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Lyngholmen

13.03.2018 - 21:20

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.

Dagestad museum, Voss

Gjernes

19.06.2018 - 18:03

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.

Slopes above the Kårdal boarding house

Mjølfjell

22.01.2019 - 13:49

Working with roof slates in the slate quarry at Nordheim around the year 1900

Nordheim

22.01.2019 - 14:48

"And here these endless kingdoms and these toils for a rich working life far and wide have lain and slept for a hundred thousand years! Right up until the Voss Railway came in 1883 and woke them, like the prince in the fairytale who awakened the Sleeping Beauty."

Kvamskogen, toward the north.

Kvamskogen

02.12.2018 - 20:57

The different bedrock types that got shoved in over Hordaland in Cambro-Silurian times still remain, layer by layer, almost like a cake. But at Kvamskogen the cake has been turned upside down.

Vesoldo

Vesoldo

27.05.2018 - 15:02

Folds are to be found everywhere in the remains of the Caledonian mountain chain. Some were formed during the collision with Greenland, others stem from the time when the mountain chain collapsed. Few can compare with the giant fold that remains in the mountain area around Tørvikenuten, Vesoldo and Hellefjellet.

Ålmerket

29.03.2018 - 22:59

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