University of Bergen- Remove Small landforms filter Small landforms
- Remove Faults filter Faults
- Remove Maritime environments filter Maritime environments
- Remove Monastery filter Monastery
- Remove Fitjar filter Fitjar
- Remove Avalanches and rock falls filter Avalanches and rock falls
- Remove Masfjorden filter Masfjorden
- Remove Sawmills filter Sawmills
- Remove Lindås, frå 2020 del av nye Alver kommune. filter Lindås, frå 2020 del av nye Alver kommune.
- Remove Late glacial filter Late glacial
- Remove Road constructions filter Road constructions
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.
Mollandseid
In Mollandsvågen, close by the river that runs from Mollandsvatnet (lake) into the fjord, are two water-powered circular saws and a mill. This small industrial centre has belonged to the farms Molland, Reknes and Duesund, which together own the rights to the waterfall
Fitjarøyane
If we study the group of islands south of Selbjørns Fjord from the air or on a sea map, we will notice that many of the islands are elongated and lie systematically in rows. The islands are divided by long sounds, for example Trollosen, Nuleia and Hjelmosen, which are oriented in a south-southeast to north-northwesterly direction.
Fitjar- potatoes
The deep agricultural soils in Fitjar are found especially in the area between Lake Storavatnet and Breivika. The many stonewalls in the area reflect that the earth probably was full of stones and stone blocks. The stones that couldn't be dug out had also a function: they stored heat that helped to grow potatoes.
