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Glacier fall at Bondhusbreen.

Bondhusdalen

19.12.2018 - 19:25

The Bondhus area in Maruanger has been a magnet for tourists ever since the stream of tourists to Norway's west coast began in the middle of the 1800s. The magnificent landscape with the "ice trail" up to Bondhusvatnet Lake, the ice falls from Bondhusbreen glacier and Keisarstigen trail up to Folgefonna are still popular tourist attractions.

Gildrehola

Gildrehola

12.03.2018 - 12:53

Gjuvsland (Svein Nord)

Gjuvsland

19.06.2018 - 16:21

From Ingahogg.

Ingahogg

20.12.2018 - 12:19

At nearly 1000 metres over sea level, on the north side of INGAHOGG mountain, the remains of a soapstone quarry have been discovered. It is said, according to the Sagas, that Inga collected the big soapstone that lies in front of the Åkra Church from here.

Hauga House at Tveito, Kvinnherad

Tveito

19.06.2018 - 16:17

Portrait of Jonas Lie

Undarheim

19.06.2018 - 16:18

Mine hole above Kvitebergsvatnet Lake, by Atramadalen.

Ølve- Mining

05.01.2019 - 15:28

All in all there are ten known copper mines and two iron mines on the Ølve peninsula. Geologically, the nine mines on Varaldsøy Island also should be figured in. The industry began at Lilledal in 1642 wth the mining of iron ore. From Jernsmauget by Dyråsen, the iron ore was sent to the iron works in eastern Norway.

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

Gullbotnen

Gullbotnen

07.12.2018 - 10:32

A barren belt where almost nothing grows, runs through the forest on the east slope of Gullbotnen. But, along the west side of the main road there is a fertile zone that flourishes with several finicky plant types. The contrasts arise from the extreme variations in the nutrient content of the bedrock.

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