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Elm - and lime tree

Andvikedalen

31.03.2018 - 19:56

Model of the king’s estate around 1300

Bergenhus

12.05.2020 - 14:50

Bergesfjellet

Bergesfjellet

12.03.2018 - 13:17

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.

Dale power station

Dale power station

18.03.2018 - 08:16

In 1923 Bergenshalvøens Kommunale Kraftselskap (BKK) expropriated large areas for power plants and development of hydropower started soon afterwards. Dale power station with the two first aggregates, each of 14 MW was put into operation on 17 November 1927. In the supply reservoir in Storefossen 5152 cubic metres of concrete were cast, and a modern and well-equipped power station was built.

A zone with nuggets from the inner earth.

Drøna

12.03.2018 - 13:01

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.

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.

Espevik

Espevik

03.01.2019 - 15:26

220 million years ago, glowing hot molten rock masses intruded into fractures in the earth's crust in the outer parts of Hordaland. Some of these are believed to have reached the surface and formed lava flows, which since have been eroded away by wind and weather. But, most of these flows solidified into diabase sills before they got to the surface.

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