- Remove Small landforms filter Small landforms
- Remove Weather phenomena filter Weather phenomena
- Remove Middle age filter Middle age
- Remove Defense filter Defense
- Remove Place filter Place
- Remove Civil servant dwellings and manors filter Civil servant dwellings and manors
- Remove Os, frå 2020 del av nye Bjørnafjorden kommune filter Os, frå 2020 del av nye Bjørnafjorden kommune
- Remove Midthordland filter Midthordland
- Remove Introduced species filter Introduced species
- Remove Fish filter Fish
- Remove Sediments filter Sediments
Ferstad
Ferstad is well worth a visit. The farm lies on a little hillock south of Lekven: a beautiful official residence from the 1700s.
Osøyro
The coastal settlement of Os begins to take form in the middle of the 1800s. This is when craftsmen and traders begin to settle at the river delta.
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.
Oselva
Oselvo is the biggest waterway on the Bergen peninsula, with sources in Gullfjellet and Sveningen. There is a fall of only 60 metres along the entire stretch from Samdalsvatnet Lake to the sandbank in Fusafjorden. It is rare to see a river like this in western Norway. There is salmon along this entire section of the Oselvo river.
Søfteland
If you drive between Søfteland and Ulven on a clear spring morning, or an evening in late autumn, you are advised to be careful on the turns. The temperature on the road can fall to under 0 °C here long before other places in the municipality. On clear, still nights the earth's surface chills quite a bit. In exposed areas a layer of cold air develops very near the ground and the road surface can easily chill to below freezing.