• Nynorsk
  • English

Universitetet i bergen logoUniversity of Bergen

Search form

Search form

Holo

Holo

07.03.2019 - 17:30

I Kvassdalen var det aktiv stølsdrift med mjølking av kyr og geitehald nokre år inn i vårt tusenår, og slik hadde det vore i meir enn to hundre år. Såleis har dalen ikkje fått gro til med kratt og skog, men er open og lys. Fortsett er det beiting av kyr og sauer.

Hana

Hana

12.03.2018 - 13:16

The potato cellar at Verastunet is still in good condition.

Verås

19.05.2018 - 19:58

Old pine forest in Husedalen.

Husedalen

27.05.2018 - 15:23

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.

Voss Spruce Toward Istad

Vossagran

06.05.2019 - 11:18

How did the spruce tree get to Voss? Did the seed or small spruce plants get help from people, for example, to make it here unscathed? Nobody knows.

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."

Slopes above the Kårdal boarding house

Mjølfjell

22.01.2019 - 13:49

Skreien

Skreien

12.03.2018 - 13:16

Kjerringafjellet

Bergsdalen

13.12.2018 - 15:03

The mountains of western Norway are lovely to wander in. In Cambro-Silurian time it was the mountain itself that wandered. The mountain, or more correctly the bedrock, first moved eastward, then back a bit westward again. All this rocking back and forth in the mountains ended about 400 million years ago.

Pages