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Ichnofossils on flysch Deba, Geopark of the Basque Coast, Basque Country, Spain. Ichnofossil: Helminthorhaphe and Paleodictyon on the right - Flysch formed at the end of the Mesozoic era, in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, caused by earthquakes, and producing after compaction and crystallization of very regular layers of sandstone and limestone, here corrected by the Pyrenean orogeny and released by erosion.Ichnofossils on flysch Deba, Geopark of the Basque Coast, Basque Country, Spain. Ichnofossil: Helminthorhaphe and Paleodictyon on the right - Flysch formed at the end of the Mesozoic era, in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, caused by earthquakes, and producing after compaction and crystallization of very regular layers of sandstone and limestone, here corrected by the Pyrenean orogeny and released by erosion.Ichnofossils on flysch Deba, Geopark of the Basque Coast, Basque Country, Spain. Ichnofossil: Helminthorhaphe and Paleodictyon on the right - Flysch formed at the end of the Mesozoic era, in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, caused by earthquakes, and producing after compaction and crystallization of very regular layers of sandstone and limestone, here corrected by the Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Ichnofossils on flysch Deba, Geopark of the Basque Coast, Basque

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

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Ichnofossils on flysch Deba, Geopark of the Basque Coast, Basque

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

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Ichnofossils on flysch Deba, Geopark of the Basque Coast, Basque

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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,

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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,

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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,

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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,

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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,

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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,

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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

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Remarkable flysch formations of Deba, Basque Coast Geopark,

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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,

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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

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Remarkable flysch formations of Deba, Basque Coast Geopark,

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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,

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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,

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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,

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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,

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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,

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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,

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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,

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Seismic station network monitoring South Pacific Caledonia ; Installation of the last eight seismic stations monitoring network in the South Pacific in New Caledonia, near the tribe of Unia, not far from the town of Yate. The equipment is installed in the vicinity of a TV relay at the top of a hill overlooking the lagoon. Green the apparatus remote data to the laboratory for live tracking (GPRS and GPS timing data). The addition of the last measuring station Caledonian will save a few precious seconds to act in case of tsunami risk in the South Pacific.Seismic station network monitoring South Pacific CaledoniaSeismic station network monitoring South Pacific Caledonia ; Installation of the last eight seismic stations monitoring network in the South Pacific in New Caledonia, near the tribe of Unia, not far from the town of Yate. The equipment is installed in the vicinity of a TV relay at the top of a hill overlooking the lagoon. Green the apparatus remote data to the laboratory for live tracking (GPRS and GPS timing data). The addition of the last measuring station Caledonian will save a few precious seconds to act in case of tsunami risk in the South Pacific.© Thibaut Vergoz / BiosphotoJPG - RMNon exclusive sale

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Seismic station network monitoring South Pacific Caledonia ;

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Volcanologist and seismological station Yasur Volcano Vanuatu ; Sylvain Todman (geophysical engineer for the Government of Vanuatu) and Sandrine Cevuard (scientific officer volcanology) verify the proper operation of the station monitoring the volcano Yasur volcano on Tanna Island in Vanuatu. This station features a acoustimètre and buried a seismometer can be monitored in real time from anywhere in the world the volcano. This volcano, like other volcanoes in Vanuatu, is subject to continuous monitoring by the Geohazards center of Port Vila, to allow a better alert the local population in the event of imminent catastrophic eruption. The relatively large increase in explosive activity of the volcano has led to a rise in ash deposits on the island, particularly on food crops, some do not support. This is particularly the case of yam, taro and cabbage Kanak, which form the basis of the traditional diet. By Sylvain checks on his computer that measurements recorded by the station coincide well with the explosions of nearby volcano.Volcanologist and seismological station Yasur Volcano VanuatuVolcanologist and seismological station Yasur Volcano Vanuatu ; Sylvain Todman (geophysical engineer for the Government of Vanuatu) and Sandrine Cevuard (scientific officer volcanology) verify the proper operation of the station monitoring the volcano Yasur volcano on Tanna Island in Vanuatu. This station features a acoustimètre and buried a seismometer can be monitored in real time from anywhere in the world the volcano. This volcano, like other volcanoes in Vanuatu, is subject to continuous monitoring by the Geohazards center of Port Vila, to allow a better alert the local population in the event of imminent catastrophic eruption. The relatively large increase in explosive activity of the volcano has led to a rise in ash deposits on the island, particularly on food crops, some do not support. This is particularly the case of yam, taro and cabbage Kanak, which form the basis of the traditional diet. By Sylvain checks on his computer that measurements recorded by the station coincide well with the explosions of nearby volcano.© Thibaut Vergoz / BiosphotoJPG - RMNon exclusive sale

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Volcanologist and seismological station Yasur Volcano Vanuatu ;

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Awareness of a tribe of Vanuatu volcanic risk  ; Visit the tribe Inomakel with Sylvain Todman (geophysical engineer for the Government of Vanuatu) and Sandrine Cevuard (scientific officer volcanology) on the island of Tanna, Vanuatu. Vanuatu, and in particular the island of Tanna, is a geologist's paradise. Indeed this archipelago combines seismic and volcanic risks. On Tanna is the Yasur volcano, strombolian type, which mixture explosions and lava flows. The Inomakel tribe lives in direct proximity to the volcano, which represents a constant threat to the population. In order to maintain good relations between scientists and local populations, and enable greater efficiency in the measures taken in case of natural disaster, these scientists Geohazards conduct information and education operations and risk behaviors to adopt disaster. This is also an opportunity to interact with people and know their perception of the volcano and its impact on their daily lives. Sylvain Todman launches a debate on the subject with the villagers. Awareness of a tribe of Vanuatu volcanic risk Awareness of a tribe of Vanuatu volcanic risk ; Visit the tribe Inomakel with Sylvain Todman (geophysical engineer for the Government of Vanuatu) and Sandrine Cevuard (scientific officer volcanology) on the island of Tanna, Vanuatu. Vanuatu, and in particular the island of Tanna, is a geologist's paradise. Indeed this archipelago combines seismic and volcanic risks. On Tanna is the Yasur volcano, strombolian type, which mixture explosions and lava flows. The Inomakel tribe lives in direct proximity to the volcano, which represents a constant threat to the population. In order to maintain good relations between scientists and local populations, and enable greater efficiency in the measures taken in case of natural disaster, these scientists Geohazards conduct information and education operations and risk behaviors to adopt disaster. This is also an opportunity to interact with people and know their perception of the volcano and its impact on their daily lives. Sylvain Todman launches a debate on the subject with the villagers. © Thibaut Vergoz / BiosphotoJPG - RMNon exclusive sale

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Awareness of a tribe of Vanuatu volcanic risk ; Visit the tribe

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Seismometer buried the Geoscope station Santo Vanuatu ; Seismometer buried the acquisition of global seismic network station Geoscope. Valérie Ballu, with his student Christian Baillard install fiber optics to improve the transmission capacity of GPS data in real time over the Internet. It is now possible to Valerie download GPS data and control devices from his office in Paris.Seismometer buried the Geoscope station Santo VanuatuSeismometer buried the Geoscope station Santo Vanuatu ; Seismometer buried the acquisition of global seismic network station Geoscope. Valérie Ballu, with his student Christian Baillard install fiber optics to improve the transmission capacity of GPS data in real time over the Internet. It is now possible to Valerie download GPS data and control devices from his office in Paris.© Thibaut Vergoz / BiosphotoJPG - RMNon exclusive sale

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Seismometer buried the Geoscope station Santo Vanuatu ;

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Seismological Station of Yasur Volcano Tanna Island Vanuatu ; Sylvain Todman (geophysical engineer for the Government of Vanuatu) and Sandrine Cevuard (scientific officer volcanology) verify the proper operation of the station volcanological monitoring Yasur volcano on Tanna Island in Vanuatu. This station features a acoustimètre and buried a seismometer can be monitored in real time from anywhere in the world the volcano. This volcano, like other volcanoes in Vanuatu, is subject to continuous monitoring by the Geohazards center of Port Vila, to allow a better alert the local population in the event of imminent catastrophic eruption. The relatively large increase in explosive activity of the volcano has led to a rise in ash deposits on the island, particularly on food crops, some do not support. This is particularly the case of yam, taro and cabbage Kanak, which form the basis of the traditional diet. By Sylvain checks on his computer that measurements recorded by the station coincide well with the explosions of nearby volcano.Seismological Station of Yasur Volcano Tanna Island VanuatuSeismological Station of Yasur Volcano Tanna Island Vanuatu ; Sylvain Todman (geophysical engineer for the Government of Vanuatu) and Sandrine Cevuard (scientific officer volcanology) verify the proper operation of the station volcanological monitoring Yasur volcano on Tanna Island in Vanuatu. This station features a acoustimètre and buried a seismometer can be monitored in real time from anywhere in the world the volcano. This volcano, like other volcanoes in Vanuatu, is subject to continuous monitoring by the Geohazards center of Port Vila, to allow a better alert the local population in the event of imminent catastrophic eruption. The relatively large increase in explosive activity of the volcano has led to a rise in ash deposits on the island, particularly on food crops, some do not support. This is particularly the case of yam, taro and cabbage Kanak, which form the basis of the traditional diet. By Sylvain checks on his computer that measurements recorded by the station coincide well with the explosions of nearby volcano.© Thibaut Vergoz / BiosphotoJPG - RMNon exclusive sale

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Seismological Station of Yasur Volcano Tanna Island Vanuatu ;

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Seismological Station of Yasur Volcano Tanna Island Vanuatu ; Sylvain Todman and Sandrine Cevuard check the proper functioning of a new seismic station was placed near the Yasur volcano on Tanna Island. Installed in April 2012 by New Zealand, it acts as a "hub transmission," the nerve center of seismic monitoring stations on the island of Tanna. It has two cam (daytime, night) that allow us to observe the volcano as real for the world, and a seismometer buried (and seals on a concrete slab has set itself the rich mother under ash), which measures the tremors generated by the Yasur volcano nearby. The data is transmitted via GSM. Sylvain and Sandrine are very satisfied with the operation of the new station, which fits very well into the future monitoring network Vanuatu. Seismological Station of Yasur Volcano Tanna Island VanuatuSeismological Station of Yasur Volcano Tanna Island Vanuatu ; Sylvain Todman and Sandrine Cevuard check the proper functioning of a new seismic station was placed near the Yasur volcano on Tanna Island. Installed in April 2012 by New Zealand, it acts as a "hub transmission," the nerve center of seismic monitoring stations on the island of Tanna. It has two cam (daytime, night) that allow us to observe the volcano as real for the world, and a seismometer buried (and seals on a concrete slab has set itself the rich mother under ash), which measures the tremors generated by the Yasur volcano nearby. The data is transmitted via GSM. Sylvain and Sandrine are very satisfied with the operation of the new station, which fits very well into the future monitoring network Vanuatu. © Thibaut Vergoz / BiosphotoJPG - RMNon exclusive sale

1874551

Seismological Station of Yasur Volcano Tanna Island Vanuatu ;

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Seismological Station of Yasur Volcano Tanna Island Vanuatu ; Sylvain Todman verifies the operation of a new seismic station was placed near the Yasur volcano on Tanna Island. Installed in April 2012 by New Zealand, it acts as a "hub transmission," the nerve center of seismic monitoring stations on the island of Tanna. It has two cam (daytime, night) that allow us to observe the volcano as real for the world, and a seismometer buried (and seals on a concrete slab has set itself the rich mother under ash), which measures the tremors generated by the Yasur volcano nearby. The data is transmitted via GSM. Sylvain and Sandrine are very satisfied with the operation of the new station, which fits very well into the future monitoring network Vanuatu.Seismological Station of Yasur Volcano Tanna Island VanuatuSeismological Station of Yasur Volcano Tanna Island Vanuatu ; Sylvain Todman verifies the operation of a new seismic station was placed near the Yasur volcano on Tanna Island. Installed in April 2012 by New Zealand, it acts as a "hub transmission," the nerve center of seismic monitoring stations on the island of Tanna. It has two cam (daytime, night) that allow us to observe the volcano as real for the world, and a seismometer buried (and seals on a concrete slab has set itself the rich mother under ash), which measures the tremors generated by the Yasur volcano nearby. The data is transmitted via GSM. Sylvain and Sandrine are very satisfied with the operation of the new station, which fits very well into the future monitoring network Vanuatu.© Thibaut Vergoz / BiosphotoJPG - RMNon exclusive sale

1874550

Seismological Station of Yasur Volcano Tanna Island Vanuatu ;

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Seismological Station of Yasur Volcano Tanna Island Vanuatu ; Sylvain Todman and Sandrine Cevuard check the proper functioning of a new seismic station was placed near the Yasur volcano on Tanna Island. Installed in April 2012 by New Zealand, it acts as a "hub transmission," the nerve center of seismic monitoring stations on the island of Tanna. It has two cam (daytime, night) that allow us to observe the volcano as real for the world, and a seismometer buried (and seals on a concrete slab has set itself the rich mother under ash), which measures the tremors generated by the Yasur volcano nearby. The data is transmitted via GSM. Sylvain and Sandrine are very satisfied with the operation of the new station, which fits very well into the future monitoring network Vanuatu.Seismological Station of Yasur Volcano Tanna Island VanuatuSeismological Station of Yasur Volcano Tanna Island Vanuatu ; Sylvain Todman and Sandrine Cevuard check the proper functioning of a new seismic station was placed near the Yasur volcano on Tanna Island. Installed in April 2012 by New Zealand, it acts as a "hub transmission," the nerve center of seismic monitoring stations on the island of Tanna. It has two cam (daytime, night) that allow us to observe the volcano as real for the world, and a seismometer buried (and seals on a concrete slab has set itself the rich mother under ash), which measures the tremors generated by the Yasur volcano nearby. The data is transmitted via GSM. Sylvain and Sandrine are very satisfied with the operation of the new station, which fits very well into the future monitoring network Vanuatu.© Thibaut Vergoz / BiosphotoJPG - RMNon exclusive sale

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Seismological Station of Yasur Volcano Tanna Island Vanuatu ;

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Instrument measuring bradyseism Solfatara volcano Italia ; Phlegraean Fields, Pozzuoli.Instrument measuring bradyseism Solfatara volcano ItaliaInstrument measuring bradyseism Solfatara volcano Italia ; Phlegraean Fields, Pozzuoli.© Annie Guégant / BiosphotoJPG - RM

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Instrument measuring bradyseism Solfatara volcano Italia ;

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Faille sismique en Sicile ItalieFaille sismique en Sicile ItalieFaille sismique en Sicile Italie© Daniel Heuclin / BiosphotoJPG - RMSale prohibited in Japan
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Faille sismique en Sicile Italie

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Faille sismique dans un mur Sicile ItalieFaille sismique dans un mur Sicile ItalieFaille sismique dans un mur Sicile Italie© Daniel Heuclin / BiosphotoJPG - RMSale prohibited in Japan
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Faille sismique dans un mur Sicile Italie

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Cyclists on the drained part of the lake Breitharlon IcelandCyclists on the drained part of the lake Breitharlon IcelandCyclists on the drained part of the lake Breitharlon Iceland© Frédérique Bidault / BiosphotoJPG - RM

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Cyclists on the drained part of the lake Breitharlon Iceland

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Partie asséchée du lac Kleifarvatn due au séisme de 2001 ; Péninsule Reykjanes IslandePartie asséchée du lac Kleifarvatn due au séisme de 2001Partie asséchée du lac Kleifarvatn due au séisme de 2001 ; Péninsule Reykjanes Islande© Frédérique Bidault / BiosphotoJPG - RM

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Partie asséchée du lac Kleifarvatn due au séisme de 2001 ;

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Woman selling products on the street, the slums of Fort National, the district was largely destroyed by the earthquake in January 2010, Port-au-Prince, Haiti, Caribbean, Central AmericaWoman selling products on the street, the slums of Fort National, the district was largely destroyed by the earthquake in January 2010, Port-au-Prince, Haiti, Caribbean, Central AmericaWoman selling products on the street, the slums of Fort National, the district was largely destroyed by the earthquake in January 2010, Port-au-Prince, Haiti, Caribbean, Central America© Florian Kopp / imageBROKER / BiosphotoJPG - RMNon exclusive sale
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Woman selling products on the street, the slums of Fort National,

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Rift caused by an earthquake, Uyuni Highlands, BoliviaRift caused by an earthquake, Uyuni Highlands, BoliviaRift caused by an earthquake, Uyuni Highlands, Bolivia© Florian Kopp / imageBROKER / BiosphotoJPG - RMNon exclusive sale
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Rift caused by an earthquake, Uyuni Highlands, Bolivia

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Laughing children in front of a shabby hut in Sarash Village near Manshera, NFP, PakistanLaughing children in front of a shabby hut in Sarash Village near Manshera, NFP, PakistanLaughing children in front of a shabby hut in Sarash Village near Manshera, NFP, Pakistan© Florian Kopp / imageBROKER / BiosphotoJPG - RMNon exclusive sale
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1606551

Laughing children in front of a shabby hut in Sarash Village near

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Woman cooking on open fire in Jabba Refugees Camp, Balakot, NWFP, Pakistan. The camp is occupied by victims of the October 2005 earthquakeWoman cooking on open fire in Jabba Refugees Camp, Balakot, NWFP, Pakistan. The camp is occupied by victims of the October 2005 earthquakeWoman cooking on open fire in Jabba Refugees Camp, Balakot, NWFP, Pakistan. The camp is occupied by victims of the October 2005 earthquake© Florian Kopp / imageBROKER / BiosphotoJPG - RMNon exclusive sale
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1606550

Woman cooking on open fire in Jabba Refugees Camp, Balakot, NWFP,

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Resident laughing from the window of her new earthquake-safe house donated by a German aid organisation, Froide River village near Port-au-Prince, Haiti, Caribbean, Central AmericaResident laughing from the window of her new earthquake-safe house donated by a German aid organisation, Froide River village near Port-au-Prince, Haiti, Caribbean, Central AmericaResident laughing from the window of her new earthquake-safe house donated by a German aid organisation, Froide River village near Port-au-Prince, Haiti, Caribbean, Central America© Florian Kopp / imageBROKER / BiosphotoJPG - RMNon exclusive sale
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1604327

Resident laughing from the window of her new earthquake-safe

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Man with corrugated iron for roofing ; Man with corrugated iron for roofing. After the massive earthquake in January 2010 a German aid organizations is training local construction workers for the building of earthquake-proof houses, Coq Chante village near Jacmel, Haiti, Caribbean, Central AmericaMan with corrugated iron for roofingMan with corrugated iron for roofing ; Man with corrugated iron for roofing. After the massive earthquake in January 2010 a German aid organizations is training local construction workers for the building of earthquake-proof houses, Coq Chante village near Jacmel, Haiti, Caribbean, Central America© Florian Kopp / imageBROKER / BiosphotoJPG - RMNon exclusive sale
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1604326

Man with corrugated iron for roofing ; Man with corrugated iron

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Shell of an earthquake-proof timber-framed house, which a German aid organization donated to victims of the January 2010 earthquake, Coq Chante village near Jacmel, Haiti, Caribbean, Central AmericaShell of an earthquake-proof timber-framed house, which a German aid organization donated to victims of the January 2010 earthquake, Coq Chante village near Jacmel, Haiti, Caribbean, Central AmericaShell of an earthquake-proof timber-framed house, which a German aid organization donated to victims of the January 2010 earthquake, Coq Chante village near Jacmel, Haiti, Caribbean, Central America© Florian Kopp / imageBROKER / BiosphotoJPG - RMNon exclusive sale
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1604325

Shell of an earthquake-proof timber-framed house, which a German

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After the massive earthquake in January 2010 a German aid organizations is training local construction workers, roofers, here the construction of earthquake-proof houses, Coq Chante village near Jacmel, Haiti, Caribbean, Central AmericaAfter the massive earthquake in January 2010 a German aid organizations is training local construction workers, roofers, here the construction of earthquake-proof houses, Coq Chante village near Jacmel, Haiti, Caribbean, Central AmericaAfter the massive earthquake in January 2010 a German aid organizations is training local construction workers, roofers, here the construction of earthquake-proof houses, Coq Chante village near Jacmel, Haiti, Caribbean, Central America© Florian Kopp / imageBROKER / BiosphotoJPG - RMNon exclusive sale
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1604324

After the massive earthquake in January 2010 a German aid

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A family, victims of the earthquake in january 2010, next to their new earthquake-proof house with truss structure, which is made available by a German aid organization, Coq Chante village near Jacmel, Haiti, Caribbean, Central AmericaA family, victims of the earthquake in january 2010, next to their new earthquake-proof house with truss structure, which is made available by a German aid organization, Coq Chante village near Jacmel, Haiti, Caribbean, Central AmericaA family, victims of the earthquake in january 2010, next to their new earthquake-proof house with truss structure, which is made available by a German aid organization, Coq Chante village near Jacmel, Haiti, Caribbean, Central America© Florian Kopp / imageBROKER / BiosphotoJPG - RMNon exclusive sale
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1604323

A family, victims of the earthquake in january 2010, next to

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A family, victims of the earthquake in january 2010, next to their new earthquake-proof house with truss structure, which is made available by a German aid organization, Coq Chante village near Jacmel, Haiti, Caribbean, Central AmericaA family, victims of the earthquake in january 2010, next to their new earthquake-proof house with truss structure, which is made available by a German aid organization, Coq Chante village near Jacmel, Haiti, Caribbean, Central AmericaA family, victims of the earthquake in january 2010, next to their new earthquake-proof house with truss structure, which is made available by a German aid organization, Coq Chante village near Jacmel, Haiti, Caribbean, Central America© Florian Kopp / imageBROKER / BiosphotoJPG - RMNon exclusive sale
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A family, victims of the earthquake in january 2010, next to

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A family, victims of the earthquake in january 2010, next to their new earthquake-proof house with truss structure, which is made available by a German aid organization, Coq Chante village near Jacmel, Haiti, Caribbean, Central AmericaA family, victims of the earthquake in january 2010, next to their new earthquake-proof house with truss structure, which is made available by a German aid organization, Coq Chante village near Jacmel, Haiti, Caribbean, Central AmericaA family, victims of the earthquake in january 2010, next to their new earthquake-proof house with truss structure, which is made available by a German aid organization, Coq Chante village near Jacmel, Haiti, Caribbean, Central America© Florian Kopp / imageBROKER / BiosphotoJPG - RMNon exclusive sale
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1604321

A family, victims of the earthquake in january 2010, next to

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Architect of a German aid organization training local skilled workers in earthquake-resistant constructions after the earthquake in January 2010, Coq Chante village near Jacmel, Haiti, Caribbean, Central AmericaArchitect of a German aid organization training local skilled workers in earthquake-resistant constructions after the earthquake in January 2010, Coq Chante village near Jacmel, Haiti, Caribbean, Central AmericaArchitect of a German aid organization training local skilled workers in earthquake-resistant constructions after the earthquake in January 2010, Coq Chante village near Jacmel, Haiti, Caribbean, Central America© Florian Kopp / imageBROKER / BiosphotoJPG - RMNon exclusive sale
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1604320

Architect of a German aid organization training local skilled

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Architecture student drawing a diagram of a earthquake-proof house with truss structure. They are being trained by a German aid organization after the devastating earthquake in January 2010, Coq Chante village near Jacmel, Haiti, Caribbean, Central AmericaArchitecture student drawing a diagram of a earthquake-proof house with truss structure. They are being trained by a German aid organization after the devastating earthquake in January 2010, Coq Chante village near Jacmel, Haiti, Caribbean, Central AmericaArchitecture student drawing a diagram of a earthquake-proof house with truss structure. They are being trained by a German aid organization after the devastating earthquake in January 2010, Coq Chante village near Jacmel, Haiti, Caribbean, Central America© Florian Kopp / imageBROKER / BiosphotoJPG - RMNon exclusive sale
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1604319

Architecture student drawing a diagram of a earthquake-proof

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Architecture students drawing a diagram of a earthquake-proof house with truss structure. They are being trained by a German aid organization after the devastating earthquake in January 2010, Coq Chante village near Jacmel, Haiti, Caribbean, Central AmericaArchitecture students drawing a diagram of a earthquake-proof house with truss structure. They are being trained by a German aid organization after the devastating earthquake in January 2010, Coq Chante village near Jacmel, Haiti, Caribbean, Central AmericaArchitecture students drawing a diagram of a earthquake-proof house with truss structure. They are being trained by a German aid organization after the devastating earthquake in January 2010, Coq Chante village near Jacmel, Haiti, Caribbean, Central America© Florian Kopp / imageBROKER / BiosphotoJPG - RMNon exclusive sale
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1604318

Architecture students drawing a diagram of a earthquake-proof

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Man in front of his traditional wooden house which was badly damaged by the earthquake in January 2010, Coq Chante village near Jacmel, Haiti, Caribbean, Central AmericaMan in front of his traditional wooden house which was badly damaged by the earthquake in January 2010, Coq Chante village near Jacmel, Haiti, Caribbean, Central AmericaMan in front of his traditional wooden house which was badly damaged by the earthquake in January 2010, Coq Chante village near Jacmel, Haiti, Caribbean, Central America© Florian Kopp / imageBROKER / BiosphotoJPG - RMNon exclusive sale
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1604317

Man in front of his traditional wooden house which was badly

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After the massive earthquake in January 2010 a German aid organizations is training local construction workers, roofers, here the construction of earthquake-proof houses, the houses get a truss structure which is then filled with mud and stones, Coq Chante village near Jacmel, Haiti, Caribbean, Central AmericaAfter the massive earthquake in January 2010 a German aid organizations is training local construction workers, roofers, here the construction of earthquake-proof houses, the houses get a truss structure which is then filled with mud and stones, Coq Chante village near Jacmel, Haiti, Caribbean, Central AmericaAfter the massive earthquake in January 2010 a German aid organizations is training local construction workers, roofers, here the construction of earthquake-proof houses, the houses get a truss structure which is then filled with mud and stones, Coq Chante village near Jacmel, Haiti, Caribbean, Central America© Florian Kopp / imageBROKER / BiosphotoJPG - RMNon exclusive sale
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1604316

After the massive earthquake in January 2010 a German aid

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After the massive earthquake in January 2010 a German aid organizations is training local construction workers, roofers, here the construction of earthquake-proof houses, Coq Chante village near Jacmel, Haiti, Caribbean, Central AmericaAfter the massive earthquake in January 2010 a German aid organizations is training local construction workers, roofers, here the construction of earthquake-proof houses, Coq Chante village near Jacmel, Haiti, Caribbean, Central AmericaAfter the massive earthquake in January 2010 a German aid organizations is training local construction workers, roofers, here the construction of earthquake-proof houses, Coq Chante village near Jacmel, Haiti, Caribbean, Central America© Florian Kopp / imageBROKER / BiosphotoJPG - RMNon exclusive sale
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1604315

After the massive earthquake in January 2010 a German aid

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Architect holding the diagram of a wooden house ; Architect holding the diagram of a wooden house. After the massive earthquake in January 2010 a German aid organizations is training local construction workers, here in the construction of earthquake-proof houses, Coq Chante village near Jacmel, Haiti, Caribbean, Central AmericaArchitect holding the diagram of a wooden houseArchitect holding the diagram of a wooden house ; Architect holding the diagram of a wooden house. After the massive earthquake in January 2010 a German aid organizations is training local construction workers, here in the construction of earthquake-proof houses, Coq Chante village near Jacmel, Haiti, Caribbean, Central America© Florian Kopp / imageBROKER / BiosphotoJPG - RMNon exclusive sale
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1604314

Architect holding the diagram of a wooden house ; Architect

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