As a result, Büdel constructed his theory of „excessive valley formation“ in cold climate zones. Büdel’s idea was to do this in an area with a climate similar to what he believed it would have been like in central Europe during the ice age and with a geological structure similar to southwestern Germany, where he wanted to understand the evolution of the landscape during the ice age. Different aspects of natural history were investigated, with a clear focus on geomorphology, the science of the landforms of the Earth’s surface, their development through changing climates and the processes involved: the evolution of the arctic landscape. The southwestern part of Barentsøya was a key area for scientific work of the German Stauferland-Expeditions between 19, led by the Geographer Julius Büdel from Würzburg in south Germany. Reindeer are roaming around in large numbers, building up their fat reserves for the winter by constantly feeding on the rich vegetation. Freemansund is separating Barentsøya from Edgeøya, the north coast of which is lying completely there with its characteristic table-shaped mountains. From the hills, you have a lovely scenic view over the tundra around you with its lakes, where flocks of geese and some Red-throated divers are slowly swimming their loops in safety from Arctic foxes. Sundneset is a tundra-lowland with some rocky hills at the southwestern corner of Barentsøya, stretching into Freemansund.
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