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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.
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.
Bordalsgjelet
Deep down between the stone polished phyllite bedrock in Bordalsgjelet canyon, there is a cascading river. In close cooperation with hard polishing stones, the water has carved into the bedrock for thousands of years - and is still doing so today.
Stalheim
Stalheim is situated between Stalheimsfossen and Sivlefossen, in a community with the farms Sivle and Brekke. The most likely explanation of the name is “the farm by Stadall”, from “standa” (stand), probably with background in the steep Stalheimskleivi. The farm has for a long time been divided into several units. At Stalheim there has been a transport exchange from the Middle Ages and the farm has been a postal farm since 1647.