- Remove Small landforms filter Small landforms
- Remove Maritime environments filter Maritime environments
- Remove Seabirds filter Seabirds
- Remove Monastery filter Monastery
- Remove Fitjar filter Fitjar
- Remove Avalanches and rock falls filter Avalanches and rock falls
- Remove Etne filter Etne
- Remove Igneous rocks filter Igneous rocks
- Remove Late glacial filter Late glacial
- Remove Os, frå 2020 del av nye Bjørnafjorden kommune filter Os, frå 2020 del av nye Bjørnafjorden kommune
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.
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.
Lysekloster- The monks and nature
Lysekloster was the largest agricultural property in the country when it was phased out during the Reformation in 1537. In its prime this cloister encompassed two-thirds of all the farms in Os. The monks introduced and cultivated new plant species and it was probably they who stocked the waters with fish not indigenous to the area. This legacy from the Middle Ages has left a lasting mark.