• Nynorsk
  • English

Universitetet i bergen logoUniversity of Bergen

Search form

Search form

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.

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.

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.

Ygre Station around 1920.

Ygre

06.06.2020 - 13:13

Ygre Station lies hidden away for highway travellers, just below the road Vossevangen-Mjølfjell. The station building at Ygre was constructed at Nesttun station in 1879-80. Almost all the stations at the Voss railway were identical. The architect was Balthazar Lange, and the type was called subsidiary station No.4. It is built in the Swiss style, as fashion of the times demanded.