University of Bergen- Remove Quarns and mills filter Quarns and mills
- Remove Basement rocks filter Basement rocks
- Remove Railroad filter Railroad
- Remove Hydro power filter Hydro power
- Remove Voss, frå 2020 del av nye Voss herad. filter Voss, frå 2020 del av nye Voss herad.
- Remove Sund, frå 2020 del av nye Øygarden kommune filter Sund, frå 2020 del av nye Øygarden kommune
- Remove Igneous rocks filter Igneous rocks
Golta- Gneiss
Over thousands of years, autumn storms and strong land-driving winds have cleaned the bare rocks of Golta. The waves can beat far in over land and make it dangerous to walk along the shoreline. When the storms have calmed, the results of their work comes into view.
Spildepollen
The oceanic crust of the North Sea was subjected to a lot of stretching both in Permian and Triassic times, and later in the Jurassic. This stretching resulted in the North Sea collapsing in and also to large faults forming west of Hordaland and on the mainland. Austefjorden in Sund follows one of these faults.
Rekvemylna
If you enter the farmyard at Rekve, some kilometres from Bulken, where the road departs to Giljarhus, you no longer meet “the miller”, Knut Hernes, in his old rural mill. But some years ago he would wish you welcome, friendly and hospitable, and show you around his mill, which had been his workplace for a generation. As light-footed as a youth he climbed in steep ladders high up into the waterfall, to let the water down on to the waterwheel.
Ygre
Ygre Station lies hidden away for highway travellers, just below the road Vossevangen-Mjølfjell. The station building at Ygre was constructed at Nesttun station in 1879-80. Almost all the stations at the Voss railway were identical. The architect was Balthazar Lange, and the type was called subsidiary station No.4. It is built in the Swiss style, as fashion of the times demanded.
