761 pictures found
© Alberto Ghizzi Panizza / Biosphoto
La Caldeirina Asturias Spain.
© Alberto Ghizzi Panizza / Biosphoto
La Caldeirina Asturias Spain.
© Alberto Ghizzi Panizza / Biosphoto
Praia das Illas Lugo Spain. panorama
© Alberto Ghizzi Panizza / Biosphoto
Praia das Illas Lugo Spain.
© Alberto Ghizzi Panizza / Biosphoto
Praia das Illas Lugo Spain.
© Alberto Ghizzi Panizza / Biosphoto
Praia das Illas Lugo Spain.
© Alberto Ghizzi Panizza / Biosphoto
La Caldeirina, Asturias, Spain.
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Common octopus (Octopus vulgaris), off Capbreton, Landes, France
© Mathieu Foulquié / Biosphoto
© Mathieu Foulquié / Biosphoto
Common octopus (Octopus vulgaris), off Capbreton, Landes, France
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Chain of Salps (Salpa sp) off Oléron Island, Charente-Maritime, France
© Mathieu Foulquié / Biosphoto
© Mathieu Foulquié / Biosphoto
Chain of Salps (Salpa sp) off Oléron Island, Charente-Maritime, France
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European eel (Anguilla anguilla) moving through seaweed in the middle of the night - Seudre estuary - Charente-Maritime - France
© Bruno Guénard / Biosphoto
© Bruno Guénard / Biosphoto
European eel (Anguilla anguilla) moving through seaweed in the middle of the night - Seudre estuary - Charente-Maritime - France
© Juan-Carlos Muñoz / Biosphoto
Surf on the Beach of Arnillas Bay of Biscay Spain
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Saxicolous foliose lichens Xanthoria aureola on black sandstone. Together with Caloplaca marina, Xanthoria aureola forms the yellow belt of rocks
© Jean-Philippe Delobelle / Biosphoto
© 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
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Dry algae on paramoudras (sandstone ball) hollows. Jaizkibel
© Jean-Philippe Delobelle / Biosphoto
© Jean-Philippe Delobelle / Biosphoto
Dry algae on paramoudras (sandstone ball) hollows. Jaizkibel coastal massif - Basque Country - Spain
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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
© 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
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The paramoudras of Jaizkibel, on Spain's Basque Coast.
© Jean-Philippe Delobelle / Biosphoto
© 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
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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
© 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
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The paramoudras of Jaizkibel, on Spain's Basque Coast.
© Jean-Philippe Delobelle / Biosphoto
© 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
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Polychrome graphics in the Jaizkibel sandstone on Spain's Basque Coast. Remarkable Eocene sandstone structures (geoforms) of partly biological origin
© Jean-Philippe Delobelle / Biosphoto
© 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
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Polychrome graphics in the Jaizkibel sandstone on Spain's Basque Coast. Remarkable Eocene sandstone structures (geoforms) of partly biological origin
© Jean-Philippe Delobelle / Biosphoto
© 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
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Natural honeycomb lace (Geoforms) in sandstone from Jaizkibel (Spanish Basque Country). Remarkable Eocene sandstone sculptures (geoforms) of partly
© Jean-Philippe Delobelle / Biosphoto
© 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
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Natural lacework (geoforms) in Jaizkibel sandstone (Spanish Basque Country). Remarkable Eocene sandstone sculptures (geoforms) of partly biological
© Jean-Philippe Delobelle / Biosphoto
© 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
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Dentelles naturelles (Géoformes) dans les grès de Jaizkibel (Pays Basque espagnol). Remarquables sculptures de grès éocènes (géoformes) d'origine en
© Jean-Philippe Delobelle / Biosphoto
© 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
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Dentelles naturelles (Géoformes) dans les grès de Jaizkibel (Pays
© Jean-Philippe Delobelle / Biosphoto
© 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
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Traditional stone granary in Galicia (Spain). The Galician granary (hórreo galego in Galician) is an agricultural building used as a granary,
© Jean-Philippe Delobelle / Biosphoto
© Jean-Philippe Delobelle / Biosphoto
Traditional stone granary in Galicia (Spain). The Galician granary (hórreo galego in Galician) is an agricultural building used as a granary, according to an architecture specific to the region of Galicia, Spain. It is used to store grain after harvest, especially corn. It consists of a narrow, elongated chamber that allows air to pass through, but is isolated from the ground to protect the grain from humidity and animals. Stone disks prevent rodents from getting through - Cabo Tourinan - Costa da morte - Galicia - Spain
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Playa de Gueirua on the Asturias coast in Spain. Low tide reveals
© Jean-Philippe Delobelle / Biosphoto
© 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
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Playa de Gueirua on the Asturias coast in Spain. Low tide reveals
© Jean-Philippe Delobelle / Biosphoto
© 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
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Sea hermitage in Galicia (Spain). Virxe do Porto - Hermitage on a rocky headland only accessible at low tide - Valdonino region north of La Coruña -
© Jean-Philippe Delobelle / Biosphoto
© Jean-Philippe Delobelle / Biosphoto
Sea hermitage in Galicia (Spain). Virxe do Porto - Hermitage on a rocky headland only accessible at low tide - Valdonino region north of La Coruña - Galicia - Spain
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The Galician coastline the day after a storm on the Cantabrian Sea. Rinlo region, Lugo province, Galicia (Spain)
© Jean-Philippe Delobelle / Biosphoto
© Jean-Philippe Delobelle / Biosphoto
The Galician coastline the day after a storm on the Cantabrian Sea. Rinlo region, Lugo province, Galicia (Spain)
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The famous Cathedrales beach in Galicia. A popular natural monument in northern Spain.
© Jean-Philippe Delobelle / Biosphoto
© Jean-Philippe Delobelle / Biosphoto
The famous Cathedrales beach in Galicia. A popular natural monument in northern Spain.
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Waterfall and pebbles by the sea on the Asturias coast (Spain).
© Jean-Philippe Delobelle / Biosphoto
© Jean-Philippe Delobelle / Biosphoto
Waterfall and pebbles by the sea on the Asturias coast (Spain). The permeability of the large pebbles means that water from the waterfall can immediately seep through.
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Plolychrome strata from the Baya del Silencio in Spain (Asturias). Spectacular straightened quartzite, sandstone and shale strata, deformed and bent
© Jean-Philippe Delobelle / Biosphoto
© 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
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Arches and goats near Playa del Silencio on the coast. Asturias -
© Jean-Philippe Delobelle / Biosphoto
© Jean-Philippe Delobelle / Biosphoto
Arches and goats near Playa del Silencio on the coast. Asturias - Spain
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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
© 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
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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
© 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
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Plolychrome strata at Playa del Silencio, Spain (Asturias).
© Jean-Philippe Delobelle / Biosphoto
© 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
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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
© 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
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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
© 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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The famous Playa del Silencio on Spain's Asturias coast. Low tide
© Jean-Philippe Delobelle / Biosphoto
© 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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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
© 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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The famous Playa del Silencio on Spain's Asturias coast. Low tide
© Jean-Philippe Delobelle / Biosphoto
© 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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The island and hermitage of Gaztelugatxe in Vizcaya, a very famous islet on the Spanish Basque coast, with an eventful history used in films and TV
© Jean-Philippe Delobelle / Biosphoto
© Jean-Philippe Delobelle / Biosphoto
The island and hermitage of Gaztelugatxe in Vizcaya, a very famous islet on the Spanish Basque coast, with an eventful history used in films and TV series. The area is a marine reserve, Protected Biotope, Spain.
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The island and hermitage of Gaztelugatxe in Vizcaya, a very famous islet on the Spanish Basque coast, with an eventful history used in films and TV series. The area is a
© Jean-Philippe Delobelle / Biosphoto
© Jean-Philippe Delobelle / Biosphoto
The island and hermitage of Gaztelugatxe in Vizcaya, a very famous islet on the Spanish Basque coast, with an eventful history used in films and TV series. The area is a marine reserve, Protected Biotope, Spain.
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Ripples in the Barrika flysch on the Spanish Basque coast. Flysch
© Jean-Philippe Delobelle / Biosphoto
© Jean-Philippe Delobelle / Biosphoto
Ripples in the Barrika flysch on the Spanish Basque coast. Flysch formed at the end of the Mesozoic era, in the Cretaceous - flysch is formed by the accumulation of sediments following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular strata of sandstone and limestone, here straightened by the Pyrenean orogeny and cleared by erosion - Biscay- Basque Country - Spain
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Ripples in the Barrika flysch on the Spanish Basque coast. Flysch formed at the end of the Mesozoic era, in the Cretaceous - flysch is formed by the
© Jean-Philippe Delobelle / Biosphoto
© Jean-Philippe Delobelle / Biosphoto
Ripples in the Barrika flysch on the Spanish Basque coast. Flysch formed at the end of the Mesozoic era, in the Cretaceous - flysch is formed by the accumulation of sediments following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular strata of sandstone and limestone, here straightened by the Pyrenean orogeny and cleared by erosion - Biscay- Basque Country - Spain
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Ripples in the Barrika flysch on the Spanish Basque coast. Flysch
© Jean-Philippe Delobelle / Biosphoto
© Jean-Philippe Delobelle / Biosphoto
Ripples in the Barrika flysch on the Spanish Basque coast. Flysch formed at the end of the Mesozoic era, in the Cretaceous - flysch is formed by the accumulation of sediments following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular strata of sandstone and limestone, here straightened by the Pyrenean orogeny and cleared by erosion - Biscay- Basque Country - Spain
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Ripples in the Barrika flysch on the Spanish Basque coast. Flysch
© Jean-Philippe Delobelle / Biosphoto
© Jean-Philippe Delobelle / Biosphoto
Ripples in the Barrika flysch on the Spanish Basque coast. Flysch formed at the end of the Mesozoic era, in the Cretaceous - flysch is formed by the accumulation of sediments following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular strata of sandstone and limestone, here straightened by the Pyrenean orogeny and cleared by erosion - Biscay- Basque Country - Spain
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Ripples in the Barrika flysch on the Spanish Basque coast. Flysch formed at the end of the Mesozoic era, in the Cretaceous - flysch is formed by the
© Jean-Philippe Delobelle / Biosphoto
© Jean-Philippe Delobelle / Biosphoto
Ripples in the Barrika flysch on the Spanish Basque coast. Flysch formed at the end of the Mesozoic era, in the Cretaceous - flysch is formed by the accumulation of sediments following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular strata of sandstone and limestone, here straightened by the Pyrenean orogeny and cleared by erosion - Biscay- Basque Country - Spain
© Mathieu Foulquié / Biosphoto
Maerl bottom off Ile de Ré, Atlantic Ocean, France