• Nynorsk
  • English

Universitetet i bergen logoUniversity of Bergen

Search form

Search form

Klokkarvatnet

Kalandsvatnet and Klokkarvatnet

03.08.2018 - 12:30

Nordåsvatnet (Helge Sunde)

Nordåsvatnet

12.06.2018 - 17:13

The Post-war Era came to Fana with its population growth and modern sanitary equipment. This had nearly catastrophic consequences for Nordåsvatnet as a recreational area. After the runoff water got re-directed to deeper water, and later also to the fjord outside, Lake Nordås won back both its swimming guests and its sports fishermen.

Store Lungegårdsvannet

Store Lungegårdsvannet

12.06.2018 - 17:14

Fra Blåmanen mot Vardegga og Ulriken.

Vidden

07.12.2018 - 14:19

Langavatnet, Åsane (Svein Nord)

Åsane

05.12.2018 - 18:44

Most associate Åsane with ridges, naturally enough (the Norwegian word for "ridge" is "Ås"). A lesser noticed trait in the landscape are the unusual flat areas that lie between the ridges. The Dalselva River, which was channeled at the end of the 1950s, runs down only 2.5 metres from Lake Langavatnet by Vågsbotn to Flatevad, where it goes over into rapids by Fossekleiva. The layers of gneiss stand nearly vertically, and the mountain surface is so even that one might think it had been planed with a planer.

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.

A silled lake at Ekse

Eksingedalen- hydropower development

13.12.2018 - 16:56

Water discharge at the outlet of the Ekso into Eidsfjord was halved after the big hydropower development in the mountainous area between Modalen and Eksingedalen and further southward toward Evanger in the 1960s, 70s and 80s. In an attempt to amend the changed environmental conditions in the waterway the developer built 35 small dams in the river.

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 the mountainous rocks just below Sandvikshytte cabin on Sandviksfjellet.

Sandviksfjellet

06.03.2019 - 15:22

On Sandviksfjellet there are old boulders that have been made into mountains. The stones have been stretched out or squeezed together between huge slabs of rock, during slow, but powerfulprocesses of transport. This conglomerate shows, in quite a special way, the enormous powers that were active during the collision between Norway and Greenland over 400 million years ago.

Svartediket med Vidden i bakgrunnen (Helge Sunde)

Isdalen

06.03.2019 - 18:12

The valley on the inside of the Svartediks dam, a five minutes' bus ride from Bergen centre, is often referred to by Bergen folk as Isdalen ("Ice Valley") - justifiably, since the area could have been described in textbooks for its ice-carved land forms. The glacier's polishing over ca. 40 ice ages has created a magnificient landscape. The original ice valley climbs up behind Ulriken at the end of Svartediket.

Pages