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Dwelling house and store from the Øystese hamlet.

Øystese- Kvam rural museum

07.12.2018 - 14:52

Lurøyane

Lurøyane

16.06.2018 - 18:49

The geology along Oster Fjord and further eastward, in cross-section and on the surface. (Haakon Fossen)

Stall

11.12.2018 - 14:43

The Bergen Arcs have an unusually sharp boundary to the bedrock in the east. Geologists think that this was caused by movements in the earth's crust during the Devonian Period. Then, the Bergen Arcs on the Lindås peninsula sank a whole 10 kilometres in relation to the Precambrian basement gneisses on the east side of Fens Fjord and Aust Fjord.

Mining pit in the steep slope at Froastad.

Froastad

19.05.2018 - 12:50

Kvamskogen, toward the north.

Kvamskogen

02.12.2018 - 20:57

The different bedrock types that got shoved in over Hordaland in Cambro-Silurian times still remain, layer by layer, almost like a cake. But at Kvamskogen the cake has been turned upside down.

Hardanger fartøyvernsenter

Hardanger Maritime Museum

03.07.2019 - 10:51