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Cross-leaved heath (Akvarell: Miranda Bødtker)

Steinevik

31.03.2018 - 19:37

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?

Frøland power station and lake Frøland.

Frøland

18.03.2018 - 08:03

Much rain, a steep drop and nearness to Bergen meant that the power-making potential of the Samnanger water system was exploited early. Samnanger was thus one of the first power-producing municipalities in western Norway. With its subsequent expansion and new power stations, about 400 gigawatts of electricity per hour were produced on average each year. This is enough to meet the energy needs of 25,000 households.

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

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.

Fadnesskaret

Fadnesskaret

31.03.2018 - 20:07

Lønaøyane

Lønaøyane

31.03.2018 - 19:10

The Strandaelvi river is forever protected from the development of hydropower. The Lønaøyane islands – which comprise the delta furthest north in Lake Lønavatnet - are a part of this water system. In 1995 the level of protection for the Lønaøyne islands was strengthened to that of a nature preserve because of the rich birdlife in this wetland.

Rekvesøyane

Rekvesøyane

29.03.2018 - 11:53

The sediment that was deposited from the river Dyrvo has created the fan-shaped delta Rekvesøyane. The bit of land farthest out toward the water gets periodically flooded, especially during snow melt and after periods of much rain.

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