860-292276 - The Petrified Forest National Park is home to thousands of fossilized tree trunks approximately 200 million years old (Triassic period). Arizona. USA.
860-292267 - Tourists visiting the Upper Antelope Canyon, 2 to 3 m wide and 400 m long, managed by the Navajo Indian tribe. Antelope Canyon. Arizona. USA.
1116-52960 - Clearing storm clouds over Shiprock in the high-desert plain of the Navajo Nation in New Mexico, USA, Shiprock, New Mexico, United States of America
1116-52834 - Stunning view of the sandy beach with surf forming a zigzag pattern in the foam next to the large, boulders lining the shores at The Baths, a famous beach in the BVI's, Virgin Gorda, British Virgin Islands, Caribbean
1116-52832 - Woman standing under the large, boulders on the seaside shores of The Baths, a famous beach in the BVI's, Virgin Gorda, British Virgin Islands, Caribbean
1350-6449 - Sunrise over the La Sal Mountains and Buck Canyon in the Island in the Sky District, Canyonlands National Park, Utah. Viewed from the Buck Canyon Overlook.
1350-6445 - Sunset light on the Shafer Canyon Overlook in the Island in the Sky District, Canyonlands National Park, Utah. Dead Horse Point at left with the La Sal Mountains behind.
1350-6439 - Above the clouds of a winter temperature inversion in Canyonlands National Park, Moab, Utah. Viewed from Buck Canyon Overlook, Island in the Sky District.
1350-6431 - Cloudy sunrise over Buck Canyon, the White Rim & the La Sal Mountains, Canyonlands National Park, Moab, Utah. Viewed from the Buck Canyon Overlook in the Island in the Sky District of Canyonlands NP.
860-290892 - Waterfall Sellfoss in the Vatnajoekull NP. Sellfoss is the first of several waterfalls of river Joekulsa a Fjoellum in the canyon Joekulsargljufur. Europe, Northern Europe, Iceland
746-91099 - Quebrada de las Conchas also called Quebrada de Cafayate. A canyon with colorful rock formations created by Rio de las Conchas. South America, Argentina, November
746-91097 - Routa 68. Quebrada de las Conchas also called Quebrada de Cafayate. A canyon with colorful rock formations created by Rio de las Conchas. South America, Argentina, November
746-91098 - Routa 68. Quebrada de las Conchas also called Quebrada de Cafayate. A canyon with colorful rock formations created by Rio de las Conchas. South America, Argentina, November
746-91096 - Routa 68. Quebrada de las Conchas also called Quebrada de Cafayate. A canyon with colorful rock formations created by Rio de las Conchas. South America, Argentina, November
1116-51673 - A switchback road leading to the town of Sunland, Washington on the bank of Wanapum Lake on the the Columbia River; Sunland, Washington, United States of America
1116-50925 - The Twelve Apostles, limestone rock formations along the coast, Great Ocean Road, Port Campbell National Park; Port Campbell, Victoria, Australia
860-290212 - Les Terres Noires de Robine sur Galabre under the snow. 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.
860-290211 - Les Terres Noires de Robine sur Galabre under the snow. 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.
860-290213 - Les Terres Noires de Robine sur Galabre under the snow. 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.
860-288797 - 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.
860-288796 - 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.