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The village of Etne
Much of the sand and gravel that the town of Etne is built on was laid down at the end of the Ice Age and is evidence of melting glaciers and roaring meltwater rivers. The uncompacted material in the big terraces leave their unmistakeable mark on the wide elongated valleys.
Tangarås
From his loft window on the doctor’s farm at Tangarås the young Hans Ernst Kinck had a view of the fjord and the Mauranger mountains. The fjord settlements in West Norway made a strong impression on the young boy when his family moved from Setesdal, from “the stifling mystique of the ballad”, to Strandebarm in 1876. The new district doctor bought the old captain’s farm at Tangarås, which had for some time been a military head farm after Håbrekke further into the settlement.
Vikøy
Through Adolph Tidemand’s detailed close-ups of smokehouses in Kvam, the vicarage in Vikøy, where he lived during his painting trips through Hardanger, has obtained a central position in the Norwegian national romanticism.
Skånevik- moraine
In Skånevik there are marks left from the ice edge that advanced during the thousand-year cold spell (Younger Dryas) that marked the end of the Ice Age roughly 11 500 years ago. The glacier first proceeded out into Åkra Fjordand and around Vannes and thereafter sent an arm in toward Skånevik. Here, the glacier lay down an end moraine up against the mountainside.
