- Remove Small landforms filter Small landforms
- Remove Middle age filter Middle age
- Remove Fish filter Fish
- Remove Waterfalls filter Waterfalls
- Remove Tysnes filter Tysnes
- Remove Os, frå 2020 del av nye Bjørnafjorden kommune filter Os, frå 2020 del av nye Bjørnafjorden kommune
- Remove Igneous rocks filter Igneous rocks
![Varghola](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_235-_x.jpg?itok=oGVCMzhh)
![Oselva](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/os_17.jpg?itok=1e-Hzb2u)
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.
![The monks leave their mark at Lysekloster](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/os_24.jpg?itok=Q5bQc7i9)
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.
![Boat bow of oak shaped like an animal head.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_223-4.jpg?itok=6Y1lzt5t)
![The walls in the boathouse in Hopssundet are built of red granite from Reksteren.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/tysnes_25.jpg?itok=_ViluBHW)
![Espevik](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/tysnes_15.jpg?itok=xW8eH-Lu)
Espevik
220 million years ago, glowing hot molten rock masses intruded into fractures in the earth's crust in the outer parts of Hordaland. Some of these are believed to have reached the surface and formed lava flows, which since have been eroded away by wind and weather. But, most of these flows solidified into diabase sills before they got to the surface.
![Lyse Monastery, reconstruction](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh-239_lysekloster.jpg?itok=bc_kHrFJ)