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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.
Etne river
There is still life to be found that is just “hanging on a string”. The Etne river has been the most important river for sports- fisherman in Hordaland after salmon fishing in Vosso was temporarily forbidden. As late as 2000, 4 tonnes of salmon and sea trout were taken out of the Etne river, the best fishing for 10 years. In the whole of the county there are only 15-20 rivers that can compete with this haul.
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.
Sæbøtunet
When you come into the well-tended farm steading at Sæbø just above Etne centre, you get the impression of a Sunnhordland farm from well before the time of the tractor; from the time of the horse and the scythe. The hamlet at Sæbø, one of the farms neighbouring to Gjerde, was taken over by Sunnhordland Folk Museum in 1938.
