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Strandvollen ved Hallaråker. Siggjo in the background

Hallaråker

19.05.2018

From Rubbestadneset.

Rubbestadneset

18.06.2018

Toward Støle and Sørheim, 1920.

The village of Etne

18.12.2018

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.

Boat engines, Norwegian Engine Museum in Skånevik

Skånevik- Norwegian engine museum

25.04.2018

Today there are only a few farmers that grow potatoes in Fitjar.

Fitjar- potatoes

19.12.2018

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.

Huglo

Huglo

19.06.2018

The majority of Huglo is bare rock. A bit of dwarf pine forest is the only vegetation able to put down roots. Along the west- and east sides, to the contrary, the landscape is unusually green and lush. The reason lies both in the bedrock and in the ice that covered the area 12 000 years ago.

Spring in the black alder forest of Hystadsmarkjo.

Hystad- the black alder forest

19.06.2018

One of the biggest black alder forests in the country is in Hystadmarkjo. Along the well prepared trail through the forest you can experience an exceptional nature with an unusual abundance of exuberant plant species. But what has laid the foundation for this richness?

Sagvåg in the early 1900s, with the gate saw and the shipyard to the right in the picture.

Sagvåg

19.06.2018

The pit saw on the property of the farm Valvatna, is the origin of the name Sagvåg. The sawmill is mentioned as early as 1564. The name of the place at that time was Fuglesalt, but soon there is only talk of Saugvog.

Bordalsgjelet

Bordalsgjelet

13.01.2019

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.

Bømoen toward the north.

Bømoen

12.01.2019

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