemary (Rosmarinus officinalis) and Sparrow-wort (Thymelaea tartonraira) on coastal limestone rocks, Calanques National Park, Bouches-du-Rhone, FrancePatch of prostrate vegetation, including Sage-leaved rock-rose (Cistus salviifolius), Rosemary (Rosmarinus officinalis) and Sparrow-wort (Thymelaea tartonraira) on coastal limestone rocks, Calanques National Park, Bouches-du-Rhone, FrancePatch of prostrate vegetation, including Sage-leaved rock-rose (Cistus salviifolius), Rosemary (Rosmarinus officinalis) and Sparrow-wort (Thymelaea tartonraira) on coastal limestone rocks, Calanques National Park, Bouches-du-Rhone, France© Marie Aymerez / BiosphotoJPG - RM
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2504988

Patch of prostrate vegetation, including Sage-leaved rock-rose

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Urgonian limestone cracked by erosion and polished by the repeated passage of hikers, Calanques National Park, Bouches-du-Rhone, FranceUrgonian limestone cracked by erosion and polished by the repeated passage of hikers, Calanques National Park, Bouches-du-Rhone, FranceUrgonian limestone cracked by erosion and polished by the repeated passage of hikers, Calanques National Park, Bouches-du-Rhone, France© Marie Aymerez / BiosphotoJPG - RM
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2504987

Urgonian limestone cracked by erosion and polished by the

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Cushion-forming Haircap moss (Plantago subulata), Calanques National Park, Bouches-du-Rhone, FranceCushion-forming Haircap moss (Plantago subulata), Calanques National Park, Bouches-du-Rhone, FranceCushion-forming Haircap moss (Plantago subulata), Calanques National Park, Bouches-du-Rhone, France© Marie Aymerez / BiosphotoJPG - RM
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2504050

Cushion-forming Haircap moss (Plantago subulata), Calanques

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Hottentot-fig (Carpobrotus edulis) flowering along coast, Calanques National Park, Bouches-du-Rhone, FranceHottentot-fig (Carpobrotus edulis) flowering along coast, Calanques National Park, Bouches-du-Rhone, FranceHottentot-fig (Carpobrotus edulis) flowering along coast, Calanques National Park, Bouches-du-Rhone, France© Marie Aymerez / BiosphotoJPG - RM
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2504001

Hottentot-fig (Carpobrotus edulis) flowering along coast,

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Flowers of Hottentot-fig (Carpobrotus edulis), Calanques National Park, Bouches-du-Rhone, FranceFlowers of Hottentot-fig (Carpobrotus edulis), Calanques National Park, Bouches-du-Rhone, FranceFlowers of Hottentot-fig (Carpobrotus edulis), Calanques National Park, Bouches-du-Rhone, France© Marie Aymerez / BiosphotoJPG - RM
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Flowers of Hottentot-fig (Carpobrotus edulis), Calanques National

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Flower of Hottentot-fig (Carpobrotus edulis), Calanques National Park, Bouches-du-Rhone, FranceFlower of Hottentot-fig (Carpobrotus edulis), Calanques National Park, Bouches-du-Rhone, FranceFlower of Hottentot-fig (Carpobrotus edulis), Calanques National Park, Bouches-du-Rhone, France© Marie Aymerez / BiosphotoJPG - RM
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2503999

Flower of Hottentot-fig (Carpobrotus edulis), Calanques National

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Hot springs crater, Tinggi Raja, Simalungun North Sumatra, IndonesiaHot springs crater, Tinggi Raja, Simalungun North Sumatra, IndonesiaHot springs crater, Tinggi Raja, Simalungun North Sumatra, Indonesia© Alain Compost / BiosphotoJPG - RM
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2498891

Hot springs crater, Tinggi Raja, Simalungun North Sumatra,

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Hot springs crater, Tinggi Raja, Simalungun North Sumatra, IndonesiaHot springs crater, Tinggi Raja, Simalungun North Sumatra, IndonesiaHot springs crater, Tinggi Raja, Simalungun North Sumatra, Indonesia© Alain Compost / BiosphotoJPG - RM
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2498890

Hot springs crater, Tinggi Raja, Simalungun North Sumatra,

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Hot springs crater, Tinggi Raja, Simalungun North Sumatra, IndonesiaHot springs crater, Tinggi Raja, Simalungun North Sumatra, IndonesiaHot springs crater, Tinggi Raja, Simalungun North Sumatra, Indonesia© Alain Compost / BiosphotoJPG - RM
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2498889

Hot springs crater, Tinggi Raja, Simalungun North Sumatra,

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Flooding torrent in the black marls, Hautes Alpes, FranceFlooding torrent in the black marls, Hautes Alpes, FranceFlooding torrent in the black marls, Hautes Alpes, France© David Tatin / BiosphotoJPG - RM
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2496946

Flooding torrent in the black marls, Hautes Alpes, France

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The Organs of Ille sur Têt and the snowy Canigou, Pyrénées-Orientales, FranceThe Organs of Ille sur Têt and the snowy Canigou, Pyrénées-Orientales, FranceThe Organs of Ille sur Têt and the snowy Canigou, Pyrénées-Orientales, France© Patrick Pons / BiosphotoJPG - RM
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2496790

The Organs of Ille sur Têt and the snowy Canigou,

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Detail of a ridge of the organs of Ille sur Têt and overview of their sedimentary structure, Pyrénées-Orientales, FranceDetail of a ridge of the organs of Ille sur Têt and overview of their sedimentary structure, Pyrénées-Orientales, FranceDetail of a ridge of the organs of Ille sur Têt and overview of their sedimentary structure, Pyrénées-Orientales, France© Patrick Pons / BiosphotoJPG - RM
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2496775

Detail of a ridge of the organs of Ille sur Têt and overview of

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Organs of Ille-sur-Têt at sunset, with the Canigou massif and peak in the background, Pyrénées-Orientales, FranceOrgans of Ille-sur-Têt at sunset, with the Canigou massif and peak in the background, Pyrénées-Orientales, FranceOrgans of Ille-sur-Têt at sunset, with the Canigou massif and peak in the background, Pyrénées-Orientales, France© Patrick Pons / BiosphotoJPG - RM
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2496774

Organs of Ille-sur-Têt at sunset, with the Canigou massif and

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Organs of Ille-sur-Têt at sunset, Pyrénées-Orientales, FranceOrgans of Ille-sur-Têt at sunset, Pyrénées-Orientales, FranceOrgans of Ille-sur-Têt at sunset, Pyrénées-Orientales, France© Patrick Pons / BiosphotoJPG - RM
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2496773

Organs of Ille-sur-Têt at sunset, Pyrénées-Orientales, France

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Terres Noires du col des Champs, dans le haut Verdon, Marnes du Jurassique (oxfordien) au col des Champs, entre Colmars et Entraunes, Alpes de Haute-Provence, FranceTerres Noires du col des Champs, dans le haut Verdon, Marnes du Jurassique (oxfordien) au col des Champs, entre Colmars et Entraunes, Alpes de Haute-Provence, FranceTerres Noires du col des Champs, dans le haut Verdon, Marnes du Jurassique (oxfordien) au col des Champs, entre Colmars et Entraunes, Alpes de Haute-Provence, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2496076

Terres Noires du col des Champs, dans le haut Verdon, Marnes du

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Cows grazing in roubines, Jurassic marl (Oxfordian) at the Col des Champs, between Colmars and Entraunes, Alpes de Haute-Provence, FranceCows grazing in roubines, Jurassic marl (Oxfordian) at the Col des Champs, between Colmars and Entraunes, Alpes de Haute-Provence, FranceCows grazing in roubines, Jurassic marl (Oxfordian) at the Col des Champs, between Colmars and Entraunes, Alpes de Haute-Provence, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2496075

Cows grazing in roubines, Jurassic marl (Oxfordian) at the Col

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Graphismes dans les roches du col des Champs, dans le haut Verdon, Strates redressées de calcaires marneux du crétacé, Col des Champs, entre Colmars et Entraunes, Alpes de Haute-Provence, FranceGraphismes dans les roches du col des Champs, dans le haut Verdon, Strates redressées de calcaires marneux du crétacé, Col des Champs, entre Colmars et Entraunes, Alpes de Haute-Provence, FranceGraphismes dans les roches du col des Champs, dans le haut Verdon, Strates redressées de calcaires marneux du crétacé, Col des Champs, entre Colmars et Entraunes, Alpes de Haute-Provence, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2496074

Graphismes dans les roches du col des Champs, dans le haut

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Cows grazing in roubines, Jurassic marl (Oxfordian) at the Col des Champs, between Colmars and Entraunes, Alpes de Haute-Provence, FranceCows grazing in roubines, Jurassic marl (Oxfordian) at the Col des Champs, between Colmars and Entraunes, Alpes de Haute-Provence, FranceCows grazing in roubines, Jurassic marl (Oxfordian) at the Col des Champs, between Colmars and Entraunes, Alpes de Haute-Provence, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2496073

Cows grazing in roubines, Jurassic marl (Oxfordian) at the Col

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Terres Noires in the Haut Verdon, Roubines in Jurassic marl, Thorame-Haute, Alpes de Haute-Provence, FranceTerres Noires in the Haut Verdon, Roubines in Jurassic marl, Thorame-Haute, Alpes de Haute-Provence, FranceTerres Noires in the Haut Verdon, Roubines in Jurassic marl, Thorame-Haute, Alpes de Haute-Provence, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2496071

Terres Noires in the Haut Verdon, Roubines in Jurassic marl,

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The Gorges de Saint Pierre, a splendid gorge carved in a thick horizontal series of cretaceous limestones - The walker on the horizontal path gives the scale! Upper Verdon valley, south of Colmars les Alpes, Alpes de Haute Provence, FranceThe Gorges de Saint Pierre, a splendid gorge carved in a thick horizontal series of cretaceous limestones - The walker on the horizontal path gives the scale! Upper Verdon valley, south of Colmars les Alpes, Alpes de Haute Provence, FranceThe Gorges de Saint Pierre, a splendid gorge carved in a thick horizontal series of cretaceous limestones - The walker on the horizontal path gives the scale! Upper Verdon valley, south of Colmars les Alpes, Alpes de Haute Provence, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2496060

The Gorges de Saint Pierre, a splendid gorge carved in a thick

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Foliose lichens (Xanthoparmelia stenophylla) on red pelites, Gorges de Daluis, Southern Alps, FranceFoliose lichens (Xanthoparmelia stenophylla) on red pelites, Gorges de Daluis, Southern Alps, FranceFoliose lichens (Xanthoparmelia stenophylla) on red pelites, Gorges de Daluis, Southern Alps, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2496051

Foliose lichens (Xanthoparmelia stenophylla) on red pelites,

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Chestnut trees in the Chambre du Roi (King's Chamber), dug in the Annot sandstone, Alpes de Haute Provence, France. Annot Sandstone (-34 to -30 Ma) the Annot Sandstone layers originate from massive arrivals of sands at the bottom of a sea by a process of submarine avalanches. Freezing and solifluction have since fractured and caused huge blocks to slide, creating narrow canyons populated by chestnut treesChestnut trees in the Chambre du Roi (King's Chamber), dug in the Annot sandstone, Alpes de Haute Provence, France. Annot Sandstone (-34 to -30 Ma) the Annot Sandstone layers originate from massive arrivals of sands at the bottom of a sea by a process of submarine avalanches. Freezing and solifluction have since fractured and caused huge blocks to slide, creating narrow canyons populated by chestnut treesChestnut trees in the Chambre du Roi (King's Chamber), dug in the Annot sandstone, Alpes de Haute Provence, France. Annot Sandstone (-34 to -30 Ma) the Annot Sandstone layers originate from massive arrivals of sands at the bottom of a sea by a process of submarine avalanches. Freezing and solifluction have since fractured and caused huge blocks to slide, creating narrow canyons populated by chestnut trees© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2495074

Chestnut trees in the Chambre du Roi (King's Chamber), dug in the

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Helminthoid flysch cliff in Haute Ubaye. Helminthoid flysch is a turbidity that dates from the Upper Cretaceous, and shows sinuous traces associated with the movements of gastropods, which grazed the mud of the sea floor creating sinuous grooves. Haute Ubaye, Alpes de Haute-Provence, FranceHelminthoid flysch cliff in Haute Ubaye. Helminthoid flysch is a turbidity that dates from the Upper Cretaceous, and shows sinuous traces associated with the movements of gastropods, which grazed the mud of the sea floor creating sinuous grooves. Haute Ubaye, Alpes de Haute-Provence, FranceHelminthoid flysch cliff in Haute Ubaye. Helminthoid flysch is a turbidity that dates from the Upper Cretaceous, and shows sinuous traces associated with the movements of gastropods, which grazed the mud of the sea floor creating sinuous grooves. Haute Ubaye, Alpes de Haute-Provence, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2495073

Helminthoid flysch cliff in Haute Ubaye. Helminthoid flysch is a

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Helminthoid flysch in Haute Ubaye. Helminthoid flysch is a turbidity that dates from the Upper Cretaceous, and shows sinuous traces associated with the movements of gastropods, which grazed the mud of the sea floor creating sinuous grooves. Haute Ubaye, Alpes de Haute-Provence, FranceHelminthoid flysch in Haute Ubaye. Helminthoid flysch is a turbidity that dates from the Upper Cretaceous, and shows sinuous traces associated with the movements of gastropods, which grazed the mud of the sea floor creating sinuous grooves. Haute Ubaye, Alpes de Haute-Provence, FranceHelminthoid flysch in Haute Ubaye. Helminthoid flysch is a turbidity that dates from the Upper Cretaceous, and shows sinuous traces associated with the movements of gastropods, which grazed the mud of the sea floor creating sinuous grooves. Haute Ubaye, Alpes de Haute-Provence, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2495072

Helminthoid flysch in Haute Ubaye. Helminthoid flysch is a

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Permian pelites in the Daluis Gorges, Alpes Maritimes, France. Permian pelites aged 250 Ma: clays of volcanic and detrital origin were oxidised under a tropical climate and slowly transformed into rocks, over a thickness of 1000 metres. Daluis Gorges, Dôme du BarrotPermian pelites in the Daluis Gorges, Alpes Maritimes, France. Permian pelites aged 250 Ma: clays of volcanic and detrital origin were oxidised under a tropical climate and slowly transformed into rocks, over a thickness of 1000 metres. Daluis Gorges, Dôme du BarrotPermian pelites in the Daluis Gorges, Alpes Maritimes, France. Permian pelites aged 250 Ma: clays of volcanic and detrital origin were oxidised under a tropical climate and slowly transformed into rocks, over a thickness of 1000 metres. Daluis Gorges, Dôme du Barrot© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2495070

Permian pelites in the Daluis Gorges, Alpes Maritimes, France.

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Permian pelites in the Daluis Gorges, Alpes Maritimes, France. Permian pelites aged 250 Ma: clays of volcanic and detrital origin were oxidised under a tropical climate and slowly transformed into rocks, over a thickness of 1000 metres. Daluis Gorges, Dôme du BarrotPermian pelites in the Daluis Gorges, Alpes Maritimes, France. Permian pelites aged 250 Ma: clays of volcanic and detrital origin were oxidised under a tropical climate and slowly transformed into rocks, over a thickness of 1000 metres. Daluis Gorges, Dôme du BarrotPermian pelites in the Daluis Gorges, Alpes Maritimes, France. Permian pelites aged 250 Ma: clays of volcanic and detrital origin were oxidised under a tropical climate and slowly transformed into rocks, over a thickness of 1000 metres. Daluis Gorges, Dôme du Barrot© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2495069

Permian pelites in the Daluis Gorges, Alpes Maritimes, France.

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Snails (Solatopupa cianensis) on Permian pelites of the Gorges du Cians, Alpes Maritimes, France. Endemic species of the Gorges du Cians and Daluis, Dôme du BarrotSnails (Solatopupa cianensis) on Permian pelites of the Gorges du Cians, Alpes Maritimes, France. Endemic species of the Gorges du Cians and Daluis, Dôme du BarrotSnails (Solatopupa cianensis) on Permian pelites of the Gorges du Cians, Alpes Maritimes, France. Endemic species of the Gorges du Cians and Daluis, Dôme du Barrot© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2495065

Snails (Solatopupa cianensis) on Permian pelites of the Gorges du

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Permian pelites of the Cians Gorges, Alpes Maritimes, France. Permian pelites aged 250 Ma: clays of volcanic and detrital origin were oxidised under a tropical climate and slowly transformed into rocks, over a thickness of 1000 metres. Gorges du Cians, Dôme du BarrotPermian pelites of the Cians Gorges, Alpes Maritimes, France. Permian pelites aged 250 Ma: clays of volcanic and detrital origin were oxidised under a tropical climate and slowly transformed into rocks, over a thickness of 1000 metres. Gorges du Cians, Dôme du BarrotPermian pelites of the Cians Gorges, Alpes Maritimes, France. Permian pelites aged 250 Ma: clays of volcanic and detrital origin were oxidised under a tropical climate and slowly transformed into rocks, over a thickness of 1000 metres. Gorges du Cians, Dôme du Barrot© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2495064

Permian pelites of the Cians Gorges, Alpes Maritimes, France.

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Mudcracks in the Permian pelites of the Cians Gorges, Alpes Maritimes, France. Permian pelites aged 250 Ma: clays of volcanic and detrital origin were oxidised under a tropical climate and slowly transformed into rocks, over a thickness of 1000 metres. Mudcracks were formed on the surface of sedimentation lagoons during dry periods in a tropical climate. Gorges du Cians, Dôme du BarrotMudcracks in the Permian pelites of the Cians Gorges, Alpes Maritimes, France. Permian pelites aged 250 Ma: clays of volcanic and detrital origin were oxidised under a tropical climate and slowly transformed into rocks, over a thickness of 1000 metres. Mudcracks were formed on the surface of sedimentation lagoons during dry periods in a tropical climate. Gorges du Cians, Dôme du BarrotMudcracks in the Permian pelites of the Cians Gorges, Alpes Maritimes, France. Permian pelites aged 250 Ma: clays of volcanic and detrital origin were oxidised under a tropical climate and slowly transformed into rocks, over a thickness of 1000 metres. Mudcracks were formed on the surface of sedimentation lagoons during dry periods in a tropical climate. Gorges du Cians, Dôme du Barrot© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2495063

Mudcracks in the Permian pelites of the Cians Gorges, Alpes

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Permian pelites of the Cians Gorges, Alpes Maritimes, France. Permian pelites aged 250 Ma: clays of volcanic and detrital origin were oxidised under a tropical climate and slowly transformed into rocks, over a thickness of 1000 metres. Gorges du Cians, Dôme du BarrotPermian pelites of the Cians Gorges, Alpes Maritimes, France. Permian pelites aged 250 Ma: clays of volcanic and detrital origin were oxidised under a tropical climate and slowly transformed into rocks, over a thickness of 1000 metres. Gorges du Cians, Dôme du BarrotPermian pelites of the Cians Gorges, Alpes Maritimes, France. Permian pelites aged 250 Ma: clays of volcanic and detrital origin were oxidised under a tropical climate and slowly transformed into rocks, over a thickness of 1000 metres. Gorges du Cians, Dôme du Barrot© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2495062

Permian pelites of the Cians Gorges, Alpes Maritimes, France.

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Mudcracks in the Permian pelites of the Cians Gorges, Alpes Maritimes, France. Permian pelites aged 250 Ma: clays of volcanic and detrital origin were oxidised under a tropical climate and slowly transformed into rocks, over a thickness of 1000 metres. Mudcracks were formed on the surface of sedimentation lagoons during dry periods in a tropical climate. Gorges du Cians, Dôme du BarrotMudcracks in the Permian pelites of the Cians Gorges, Alpes Maritimes, France. Permian pelites aged 250 Ma: clays of volcanic and detrital origin were oxidised under a tropical climate and slowly transformed into rocks, over a thickness of 1000 metres. Mudcracks were formed on the surface of sedimentation lagoons during dry periods in a tropical climate. Gorges du Cians, Dôme du BarrotMudcracks in the Permian pelites of the Cians Gorges, Alpes Maritimes, France. Permian pelites aged 250 Ma: clays of volcanic and detrital origin were oxidised under a tropical climate and slowly transformed into rocks, over a thickness of 1000 metres. Mudcracks were formed on the surface of sedimentation lagoons during dry periods in a tropical climate. Gorges du Cians, Dôme du Barrot© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2495061

Mudcracks in the Permian pelites of the Cians Gorges, Alpes

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Cretaceous limestone in the Buëch. Cluse de Champ Bertrand, Upper Buëch Valley, Hautes-Alpes, FranceCretaceous limestone in the Buëch. Cluse de Champ Bertrand, Upper Buëch Valley, Hautes-Alpes, FranceCretaceous limestone in the Buëch. Cluse de Champ Bertrand, Upper Buëch Valley, Hautes-Alpes, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2495060

Cretaceous limestone in the Buëch. Cluse de Champ Bertrand, Upper

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Cretaceous limestone in the Buëch. Cluse de Champ Bertrand, Upper Buëch Valley, Hautes-Alpes, FranceCretaceous limestone in the Buëch. Cluse de Champ Bertrand, Upper Buëch Valley, Hautes-Alpes, FranceCretaceous limestone in the Buëch. Cluse de Champ Bertrand, Upper Buëch Valley, Hautes-Alpes, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2495059

Cretaceous limestone in the Buëch. Cluse de Champ Bertrand, Upper

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Chestnut trees in the Chambre du Roi (King's Chamber), dug in the Annot sandstone, Alpes de Haute Provence, France. Annot Sandstone (-34 to -30 Ma) the Annot Sandstone layers originate from massive arrivals of sands at the bottom of a sea by a process of submarine avalanches. Freezing and solifluction have since fractured and caused huge blocks to slide, creating narrow canyons populated by chestnut treesChestnut trees in the Chambre du Roi (King's Chamber), dug in the Annot sandstone, Alpes de Haute Provence, France. Annot Sandstone (-34 to -30 Ma) the Annot Sandstone layers originate from massive arrivals of sands at the bottom of a sea by a process of submarine avalanches. Freezing and solifluction have since fractured and caused huge blocks to slide, creating narrow canyons populated by chestnut treesChestnut trees in the Chambre du Roi (King's Chamber), dug in the Annot sandstone, Alpes de Haute Provence, France. Annot Sandstone (-34 to -30 Ma) the Annot Sandstone layers originate from massive arrivals of sands at the bottom of a sea by a process of submarine avalanches. Freezing and solifluction have since fractured and caused huge blocks to slide, creating narrow canyons populated by chestnut trees© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2495052

Chestnut trees in the Chambre du Roi (King's Chamber), dug in the

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Chestnut trees in the Chambre du Roi (King's Chamber), dug in the Annot sandstone, Alpes de Haute Provence, France. Annot Sandstone (-34 to -30 Ma) the Annot Sandstone layers originate from massive arrivals of sands at the bottom of a sea by a process of submarine avalanches. Freezing and solifluction have since fractured and caused huge blocks to slide, creating narrow canyons populated by chestnut treesChestnut trees in the Chambre du Roi (King's Chamber), dug in the Annot sandstone, Alpes de Haute Provence, France. Annot Sandstone (-34 to -30 Ma) the Annot Sandstone layers originate from massive arrivals of sands at the bottom of a sea by a process of submarine avalanches. Freezing and solifluction have since fractured and caused huge blocks to slide, creating narrow canyons populated by chestnut treesChestnut trees in the Chambre du Roi (King's Chamber), dug in the Annot sandstone, Alpes de Haute Provence, France. Annot Sandstone (-34 to -30 Ma) the Annot Sandstone layers originate from massive arrivals of sands at the bottom of a sea by a process of submarine avalanches. Freezing and solifluction have since fractured and caused huge blocks to slide, creating narrow canyons populated by chestnut trees© Jean-Philippe Delobelle / BiosphotoJPG - RM
2495051

2495051

Chestnut trees in the Chambre du Roi (King's Chamber), dug in the

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Limestone concretion on oak leaf in water, Ardeche, FranceLimestone concretion on oak leaf in water, Ardeche, FranceLimestone concretion on oak leaf in water, Ardeche, France© Stéphane Vitzthum / BiosphotoJPG - RM
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2494291

Limestone concretion on oak leaf in water, Ardeche, France

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Flysch, detrital sedimentary deposit, geology, Bidart, Basque coast, Pyrénées Atlantiques, FranceFlysch, detrital sedimentary deposit, geology, Bidart, Basque coast, Pyrénées Atlantiques, FranceFlysch, detrital sedimentary deposit, geology, Bidart, Basque coast, Pyrénées Atlantiques, France© Laurent Lhoté / BiosphotoJPG - RM
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2492328

Flysch, detrital sedimentary deposit, geology, Bidart, Basque

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Flysch, detrital sedimentary deposit, geology, Bidart, Basque coast, Pyrénées Atlantiques, FranceFlysch, detrital sedimentary deposit, geology, Bidart, Basque coast, Pyrénées Atlantiques, FranceFlysch, detrital sedimentary deposit, geology, Bidart, Basque coast, Pyrénées Atlantiques, France© Laurent Lhoté / BiosphotoJPG - RM
2492324

2492324

Flysch, detrital sedimentary deposit, geology, Bidart, Basque

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Ochres of the Luberon, FranceOchres of the Luberon, FranceOchres of the Luberon, France© David Tatin / BiosphotoJPG - RM
2490406

2490406

Ochres of the Luberon, France

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