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Bjellandsvatnet (Bjørn Moe)

Bjellandsvatnet

06.05.2019 - 09:44

Lake Bjellandsvatnet is one of the richest wetland areas in Sveio. But, everything has its limit, and the supply of nutrients can be too much. This is what was about to happen in Lake Bjellandsvatnet.

Bjørsvik

Bjørsvik

24.06.2018 - 15:41

The industrial settlement Bjørsvik

A “chest piece” from Bu museum.

Bu

29.04.2018 - 11:23

Byrkjehaugen, Voss

Byrkjehaugen

19.06.2018 - 17:50

On the farm Bø, close to the highway between Bulken and Voss lies Byrkjehaugen, one of the largest burial mounds in West Norway. Originally it was around 50m across and 5m high, but following the excavation in 1908 and chipping off by both railway and road construction, the cross-section has shrunk to 37m and the height to 4m. All the same, it is an impressive burial monument for the passing traveller to see.

Bømoen toward the north.

Bømoen

12.01.2019 - 16:32

Bronze keys and remains of a wooden stick from Døso.

Døso

16.06.2018 - 14:11

Blanks for bowls and ladles

Eidsbøen

13.03.2018 - 20:58

Where the school and the sports facility lie at Eidsbøen there was previously a bog surrounded by small hillocks. More than 1000 years ago this was a holy place, where the dead were buried.

Eio

Eio

18.03.2019 - 09:21

A silled lake at Ekse

Eksingedalen- hydropower development

13.12.2018 - 16:56

Water discharge at the outlet of the Ekso into Eidsfjord was halved after the big hydropower development in the mountainous area between Modalen and Eksingedalen and further southward toward Evanger in the 1960s, 70s and 80s. In an attempt to amend the changed environmental conditions in the waterway the developer built 35 small dams in the river.

Flatekvål

Eksingedalen- landscape

13.12.2018 - 17:06

Eksingedalen alternates between wide, flat flood plains with good farmland, and narrow passages with waterfalls where the roads cling to the mountainsides. The alternations in the landscape are a result of the sculpturing work by glaciers over several ice ages, and the deposition of the glacial river deposits when the last glacier finally melted back.

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