University of Bergen- Remove Smallholdings filter Smallholdings
- Remove Maritime environments filter Maritime environments
- Remove Avalanches and rock falls filter Avalanches and rock falls
- Remove Churches filter Churches
- Remove Eidfjord filter Eidfjord
- Remove Late glacial filter Late glacial
- Remove Fitjar filter Fitjar
- Remove Austrheim filter Austrheim
- Remove Farming and forestry filter Farming and forestry
- Remove Basement rocks filter Basement rocks
- Remove Lindås, frå 2020 del av nye Alver kommune. filter Lindås, frå 2020 del av nye Alver kommune.
- Remove Faults filter Faults
Fruo
At Fruo, nature has built its own little "Chinese wall ". Some kilometers south of the Vøringsfossen waterfall, there are a number of moraine ridges, the longest and most notable of their kind in Hordaland.
Hæreid- geology
The Eidfjord terrace is a gigantic ridge that reaches up more than one hundred metres from the city centre in Eidfjord. It serves as a powerful natural monument left behind by the ice when it retreated.
Krossøy
Furthest north in the island community Rongevær, at the entrance to Fensfjorden, lies Krossøy. Belonging to the farm are the islands of Krossøy, Husøy, Kårøy, Lyngkjerringa, Søre Kjerringa, Rotøy and Kuhovet. All of them have been inhabited. On Krossøy itself today there are four holdings. The marine use environment here is one of the best preserved along the West Norwegian coast.
Lygra
The heath landscape on outer Lygra, Utluro and Lurekalven will in future become part of a landscape protection area, to be maintained through traditional activities with year-round outdoor sheep, grazing and burning. The West Norwegian heath country belongs to a large North Atlantic coastal landscape stretching from the Bay of Biscay to the Lofoten islands.
Stall
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.
