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    1853 pictures found

    Wild horse near the Merrick butte. Monument valley national park. Arizona. USA.

    RM2572016JPG

    Wild horse near the Merrick butte. Monument valley national park. Arizona. USA.

    © Antoine Lorgnier / Biosphoto

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    © Antoine Lorgnier / Biosphoto

    Wild horse near the Merrick butte. Monument valley national park. Arizona. USA.

    Antelope Canyon. The Upper Antelope Canyon, 2 to 3 m wide and 400 m long, managed by the Navajo Indian tribe, Arizona, USA.

    RM2571996JPG

    Antelope Canyon. The Upper Antelope Canyon, 2 to 3 m wide and 400 m long, managed by the Navajo Indian tribe, Arizona, USA.

    © Antoine Lorgnier / Biosphoto

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    © Antoine Lorgnier / Biosphoto

    Antelope Canyon. The Upper Antelope Canyon, 2 to 3 m wide and 400 m long, managed by the Navajo Indian tribe, Arizona, USA.

    Long-nosed Leopard Lizard (Gambelia wislizenii) during basking in the morning, Arches national park, Utah, USA

    RM2553578JPG

    Long-nosed Leopard Lizard (Gambelia wislizenii) during basking in the morning, Arches national park, Utah, USA

    © Tonči Maletic / Biosphoto

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    © Tonči Maletic / Biosphoto

    Long-nosed Leopard Lizard (Gambelia wislizenii) during basking in the morning, Arches national park, Utah, USA

    Kestrel (Falco tinnunculus) emerging from its nest in an old sandstone wall, France

    RM2101586JPG

    Kestrel (Falco tinnunculus) emerging from its nest in an old sandstone wall, France

    © Olivier Gutfreund / Biosphoto

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    © Olivier Gutfreund / Biosphoto

    Kestrel (Falco tinnunculus) emerging from its nest in an old sandstone wall, France

    Puma (Puma concolor) leaping on a rocky ledge, USA

    RM2088911JPG

    Puma (Puma concolor) leaping on a rocky ledge, USA

    © Juan-Carlos Muñoz / Biosphoto

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    © Juan-Carlos Muñoz / Biosphoto

    Puma (Puma concolor) leaping on a rocky ledge, USA

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

    RM2033220JPG

    Bristlecone pine multimillennial - Cedar Breaks NM Utah USA ; Older than 2000 years
    Pines growing at very high altitude (3000 m) and can survive

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

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

    Blackjack pines and Hoodoos - Bryce Canyon NP Utah USA ; Amphiteatre<br>Deltaic sediments of Jurassic age (Claron Formation) of sandstone, dolomite and marl colored by iron oxides and carved by erosion in an amphitheater of hoodoos (pinnacles) arches and bridgesThe reflected light (spectral) from sunrise sun enriched natural polychrome these high walls sometimes nearly 50 meters

    RM2033217JPG

    Blackjack pines and Hoodoos - Bryce Canyon NP Utah USA ; Amphiteatre
    Deltaic sediments of Jurassic age (Claron Formation) of sandstone, dolomite

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Blackjack pines and Hoodoos - Bryce Canyon NP Utah USA ; Amphiteatre
    Deltaic sediments of Jurassic age (Claron Formation) of sandstone, dolomite and marl colored by iron oxides and carved by erosion in an amphitheater of hoodoos (pinnacles) arches and bridgesThe reflected light (spectral) from sunrise sun enriched natural polychrome these high walls sometimes nearly 50 meters

    Dome Navajo sandstone - Grand Staircase-Escalante NM Utah ; Petrified wave<br>The Navajo Sandstone is from wind (petrified dunes) and date from the early Jurassic (desert on the west side of Pangaea)

    RM2033183JPG

    Dome Navajo sandstone - Grand Staircase-Escalante NM Utah ; Petrified wave
    The Navajo Sandstone is from wind (petrified dunes) and date from the

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Dome Navajo sandstone - Grand Staircase-Escalante NM Utah ; Petrified wave
    The Navajo Sandstone is from wind (petrified dunes) and date from the early Jurassic (desert on the west side of Pangaea)

    Eroded sandstone massif Jaizkibel Basque Country Spain

    RM1871696JPG

    Eroded sandstone massif Jaizkibel Basque Country Spain

    © Juan-Carlos Muñoz / Biosphoto

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    © Juan-Carlos Muñoz / Biosphoto

    Eroded sandstone massif Jaizkibel Basque Country Spain

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    • Non exclusive sale, exclusive sale possible in France
    Sunrise at Mesa Arch stone arch, Canyonlands National Park, near Moab, Utah, United States, North America

    RM2093928JPG

    Sunrise at Mesa Arch stone arch, Canyonlands National Park, near Moab, Utah, United States, North America

    © Michael Rucker / imageBROKER / Biosphoto

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    © Michael Rucker / imageBROKER / Biosphoto

    Sunrise at Mesa Arch stone arch, Canyonlands National Park, near Moab, Utah, United States, North America

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    The cave dwellings of Graufthal, Bas-Rhin, Alsace, France

    RM2602204JPG

    The cave dwellings of Graufthal, Bas-Rhin, Alsace, France

    © Yann Avril / Biosphoto

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    © Yann Avril / Biosphoto

    The cave dwellings of Graufthal, Bas-Rhin, Alsace, France

    The cave dwellings of Graufthal, Bas-Rhin, Alsace, France

    RM2602203JPG

    The cave dwellings of Graufthal, Bas-Rhin, Alsace, France

    © Yann Avril / Biosphoto

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    © Yann Avril / Biosphoto

    The cave dwellings of Graufthal, Bas-Rhin, Alsace, France

    Landscape of the Tabernas Desert, Andalusia (Spain). An ancient Miocene sedimentary basin (- 8Ma) at the foot of the Sierra Nevada. The arid climate of the Tabernas makes it Europe's only desert, expanding as a result of the increasing drought in southern Spain.

    RM2600325JPG

    Landscape of the Tabernas Desert, Andalusia (Spain). An ancient

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Landscape of the Tabernas Desert, Andalusia (Spain). An ancient Miocene sedimentary basin (- 8Ma) at the foot of the Sierra Nevada. The arid climate of the Tabernas makes it Europe's only desert, expanding as a result of the increasing drought in southern Spain.

    Landscape of the Tabernas Desert, Andalusia (Spain). An ancient Miocene sedimentary basin (- 8Ma) at the foot of the Sierra Nevada. The arid climate of the Tabernas makes it Europe's only desert, expanding as a result of the increasing drought in southern Spain.

    RM2600324JPG

    Landscape of the Tabernas Desert, Andalusia (Spain). An ancient Miocene sedimentary basin (- 8Ma) at the foot of the Sierra Nevada. The arid climate

    © Jean-Philippe Delobelle / Biosphoto

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    2600324
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    © Jean-Philippe Delobelle / Biosphoto

    Landscape of the Tabernas Desert, Andalusia (Spain). An ancient Miocene sedimentary basin (- 8Ma) at the foot of the Sierra Nevada. The arid climate of the Tabernas makes it Europe's only desert, expanding as a result of the increasing drought in southern Spain.

    Flysch in the Tabernas Desert, Andalusia (Spain). Barranco del infierno - Alternating sandstones and marls deposited in the Miocene ( - 8 Ma) in a sedimentary basin at the foot of the Sierra Nevada, then folded and straightened by recent tectonics. The arid climate of the Tabernas makes it Europe's only desert, expanding as a result of the increasing drought in southern Spain.

    RM2600323JPG

    Flysch in the Tabernas Desert, Andalusia (Spain). Barranco del infierno - Alternating sandstones and marls deposited in the Miocene ( - 8 Ma) in a

    © Jean-Philippe Delobelle / Biosphoto

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    2600323
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    © Jean-Philippe Delobelle / Biosphoto

    Flysch in the Tabernas Desert, Andalusia (Spain). Barranco del infierno - Alternating sandstones and marls deposited in the Miocene ( - 8 Ma) in a sedimentary basin at the foot of the Sierra Nevada, then folded and straightened by recent tectonics. The arid climate of the Tabernas makes it Europe's only desert, expanding as a result of the increasing drought in southern Spain.

    Flysch in the Tabernas Desert, Andalusia (Spain). Barranco del infierno - Alternating sandstones and marls deposited in the Miocene ( - 8 Ma) in a sedimentary basin at the foot of the Sierra Nevada, then folded and straightened by recent tectonics. The arid climate of the Tabernas makes it Europe's only desert, expanding as a result of the increasing drought in southern Spain.

    RM2600322JPG

    Flysch in the Tabernas Desert, Andalusia (Spain). Barranco del

    © Jean-Philippe Delobelle / Biosphoto

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    2600322
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    © Jean-Philippe Delobelle / Biosphoto

    Flysch in the Tabernas Desert, Andalusia (Spain). Barranco del infierno - Alternating sandstones and marls deposited in the Miocene ( - 8 Ma) in a sedimentary basin at the foot of the Sierra Nevada, then folded and straightened by recent tectonics. The arid climate of the Tabernas makes it Europe's only desert, expanding as a result of the increasing drought in southern Spain.

    Flysch in the Tabernas Desert, Andalusia (Spain). Barranco del infierno - Alternating sandstones and marls deposited in the Miocene ( - 8 Ma) in a sedimentary basin at the foot of the Sierra Nevada, then folded and straightened by recent tectonics. The arid climate of the Tabernas makes it Europe's only desert, expanding as a result of the increasing drought in southern Spain.

    RM2600321JPG

    Flysch in the Tabernas Desert, Andalusia (Spain). Barranco del infierno - Alternating sandstones and marls deposited in the Miocene ( - 8 Ma) in a

    © Jean-Philippe Delobelle / Biosphoto

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    2600321
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    © Jean-Philippe Delobelle / Biosphoto

    Flysch in the Tabernas Desert, Andalusia (Spain). Barranco del infierno - Alternating sandstones and marls deposited in the Miocene ( - 8 Ma) in a sedimentary basin at the foot of the Sierra Nevada, then folded and straightened by recent tectonics. The arid climate of the Tabernas makes it Europe's only desert, expanding as a result of the increasing drought in southern Spain.

    Flysch in the Tabernas Desert, Andalusia (Spain). Barranco del infierno - Alternating sandstones and marls deposited in the Miocene ( - 8 Ma) in a sedimentary basin at the foot of the Sierra Nevada, then folded and straightened by recent tectonics. The arid climate of the Tabernas makes it Europe's only desert, expanding as a result of the increasing drought in southern Spain.

    RM2600320JPG

    Flysch in the Tabernas Desert, Andalusia (Spain). Barranco del infierno - Alternating sandstones and marls deposited in the Miocene ( - 8 Ma) in a

    © Jean-Philippe Delobelle / Biosphoto

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    2600320
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    © Jean-Philippe Delobelle / Biosphoto

    Flysch in the Tabernas Desert, Andalusia (Spain). Barranco del infierno - Alternating sandstones and marls deposited in the Miocene ( - 8 Ma) in a sedimentary basin at the foot of the Sierra Nevada, then folded and straightened by recent tectonics. The arid climate of the Tabernas makes it Europe's only desert, expanding as a result of the increasing drought in southern Spain.

    Flysch in the Tabernas Desert, Andalusia (Spain). Alternating sandstones and marls deposited in the Miocene (- 8 Ma) in a sedimentary basin at the foot of the Sierra Nevada, then folded and straightened by recent tectonics. The arid climate of the Tabernas makes it Europe's only desert, expanding as a result of the increasing drought in southern Spain.

    RM2600319JPG

    Flysch in the Tabernas Desert, Andalusia (Spain). Alternating

    © Jean-Philippe Delobelle / Biosphoto

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    2600319
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    © Jean-Philippe Delobelle / Biosphoto

    Flysch in the Tabernas Desert, Andalusia (Spain). Alternating sandstones and marls deposited in the Miocene (- 8 Ma) in a sedimentary basin at the foot of the Sierra Nevada, then folded and straightened by recent tectonics. The arid climate of the Tabernas makes it Europe's only desert, expanding as a result of the increasing drought in southern Spain.

    Flysch in the Tabernas Desert, Andalusia (Spain). Alternating sandstones and marls deposited in the Miocene (- 8 Ma) in a sedimentary basin at the foot of the Sierra Nevada, then folded and straightened by recent tectonics. The arid climate of the Tabernas makes it Europe's only desert, expanding as a result of the increasing drought in southern Spain.

    RM2600318JPG

    Flysch in the Tabernas Desert, Andalusia (Spain). Alternating

    © Jean-Philippe Delobelle / Biosphoto

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    2600318
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    © Jean-Philippe Delobelle / Biosphoto

    Flysch in the Tabernas Desert, Andalusia (Spain). Alternating sandstones and marls deposited in the Miocene (- 8 Ma) in a sedimentary basin at the foot of the Sierra Nevada, then folded and straightened by recent tectonics. The arid climate of the Tabernas makes it Europe's only desert, expanding as a result of the increasing drought in southern Spain.

    Sandstone densely covered with lichens in Spain. Saxicolous crustaceous lichens - Malaga region, Andalusia

    RM2600312JPG

    Sandstone densely covered with lichens in Spain. Saxicolous

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Sandstone densely covered with lichens in Spain. Saxicolous crustaceous lichens - Malaga region, Andalusia

    Sandstone densely covered with lichens in Spain. Saxicolous crustaceous lichens - Malaga region, Andalusia

    RM2600311JPG

    Sandstone densely covered with lichens in Spain. Saxicolous crustaceous lichens - Malaga region, Andalusia

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Sandstone densely covered with lichens in Spain. Saxicolous crustaceous lichens - Malaga region, Andalusia

    The Old Man of Hoy, on the island Hoy, part of the Orkney Islands, Europe, Great Britain, Scotland Northern Isles, Orkney

    RM2599745JPG

    The Old Man of Hoy, on the island Hoy, part of the Orkney Islands, Europe, Great Britain, Scotland Northern Isles, Orkney

    © Martin Zwick / Biosphoto

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    © Martin Zwick / Biosphoto

    The Old Man of Hoy, on the island Hoy, part of the Orkney Islands, Europe, Great Britain, Scotland Northern Isles, Orkney

    The Old Man of Hoy, on the island Hoy, part of the Orkney Islands, Europe, Great Britain, Scotland Northern Isles, Orkney

    RM2599744JPG

    The Old Man of Hoy, on the island Hoy, part of the Orkney Islands,

    © Martin Zwick / Biosphoto

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    © Martin Zwick / Biosphoto

    The Old Man of Hoy, on the island Hoy, part of the Orkney Islands, Europe, Great Britain, Scotland Northern Isles, Orkney

    The Old Man of Hoy, on the island Hoy, part of the Orkney Islands, Europe, Great Britain, Scotland Northern Isles, Orkney

    RM2599743JPG

    The Old Man of Hoy, on the island Hoy, part of the Orkney Islands,

    © Martin Zwick / Biosphoto

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    © Martin Zwick / Biosphoto

    The Old Man of Hoy, on the island Hoy, part of the Orkney Islands, Europe, Great Britain, Scotland Northern Isles, Orkney

    The Old Man of Hoy, on the island Hoy, part of the Orkney Islands, Europe, Great Britain, Scotland Northern Isles, Orkney

    RM2599742JPG

    The Old Man of Hoy, on the island Hoy, part of the Orkney Islands, Europe, Great Britain, Scotland Northern Isles, Orkney

    © Martin Zwick / Biosphoto

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    © Martin Zwick / Biosphoto

    The Old Man of Hoy, on the island Hoy, part of the Orkney Islands, Europe, Great Britain, Scotland Northern Isles, Orkney

    Landscape of the Maures plain with sandstone slabs and umbrella pines in autumn, National Reserve protected site. Plot of land spared by fires in recent years, near Les Mayons, Var, France

    RM2595852JPG

    Landscape of the Maures plain with sandstone slabs and umbrella pines in autumn, National Reserve protected site. Plot of land spared by fires in

    © André Simon / Biosphoto

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    © André Simon / Biosphoto

    Landscape of the Maures plain with sandstone slabs and umbrella pines in autumn, National Reserve protected site. Plot of land spared by fires in recent years, near Les Mayons, Var, France

    Ocellated lizard (Timon lepidus) observed on a sandstone slab in early summer, Plaine des Maures National Reserve, Var, France

    RM2595838JPG

    Ocellated lizard (Timon lepidus) observed on a sandstone slab in early summer, Plaine des Maures National Reserve, Var, France

    © André Simon / Biosphoto

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    © André Simon / Biosphoto

    Ocellated lizard (Timon lepidus) observed on a sandstone slab in early summer, Plaine des Maures National Reserve, Var, France

    Saxicolous foliose lichens Xanthoria aureola on black sandstone. Together with Caloplaca marina, Xanthoria aureola forms the yellow belt of rocks rarely reached by waves in a rocky coastal environment - Jaizkibel Coastal Massif - Basque Country - Spain

    RM2595771JPG

    Saxicolous foliose lichens Xanthoria aureola on black sandstone. Together with Caloplaca marina, Xanthoria aureola forms the yellow belt of rocks

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Saxicolous foliose lichens Xanthoria aureola on black sandstone. Together with Caloplaca marina, Xanthoria aureola forms the yellow belt of rocks rarely reached by waves in a rocky coastal environment - Jaizkibel Coastal Massif - Basque Country - Spain

    Dry algae on paramoudras (sandstone ball) hollows. Jaizkibel coastal massif - Basque Country - Spain

    RM2595759JPG

    Dry algae on paramoudras (sandstone ball) hollows. Jaizkibel

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Dry algae on paramoudras (sandstone ball) hollows. Jaizkibel coastal massif - Basque Country - Spain

    The paramoudras of Jaizkibel, on Spain's Basque Coast. Spectacular sandstone fossil concretions formed around the burrows of marine worms living several hundred meters deep, 45 million years ago (Eocene) - These spheres or tubes are 20 to 40 cm in diameter and were originally flexible - The holes are the worms' galleries - Jaizkibel coastal massif - Basque Country - Spain

    RM2595758JPG

    The paramoudras of Jaizkibel, on Spain's Basque Coast. Spectacular sandstone fossil concretions formed around the burrows of marine worms living

    © Jean-Philippe Delobelle / Biosphoto

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    2595758
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    © Jean-Philippe Delobelle / Biosphoto

    The paramoudras of Jaizkibel, on Spain's Basque Coast. Spectacular sandstone fossil concretions formed around the burrows of marine worms living several hundred meters deep, 45 million years ago (Eocene) - These spheres or tubes are 20 to 40 cm in diameter and were originally flexible - The holes are the worms' galleries - Jaizkibel coastal massif - Basque Country - Spain

    The paramoudras of Jaizkibel, on Spain's Basque Coast. Spectacular sandstone fossil concretions formed around the burrows of marine worms living several hundred meters deep, 45 million years ago (Eocene) - These spheres or tubes are 20 to 40 cm in diameter and were originally flexible - The holes are the worms' galleries - Jaizkibel coastal massif - Basque Country - Spain

    RM2595757JPG

    The paramoudras of Jaizkibel, on Spain's Basque Coast.

    © Jean-Philippe Delobelle / Biosphoto

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    2595757
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    © Jean-Philippe Delobelle / Biosphoto

    The paramoudras of Jaizkibel, on Spain's Basque Coast. Spectacular sandstone fossil concretions formed around the burrows of marine worms living several hundred meters deep, 45 million years ago (Eocene) - These spheres or tubes are 20 to 40 cm in diameter and were originally flexible - The holes are the worms' galleries - Jaizkibel coastal massif - Basque Country - Spain

    The paramoudras of Jaizkibel, on Spain's Basque Coast. Spectacular sandstone fossil concretions formed around the burrows of marine worms living several hundred meters deep, 45 million years ago (Eocene) - These spheres or tubes are 20 to 40 cm in diameter and were originally flexible - The holes are the worms' galleries - Jaizkibel coastal massif - Basque Country - Spain

    RM2595756JPG

    The paramoudras of Jaizkibel, on Spain's Basque Coast. Spectacular sandstone fossil concretions formed around the burrows of marine worms living

    © Jean-Philippe Delobelle / Biosphoto

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    2595756
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    © Jean-Philippe Delobelle / Biosphoto

    The paramoudras of Jaizkibel, on Spain's Basque Coast. Spectacular sandstone fossil concretions formed around the burrows of marine worms living several hundred meters deep, 45 million years ago (Eocene) - These spheres or tubes are 20 to 40 cm in diameter and were originally flexible - The holes are the worms' galleries - Jaizkibel coastal massif - Basque Country - Spain

    The paramoudras of Jaizkibel, on Spain's Basque Coast. Spectacular sandstone fossil concretions formed around the burrows of marine worms living several hundred meters deep, 45 million years ago (Eocene) - These spheres or tubes are 20 to 40 cm in diameter and were originally flexible - The holes are the worms' galleries - Jaizkibel coastal massif - Basque Country - Spain

    RM2595755JPG

    The paramoudras of Jaizkibel, on Spain's Basque Coast.

    © Jean-Philippe Delobelle / Biosphoto

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    2595755
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    © Jean-Philippe Delobelle / Biosphoto

    The paramoudras of Jaizkibel, on Spain's Basque Coast. Spectacular sandstone fossil concretions formed around the burrows of marine worms living several hundred meters deep, 45 million years ago (Eocene) - These spheres or tubes are 20 to 40 cm in diameter and were originally flexible - The holes are the worms' galleries - Jaizkibel coastal massif - Basque Country - Spain

    Polychrome graphics in the Jaizkibel sandstone on Spain's Basque Coast. Remarkable Eocene sandstone structures (geoforms) of partly biological origin (fossilized biological activity) and uncovered by erosion - the yellow discs are "paramoudras", concretions around the burrows of deep-sea marine worms - Jaizkibel coastal massif - Spain

    RM2595750JPG

    Polychrome graphics in the Jaizkibel sandstone on Spain's Basque Coast. Remarkable Eocene sandstone structures (geoforms) of partly biological origin

    © Jean-Philippe Delobelle / Biosphoto

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    2595750
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    © Jean-Philippe Delobelle / Biosphoto

    Polychrome graphics in the Jaizkibel sandstone on Spain's Basque Coast. Remarkable Eocene sandstone structures (geoforms) of partly biological origin (fossilized biological activity) and uncovered by erosion - the yellow discs are "paramoudras", concretions around the burrows of deep-sea marine worms - Jaizkibel coastal massif - Spain

    Polychrome graphics in the Jaizkibel sandstone on Spain's Basque Coast. Remarkable Eocene sandstone structures (geoforms) of partly biological origin (fossilized biological activity) and uncovered by erosion - the yellow discs are "paramoudras", concretions around the burrows of deep-sea marine worms - Jaizkibel coastal massif - Spain

    RM2595749JPG

    Polychrome graphics in the Jaizkibel sandstone on Spain's Basque Coast. Remarkable Eocene sandstone structures (geoforms) of partly biological origin

    © Jean-Philippe Delobelle / Biosphoto

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    2595749
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    © Jean-Philippe Delobelle / Biosphoto

    Polychrome graphics in the Jaizkibel sandstone on Spain's Basque Coast. Remarkable Eocene sandstone structures (geoforms) of partly biological origin (fossilized biological activity) and uncovered by erosion - the yellow discs are "paramoudras", concretions around the burrows of deep-sea marine worms - Jaizkibel coastal massif - Spain

    Natural honeycomb lace (Geoforms) in sandstone from Jaizkibel (Spanish Basque Country). Remarkable Eocene sandstone sculptures (geoforms) of partly biological origin (fossil biological activities called Paramoudra, concretions around marine worm burrows) and uncovered then sculpted into honeycomb shapes by erosion - Jaizkibel coastal massif - Spain

    RM2595748JPG

    Natural honeycomb lace (Geoforms) in sandstone from Jaizkibel (Spanish Basque Country). Remarkable Eocene sandstone sculptures (geoforms) of partly

    © Jean-Philippe Delobelle / Biosphoto

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    2595748
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    © Jean-Philippe Delobelle / Biosphoto

    Natural honeycomb lace (Geoforms) in sandstone from Jaizkibel (Spanish Basque Country). Remarkable Eocene sandstone sculptures (geoforms) of partly biological origin (fossil biological activities called Paramoudra, concretions around marine worm burrows) and uncovered then sculpted into honeycomb shapes by erosion - Jaizkibel coastal massif - Spain

    Natural lacework (geoforms) in Jaizkibel sandstone (Spanish Basque Country). Remarkable Eocene sandstone sculptures (geoforms) of partly biological origin (fossilized biological activities known as Paramoudra, concretions around marine worm burrows) uncovered and sculpted into honeycomb shapes by erosion - Jaizkibel coastal massif - Spain

    RM2595747JPG

    Natural lacework (geoforms) in Jaizkibel sandstone (Spanish Basque Country). Remarkable Eocene sandstone sculptures (geoforms) of partly biological

    © Jean-Philippe Delobelle / Biosphoto

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    2595747
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    © Jean-Philippe Delobelle / Biosphoto

    Natural lacework (geoforms) in Jaizkibel sandstone (Spanish Basque Country). Remarkable Eocene sandstone sculptures (geoforms) of partly biological origin (fossilized biological activities known as Paramoudra, concretions around marine worm burrows) uncovered and sculpted into honeycomb shapes by erosion - Jaizkibel coastal massif - Spain

    Dentelles naturelles (Géoformes) dans les grès de Jaizkibel (Pays Basque espagnol). Remarquables sculptures de grès éocènes (géoformes) d'origine en partie biologique (activités biologiques fossiles appelées Paramoudra, concrétions autour des terriers de vers marins) et mises à jour puis sculptées en nid d'abeille par l'érosion - Massif côtier de Jaizkibel - Espagne

    RM2595746JPG

    Dentelles naturelles (Géoformes) dans les grès de Jaizkibel (Pays Basque espagnol). Remarquables sculptures de grès éocènes (géoformes) d'origine en

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Dentelles naturelles (Géoformes) dans les grès de Jaizkibel (Pays Basque espagnol). Remarquables sculptures de grès éocènes (géoformes) d'origine en partie biologique (activités biologiques fossiles appelées Paramoudra, concrétions autour des terriers de vers marins) et mises à jour puis sculptées en nid d'abeille par l'érosion - Massif côtier de Jaizkibel - Espagne

    Dentelles naturelles (Géoformes) dans les grès de Jaizkibel (Pays Basque espagnol). Remarquables sculptures de grès éocènes (géoformes) d'origine en partie biologique (activités biologiques fossiles appelées Paramoudra, concrétions autour des terriers de vers marins) et mises à jour puis sculptées en nid d'abeille par l'érosion - Massif côtier de Jaizkibel - Espagne

    RM2595745JPG

    Dentelles naturelles (Géoformes) dans les grès de Jaizkibel (Pays

    © Jean-Philippe Delobelle / Biosphoto

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    2595745
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    © Jean-Philippe Delobelle / Biosphoto

    Dentelles naturelles (Géoformes) dans les grès de Jaizkibel (Pays Basque espagnol). Remarquables sculptures de grès éocènes (géoformes) d'origine en partie biologique (activités biologiques fossiles appelées Paramoudra, concrétions autour des terriers de vers marins) et mises à jour puis sculptées en nid d'abeille par l'érosion - Massif côtier de Jaizkibel - Espagne

    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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    2595739
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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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    2595738
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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 from 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

    RM2595719JPG

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

    © Jean-Philippe Delobelle / Biosphoto

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    2595719
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    © Jean-Philippe Delobelle / Biosphoto

    Plolychrome strata from 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

    Arches and goats near Playa del Silencio on the coast. Asturias - Spain

    RM2595718JPG

    Arches and goats near Playa del Silencio on the coast. Asturias -

    © Jean-Philippe Delobelle / Biosphoto

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    2595718
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    © Jean-Philippe Delobelle / Biosphoto

    Arches and goats near Playa del Silencio on the coast. Asturias - Spain

    The famous Playa del Silencio on the Asturias coast in Spain. Famous bay on the Asturias coast, with remarkable geology - Spain

    RM2595717JPG

    The famous Playa del Silencio on the Asturias coast in Spain. Famous bay on the Asturias coast, with remarkable geology - Spain

    © Jean-Philippe Delobelle / Biosphoto

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    2595717
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    © Jean-Philippe Delobelle / Biosphoto

    The famous Playa del Silencio on the Asturias coast in Spain. Famous bay on the Asturias coast, with remarkable geology - 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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    2595716
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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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    2595715
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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

    Graphics on rocks at low tide. Geological strata and shells form natural tableaux at low tide - Playa del Silencio on the Asturias coast in Spain

    RM2595714JPG

    Graphics on rocks at low tide. Geological strata and shells form natural tableaux at low tide - Playa del Silencio on the Asturias coast in Spain

    © Jean-Philippe Delobelle / Biosphoto

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    2595714
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    © Jean-Philippe Delobelle / Biosphoto

    Graphics on rocks at low tide. Geological strata and shells form natural tableaux at low tide - Playa del Silencio on the Asturias coast in Spain

    The famous Playa del Silencio on Spain's Asturias coast. Low tide reveals the remarkable polychrome strata of quartzite, sandstone and shale, deformed by tectonics and dating from the Paleozoic (Cambrian/Ordovician) - Asturias - Spain

    RM2595713JPG

    The famous Playa del Silencio on Spain's Asturias coast. Low tide reveals the remarkable polychrome strata of quartzite, sandstone and shale,

    © Jean-Philippe Delobelle / Biosphoto

    LightboxinfoDownload low resolution image

    2595713
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    © Jean-Philippe Delobelle / Biosphoto

    The famous Playa del Silencio on Spain's Asturias coast. Low tide reveals the remarkable polychrome strata of quartzite, sandstone and shale, deformed by tectonics and dating from the Paleozoic (Cambrian/Ordovician) - Asturias - Spain

    The famous Playa del Silencio on Spain's Asturias coast. Low tide reveals the remarkable polychrome strata of quartzite, sandstone and shale, deformed by tectonics and dating from the Paleozoic (Cambrian/Ordovician) - Asturias - Spain

    RM2595712JPG

    The famous Playa del Silencio on Spain's Asturias coast. Low tide

    © Jean-Philippe Delobelle / Biosphoto

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    2595712
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    © Jean-Philippe Delobelle / Biosphoto

    The famous Playa del Silencio on Spain's Asturias coast. Low tide reveals the remarkable polychrome strata of quartzite, sandstone and shale, deformed by tectonics and dating from the Paleozoic (Cambrian/Ordovician) - Asturias - Spain

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