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Borgåsen
In Etne there are no less than four defensive refuges. They are all situated in strategic positions, so that they have served as places of refuge and protection for central parts of the district
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.
Etnedeltaet
During the latter half of the 1900s the big natural river deltas on Westland disappeared. Until the 1980s there was still a small, but significant remnant of the original river delta from the Etneelva river, but today most of this, too, is industrial land.
Helgaberget
Helgaberget – the holy hill – is a little rocky crag which thrusts itself a few metres above the terraced surface of Støle. The surface of the rock is strewn with figures inscribed in the rock and it was, as far as one can judge, a cult centre in the Bronze Ages. The name could indicate that the tradition of holiness can have lasted for almost 3,000 years.
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.
Rimbareid- Vestbøstad
At nesting time you cannot avoid hearing the calls of the curlew or the snipe along the narrow road through the cultural landscape from Rimbareid to Vestbøstad. And on late summer evenings, the intense song of the sedge warbler rings out over the two characteristic tarns in the area.
Rimsvarden
Rimsvarden lies high and unencumbered, an enormous stone mound on the highest top with a wide view of the Fitjar rural community. With its 30 meters across and almost 4 meters high, this is one of the largest prehistoric burial relics existing in Hordaland.
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.
