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Search result Metamorphic rock

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    429 pictures found

    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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    © 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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    © 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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    © 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

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    2543289
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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

    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

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    2543288
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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

    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

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    2543287
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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, 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

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    2543286
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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, 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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    © 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

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    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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    © 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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    © 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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    © 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

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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

    RM2496042JPG

    The Gardon de Sainte Croix in the Cévennes, very ancient

    © Jean-Philippe Delobelle / Biosphoto

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    2496042
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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

    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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    © 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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    © Jean-Philippe Delobelle / Biosphoto

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

    La Cougourde and the small lake of Sagnes, Mercantour National Park, Haut Vallon du Boréon. La Cougourde (squash), made of gneiss, is one of the most famous summits of the Alpes-Maritimes, and a major climbing spot in the Mercantour National Park, Alpes-Maritimes, France

    RM2495084JPG

    La Cougourde and the small lake of Sagnes, Mercantour National Park, Haut Vallon du Boréon. La Cougourde (squash), made of gneiss, is one of the most

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    La Cougourde and the small lake of Sagnes, Mercantour National Park, Haut Vallon du Boréon. La Cougourde (squash), made of gneiss, is one of the most famous summits of the Alpes-Maritimes, and a major climbing spot in the Mercantour National Park, Alpes-Maritimes, France

    Graphics in grey-blue shales from the Brioverian period in Brittany. Brioverian shale in the cove of Ty Marc, Saint Nic, Bay of Douarnenez, Finistère, Brittany, France

    RM2489743JPG

    Graphics in grey-blue shales from the Brioverian period in Brittany. Brioverian shale in the cove of Ty Marc, Saint Nic, Bay of Douarnenez,

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Graphics in grey-blue shales from the Brioverian period in Brittany. Brioverian shale in the cove of Ty Marc, Saint Nic, Bay of Douarnenez, Finistère, Brittany, France

    Graphics in grey-blue shales from the Brioverian period in Brittany. Brioverian shale in the cove of Ty Marc, Saint Nic, Bay of Douarnenez, Finistère, Brittany, France

    RM2489742JPG

    Graphics in grey-blue shales from the Brioverian period in

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Graphics in grey-blue shales from the Brioverian period in Brittany. Brioverian shale in the cove of Ty Marc, Saint Nic, Bay of Douarnenez, Finistère, Brittany, France

    Graphics in grey-blue shales from the Brioverian period in Brittany. Brioverian shale in the cove of Ty Marc, Saint Nic, Bay of Douarnenez, Finistère, Brittany, France

    RM2489741JPG

    Graphics in grey-blue shales from the Brioverian period in

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Graphics in grey-blue shales from the Brioverian period in Brittany. Brioverian shale in the cove of Ty Marc, Saint Nic, Bay of Douarnenez, Finistère, Brittany, France

    Graphics in grey-blue shales from the Brioverian period in Brittany. Brioverian shale in the cove of Ty Marc, Saint Nic, Bay of Douarnenez, Finistère, Brittany, France

    RM2489740JPG

    Graphics in grey-blue shales from the Brioverian period in Brittany. Brioverian shale in the cove of Ty Marc, Saint Nic, Bay of Douarnenez,

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Graphics in grey-blue shales from the Brioverian period in Brittany. Brioverian shale in the cove of Ty Marc, Saint Nic, Bay of Douarnenez, Finistère, Brittany, France

    Milliau Island hornfels. Very old metamorphic rocks, dating from the Precambrian (Cadomian orogeny, around minus 600 Ma). The beds correspond to turbidites, Cadomian submarine avalanches, the light beds were sands, the dark beds were clays, Trebeurden, Côtes d'Armor, Brittany, France

    RM2489664JPG

    Milliau Island hornfels. Very old metamorphic rocks, dating from the Precambrian (Cadomian orogeny, around minus 600 Ma). The beds correspond to

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Milliau Island hornfels. Very old metamorphic rocks, dating from the Precambrian (Cadomian orogeny, around minus 600 Ma). The beds correspond to turbidites, Cadomian submarine avalanches, the light beds were sands, the dark beds were clays, Trebeurden, Côtes d'Armor, Brittany, France

    Milliau Island hornfels. Very old metamorphic rocks, dating from the Precambrian (Cadomian orogeny, around minus 600 Ma). The beds correspond to turbidites, Cadomian submarine avalanches, the light beds were sands, the dark beds were clays, Trebeurden, Côtes d'Armor, Brittany, France

    RM2489663JPG

    Milliau Island hornfels. Very old metamorphic rocks, dating from

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Milliau Island hornfels. Very old metamorphic rocks, dating from the Precambrian (Cadomian orogeny, around minus 600 Ma). The beds correspond to turbidites, Cadomian submarine avalanches, the light beds were sands, the dark beds were clays, Trebeurden, Côtes d'Armor, Brittany, France

    Milliau Island hornfels. Very old metamorphic rocks, dating from the Precambrian (Cadomian orogeny, around minus 600 Ma). The beds correspond to turbidites, Cadomian submarine avalanches, the light beds were sands, the dark beds were clays, Trebeurden, Côtes d'Armor, Brittany, France

    RM2489662JPG

    Milliau Island hornfels. Very old metamorphic rocks, dating from

    © Jean-Philippe Delobelle / Biosphoto

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    2489662
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    © Jean-Philippe Delobelle / Biosphoto

    Milliau Island hornfels. Very old metamorphic rocks, dating from the Precambrian (Cadomian orogeny, around minus 600 Ma). The beds correspond to turbidites, Cadomian submarine avalanches, the light beds were sands, the dark beds were clays, Trebeurden, Côtes d'Armor, Brittany, France

    Pink granites and hornfels enclaves of Milliau Island. Very ancient metamorphic rocks, dating from the Precambrian (Cadomian orogeny, around minus 600 Ma). The beds correspond to turbidites, Cadomian submarine avalanches, the light beds were sands, the dark beds clays, the granites are more recent (- 295 Ma), Trebeurden, Côtes d'Armor, Brittany, France

    RM2489661JPG

    Pink granites and hornfels enclaves of Milliau Island. Very ancient metamorphic rocks, dating from the Precambrian (Cadomian orogeny, around minus

    © Jean-Philippe Delobelle / Biosphoto

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    2489661
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    © Jean-Philippe Delobelle / Biosphoto

    Pink granites and hornfels enclaves of Milliau Island. Very ancient metamorphic rocks, dating from the Precambrian (Cadomian orogeny, around minus 600 Ma). The beds correspond to turbidites, Cadomian submarine avalanches, the light beds were sands, the dark beds clays, the granites are more recent (- 295 Ma), Trebeurden, Côtes d'Armor, Brittany, France

    Milliau Island hornfels. Very old metamorphic rocks, dating from the Precambrian (Cadomian orogeny, around minus 600 Ma). The beds correspond to turbidites, Cadomian submarine avalanches, the light beds were sands, the dark beds were clays, Trebeurden, Côtes d'Armor, Brittany, France

    RM2489660JPG

    Milliau Island hornfels. Very old metamorphic rocks, dating from the Precambrian (Cadomian orogeny, around minus 600 Ma). The beds correspond to

    © Jean-Philippe Delobelle / Biosphoto

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    2489660
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    © Jean-Philippe Delobelle / Biosphoto

    Milliau Island hornfels. Very old metamorphic rocks, dating from the Precambrian (Cadomian orogeny, around minus 600 Ma). The beds correspond to turbidites, Cadomian submarine avalanches, the light beds were sands, the dark beds were clays, Trebeurden, Côtes d'Armor, Brittany, France

    Milliau Island hornfels. Very old metamorphic rocks, dating from the Precambrian (Cadomian orogeny, around minus 600 Ma). The beds correspond to turbidites, Cadomian submarine avalanches, the light beds were sands, the dark beds were clays, Trebeurden, Côtes d'Armor, Brittany, France

    RM2489659JPG

    Milliau Island hornfels. Very old metamorphic rocks, dating from the Precambrian (Cadomian orogeny, around minus 600 Ma). The beds correspond to

    © Jean-Philippe Delobelle / Biosphoto

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    2489659
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    © Jean-Philippe Delobelle / Biosphoto

    Milliau Island hornfels. Very old metamorphic rocks, dating from the Precambrian (Cadomian orogeny, around minus 600 Ma). The beds correspond to turbidites, Cadomian submarine avalanches, the light beds were sands, the dark beds were clays, Trebeurden, Côtes d'Armor, Brittany, France

    Milliau Island hornfels. Very old metamorphic rocks, dating from the Precambrian (Cadomian orogeny, around minus 600 Ma). The beds correspond to turbidites, Cadomian submarine avalanches, the light beds were sands, the dark beds were clays, Trebeurden, Côtes d'Armor, Brittany, France

    RM2489658JPG

    Milliau Island hornfels. Very old metamorphic rocks, dating from

    © Jean-Philippe Delobelle / Biosphoto

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    2489658
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    © Jean-Philippe Delobelle / Biosphoto

    Milliau Island hornfels. Very old metamorphic rocks, dating from the Precambrian (Cadomian orogeny, around minus 600 Ma). The beds correspond to turbidites, Cadomian submarine avalanches, the light beds were sands, the dark beds were clays, Trebeurden, Côtes d'Armor, Brittany, France

    Pink granites and hornfels of Milliau Island. Very ancient metamorphic rocks, dating from the Precambrian (Cadomian orogeny, around minus 600 Ma). The beds correspond to turbidites, Cadomian submarine avalanches; the light beds were sands, the dark beds clays - The granites are more recent (- 295 Ma), Trebeurden, Côtes d'Armor, Brittany, France

    RM2489657JPG

    Pink granites and hornfels of Milliau Island. Very ancient

    © Jean-Philippe Delobelle / Biosphoto

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    2489657
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    © Jean-Philippe Delobelle / Biosphoto

    Pink granites and hornfels of Milliau Island. Very ancient metamorphic rocks, dating from the Precambrian (Cadomian orogeny, around minus 600 Ma). The beds correspond to turbidites, Cadomian submarine avalanches; the light beds were sands, the dark beds clays - The granites are more recent (- 295 Ma), Trebeurden, Côtes d'Armor, Brittany, France

    Milliau Island hornfels. Very old metamorphic rocks, dating from the Precambrian (Cadomian orogeny, around minus 600 Ma). The beds correspond to turbidites, Cadomian submarine avalanches, the light beds were sands, the dark beds were clays, Trebeurden, Côtes d'Armor, Brittany, France

    RM2489656JPG

    Milliau Island hornfels. Very old metamorphic rocks, dating from

    © Jean-Philippe Delobelle / Biosphoto

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    2489656
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    © Jean-Philippe Delobelle / Biosphoto

    Milliau Island hornfels. Very old metamorphic rocks, dating from the Precambrian (Cadomian orogeny, around minus 600 Ma). The beds correspond to turbidites, Cadomian submarine avalanches, the light beds were sands, the dark beds were clays, Trebeurden, Côtes d'Armor, Brittany, France

    Milliau Island hornfels. Very old metamorphic rocks, dating from the Precambrian (Cadomian orogeny, around minus 600 Ma). The beds correspond to turbidites, Cadomian submarine avalanches, the light beds were sands, the dark beds were clays, Trebeurden, Côtes d'Armor, Brittany, France

    RM2489655JPG

    Milliau Island hornfels. Very old metamorphic rocks, dating from the Precambrian (Cadomian orogeny, around minus 600 Ma). The beds correspond to

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Milliau Island hornfels. Very old metamorphic rocks, dating from the Precambrian (Cadomian orogeny, around minus 600 Ma). The beds correspond to turbidites, Cadomian submarine avalanches, the light beds were sands, the dark beds were clays, Trebeurden, Côtes d'Armor, Brittany, France

    Pink granites and hornfels of Milliau Island. Very ancient metamorphic rocks, dating from the Precambrian (Cadomian orogeny, around minus 600 Ma). The beds correspond to turbidites, Cadomian submarine avalanches; the light beds were sands, the dark beds clays - The granites are more recent (- 295 Ma), Trebeurden, Côtes d'Armor, Brittany, France

    RM2489654JPG

    Pink granites and hornfels of Milliau Island. Very ancient

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Pink granites and hornfels of Milliau Island. Very ancient metamorphic rocks, dating from the Precambrian (Cadomian orogeny, around minus 600 Ma). The beds correspond to turbidites, Cadomian submarine avalanches; the light beds were sands, the dark beds clays - The granites are more recent (- 295 Ma), Trebeurden, Côtes d'Armor, Brittany, France

    Rocky coastline at low tide, Postolonnec shale. Anse de Verac'h and Tas de Pois, Presqu'ile de Crozon, Finistère, Brittany, France

    RM2489629JPG

    Rocky coastline at low tide, Postolonnec shale. Anse de Verac'h and Tas de Pois, Presqu'ile de Crozon, Finistère, Brittany, France

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Rocky coastline at low tide, Postolonnec shale. Anse de Verac'h and Tas de Pois, Presqu'ile de Crozon, Finistère, Brittany, France

    Rocky coastline at low tide, Postolonnec shale. Anse de Verac'h and Tas de Pois, Presqu'ile de Crozon, Finistère, Brittany, France

    RM2489628JPG

    Rocky coastline at low tide, Postolonnec shale. Anse de Verac'h

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Rocky coastline at low tide, Postolonnec shale. Anse de Verac'h and Tas de Pois, Presqu'ile de Crozon, Finistère, Brittany, France

    Pointe de Bihit at dusk. Very old metamorphic rocks, dating from the Precambrian (Cadomian orogeny, around minus 600 Ma), Trebeurden, Côtes d'Armor, Brittany, France

    RM2489611JPG

    Pointe de Bihit at dusk. Very old metamorphic rocks, dating from the Precambrian (Cadomian orogeny, around minus 600 Ma), Trebeurden, Côtes d'Armor,

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Pointe de Bihit at dusk. Very old metamorphic rocks, dating from the Precambrian (Cadomian orogeny, around minus 600 Ma), Trebeurden, Côtes d'Armor, Brittany, France

    Pointe de Bihit at dusk. Very old metamorphic rocks, dating from the Precambrian (Cadomian orogeny, around minus 600 Ma), Trebeurden, Côtes d'Armor, Brittany, France

    RM2489610JPG

    Pointe de Bihit at dusk. Very old metamorphic rocks, dating from

    © Jean-Philippe Delobelle / Biosphoto

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    2489610
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    © Jean-Philippe Delobelle / Biosphoto

    Pointe de Bihit at dusk. Very old metamorphic rocks, dating from the Precambrian (Cadomian orogeny, around minus 600 Ma), Trebeurden, Côtes d'Armor, Brittany, France

    Garnet amphibolite thin section under cross-polarized light, Field of view - FOV = 3.4 mm , rolled block in the river Aube, France. Mention : UniLaSalle collection

    RM2486746JPG

    Garnet amphibolite thin section under cross-polarized light, Field of view - FOV = 3.4 mm , rolled block in the river Aube, France. Mention :

    © Jean-Yves Grospas / Biosphoto

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    © Jean-Yves Grospas / Biosphoto

    Garnet amphibolite thin section under cross-polarized light, Field of view - FOV = 3.4 mm , rolled block in the river Aube, France. Mention : UniLaSalle collection

    Restrictions:
    • Non exclusive sale
    • Collection's name mandatory
    Talc thin section under cross-polarized light, Field of view - FOV = 3.4 mm , Mention : UniLaSalle collection

    RM2486745JPG

    Talc thin section under cross-polarized light, Field of view - FOV = 3.4 mm , Mention : UniLaSalle collection

    © Jean-Yves Grospas / Biosphoto

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    © Jean-Yves Grospas / Biosphoto

    Talc thin section under cross-polarized light, Field of view - FOV = 3.4 mm , Mention : UniLaSalle collection

    Restrictions:
    • Non exclusive sale
    • Collection's name mandatory
    Gn,eiss thin section under cross-polarized light, Field of view - FOV = 3.4 mm , Mention : UniLaSalle collection

    RM2486743JPG

    Gn,eiss thin section under cross-polarized light, Field of view - FOV = 3.4 mm , Mention : UniLaSalle collection

    © Jean-Yves Grospas / Biosphoto

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    2486743
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    © Jean-Yves Grospas / Biosphoto

    Gn,eiss thin section under cross-polarized light, Field of view - FOV = 3.4 mm , Mention : UniLaSalle collection

    Restrictions:
    • Non exclusive sale
    • Collection's name mandatory
    Hosta 'Wide Brim' attacked by insects in summer, Moselle, France

    RM2459966JPG

    Hosta 'Wide Brim' attacked by insects in summer, Moselle, France

    © Yann Avril / Biosphoto

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    © Yann Avril / Biosphoto

    Hosta 'Wide Brim' attacked by insects in summer, Moselle, France

    Hosta 'Wide Brim' attacked by insects in summer, Moselle, France

    RM2459965JPG

    Hosta 'Wide Brim' attacked by insects in summer, Moselle, France

    © Yann Avril / Biosphoto

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    © Yann Avril / Biosphoto

    Hosta 'Wide Brim' attacked by insects in summer, Moselle, France

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