• Nynorsk
  • English

Universitetet i bergen logoUniversity of Bergen

Search form

Search form

The Hopland mills around 1940.

Kvernhusvågen

30.03.2018 - 09:08

Pilot vessel at Fedje.

Fedje traffic office

19.05.2018 - 19:54

Bjørsvik

Bjørsvik

24.06.2018 - 15:41

The industrial settlement Bjørsvik

Lindås locks at the beginning of the 1900s.

Spjutøy

16.06.2018 - 18:51

At Spjutøy and Straumsosen there are three entrances from Lurefjorden to the fjord basin inside. Right up the end of the 1800s the ferry could not reach further than to Mølna at Spjutøy. At Skallestraumen there was a bark mill driven by the powerful tidal current in the sound. Here was also a store, a bakery and a hostelry place around the middle of the 1800s.

Cirque in Dyrdal in Lindås

Dyrdal

13.12.2018 - 08:58

If you journey along Austfjorden, you at the same time turn the pages of time back through Ice Age history. The landforms show how the landscape has developed gradually as the glaciers have grown - and melted again - in several episodes: from small cirques, we see innermost at Dyrdal, to larger fjords, like at Mas fjord further out.

Eclogite bedrock at Ådnefjellet.

Eldsfjellet

13.12.2018 - 09:04

The eclogites in western Norway were formed when Precambrian basement rocks were squeezed and pressed down under great pressure deep under the Caledonian mountain chain. The process may well have triggered some of the deepest earthquakes the world has ever known. The clearest traces of this drama are found in and around Mt. Eldsfjellet, in peaceful Meland.

Two of the rowlocks which have been found in the bogs Mangersnes, Radøy

Mangersnes

18.06.2018 - 20:07

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.