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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.
Kyrping
The trading post down by the fjord at Kyrping does not belong to the oldest group of trading posts from the 1600s and 1700s. It was only after the liberalisation of the trading legislation that trade was established here.
Skånevik- the trading post
There are only two buildings left of the old trading and guesthouse settlement in Skånevik. They are in the centre, close to the main road passing through the settlement. The other buildings that belonged to the place, the lodging house (“Holteriet”), the bakery, the courthouse, the boathouse and the sea house with the store, were pulled down in the last century.
Støle
High above the sea and the beach flats, on one of the wide terraces shaped by the sea and the ice, lies the farm Støle (Stødle). The Old Norse name of Studla is derived from studill “support, shelf”. As far back as Viking times Støle has been a chieftain’s farm, a good farm on the plains formed by the moraine masses.
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.