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Potholes

Hausberget

31.03.2018 - 21:20

Fossen cliff

Fossen Bratte

07.12.2018 - 09:36

The steep drop by Fossen cliff has been the biggest challenge for those who wished to make a road over Kvamskogen through the years. Leave the car by the monument on the old road and take a walk down to the bend by the waterfall that Bergen-folk call "The bridal veil". Why is there a waterfall just here?

Gneiss.

Frøland- Liarostunnel

16.06.2018 - 17:24

Soft shapes in the hard mountain.

Grasdalen

12.03.2018 - 13:08

The combination building at Nordvik.

Nordvik

16.06.2018 - 17:27

“Prospectus of Frekhaug”. J.F.L.Dreier, 1812

Frekhaug

17.06.2018 - 16:38

Frekhaug has been a large farm with well-off owners through many generations. The main house, a two storey building with a hipped roof, must have been erected about 1780.

Husebø

Husebø

17.06.2018 - 16:39

When the Corncrake returned to Nordhordland, it came as no surprise that Husebø was the place it chose. Here, remnants of the old cultural landscape are still in good condition. And the Corncrake is not alone in appreciating this.

Otterstadstølen

Otterstadstølen

18.10.2018 - 08:54

Otterstadstølen lies in an idyllic grassy plain surrounded by rich forest, but also with high mountains close by. The mountainsides are steep and typical of this part of the county. The same cannot be said about the forest. This spruce forest has been able to develop freely for hundreds of years. Otherwise in the county, only Voss has spruce forest.

Einstapevoll

Einstapevoll- the farm

19.06.2018 - 17:10

Einstapevoll (from einstape: “bregne” (fern)) lies on the west side of the Tittelsnes peninsula. Up to 1831 the farm was a vicarage belonging to Stord parish. The priests had leasing rights. Land rent and other fees from the farm was part of their salaries.

Bordalsgjelet

Bordalsgjelet

13.01.2019 - 13:52

Deep down between the stone polished phyllite bedrock in Bordalsgjelet canyon, there is a cascading river. In close cooperation with hard polishing stones, the water has carved into the bedrock for thousands of years - and is still doing so today.

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