• Nynorsk
  • English

Universitetet i bergen logoUniversity of Bergen

Search form

Search form

Garnes station

Garnes

12.06.2018 - 19:16

At lake Gaupåsvatnet.

Gaupås

19.05.2018 - 19:24

Marmorøyen

05.12.2018 - 16:24

Stend station in 1935

Stend station

12.06.2018 - 19:19

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.

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.