Robert Harding

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832-403584 - Mountain landscape with steep rocky peaks and lake Tennesvatnet, Krokvatnet and Fjerddalsvatnet, in the back peak of Hermannsdalstinden, view from the top of Munken, Moskenesoya, Lofoten, Nordland, Norway, Europe
832-397656 - Panoramic road, gravel road in Monument Valley, prominent rocks, West Mitten Butte, East Mitten Butte, Merrick Butte on the horizon, dusk, film set, Arizona, USA, North America
832-394648 - Hiker looking at mountains under dramatic clouds, view from the summit of the Westliche Toerlspitze, in the back Partenkirchner Dreitorspitze, Wetterstein Mountains, Garmisch-Partenkirchen, Bavaria, Germany, Europe
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.
832-389210 - Mountain peak (Aurora borealis) Stetind, arctic winter landscape, night view, starry sky, northern lights Northern Lights, in front ice floes, Stetinden, Nordland, Norway, Europe