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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.
Engesund
For more than 350 years Engesund has been a place for hostelries and trading in the Fitjar islands. The place is centrally placed in the shipping lane, with a sheltered harbour close to the exposed Selbjørnsfjorden. Engesund was once part of the great network of historical stopover places on the coast.
Færøysund
The old trading post lies at the sound between Stord and Færøy in Langenuen. There was a country store and steamship forwarding agent up to 1964. The trade was then moved over to the new ferry harbour of Sandvikvåg.
Fitjarøyane
If we study the group of islands south of Selbjørns Fjord from the air or on a sea map, we will notice that many of the islands are elongated and lie systematically in rows. The islands are divided by long sounds, for example Trollosen, Nuleia and Hjelmosen, which are oriented in a south-southeast to north-northwesterly direction.
Fitjar- potatoes
The deep agricultural soils in Fitjar are found especially in the area between Lake Storavatnet and Breivika. The many stonewalls in the area reflect that the earth probably was full of stones and stone blocks. The stones that couldn't be dug out had also a function: they stored heat that helped to grow potatoes.
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.