+33 490 162 042 Call us
Facebook About us Français

Search result Geologic stratum

  • Page
  • / 20

987 pictures found

The Cheran gorges in autumn, River draining the Bauges massif, to Hery sur Alby, Savoie, Alps, FranceThe Cheran gorges in autumn, River draining the Bauges massif, to Hery sur Alby, Savoie, Alps, FranceThe Cheran gorges in autumn, River draining the Bauges massif, to Hery sur Alby, Savoie, Alps, France© Jean-Philippe Delobelle / BiosphotoJPG - RM

2172561

The Cheran gorges in autumn, River draining the Bauges massif, to

RMRight Managed

JPG

LightboxDownload low resolution image

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 metersBlackjack pines and Hoodoos - Bryce Canyon NP Utah USABlackjack 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
© Jean-Philippe Delobelle / BiosphotoJPG - RM

2033217

Blackjack pines and Hoodoos - Bryce Canyon NP Utah USA ;

RMRight Managed

JPG

LightboxDownload low resolution image

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)Dome Navajo sandstone - Grand Staircase-Escalante NM UtahDome 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)
© Jean-Philippe Delobelle / BiosphotoJPG - RM

2033183

Dome Navajo sandstone - Grand Staircase-Escalante NM Utah ;

RMRight Managed

JPG

LightboxDownload low resolution image

The 12 Apostles Port Campbell National Park, AustraliaThe 12 Apostles Port Campbell National Park, AustraliaThe 12 Apostles Port Campbell National Park, Australia© Edouard Bense / BiosphotoJPG - RM

1897272

The 12 Apostles Port Campbell National Park, Australia

RMRight Managed

JPG

LightboxDownload low resolution image

The 12 Apostles Port Campbell National Park, AustraliaThe 12 Apostles Port Campbell National Park, AustraliaThe 12 Apostles Port Campbell National Park, Australia© Cyril Ruoso / BiosphotoJPG - RMNon exclusive sale
Use for exhibitions prohibited

521090

The 12 Apostles Port Campbell National Park, Australia

RMRight Managed

JPG

LightboxWarningDownload low resolution image

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

2462015

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

RMRight Managed

JPG

LightboxDownload low resolution image

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

2462010

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

RMRight Managed

JPG

LightboxDownload low resolution image

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

2462008

Landscape of the Geological Reserve of Digne, Thitonique

RMRight Managed

JPG

LightboxDownload low resolution image

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

2462000

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

RMRight Managed

JPG

LightboxDownload low resolution image

Desert landscape, Sultanate of OmanDesert landscape, Sultanate of OmanDesert landscape, Sultanate of Oman© Michel Gunther / BiosphotoJPG - RM

2461971

Desert landscape, Sultanate of Oman

RMRight Managed

JPG

LightboxDownload low resolution image

Remarkable folding in flysch, Vallée du Bachelard, Alpes de Haute Provence, FranceRemarkable folding in flysch, Vallée du Bachelard, Alpes de Haute Provence, FranceRemarkable folding in flysch, Vallée du Bachelard, Alpes de Haute Provence, France© Jean-Philippe Delobelle / BiosphotoJPG - RM

2461315

Remarkable folding in flysch, Vallée du Bachelard, Alpes de

RMRight Managed

JPG

LightboxDownload low resolution image

Les Mourres de Forcalquier, limestone erosion figures, Provence, FranceLes Mourres de Forcalquier, limestone erosion figures, Provence, FranceLes Mourres de Forcalquier, limestone erosion figures, Provence, France© David Tatin / BiosphotoJPG - RM

2459564

Les Mourres de Forcalquier, limestone erosion figures, Provence,

RMRight Managed

JPG

LightboxDownload low resolution image

Les Mourres de Forcalquier, limestone erosion figures, Provence, FranceLes Mourres de Forcalquier, limestone erosion figures, Provence, FranceLes Mourres de Forcalquier, limestone erosion figures, Provence, France© David Tatin / BiosphotoJPG - RM

2459563

Les Mourres de Forcalquier, limestone erosion figures, Provence,

RMRight Managed

JPG

LightboxDownload low resolution image

The Var river in the Gorges de Daluis, Mercantour National Park, Alps, FranceThe Var river in the Gorges de Daluis, Mercantour National Park, Alps, FranceThe Var river in the Gorges de Daluis, Mercantour National Park, Alps, France© Michel Rauch / BiosphotoJPG - RM

2459111

The Var river in the Gorges de Daluis, Mercantour National Park,

RMRight Managed

JPG

LightboxDownload low resolution image

Banded formations on a wall of a former iron mine gallery in sandstone, Vosges du Nord Regional Nature Park, FranceBanded formations on a wall of a former iron mine gallery in sandstone, Vosges du Nord Regional Nature Park, FranceBanded formations on a wall of a former iron mine gallery in sandstone, Vosges du Nord Regional Nature Park, France© Michel Rauch / BiosphotoJPG - RM

2459104

Banded formations on a wall of a former iron mine gallery in

RMRight Managed

JPG

LightboxDownload low resolution image

Phreato-magmatic deposits in Molines, in Ardèche. The maar of Echamps is a vast plateau resulting from the cooling of a lava lake. An active quarry located in Molines shows a beautiful cut in the maar deposits - site of the Geopark des Monts d'Ardèche - FrancePhreato-magmatic deposits in Molines, in Ardèche. The maar of Echamps is a vast plateau resulting from the cooling of a lava lake. An active quarry located in Molines shows a beautiful cut in the maar deposits - site of the Geopark des Monts d'Ardèche - FrancePhreato-magmatic deposits in Molines, in Ardèche. The maar of Echamps is a vast plateau resulting from the cooling of a lava lake. An active quarry located in Molines shows a beautiful cut in the maar deposits - site of the Geopark des Monts d'Ardèche - France© Jean-Philippe Delobelle / BiosphotoJPG - RM

2458319

Phreato-magmatic deposits in Molines, in Ardèche. The maar of

RMRight Managed

JPG

LightboxDownload low resolution image

Cedar Breaks National Monument at sunset, Utah.Cedar Breaks National Monument at sunset, Utah.Cedar Breaks National Monument at sunset, Utah.© Stuart Wilson / BiosphotoJPG - RMNon exclusive sale

2455555

Cedar Breaks National Monument at sunset, Utah.

RMRight Managed

JPG

LightboxDownload low resolution image

Flysch from Pic de Goléon, the Aiguille du Goléon is a pyramid cut entirely in the nummulitic flysch, Ecrins National Park, north of La Grave, Alps, FranceFlysch from Pic de Goléon, the Aiguille du Goléon is a pyramid cut entirely in the nummulitic flysch, Ecrins National Park, north of La Grave, Alps, FranceFlysch from Pic de Goléon, the Aiguille du Goléon is a pyramid cut entirely in the nummulitic flysch, Ecrins National Park, north of La Grave, Alps, France© Jean-Philippe Delobelle / BiosphotoJPG - RM

2446307

Flysch from Pic de Goléon, the Aiguille du Goléon is a pyramid

RMRight Managed

JPG

LightboxDownload low resolution image

Lourtuais beach from a Cap d'Erquy trail, Brittany, FranceLourtuais beach from a Cap d'Erquy trail, Brittany, FranceLourtuais beach from a Cap d'Erquy trail, Brittany, France© Jean-Luc & Françoise Ziegler / BiosphotoJPG - RM

2441566

Lourtuais beach from a Cap d'Erquy trail, Brittany, France

RMRight Managed

JPG

LightboxDownload low resolution image

Spectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, PortugalSpectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, PortugalSpectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, Portugal© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437622

Spectacular flysch formations in southern Portugal, The flysch

RMRight Managed

JPG

LightboxDownload low resolution image

Spectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, PortugalSpectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, PortugalSpectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, Portugal© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437621

Spectacular flysch formations in southern Portugal, The flysch

RMRight Managed

JPG

LightboxDownload low resolution image

Spectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, PortugalSpectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, PortugalSpectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, Portugal© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437620

Spectacular flysch formations in southern Portugal, The flysch

RMRight Managed

JPG

LightboxDownload low resolution image

Spectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, PortugalSpectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, PortugalSpectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, Portugal© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437619

Spectacular flysch formations in southern Portugal, The flysch

RMRight Managed

JPG

LightboxDownload low resolution image

Spectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, PortugalSpectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, PortugalSpectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, Portugal© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437618

Spectacular flysch formations in southern Portugal, The flysch

RMRight Managed

JPG

LightboxDownload low resolution image

Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437366

Remarkable flysch formations of Deba, Basque Coast Geopark,

RMRight Managed

JPG

LightboxDownload low resolution image

Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437365

Remarkable flysch formations of Deba, Basque Coast Geopark,

RMRight Managed

JPG

LightboxDownload low resolution image

Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437364

Remarkable flysch formations of Deba, Basque Coast Geopark,

RMRight Managed

JPG

LightboxDownload low resolution image

Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437363

Remarkable flysch formations of Deba, Basque Coast Geopark,

RMRight Managed

JPG

LightboxDownload low resolution image

Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437362

Remarkable flysch formations of Deba, Basque Coast Geopark,

RMRight Managed

JPG

LightboxDownload low resolution image

Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437361

Remarkable flysch formations of Deba, Basque Coast Geopark,

RMRight Managed

JPG

LightboxDownload low resolution image

Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437360

Remarkable flysch formations of Deba, Basque Coast Geopark,

RMRight Managed

JPG

LightboxDownload low resolution image

Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437359

Remarkable flysch formations of Deba, Basque Coast Geopark,

RMRight Managed

JPG

LightboxDownload low resolution image

Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437358

Remarkable flysch formations of Deba, Basque Coast Geopark,

RMRight Managed

JPG

LightboxDownload low resolution image

Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437357

Remarkable flysch formations of Deba, Basque Coast Geopark,

RMRight Managed

JPG

LightboxDownload low resolution image

Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437356

Remarkable flysch formations of Deba, Basque Coast Geopark,

RMRight Managed

JPG

LightboxDownload low resolution image

Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437355

Remarkable flysch formations of Deba, Basque Coast Geopark,

RMRight Managed

JPG

LightboxDownload low resolution image

Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437354

Remarkable flysch formations of Deba, Basque Coast Geopark,

RMRight Managed

JPG

LightboxDownload low resolution image

Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437353

Remarkable flysch formations of Deba, Basque Coast Geopark,

RMRight Managed

JPG

LightboxDownload low resolution image

Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437352

Remarkable flysch formations of Deba, Basque Coast Geopark,

RMRight Managed

JPG

LightboxDownload low resolution image

Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437351

Remarkable flysch formations of Deba, Basque Coast Geopark,

RMRight Managed

JPG

LightboxDownload low resolution image

Polychrome strata of Playa del Silencio, Asturias, Spain. Spectacular variegated and tortured strata of quartzite, sandstone and schists, deformed by the tectonic and dating from the Paleozoic (Cambrian / Ordovician)Polychrome strata of Playa del Silencio, Asturias, Spain. Spectacular variegated and tortured strata of quartzite, sandstone and schists, deformed by the tectonic and dating from the Paleozoic (Cambrian / Ordovician)Polychrome strata of Playa del Silencio, Asturias, Spain. Spectacular variegated and tortured strata of quartzite, sandstone and schists, deformed by the tectonic and dating from the Paleozoic (Cambrian / Ordovician)© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437333

Polychrome strata of Playa del Silencio, Asturias, Spain.

RMRight Managed

JPG

LightboxDownload low resolution image

Petrified quartzite wave from Playa del Silencio, Asturias, Spain. Spectacular variegated and tortured strata of quartzite, sandstone and schists, deformed by the tectonic and dating from the Paleozoic (Cambrian / Ordovician)Petrified quartzite wave from Playa del Silencio, Asturias, Spain. Spectacular variegated and tortured strata of quartzite, sandstone and schists, deformed by the tectonic and dating from the Paleozoic (Cambrian / Ordovician)Petrified quartzite wave from Playa del Silencio, Asturias, Spain. Spectacular variegated and tortured strata of quartzite, sandstone and schists, deformed by the tectonic and dating from the Paleozoic (Cambrian / Ordovician)© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437332

Petrified quartzite wave from Playa del Silencio, Asturias,

RMRight Managed

JPG

LightboxDownload low resolution image

Petrified quartzite wave from Playa del Silencio, Asturias, Spain. Spectacular variegated and tortured strata of quartzite, sandstone and schists, deformed by the tectonic and dating from the Paleozoic (Cambrian / Ordovician)Petrified quartzite wave from Playa del Silencio, Asturias, Spain. Spectacular variegated and tortured strata of quartzite, sandstone and schists, deformed by the tectonic and dating from the Paleozoic (Cambrian / Ordovician)Petrified quartzite wave from Playa del Silencio, Asturias, Spain. Spectacular variegated and tortured strata of quartzite, sandstone and schists, deformed by the tectonic and dating from the Paleozoic (Cambrian / Ordovician)© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437331

Petrified quartzite wave from Playa del Silencio, Asturias,

RMRight Managed

JPG

LightboxDownload low resolution image

Polychrome strata of Playa del Silencio, Asturias, Spain. Spectacular variegated and tortured strata of quartzite, sandstone and schists, deformed by the tectonic and dating from the Paleozoic (Cambrian / Ordovician)Polychrome strata of Playa del Silencio, Asturias, Spain. Spectacular variegated and tortured strata of quartzite, sandstone and schists, deformed by the tectonic and dating from the Paleozoic (Cambrian / Ordovician)Polychrome strata of Playa del Silencio, Asturias, Spain. Spectacular variegated and tortured strata of quartzite, sandstone and schists, deformed by the tectonic and dating from the Paleozoic (Cambrian / Ordovician)© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437330

Polychrome strata of Playa del Silencio, Asturias, Spain.

RMRight Managed

JPG

LightboxDownload low resolution image

Polychrome strata of Playa del Silencio, Asturias, Spain. Spectacular variegated and tortured strata of quartzite, sandstone and schists, deformed by the tectonic and dating from the Paleozoic (Cambrian / Ordovician)Polychrome strata of Playa del Silencio, Asturias, Spain. Spectacular variegated and tortured strata of quartzite, sandstone and schists, deformed by the tectonic and dating from the Paleozoic (Cambrian / Ordovician)Polychrome strata of Playa del Silencio, Asturias, Spain. Spectacular variegated and tortured strata of quartzite, sandstone and schists, deformed by the tectonic and dating from the Paleozoic (Cambrian / Ordovician)© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437329

Polychrome strata of Playa del Silencio, Asturias, Spain.

RMRight Managed

JPG

LightboxDownload low resolution image

Polychrome strata of Playa del Silencio, Asturias, Spain. Spectacular variegated and tortured strata of quartzite, sandstone and schists, deformed by the tectonic and dating from the Paleozoic (Cambrian / Ordovician)Polychrome strata of Playa del Silencio, Asturias, Spain. Spectacular variegated and tortured strata of quartzite, sandstone and schists, deformed by the tectonic and dating from the Paleozoic (Cambrian / Ordovician)Polychrome strata of Playa del Silencio, Asturias, Spain. Spectacular variegated and tortured strata of quartzite, sandstone and schists, deformed by the tectonic and dating from the Paleozoic (Cambrian / Ordovician)© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437328

Polychrome strata of Playa del Silencio, Asturias, Spain.

RMRight Managed

JPG

LightboxDownload low resolution image

Polychrome strata of Playa del Silencio, Asturias, Spain. Spectacular variegated and tortured strata of quartzite, sandstone and schists, deformed by the tectonic and dating from the Paleozoic (Cambrian / Ordovician)Polychrome strata of Playa del Silencio, Asturias, Spain. Spectacular variegated and tortured strata of quartzite, sandstone and schists, deformed by the tectonic and dating from the Paleozoic (Cambrian / Ordovician)Polychrome strata of Playa del Silencio, Asturias, Spain. Spectacular variegated and tortured strata of quartzite, sandstone and schists, deformed by the tectonic and dating from the Paleozoic (Cambrian / Ordovician)© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437327

Polychrome strata of Playa del Silencio, Asturias, Spain.

RMRight Managed

JPG

LightboxDownload low resolution image

Cliff with remarkable stratifications, folded layers of marls and limestones of the Lower Jurassic, above Bassey near Bourg d'Oisan, Ecrins NP, Alps, FranceCliff with remarkable stratifications, folded layers of marls and limestones of the Lower Jurassic, above Bassey near Bourg d'Oisan, Ecrins NP, Alps, FranceCliff with remarkable stratifications, folded layers of marls and limestones of the Lower Jurassic, above Bassey near Bourg d'Oisan, Ecrins NP, Alps, France© Jean-Philippe Delobelle / BiosphotoJPG - RM

2425947

Cliff with remarkable stratifications, folded layers of marls and

RMRight Managed

JPG

LightboxDownload low resolution image

Cliff with remarkable stratifications, folded layers of marls and limestones of the Lower Jurassic, above Bassey near Bourg d'Oisan, Ecrins NP, Alps, FranceCliff with remarkable stratifications, folded layers of marls and limestones of the Lower Jurassic, above Bassey near Bourg d'Oisan, Ecrins NP, Alps, FranceCliff with remarkable stratifications, folded layers of marls and limestones of the Lower Jurassic, above Bassey near Bourg d'Oisan, Ecrins NP, Alps, France© Jean-Philippe Delobelle / BiosphotoJPG - RM

2425946

Cliff with remarkable stratifications, folded layers of marls and

RMRight Managed

JPG

LightboxDownload low resolution image

Ochre, Collet de Flaqueyrol, Luberon, Vaucluse, FranceOchre, Collet de Flaqueyrol, Luberon, Vaucluse, FranceOchre, Collet de Flaqueyrol, Luberon, Vaucluse, France© David Tatin / BiosphotoJPG - RM

2421921

Ochre, Collet de Flaqueyrol, Luberon, Vaucluse, France

RMRight Managed

JPG

LightboxDownload low resolution image

Next page
1 / 20

Your request is processing. Please wait...

Galleries General conditions Legal notices Photographers area





Your request has been registered.

To use this feature you must first register or login.

Log in

To organize photos in lightboxes you must first register or login. Registration is FREE! Lightboxes allow you to categorize your photos, to keep them when you sign in and send them by email.

Log in

A Biosphoto authorization has to be granted prior using this feature. We'll get in touch shortly, please check that your contact info is up to date. Feel free to contact us in case of no answer during office hours (Paris time).

Delete permanently this lightbox?

Delete permanently all items?



The lightbox has been duplicated

The lightbox has been copied in your personal account

Your request has been registered. You will receive an e-mail shortly in order to download your images.

You can insert a comment that will appear within your downloads reports.





Your lightbox has been sent.

In case of modification, changes will be seen by your recipient.

If deleted, your lightbox won't be avalaible for your recipient anymore.