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Les Terres Noires de Robine sur Galabre under the snow. Jurassic (Toarcian) marls rich in organic matter, tender and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Digne Geological Reserve, Alpes de Haute Provence, France.Les Terres Noires de Robine sur Galabre under the snow. Jurassic (Toarcian) marls rich in organic matter, tender and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Digne Geological Reserve, Alpes de Haute Provence, France.Les Terres Noires de Robine sur Galabre under the snow. Jurassic (Toarcian) marls rich in organic matter, tender and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Digne Geological Reserve, Alpes de Haute Provence, France.© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2462017

Les Terres Noires de Robine sur Galabre under the snow. Jurassic

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Crumpling in the Helminthoid Flysch, Ubaye Valley, Alpes de Haute Provence, FranceCrumpling in the Helminthoid Flysch, Ubaye Valley, Alpes de Haute Provence, FranceCrumpling in the Helminthoid Flysch, Ubaye Valley, Alpes de Haute Provence, France© David Tatin / BiosphotoJPG - RM
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2546179

Crumpling in the Helminthoid Flysch, Ubaye Valley, Alpes de Haute

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Crumpling in the Helminthoid Flysch, Ubaye Valley, Alpes de Haute Provence, FranceCrumpling in the Helminthoid Flysch, Ubaye Valley, Alpes de Haute Provence, FranceCrumpling in the Helminthoid Flysch, Ubaye Valley, Alpes de Haute Provence, France© David Tatin / BiosphotoJPG - RM
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2546178

Crumpling in the Helminthoid Flysch, Ubaye Valley, Alpes de Haute

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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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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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Folded strata in the Haut Verdon, alternating Cretaceous marl and limestone, Thorame-Haute, Alpes de Haute-Provence, FranceFolded strata in the Haut Verdon, alternating Cretaceous marl and limestone, Thorame-Haute, Alpes de Haute-Provence, FranceFolded strata in the Haut Verdon, alternating Cretaceous marl and limestone, Thorame-Haute, Alpes de Haute-Provence, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2496072

Folded strata in the Haut Verdon, alternating Cretaceous marl and

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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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Strates plissotées dans le Haut Verdon, Marnes et calcaires crétacés alternés, Thorame-Haute, Alpes de Haute-Provence, FranceStrates plissotées dans le Haut Verdon, Marnes et calcaires crétacés alternés, Thorame-Haute, Alpes de Haute-Provence, FranceStrates plissotées dans le Haut Verdon, Marnes et calcaires crétacés alternés, Thorame-Haute, Alpes de Haute-Provence, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2496070

Strates plissotées dans le Haut Verdon, Marnes et calcaires

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The cliffs of Chaudeirolles in the Haut Verdon, Cretaceous limestone strata, Thorame-Haute, Alpes de Haute-Provence, FranceThe cliffs of Chaudeirolles in the Haut Verdon, Cretaceous limestone strata, Thorame-Haute, Alpes de Haute-Provence, FranceThe cliffs of Chaudeirolles in the Haut Verdon, Cretaceous limestone strata, Thorame-Haute, Alpes de Haute-Provence, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2496069

The cliffs of Chaudeirolles in the Haut Verdon, Cretaceous

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The cliffs of Chaudeirolles in the Haut Verdon, Cretaceous limestone strata, Thorame-Haute, Alpes de Haute-Provence, FranceThe cliffs of Chaudeirolles in the Haut Verdon, Cretaceous limestone strata, Thorame-Haute, Alpes de Haute-Provence, FranceThe cliffs of Chaudeirolles in the Haut Verdon, Cretaceous limestone strata, Thorame-Haute, Alpes de Haute-Provence, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2496068

The cliffs of Chaudeirolles in the Haut Verdon, Cretaceous

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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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Footprints consisting of three fan-shaped fingers, on average 15 cm long. They were left by bipedal dinosaurs (Grallator minusculus), in the Jurassic period, in the background the Causse Mejean and the Tarnon valley, Cevennes, FranceFootprints consisting of three fan-shaped fingers, on average 15 cm long. They were left by bipedal dinosaurs (Grallator minusculus), in the Jurassic period, in the background the Causse Mejean and the Tarnon valley, Cevennes, FranceFootprints consisting of three fan-shaped fingers, on average 15 cm long. They were left by bipedal dinosaurs (Grallator minusculus), in the Jurassic period, in the background the Causse Mejean and the Tarnon valley, Cevennes, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2496041

Footprints consisting of three fan-shaped fingers, on average 15

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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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The Espinasses lake, under the Serre Ponçon lake in summer. Jurassic marl and limestone, Hautes Alpes, FranceThe Espinasses lake, under the Serre Ponçon lake in summer. Jurassic marl and limestone, Hautes Alpes, FranceThe Espinasses lake, under the Serre Ponçon lake in summer. Jurassic marl and limestone, Hautes Alpes, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2495071

The Espinasses lake, under the Serre Ponçon lake in summer.

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Crêtes de Maleterre et Rocamaire, rocks of Cretaceous and Eocene age, Le haut Val Daluis, Alpes Maritimes, FranceCrêtes de Maleterre et Rocamaire, rocks of Cretaceous and Eocene age, Le haut Val Daluis, Alpes Maritimes, FranceCrêtes de Maleterre et Rocamaire, rocks of Cretaceous and Eocene age, Le haut Val Daluis, Alpes Maritimes, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2495068

Crêtes de Maleterre et Rocamaire, rocks of Cretaceous and Eocene

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Peine water gap, Tartonne, Jurassic limestone strata, Geological Reserve of Haute Provence, Alpes de Haute Provence, FrancePeine water gap, Tartonne, Jurassic limestone strata, Geological Reserve of Haute Provence, Alpes de Haute Provence, FrancePeine water gap, Tartonne, Jurassic limestone strata, Geological Reserve of Haute Provence, Alpes de Haute Provence, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2495067

Peine water gap, Tartonne, Jurassic limestone strata, Geological

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Peine water gap, Tartonne, Jurassic limestone strata, Geological Reserve of Haute Provence, Alpes de Haute Provence, FrancePeine water gap, Tartonne, Jurassic limestone strata, Geological Reserve of Haute Provence, Alpes de Haute Provence, FrancePeine water gap, Tartonne, Jurassic limestone strata, Geological Reserve of Haute Provence, Alpes de Haute Provence, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2495066

Peine water gap, Tartonne, Jurassic limestone strata, Geological

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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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Gabedaille peak located on the border with Spain: massif showing the red sandstone of the permo-trias, Pyrenees National Park, Aspe Valley, Pyrénées-Atlantiques, FranceGabedaille peak located on the border with Spain: massif showing the red sandstone of the permo-trias, Pyrenees National Park, Aspe Valley, Pyrénées-Atlantiques, FranceGabedaille peak located on the border with Spain: massif showing the red sandstone of the permo-trias, Pyrenees National Park, Aspe Valley, Pyrénées-Atlantiques, France© Georges Lopez / BiosphotoJPG - RM
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2493392

Gabedaille peak located on the border with Spain: massif showing

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Cirque d'Aspe : Upper cretaceous limestone, Pyrenees National Park, Aspe Valley, Pyrénées-Atlantiques, FranceCirque d'Aspe : Upper cretaceous limestone, Pyrenees National Park, Aspe Valley, Pyrénées-Atlantiques, FranceCirque d'Aspe : Upper cretaceous limestone, Pyrenees National Park, Aspe Valley, Pyrénées-Atlantiques, France© Georges Lopez / BiosphotoJPG - RM
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2493391

Cirque d'Aspe : Upper cretaceous limestone, Pyrenees National

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Les Terres Noires de Robine sur Galabre under the snow. Jurassic (Toarcian) marls rich in organic matter, tender and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Digne Geological Reserve, Alpes de Haute Provence, France.Les Terres Noires de Robine sur Galabre under the snow. Jurassic (Toarcian) marls rich in organic matter, tender and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Digne Geological Reserve, Alpes de Haute Provence, France.Les Terres Noires de Robine sur Galabre under the snow. Jurassic (Toarcian) marls rich in organic matter, tender and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Digne Geological Reserve, Alpes de Haute Provence, France.© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2462021

Les Terres Noires de Robine sur Galabre under the snow. Jurassic

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Les Terres Noires de Robine sur Galabre under the snow. Jurassic (Toarcian) marls rich in organic matter, tender and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Digne Geological Reserve, Alpes de Haute Provence, France.Les Terres Noires de Robine sur Galabre under the snow. Jurassic (Toarcian) marls rich in organic matter, tender and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Digne Geological Reserve, Alpes de Haute Provence, France.Les Terres Noires de Robine sur Galabre under the snow. Jurassic (Toarcian) marls rich in organic matter, tender and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Digne Geological Reserve, Alpes de Haute Provence, France.© Jean-Philippe Delobelle / BiosphotoJPG - RM
2462020

2462020

Les Terres Noires de Robine sur Galabre under the snow. Jurassic

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Les Terres Noires de Robine sur Galabre under the snow. Jurassic (Toarcian) marls rich in organic matter, tender and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Digne Geological Reserve, Alpes de Haute Provence, France.Les Terres Noires de Robine sur Galabre under the snow. Jurassic (Toarcian) marls rich in organic matter, tender and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Digne Geological Reserve, Alpes de Haute Provence, France.Les Terres Noires de Robine sur Galabre under the snow. Jurassic (Toarcian) marls rich in organic matter, tender and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Digne Geological Reserve, Alpes de Haute Provence, France.© Jean-Philippe Delobelle / BiosphotoJPG - RM
2462019

2462019

Les Terres Noires de Robine sur Galabre under the snow. Jurassic

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Les Terres Noires de Robine sur Galabre under the snow. Jurassic (Toarcian) marls rich in organic matter, tender and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Digne Geological Reserve, Alpes de Haute Provence, France.Les Terres Noires de Robine sur Galabre under the snow. Jurassic (Toarcian) marls rich in organic matter, tender and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Digne Geological Reserve, Alpes de Haute Provence, France.Les Terres Noires de Robine sur Galabre under the snow. Jurassic (Toarcian) marls rich in organic matter, tender and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Digne Geological Reserve, Alpes de Haute Provence, France.© Jean-Philippe Delobelle / BiosphotoJPG - RM
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2462018

Les Terres Noires de Robine sur Galabre under the snow. Jurassic

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The Black Earths of the nappe of Digne, above Draix. Jurassic marls rich in organic matter, soft and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Geological Reserve of Digne, Alpes de Haute Provence, France.The Black Earths of the nappe of Digne, above Draix. Jurassic marls rich in organic matter, soft and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Geological Reserve of Digne, Alpes de Haute Provence, France.The Black Earths of the nappe of Digne, above Draix. Jurassic marls rich in organic matter, soft and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Geological Reserve of Digne, Alpes de Haute Provence, France.© Jean-Philippe Delobelle / BiosphotoJPG - RM
2462016

2462016

The Black Earths of the nappe of Digne, above Draix. Jurassic

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Paysage de la Réserve Géologique de Digne, Lobe de Cousson, Strates du Trias et du Jurassique, Réserve Géologique de Digne, Alpes de Haute Provence, FrancePaysage de la Réserve Géologique de Digne, Lobe de Cousson, Strates du Trias et du Jurassique, Réserve Géologique de Digne, Alpes de Haute Provence, FrancePaysage de la Réserve Géologique de Digne, Lobe de Cousson, Strates du Trias et du Jurassique, Réserve Géologique de Digne, Alpes de Haute Provence, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
2462015

2462015

Paysage de la Réserve Géologique de Digne, Lobe de Cousson,

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Les Terres Noires de Robine sur Galabre. Jurassic (Toarcian) marls rich in organic matter, tender and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Digne Geological Reserve, Alpes de Haute Provence, France.Les Terres Noires de Robine sur Galabre. Jurassic (Toarcian) marls rich in organic matter, tender and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Digne Geological Reserve, Alpes de Haute Provence, France.Les Terres Noires de Robine sur Galabre. Jurassic (Toarcian) marls rich in organic matter, tender and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Digne Geological Reserve, Alpes de Haute Provence, France.© Jean-Philippe Delobelle / BiosphotoJPG - RM
2462014

2462014

Les Terres Noires de Robine sur Galabre. Jurassic (Toarcian)

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Les Terres Noires de Robine sur Galabre. Jurassic (Toarcian) marls rich in organic matter, tender and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Digne Geological Reserve, Alpes de Haute Provence, France.Les Terres Noires de Robine sur Galabre. Jurassic (Toarcian) marls rich in organic matter, tender and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Digne Geological Reserve, Alpes de Haute Provence, France.Les Terres Noires de Robine sur Galabre. Jurassic (Toarcian) marls rich in organic matter, tender and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Digne Geological Reserve, Alpes de Haute Provence, France.© Jean-Philippe Delobelle / BiosphotoJPG - RM
2462013

2462013

Les Terres Noires de Robine sur Galabre. Jurassic (Toarcian)

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Les Terres Noires de Robine sur Galabre. Jurassic (Toarcian) marls rich in organic matter, tender and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Digne Geological Reserve, Alpes de Haute Provence, France.Les Terres Noires de Robine sur Galabre. Jurassic (Toarcian) marls rich in organic matter, tender and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Digne Geological Reserve, Alpes de Haute Provence, France.Les Terres Noires de Robine sur Galabre. Jurassic (Toarcian) marls rich in organic matter, tender and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Digne Geological Reserve, Alpes de Haute Provence, France.© Jean-Philippe Delobelle / BiosphotoJPG - RM
2462012

2462012

Les Terres Noires de Robine sur Galabre. Jurassic (Toarcian)

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Les Terres Noires de Robine sur Galabre. Jurassic (Toarcian) marls rich in organic matter, tender and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Digne Geological Reserve, Alpes de Haute Provence, France.Les Terres Noires de Robine sur Galabre. Jurassic (Toarcian) marls rich in organic matter, tender and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Digne Geological Reserve, Alpes de Haute Provence, France.Les Terres Noires de Robine sur Galabre. Jurassic (Toarcian) marls rich in organic matter, tender and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Digne Geological Reserve, Alpes de Haute Provence, France.© Jean-Philippe Delobelle / BiosphotoJPG - RM
2462011

2462011

Les Terres Noires de Robine sur Galabre. Jurassic (Toarcian)

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Les Terres Noires de Robine sur Galabre. Jurassic (Toarcian) marls rich in organic matter, tender and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Digne Geological Reserve, Alpes de Haute Provence, France.Les Terres Noires de Robine sur Galabre. Jurassic (Toarcian) marls rich in organic matter, tender and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Digne Geological Reserve, Alpes de Haute Provence, France.Les Terres Noires de Robine sur Galabre. Jurassic (Toarcian) marls rich in organic matter, tender and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Digne Geological Reserve, Alpes de Haute Provence, France.© Jean-Philippe Delobelle / BiosphotoJPG - RM
2462010

2462010

Les Terres Noires de Robine sur Galabre. Jurassic (Toarcian)

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Les Terres Noires de Robine sur Galabre. Jurassic (Toarcian) marls rich in organic matter, tender and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Digne Geological Reserve, Alpes de Haute Provence, France.Les Terres Noires de Robine sur Galabre. Jurassic (Toarcian) marls rich in organic matter, tender and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Digne Geological Reserve, Alpes de Haute Provence, France.Les Terres Noires de Robine sur Galabre. Jurassic (Toarcian) marls rich in organic matter, tender and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Digne Geological Reserve, Alpes de Haute Provence, France.© Jean-Philippe Delobelle / BiosphotoJPG - RM
2462009

2462009

Les Terres Noires de Robine sur Galabre. Jurassic (Toarcian)

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Landscape of the Geological Reserve of Digne, Thitonique limestone bar and at the bottom the nappe of Digne (Mountain of Blayeul), above the Bes valley, downstream of the Clue de Barles, Geological Reserve of Digne, Alpes de Haute Provence, FranceLandscape of the Geological Reserve of Digne, Thitonique limestone bar and at the bottom the nappe of Digne (Mountain of Blayeul), above the Bes valley, downstream of the Clue de Barles, Geological Reserve of Digne, Alpes de Haute Provence, FranceLandscape of the Geological Reserve of Digne, Thitonique limestone bar and at the bottom the nappe of Digne (Mountain of Blayeul), above the Bes valley, downstream of the Clue de Barles, Geological Reserve of Digne, Alpes de Haute Provence, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
2462008

2462008

Landscape of the Geological Reserve of Digne, Thitonique

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Les Terres Noires de Robine sur Galabre. Jurassic (Toarcian) marls rich in organic matter, tender and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Digne Geological Reserve, Alpes de Haute Provence, France.Les Terres Noires de Robine sur Galabre. Jurassic (Toarcian) marls rich in organic matter, tender and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Digne Geological Reserve, Alpes de Haute Provence, France.Les Terres Noires de Robine sur Galabre. Jurassic (Toarcian) marls rich in organic matter, tender and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Digne Geological Reserve, Alpes de Haute Provence, France.© Jean-Philippe Delobelle / BiosphotoJPG - RM
2462006

2462006

Les Terres Noires de Robine sur Galabre. Jurassic (Toarcian)

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Les Terres Noires de Robine sur Galabre. Jurassic (Toarcian) marls rich in organic matter, tender and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Digne Geological Reserve, Alpes de Haute Provence, France.Les Terres Noires de Robine sur Galabre. Jurassic (Toarcian) marls rich in organic matter, tender and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Digne Geological Reserve, Alpes de Haute Provence, France.Les Terres Noires de Robine sur Galabre. Jurassic (Toarcian) marls rich in organic matter, tender and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Digne Geological Reserve, Alpes de Haute Provence, France.© Jean-Philippe Delobelle / BiosphotoJPG - RM
2462005

2462005

Les Terres Noires de Robine sur Galabre. Jurassic (Toarcian)

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Les Terres Noires de Robine sur Galabre. Jurassic (Toarcian) marls rich in organic matter, tender and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Digne Geological Reserve, Alpes de Haute Provence, France.Les Terres Noires de Robine sur Galabre. Jurassic (Toarcian) marls rich in organic matter, tender and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Digne Geological Reserve, Alpes de Haute Provence, France.Les Terres Noires de Robine sur Galabre. Jurassic (Toarcian) marls rich in organic matter, tender and very sensitive to gullying, colonized mainly by Scots pines and forming remarkable reliefs in the Digne Geological Reserve, Alpes de Haute Provence, France.© Jean-Philippe Delobelle / BiosphotoJPG - RM
2462004

2462004

Les Terres Noires de Robine sur Galabre. Jurassic (Toarcian)

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The Ammonite Slab in the rising sun in the rain. Over 320 square meters, there are more than 1550 ammonites of all sizes, the largest of which have a diameter of 70 cm! Main species: Coroniceras multicostatum (200 Ma), Digne Geological Reserve, Alpes de Haute Provence, FranceThe Ammonite Slab in the rising sun in the rain. Over 320 square meters, there are more than 1550 ammonites of all sizes, the largest of which have a diameter of 70 cm! Main species: Coroniceras multicostatum (200 Ma), Digne Geological Reserve, Alpes de Haute Provence, FranceThe Ammonite Slab in the rising sun in the rain. Over 320 square meters, there are more than 1550 ammonites of all sizes, the largest of which have a diameter of 70 cm! Main species: Coroniceras multicostatum (200 Ma), Digne Geological Reserve, Alpes de Haute Provence, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
2462002

2462002

The Ammonite Slab in the rising sun in the rain. Over 320 square

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The Ammonite Slab in the rising sun in the rain. Over 320 square meters, there are more than 1550 ammonites of all sizes, the largest of which have a diameter of 70 cm! Main species: Coroniceras multicostatum (200 Ma), Digne Geological Reserve, Alpes de Haute Provence, FranceThe Ammonite Slab in the rising sun in the rain. Over 320 square meters, there are more than 1550 ammonites of all sizes, the largest of which have a diameter of 70 cm! Main species: Coroniceras multicostatum (200 Ma), Digne Geological Reserve, Alpes de Haute Provence, FranceThe Ammonite Slab in the rising sun in the rain. Over 320 square meters, there are more than 1550 ammonites of all sizes, the largest of which have a diameter of 70 cm! Main species: Coroniceras multicostatum (200 Ma), Digne Geological Reserve, Alpes de Haute Provence, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
2462001

2462001

The Ammonite Slab in the rising sun in the rain. Over 320 square

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La Dalle aux Ammonites near Digne - Geological Reserve of. Over 320 square meters, there are more than 1550 ammonites of all sizes, the largest of which have a diameter of 70 cm! Main species: Coroniceras multicostatum (200 Ma), Digne Geological Reserve, Alpes de Haute Provence, FranceLa Dalle aux Ammonites near Digne - Geological Reserve of. Over 320 square meters, there are more than 1550 ammonites of all sizes, the largest of which have a diameter of 70 cm! Main species: Coroniceras multicostatum (200 Ma), Digne Geological Reserve, Alpes de Haute Provence, FranceLa Dalle aux Ammonites near Digne - Geological Reserve of. Over 320 square meters, there are more than 1550 ammonites of all sizes, the largest of which have a diameter of 70 cm! Main species: Coroniceras multicostatum (200 Ma), Digne Geological Reserve, Alpes de Haute Provence, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
2462000

2462000

La Dalle aux Ammonites near Digne - Geological Reserve of. Over

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La Dalle aux Ammonites near Digne - Geological Reserve of. Over 320 square meters, there are more than 1550 ammonites of all sizes, the largest of which have a diameter of 70 cm! Main species: Coroniceras multicostatum (200 Ma), Digne Geological Reserve, Alpes de Haute Provence, FranceLa Dalle aux Ammonites near Digne - Geological Reserve of. Over 320 square meters, there are more than 1550 ammonites of all sizes, the largest of which have a diameter of 70 cm! Main species: Coroniceras multicostatum (200 Ma), Digne Geological Reserve, Alpes de Haute Provence, FranceLa Dalle aux Ammonites near Digne - Geological Reserve of. Over 320 square meters, there are more than 1550 ammonites of all sizes, the largest of which have a diameter of 70 cm! Main species: Coroniceras multicostatum (200 Ma), Digne Geological Reserve, Alpes de Haute Provence, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
2461999

2461999

La Dalle aux Ammonites near Digne - Geological Reserve of. Over

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Terres Noires above Barcelonnette, in the Ubaye valley, Marls and very gullied limestones from the Jurassic period, Alpes de Haute Provence, FranceTerres Noires above Barcelonnette, in the Ubaye valley, Marls and very gullied limestones from the Jurassic period, Alpes de Haute Provence, FranceTerres Noires above Barcelonnette, in the Ubaye valley, Marls and very gullied limestones from the Jurassic period, Alpes de Haute Provence, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
2461314

2461314

Terres Noires above Barcelonnette, in the Ubaye valley, Marls and

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Terres Noires above Barcelonnette, in the Ubaye valley. Very gullied Jurassic marls and limestones dating from the Jurassic period, Alpes de Haute Provence, FranceTerres Noires above Barcelonnette, in the Ubaye valley. Very gullied Jurassic marls and limestones dating from the Jurassic period, Alpes de Haute Provence, FranceTerres Noires above Barcelonnette, in the Ubaye valley. Very gullied Jurassic marls and limestones dating from the Jurassic period, Alpes de Haute Provence, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
2461308

2461308

Terres Noires above Barcelonnette, in the Ubaye valley. Very

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Lake Bersau surrounded by the red sandstones of Permo-Trias, PN des Pyrénées, Vallée d'Ossau, Pyrénées Atlantiques, FranceLake Bersau surrounded by the red sandstones of Permo-Trias, PN des Pyrénées, Vallée d'Ossau, Pyrénées Atlantiques, FranceLake Bersau surrounded by the red sandstones of Permo-Trias, PN des Pyrénées, Vallée d'Ossau, Pyrénées Atlantiques, France© Georges Lopez / BiosphotoJPG - RM
2455344

2455344

Lake Bersau surrounded by the red sandstones of Permo-Trias, PN

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Fossilised (fossilized) shells, plants and crinoids. Karoo, Western Cape, South Africa.Fossilised (fossilized) shells, plants and crinoids. Karoo, Western Cape, South Africa.Fossilised (fossilized) shells, plants and crinoids. Karoo, Western Cape, South Africa.© Roger de La Harpe / BiosphotoJPG - RMNon exclusive sale
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2451817

Fossilised (fossilized) shells, plants and crinoids. Karoo,

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The famous Rosans sandstone balls: spheres formed by crystallization of quartz in secondary age sandstone (- 110 ma) - their size can reach more than a meter in diameter - We find these rare structures in the Spanish Basque Country ( jaizkibel) and on the Pacific coast (Oregon and California) - Saint André de Rosans region, Serre d'Autruy, Baronnies, Hautes Alpes, FranceThe famous Rosans sandstone balls: spheres formed by crystallization of quartz in secondary age sandstone (- 110 ma) - their size can reach more than a meter in diameter - We find these rare structures in the Spanish Basque Country ( jaizkibel) and on the Pacific coast (Oregon and California) - Saint André de Rosans region, Serre d'Autruy, Baronnies, Hautes Alpes, FranceThe famous Rosans sandstone balls: spheres formed by crystallization of quartz in secondary age sandstone (- 110 ma) - their size can reach more than a meter in diameter - We find these rare structures in the Spanish Basque Country ( jaizkibel) and on the Pacific coast (Oregon and California) - Saint André de Rosans region, Serre d'Autruy, Baronnies, Hautes Alpes, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
2446333

2446333

The famous Rosans sandstone balls: spheres formed by

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The famous Rosans sandstone balls: spheres formed by crystallization of quartz in secondary age sandstone (- 110 ma) - their size can reach more than a meter in diameter - We find these rare structures in the Spanish Basque Country ( jaizkibel) and on the Pacific coast (Oregon and California) - Saint André de Rosans region, Serre d'Autruy, Baronnies, Hautes Alpes, FranceThe famous Rosans sandstone balls: spheres formed by crystallization of quartz in secondary age sandstone (- 110 ma) - their size can reach more than a meter in diameter - We find these rare structures in the Spanish Basque Country ( jaizkibel) and on the Pacific coast (Oregon and California) - Saint André de Rosans region, Serre d'Autruy, Baronnies, Hautes Alpes, FranceThe famous Rosans sandstone balls: spheres formed by crystallization of quartz in secondary age sandstone (- 110 ma) - their size can reach more than a meter in diameter - We find these rare structures in the Spanish Basque Country ( jaizkibel) and on the Pacific coast (Oregon and California) - Saint André de Rosans region, Serre d'Autruy, Baronnies, Hautes Alpes, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
2446332

2446332

The famous Rosans sandstone balls: spheres formed by

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The famous Rosans sandstone balls: spheres formed by crystallization of quartz in secondary age sandstone (- 110 ma) - their size can reach more than a meter in diameter - We find these rare structures in the Spanish Basque Country ( jaizkibel) and on the Pacific coast (Oregon and California) - Saint André de Rosans region, Serre d'Autruy, Baronnies, Hautes Alpes, FranceThe famous Rosans sandstone balls: spheres formed by crystallization of quartz in secondary age sandstone (- 110 ma) - their size can reach more than a meter in diameter - We find these rare structures in the Spanish Basque Country ( jaizkibel) and on the Pacific coast (Oregon and California) - Saint André de Rosans region, Serre d'Autruy, Baronnies, Hautes Alpes, FranceThe famous Rosans sandstone balls: spheres formed by crystallization of quartz in secondary age sandstone (- 110 ma) - their size can reach more than a meter in diameter - We find these rare structures in the Spanish Basque Country ( jaizkibel) and on the Pacific coast (Oregon and California) - Saint André de Rosans region, Serre d'Autruy, Baronnies, Hautes Alpes, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
2446331

2446331

The famous Rosans sandstone balls: spheres formed by

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Helminthoid flysch, Traces of fossil activity characteristic of flysch in the Embrun region, Vallon du Rabioux, Ecrins National Park, Hautes Alpes, FranceHelminthoid flysch, Traces of fossil activity characteristic of flysch in the Embrun region, Vallon du Rabioux, Ecrins National Park, Hautes Alpes, FranceHelminthoid flysch, Traces of fossil activity characteristic of flysch in the Embrun region, Vallon du Rabioux, Ecrins National Park, Hautes Alpes, France© Jean-Philippe Delobelle / BiosphotoJPG - RM
2446309

2446309

Helminthoid flysch, Traces of fossil activity characteristic of

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