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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.

Bømoen toward the north.

Bømoen

12.01.2019 - 16:32

Brekkhus

Brekkhus

19.06.2018 - 18:03

Evanger sentrum før brannen i 1923

Evanger

19.06.2018 - 18:11

Evanger (from Old Norse ålvangr, “vang”, “voll” (field) where the horses may graze) is the place where the river from Vangsvatnet, the Voss watercourse, runs out into Evangervatnet. From here Teigdalen valley runs to the north, towards Eksingedalen, and from here there is a short distance to Bergsdalen in the south.

Fadnesskaret

Fadnesskaret

31.03.2018 - 20:07

Dagestad museum, Voss

Gjernes

19.06.2018 - 18:03

The rock painting “running dog”

Gjøstein

13.03.2018 - 21:23

From Hamlagrøhornet one sees a division between the fertile phyllite and the naked Precambrian basement rock types in the landscape

Hamlagrø

13.01.2019 - 16:38

The type of underlying rock can be decisive for how many different types of plants are found in an area. In the area around Hamlagrø-lake the diversity is especially obvious. The geological conditions change much here within a short distance.

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.

Slopes above the Kårdal boarding house

Mjølfjell

22.01.2019 - 13:49

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