Robert Harding

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832-395104 - Aerial view, Landscape panorama, Dramatic volcanic landscape, Colourful erosion landscape with mountains, Lava field, Landmannalaugar, Fjallabak Nature Reserve, Suourland, Iceland, Europe
832-393351 - Chamois (Rupicapra rupicapra) and mountain landscape above clouds at Rosskofel, called Monte Cavallo di Pontebba, is located in the west of the ski area Nassfeld and is a karst mountain, Austria, 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.
832-392853 - Primeval landscape in the Leidinghofer valley, Mathelbach, karst, rocks, overhang, near Leidingshof, part of Markt Heiligenstadt, Franconian Switzerland, Upper Franconia, Franconia, Bavaria, Germany, Europe
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.