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    The organs of Valsenestre, in the Ecrins massif. A spectacular geological site, the Orgues de Valsenestre (or Grande Bibliothèque - Great Library) are formed of thin strata, dating from the Lias, of blue-grey limestone and softer, more eroded schistose marl, compressed and laminated and raised vertically by the Alpine orogeny - Valsenestre - Massif des Ecrins - Alpes

    RM2568016JPG

    The organs of Valsenestre, in the Ecrins massif. A spectacular geological site, the Orgues de Valsenestre (or Grande Bibliothèque - Great Library)

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    The organs of Valsenestre, in the Ecrins massif. A spectacular geological site, the Orgues de Valsenestre (or Grande Bibliothèque - Great Library) are formed of thin strata, dating from the Lias, of blue-grey limestone and softer, more eroded schistose marl, compressed and laminated and raised vertically by the Alpine orogeny - Valsenestre - Massif des Ecrins - Alpes

    The organs of Valsenestre, in the Ecrins massif. A spectacular geological site, the Orgues de Valsenestre (or Grande Bibliothèque - Great Library) are formed of thin strata, dating from the Lias, of blue-grey limestone and softer, more eroded schistose marl, compressed and laminated and raised vertically by the Alpine orogeny - Valsenestre - Massif des Ecrins - Alpes

    RM2568011JPG

    The organs of Valsenestre, in the Ecrins massif. A spectacular geological site, the Orgues de Valsenestre (or Grande Bibliothèque - Great Library)

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    The organs of Valsenestre, in the Ecrins massif. A spectacular geological site, the Orgues de Valsenestre (or Grande Bibliothèque - Great Library) are formed of thin strata, dating from the Lias, of blue-grey limestone and softer, more eroded schistose marl, compressed and laminated and raised vertically by the Alpine orogeny - Valsenestre - Massif des Ecrins - Alpes

    Palmieri fountain and washhouse, built in the 19th century beneath an impressive schist wall. The village is not very touristy, but it is nonetheless a magical place with the look of a medieval film. Cannelle, Corse-du-Sud, France

    RM2602735JPG

    Palmieri fountain and washhouse, built in the 19th century beneath an impressive schist wall. The village is not very touristy, but it is nonetheless

    © Hyacinthe Sambroni / Biosphoto

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    © Hyacinthe Sambroni / Biosphoto

    Palmieri fountain and washhouse, built in the 19th century beneath an impressive schist wall. The village is not very touristy, but it is nonetheless a magical place with the look of a medieval film. Cannelle, Corse-du-Sud, France

    Carpet of lichens on coastal rocks in Galicia (Spain). The hypermumid maritime climate of the Galician coast is ideal for these fruticose lichens, which form veritable lawns on the rocks. Species: Ramalina siliquosa, characteristic of the humid maritime environment. Punta Nariga Cape - Province of A Coruña - Galicia - Spain

    RM2595763JPG

    Carpet of lichens on coastal rocks in Galicia (Spain). The hypermumid maritime climate of the Galician coast is ideal for these fruticose lichens,

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Carpet of lichens on coastal rocks in Galicia (Spain). The hypermumid maritime climate of the Galician coast is ideal for these fruticose lichens, which form veritable lawns on the rocks. Species: Ramalina siliquosa, characteristic of the humid maritime environment. Punta Nariga Cape - Province of A Coruña - Galicia - Spain

    Rochers couverts de lichens (Ramalina siliquosa) et phare en Galice. Ramalina siliquosa est un lichen caractéristique des côtes rocheuses humides - Le phare de Punta Nariga est érigé à l'extrémité d'un promontoire exposé aux pluies abondantes de l’océan atlantique - Province de La Corogne - Galice - Espagne

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    Rochers couverts de lichens (Ramalina siliquosa) et phare en

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Rochers couverts de lichens (Ramalina siliquosa) et phare en Galice. Ramalina siliquosa est un lichen caractéristique des côtes rocheuses humides - Le phare de Punta Nariga est érigé à l'extrémité d'un promontoire exposé aux pluies abondantes de l’océan atlantique - Province de La Corogne - Galice - Espagne

    Lichens on a rocky coast in Galicia (Spain). Fruticose lichen: Ramalina siliquosa, characteristic of a humid maritime environment - crustaceous lichen of the genus Pertusaria, no doubt.

    RM2595761JPG

    Lichens on a rocky coast in Galicia (Spain). Fruticose lichen:

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Lichens on a rocky coast in Galicia (Spain). Fruticose lichen: Ramalina siliquosa, characteristic of a humid maritime environment - crustaceous lichen of the genus Pertusaria, no doubt.

    Playa de Gueirua on the Asturias coast in Spain. Low tide reveals the remarkable polychrome strata of quartzite, sandstone and shale, deformed by tectonics and dating from the Paleozoic (Cambrian/Ordovician) - Asturias - Spain

    RM2595739JPG

    Playa de Gueirua on the Asturias coast in Spain. Low tide reveals

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Playa de Gueirua on the Asturias coast in Spain. Low tide reveals the remarkable polychrome strata of quartzite, sandstone and shale, deformed by tectonics and dating from the Paleozoic (Cambrian/Ordovician) - Asturias - Spain

    Playa de Gueirua on the Asturias coast in Spain. Low tide reveals the remarkable polychrome strata of quartzite, sandstone and shale, deformed by tectonics and dating from the Paleozoic (Cambrian/Ordovician) - Asturias - Spain

    RM2595738JPG

    Playa de Gueirua on the Asturias coast in Spain. Low tide reveals

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Playa de Gueirua on the Asturias coast in Spain. Low tide reveals the remarkable polychrome strata of quartzite, sandstone and shale, deformed by tectonics and dating from the Paleozoic (Cambrian/Ordovician) - Asturias - Spain

    Plolychrome strata of the Baya del Silencio in Spain (Asturias). Spectacular straightened quartzite, sandstone and shale strata, deformed and bent by tectonics, dating from the Paleozoic (Cambrian/Ordovician) - Baya del Silencio, Asturias, Spain

    RM2595716JPG

    Plolychrome strata of the Baya del Silencio in Spain (Asturias). Spectacular straightened quartzite, sandstone and shale strata, deformed and bent by

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Plolychrome strata of the Baya del Silencio in Spain (Asturias). Spectacular straightened quartzite, sandstone and shale strata, deformed and bent by tectonics, dating from the Paleozoic (Cambrian/Ordovician) - Baya del Silencio, Asturias, Spain

    Plolychrome strata at Playa del Silencio, Spain (Asturias). Remarkable tectonically straightened quartzite, sandstone and shale strata from the Paleozoic (Cambrian/Ordovician) - Baya del Silencio, Asturias, Spain

    RM2595715JPG

    Plolychrome strata at Playa del Silencio, Spain (Asturias).

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Plolychrome strata at Playa del Silencio, Spain (Asturias). Remarkable tectonically straightened quartzite, sandstone and shale strata from the Paleozoic (Cambrian/Ordovician) - Baya del Silencio, Asturias, Spain

    Crustacean lichens of the genus Rhizocarpon (geographicum) on quartzite. Vanoise National Park, Savoie, France

    RM2592851JPG

    Crustacean lichens of the genus Rhizocarpon (geographicum) on quartzite. Vanoise National Park, Savoie, France

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Crustacean lichens of the genus Rhizocarpon (geographicum) on quartzite. Vanoise National Park, Savoie, France

    Rue de la pierre perdue, by Michel Rousseau, born in 1936, mason with the Compagnons du devoir, also worked in factories, he recovers bricks, tiles, slates and tiles, for objects he goes to bric-a-brac, he wants to denounce waste. Besse-sur-Braye, Sarthe, France

    RM2581294JPG

    Rue de la pierre perdue, by Michel Rousseau, born in 1936, mason with the Compagnons du devoir, also worked in factories, he recovers bricks, tiles,

    © Michel Gile / Biosphoto

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    © Michel Gile / Biosphoto

    Rue de la pierre perdue, by Michel Rousseau, born in 1936, mason with the Compagnons du devoir, also worked in factories, he recovers bricks, tiles, slates and tiles, for objects he goes to bric-a-brac, he wants to denounce waste. Besse-sur-Braye, Sarthe, France

    Rue de la pierre perdue, by Michel Rousseau, born in 1936, mason with the Compagnons du devoir, also worked in factories, he recovers bricks, tiles, slates and tiles, for objects he goes to bric-a-brac, he wants to denounce waste. Besse-sur-Braye, Sarthe, France

    RM2581293JPG

    Rue de la pierre perdue, by Michel Rousseau, born in 1936, mason with the Compagnons du devoir, also worked in factories, he recovers bricks, tiles,

    © Michel Gile / Biosphoto

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    © Michel Gile / Biosphoto

    Rue de la pierre perdue, by Michel Rousseau, born in 1936, mason with the Compagnons du devoir, also worked in factories, he recovers bricks, tiles, slates and tiles, for objects he goes to bric-a-brac, he wants to denounce waste. Besse-sur-Braye, Sarthe, France

    Rue de la pierre perdue, by Michel Rousseau, born in 1936, mason with the Compagnons du devoir, also worked in factories, he recovers bricks, tiles, slates and tiles, for objects he goes to bric-a-brac, he wants to denounce waste. Besse-sur-Braye, Sarthe, France

    RM2581292JPG

    Rue de la pierre perdue, by Michel Rousseau, born in 1936,

    © Michel Gile / Biosphoto

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    © Michel Gile / Biosphoto

    Rue de la pierre perdue, by Michel Rousseau, born in 1936, mason with the Compagnons du devoir, also worked in factories, he recovers bricks, tiles, slates and tiles, for objects he goes to bric-a-brac, he wants to denounce waste. Besse-sur-Braye, Sarthe, France

    Rue de la pierre perdue, by Michel Rousseau, born in 1936, mason with the Compagnons du devoir, also worked in factories, he recovers bricks, tiles, slates and tiles, for objects he goes to bric-a-brac, he wants to denounce waste. Besse-sur-Braye, Sarthe, France

    RM2581291JPG

    Rue de la pierre perdue, by Michel Rousseau, born in 1936, mason with the Compagnons du devoir, also worked in factories, he recovers bricks, tiles,

    © Michel Gile / Biosphoto

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    © Michel Gile / Biosphoto

    Rue de la pierre perdue, by Michel Rousseau, born in 1936, mason with the Compagnons du devoir, also worked in factories, he recovers bricks, tiles, slates and tiles, for objects he goes to bric-a-brac, he wants to denounce waste. Besse-sur-Braye, Sarthe, France

    La Grand Pallière Neolithic tomb in the Cévennes. La Grand Pallière Neolithic necropolis, on the Cévennes heights at around 440m altitude in the Anduze region: central-chest mounds, dating from the late Neolithic to the Iron Age - Cévennes (Gard) - France

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    La Grand Pallière Neolithic tomb in the Cévennes. La Grand Pallière Neolithic necropolis, on the Cévennes heights at around 440m altitude in the

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    La Grand Pallière Neolithic tomb in the Cévennes. La Grand Pallière Neolithic necropolis, on the Cévennes heights at around 440m altitude in the Anduze region: central-chest mounds, dating from the late Neolithic to the Iron Age - Cévennes (Gard) - France

    The organs of Valsenestre, in the Ecrins massif. A spectacular geological site, the Orgues de Valsenestre (or Grande Bibliothèque - Great Library) are formed of thin strata, dating from the Lias, of blue-grey limestone and softer, more eroded schistose marl, compressed and laminated and raised vertically by the Alpine orogeny - Valsenestre - Massif des Ecrins - Alpes

    RM2568015JPG

    The organs of Valsenestre, in the Ecrins massif. A spectacular

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    The organs of Valsenestre, in the Ecrins massif. A spectacular geological site, the Orgues de Valsenestre (or Grande Bibliothèque - Great Library) are formed of thin strata, dating from the Lias, of blue-grey limestone and softer, more eroded schistose marl, compressed and laminated and raised vertically by the Alpine orogeny - Valsenestre - Massif des Ecrins - Alpes

    The organs of Valsenestre, in the Ecrins massif. A spectacular geological site, the Orgues de Valsenestre (or Grande Bibliothèque - Great Library) are formed of thin strata, dating from the Lias, of blue-grey limestone and softer, more eroded schistose marl, compressed and laminated and raised vertically by the Alpine orogeny - Valsenestre - Massif des Ecrins - Alpes

    RM2568014JPG

    The organs of Valsenestre, in the Ecrins massif. A spectacular

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    The organs of Valsenestre, in the Ecrins massif. A spectacular geological site, the Orgues de Valsenestre (or Grande Bibliothèque - Great Library) are formed of thin strata, dating from the Lias, of blue-grey limestone and softer, more eroded schistose marl, compressed and laminated and raised vertically by the Alpine orogeny - Valsenestre - Massif des Ecrins - Alpes

    The organs of Valsenestre, in the Ecrins massif. A spectacular geological site, the Orgues de Valsenestre (or Grande Bibliothèque - Great Library) are formed of thin strata, dating from the Lias, of blue-grey limestone and softer, more eroded schistose marl, compressed and laminated and raised vertically by the Alpine orogeny - Valsenestre - Massif des Ecrins - Alpes

    RM2568013JPG

    The organs of Valsenestre, in the Ecrins massif. A spectacular

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    The organs of Valsenestre, in the Ecrins massif. A spectacular geological site, the Orgues de Valsenestre (or Grande Bibliothèque - Great Library) are formed of thin strata, dating from the Lias, of blue-grey limestone and softer, more eroded schistose marl, compressed and laminated and raised vertically by the Alpine orogeny - Valsenestre - Massif des Ecrins - Alpes

    The organs of Valsenestre, in the Ecrins massif. A spectacular geological site, the Orgues de Valsenestre (or Grande Bibliothèque - Great Library) are formed of thin strata, dating from the Lias, of blue-grey limestone and softer, more eroded schistose marl, compressed and laminated and raised vertically by the Alpine orogeny - Valsenestre - Massif des Ecrins - Alpes

    RM2568012JPG

    The organs of Valsenestre, in the Ecrins massif. A spectacular geological site, the Orgues de Valsenestre (or Grande Bibliothèque - Great Library)

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    The organs of Valsenestre, in the Ecrins massif. A spectacular geological site, the Orgues de Valsenestre (or Grande Bibliothèque - Great Library) are formed of thin strata, dating from the Lias, of blue-grey limestone and softer, more eroded schistose marl, compressed and laminated and raised vertically by the Alpine orogeny - Valsenestre - Massif des Ecrins - Alpes

    The organs of Valsenestre, in the Ecrins massif. A spectacular geological site, the Orgues de Valsenestre (or Grande Bibliothèque - Great Library) are formed of thin strata, dating from the Lias, of blue-grey limestone and softer, more eroded schistose marl, compressed and laminated and raised vertically by the Alpine orogeny - Valsenestre - Massif des Ecrins - Alpes

    RM2568010JPG

    The organs of Valsenestre, in the Ecrins massif. A spectacular geological site, the Orgues de Valsenestre (or Grande Bibliothèque - Great Library)

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    The organs of Valsenestre, in the Ecrins massif. A spectacular geological site, the Orgues de Valsenestre (or Grande Bibliothèque - Great Library) are formed of thin strata, dating from the Lias, of blue-grey limestone and softer, more eroded schistose marl, compressed and laminated and raised vertically by the Alpine orogeny - Valsenestre - Massif des Ecrins - Alpes

    Serpentinite at Cap Corse. This rock forms at oceanic ridges where magma is altered by hydrothermal fluids. This alteration, which takes the form of veinlets on the rock, corresponds to the serpentinization of mantle peridotites by hydration (transformation of the minerals olivine and pyroxene into serpentine by reaction with these fluids). Serpentinites are particularly common in ophiolites, as seen here on Cap Corse.

    RM2565931JPG

    Serpentinite at Cap Corse. This rock forms at oceanic ridges where magma is altered by hydrothermal fluids. This alteration, which takes the form of

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Serpentinite at Cap Corse. This rock forms at oceanic ridges where magma is altered by hydrothermal fluids. This alteration, which takes the form of veinlets on the rock, corresponds to the serpentinization of mantle peridotites by hydration (transformation of the minerals olivine and pyroxene into serpentine by reaction with these fluids). Serpentinites are particularly common in ophiolites, as seen here on Cap Corse.

    Serpentinite outcrop at Cap Corse. This rock forms at oceanic ridges, where magma is altered by hydrothermal fluids. This alteration, which takes the form of veinlets on the rock, corresponds to the serpentinization of mantle peridotites by hydration (transformation of the minerals olivine and pyroxene into serpentine by reaction with these fluids). Serpentinites outcrop in ophiolites, as seen here at Cap Corse. (seafloor obduction)

    RM2565930JPG

    Serpentinite outcrop at Cap Corse. This rock forms at oceanic ridges, where magma is altered by hydrothermal fluids. This alteration, which takes the

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Serpentinite outcrop at Cap Corse. This rock forms at oceanic ridges, where magma is altered by hydrothermal fluids. This alteration, which takes the form of veinlets on the rock, corresponds to the serpentinization of mantle peridotites by hydration (transformation of the minerals olivine and pyroxene into serpentine by reaction with these fluids). Serpentinites outcrop in ophiolites, as seen here at Cap Corse. (seafloor obduction)

    Mountain landscape in Scoresby Sound, Greenland, with icebergs drifting in the Ofjord at the foot of Grundtvigskirken.

    RM2564271JPG

    Mountain landscape in Scoresby Sound, Greenland, with icebergs drifting in the Ofjord at the foot of Grundtvigskirken.

    © Raphaël Sané / Biosphoto

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    © Raphaël Sané / Biosphoto

    Mountain landscape in Scoresby Sound, Greenland, with icebergs drifting in the Ofjord at the foot of Grundtvigskirken.

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    Islet of metamorphic rock polished by the ancient movements of a glacier, Dahlbreen, Spitsbergen, Svalbard archipelago

    RM2563645JPG

    Islet of metamorphic rock polished by the ancient movements of a glacier, Dahlbreen, Spitsbergen, Svalbard archipelago

    © Raphaël Sané / Biosphoto

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    © Raphaël Sané / Biosphoto

    Islet of metamorphic rock polished by the ancient movements of a glacier, Dahlbreen, Spitsbergen, Svalbard archipelago

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    Marble lion's head covered in moss and various other plants, Fontaine de l'Intendance, Montpellier, Herault, France

    RM2552471JPG

    Marble lion's head covered in moss and various other plants,

    © Marie Aymerez / Biosphoto

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    © Marie Aymerez / Biosphoto

    Marble lion's head covered in moss and various other plants, Fontaine de l'Intendance, Montpellier, Herault, France

    Labret in gneiss. Mali, Neolithic. 7 cm.

    RM2552257JPG

    Labret in gneiss. Mali, Neolithic. 7 cm.

    © Pascal Goetgheluck / Biosphoto

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    © Pascal Goetgheluck / Biosphoto

    Labret in gneiss. Mali, Neolithic. 7 cm.

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    Labret in gneiss. Mali, Neolithic. 7 cm.

    RM2552256JPG

    Labret in gneiss. Mali, Neolithic. 7 cm.

    © Pascal Goetgheluck / Biosphoto

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    © Pascal Goetgheluck / Biosphoto

    Labret in gneiss. Mali, Neolithic. 7 cm.

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    Spatula ax with long pointed heel. Gray quartzite. North Africa, Neolithic. 20.5cm.

    RM2552190JPG

    Spatula ax with long pointed heel. Gray quartzite. North Africa,

    © Pascal Goetgheluck / Biosphoto

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    © Pascal Goetgheluck / Biosphoto

    Spatula ax with long pointed heel. Gray quartzite. North Africa, Neolithic. 20.5cm.

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    Polished gneiss axe. North Africa, Neolithic. 5.2cm.

    RM2552148JPG

    Polished gneiss axe. North Africa, Neolithic. 5.2cm.

    © Pascal Goetgheluck / Biosphoto

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    © Pascal Goetgheluck / Biosphoto

    Polished gneiss axe. North Africa, Neolithic. 5.2cm.

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    Triangular polished ax in gneiss. Neolithic period. Sub-Saharan Africa. 4.2cm.

    RM2552140JPG

    Triangular polished ax in gneiss. Neolithic period. Sub-Saharan Africa. 4.2cm.

    © Pascal Goetgheluck / Biosphoto

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    © Pascal Goetgheluck / Biosphoto

    Triangular polished ax in gneiss. Neolithic period. Sub-Saharan Africa. 4.2cm.

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    Polished gneiss axe. North Africa, Neolithic. 6,5cm.

    RM2552133JPG

    Polished gneiss axe. North Africa, Neolithic. 6,5cm.

    © Pascal Goetgheluck / Biosphoto

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    © Pascal Goetgheluck / Biosphoto

    Polished gneiss axe. North Africa, Neolithic. 6,5cm.

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    Crustose lichen Xanthoria elegans on a quartzite wall, Saxicolous, nitrophilous, thermophilous and heliophilous species with mountainous tendencies, Grande Sassière Reserve, Vanoise, Savoie, France

    RM2551592JPG

    Crustose lichen Xanthoria elegans on a quartzite wall, Saxicolous, nitrophilous, thermophilous and heliophilous species with mountainous tendencies,

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Crustose lichen Xanthoria elegans on a quartzite wall, Saxicolous, nitrophilous, thermophilous and heliophilous species with mountainous tendencies, Grande Sassière Reserve, Vanoise, Savoie, France

    Crustose lichen Xanthoria elegans on a quartzite wall, Saxicolous, nitrophilous, thermophilous and heliophilous species with mountainous tendencies, Grande Sassière Reserve, Vanoise, Savoie, France

    RM2551591JPG

    Crustose lichen Xanthoria elegans on a quartzite wall, Saxicolous, nitrophilous, thermophilous and heliophilous species with mountainous tendencies,

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Crustose lichen Xanthoria elegans on a quartzite wall, Saxicolous, nitrophilous, thermophilous and heliophilous species with mountainous tendencies, Grande Sassière Reserve, Vanoise, Savoie, France

    Waterfall in the Clou valley. The Clou stream runs through very resistant quartzite. The Clou valley, located in the commune of Sainte-Foy-Tarentaise, is listed as a "classified site" in the Savoie department. Alps, France

    RM2551308JPG

    Waterfall in the Clou valley. The Clou stream runs through very resistant quartzite. The Clou valley, located in the commune of

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Waterfall in the Clou valley. The Clou stream runs through very resistant quartzite. The Clou valley, located in the commune of Sainte-Foy-Tarentaise, is listed as a "classified site" in the Savoie department. Alps, France

    Standing Stones of Callanish (Callanish 1) on the Isle of Lewis in the Outer Hebrides. The megalithic monument is cross shaped with a central ring of stones and was buildt between 2900 and 2600 BC. It is probably oriented towards the moon not the sun. Europe, Scotland, July

    RM2543292JPG

    Standing Stones of Callanish (Callanish 1) on the Isle of Lewis in the Outer Hebrides. The megalithic monument is cross shaped with

    © Martin Zwick / Biosphoto

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    2543292
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    © Martin Zwick / Biosphoto

    Standing Stones of Callanish (Callanish 1) on the Isle of Lewis in the Outer Hebrides. The megalithic monument is cross shaped with a central ring of stones and was buildt between 2900 and 2600 BC. It is probably oriented towards the moon not the sun. Europe, Scotland, July

    Standing Stones of Callanish (Callanish 1) on the Isle of Lewis in the Outer Hebrides. The megalithic monument is cross shaped with a central ring of stones and was buildt between 2900 and 2600 BC. It is probably oriented towards the moon not the sun. Europe, Scotland, July

    RM2543291JPG

    Standing Stones of Callanish (Callanish 1) on the Isle of Lewis in the Outer Hebrides. The megalithic monument is cross shaped with

    © Martin Zwick / Biosphoto

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    2543291
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    © Martin Zwick / Biosphoto

    Standing Stones of Callanish (Callanish 1) on the Isle of Lewis in the Outer Hebrides. The megalithic monument is cross shaped with a central ring of stones and was buildt between 2900 and 2600 BC. It is probably oriented towards the moon not the sun. Europe, Scotland, July

    Standing Stones of Callanish (Callanish 1) on the Isle of Lewis in the Outer Hebrides. The megalithic monument is cross shaped with a central ring of stones and was buildt between 2900 and 2600 BC. It is probably oriented towards the moon not the sun. Europe, Scotland, July

    RM2543290JPG

    Standing Stones of Callanish (Callanish 1) on the Isle of Lewis in the Outer Hebrides. The megalithic monument is cross shaped with

    © Martin Zwick / Biosphoto

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    2543290
    Right Managed

    © Martin Zwick / Biosphoto

    Standing Stones of Callanish (Callanish 1) on the Isle of Lewis in the Outer Hebrides. The megalithic monument is cross shaped with a central ring of stones and was buildt between 2900 and 2600 BC. It is probably oriented towards the moon not the sun. Europe, Scotland, July

    Standing Stones of Callanish (Callanish 1) on the Isle of Lewis in the Outer Hebrides. The megalithic monument is cross shaped with a central ring of stones and was buildt between 2900 and 2600 BC. It is probably oriented towards the moon not the sun. Europe, Scotland, July

    RM2543289JPG

    Standing Stones of Callanish (Callanish 1) on the Isle of Lewis in the Outer Hebrides. The megalithic monument is cross shaped with

    © Martin Zwick / Biosphoto

    LightboxinfoDownload low resolution image

    2543289
    Right Managed

    © Martin Zwick / Biosphoto

    Standing Stones of Callanish (Callanish 1) on the Isle of Lewis in the Outer Hebrides. The megalithic monument is cross shaped with a central ring of stones and was buildt between 2900 and 2600 BC. It is probably oriented towards the moon not the sun. Europe, Scotland, July

    Standing Stones of Callanish (Callanish 1) on the Isle of Lewis in the Outer Hebrides. The megalithic monument is cross shaped with a central ring of stones and was buildt between 2900 and 2600 BC. It is probably oriented towards the moon not the sun. Europe, Scotland, July

    RM2543288JPG

    Standing Stones of Callanish (Callanish 1) on the Isle of Lewis in the Outer Hebrides. The megalithic monument is cross shaped

    © Martin Zwick / Biosphoto

    LightboxinfoDownload low resolution image

    2543288
    Right Managed

    © Martin Zwick / Biosphoto

    Standing Stones of Callanish (Callanish 1) on the Isle of Lewis in the Outer Hebrides. The megalithic monument is cross shaped with a central ring of stones and was buildt between 2900 and 2600 BC. It is probably oriented towards the moon not the sun. Europe, Scotland, July

    Standing Stones of Callanish (Callanish 1) on the Isle of Lewis in the Outer Hebrides. The megalithic monument is cross shaped with a central ring of stones and was buildt between 2900 and 2600 BC. It is probably oriented towards the moon not the sun. Europe, Scotland, July

    RM2543287JPG

    Standing Stones of Callanish (Callanish 1) on the Isle of Lewis in the Outer Hebrides. The megalithic monument is cross shaped with a central ring

    © Martin Zwick / Biosphoto

    LightboxinfoDownload low resolution image

    2543287
    Right Managed

    © Martin Zwick / Biosphoto

    Standing Stones of Callanish (Callanish 1) on the Isle of Lewis in the Outer Hebrides. The megalithic monument is cross shaped with a central ring of stones and was buildt between 2900 and 2600 BC. It is probably oriented towards the moon not the sun. Europe, Scotland, July

    Standing Stones of Callanish (Callanish 1) on the Isle of Lewis in the Outer Hebrides. The megalithic monument is cross shaped with a central ring of stones and was buildt between 2900 and 2600 BC. It is probably oriented towards the moon not the sun. Europe, Scotland, June

    RM2543286JPG

    Standing Stones of Callanish (Callanish 1) on the Isle of Lewis in the Outer Hebrides. The megalithic monument is cross shaped with

    © Martin Zwick / Biosphoto

    LightboxinfoDownload low resolution image

    2543286
    Right Managed

    © Martin Zwick / Biosphoto

    Standing Stones of Callanish (Callanish 1) on the Isle of Lewis in the Outer Hebrides. The megalithic monument is cross shaped with a central ring of stones and was buildt between 2900 and 2600 BC. It is probably oriented towards the moon not the sun. Europe, Scotland, June

    Worked marble beam, located in the submerged Nymphaeum of Emperor Claudius, near Punta Epitaffio , Marine Protected Area of Baia, Naples, Italy, Tyrrhenian Sea

    RM2497309JPG

    Worked marble beam, located in the submerged Nymphaeum of Emperor Claudius, near Punta Epitaffio , Marine Protected Area of Baia, Naples, Italy,

    © Franco Banfi / Biosphoto

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    2497309
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    © Franco Banfi / Biosphoto

    Worked marble beam, located in the submerged Nymphaeum of Emperor Claudius, near Punta Epitaffio , Marine Protected Area of Baia, Naples, Italy, Tyrrhenian Sea

    Restrictions:
    • Non exclusive sale, exclusive sale possible in France
    Rock-shield Lichen (Xanthoparmelia conspersa) on shale in the Cevennes, France

    RM2496078JPG

    Rock-shield Lichen (Xanthoparmelia conspersa) on shale in the Cevennes, France

    © Jean-Philippe Delobelle / Biosphoto

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    2496078
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    © Jean-Philippe Delobelle / Biosphoto

    Rock-shield Lichen (Xanthoparmelia conspersa) on shale in the Cevennes, France

    The Gardon de Sainte Croix in the Cévennes, very ancient micaschists of Cambrian/Ordovician age deformed by Hercynian tectonics, Le Martinet, St Etienne Vallée Française, Cévennes, France

    RM2496045JPG

    The Gardon de Sainte Croix in the Cévennes, very ancient

    © Jean-Philippe Delobelle / Biosphoto

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    2496045
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    © Jean-Philippe Delobelle / Biosphoto

    The Gardon de Sainte Croix in the Cévennes, very ancient micaschists of Cambrian/Ordovician age deformed by Hercynian tectonics, Le Martinet, St Etienne Vallée Française, Cévennes, France

    The Gardon de Sainte Croix in the Cévennes, very ancient micaschists of Cambrian/Ordovician age deformed by Hercynian tectonics, Le Martinet, St Etienne Vallée Française, Cévennes, France

    RM2496044JPG

    The Gardon de Sainte Croix in the Cévennes, very ancient micaschists of Cambrian/Ordovician age deformed by Hercynian tectonics, Le Martinet, St

    © Jean-Philippe Delobelle / Biosphoto

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    2496044
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    © Jean-Philippe Delobelle / Biosphoto

    The Gardon de Sainte Croix in the Cévennes, very ancient micaschists of Cambrian/Ordovician age deformed by Hercynian tectonics, Le Martinet, St Etienne Vallée Française, Cévennes, France

    The Gardon de Sainte Croix in the Cévennes, very ancient micaschists of Cambrian/Ordovician age deformed by Hercynian tectonics, Le Martinet, St Etienne Vallée Française, Cévennes, France

    RM2496043JPG

    The Gardon de Sainte Croix in the Cévennes, very ancient micaschists of Cambrian/Ordovician age deformed by Hercynian tectonics, Le Martinet, St

    © Jean-Philippe Delobelle / Biosphoto

    LightboxinfoDownload low resolution image

    2496043
    Right Managed

    © Jean-Philippe Delobelle / Biosphoto

    The Gardon de Sainte Croix in the Cévennes, very ancient micaschists of Cambrian/Ordovician age deformed by Hercynian tectonics, Le Martinet, St Etienne Vallée Française, Cévennes, France

    The Gardon de Sainte Croix in the Cévennes, very ancient micaschists of Cambrian/Ordovician age deformed by Hercynian tectonics, Le Martinet, St Etienne Vallée Française, Cévennes, France

    RM2496042JPG

    The Gardon de Sainte Croix in the Cévennes, very ancient

    © Jean-Philippe Delobelle / Biosphoto

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    2496042
    Right Managed

    © Jean-Philippe Delobelle / Biosphoto

    The Gardon de Sainte Croix in the Cévennes, very ancient micaschists of Cambrian/Ordovician age deformed by Hercynian tectonics, Le Martinet, St Etienne Vallée Française, Cévennes, France

    Cladonia lichens (white: Cladonia portentosa, green: Cladonia coniocraea), Polypodial and Capillary ferns, and various mosses on shale, Cevennes, France

    RM2496038JPG

    Cladonia lichens (white: Cladonia portentosa, green: Cladonia

    © Jean-Philippe Delobelle / Biosphoto

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    2496038
    Right Managed

    © Jean-Philippe Delobelle / Biosphoto

    Cladonia lichens (white: Cladonia portentosa, green: Cladonia coniocraea), Polypodial and Capillary ferns, and various mosses on shale, Cevennes, France

    Old bridge in the Cevennes, Saint-Martin-de-Boubaux, Galaizon Valley, Cevennes, France

    RM2496036JPG

    Old bridge in the Cevennes, Saint-Martin-de-Boubaux, Galaizon Valley, Cevennes, France

    © Jean-Philippe Delobelle / Biosphoto

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    2496036
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    © Jean-Philippe Delobelle / Biosphoto

    Old bridge in the Cevennes, Saint-Martin-de-Boubaux, Galaizon Valley, Cevennes, France

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