• Nynorsk
  • English

Universitetet i bergen logoUniversity of Bergen

Search form

Search form

Barn with stone end wall

Andviki

19.05.2018 - 19:59

The “Bualoft” at Kjetland from the 1600s or 1700s.

Kjetland

17.06.2018 - 16:34

The south side of Raunøya.

Raunøya

31.03.2018 - 21:11

The sea birds discovered it long ago. Raunøya and the surrounding islands are the most beautiful places in Masfjorden.

Stordalen

Stordalen

14.02.2019 - 14:39

When the Etne water system was protected in 1994, preservation of the cultural landscape in Stordalen Valley was a a main objective. This is a valley with an exceptional abundance of Different types of plants and animals. In the grey alder forest in Stordalen there are more bird species than in most other places, in fact, denser than one tends to find in a tropical rainforest.

Section from a sea map from the Danish Sea Map Archive from 1798, drawn by Poul Løvernørn.

Fitjarøyane

18.06.2018 - 20:30

If we study the group of islands south of Selbjørns Fjord from the air or on a sea map, we will notice that many of the islands are elongated and lie systematically in rows. The islands are divided by long sounds, for example Trollosen, Nuleia and Hjelmosen, which are oriented in a south-southeast to north-northwesterly direction.

Strandflat and scree by land

Landa

19.06.2018 - 16:06

Liarbø, Fitjar

Liarbø

19.06.2018 - 16:07

Smedholmen, Fitjar

Smedholmen

30.03.2018 - 20:10

The farm steading of Årskog.

Årskog

19.06.2018 - 16:08

Årskog farm is situated in a typical coastal landscape in a gentle terrain that slopes down from the outlying heaths down towards the fjord. The farm steading exists as it was in the 1800s. In 1980 the two brothers, Lars and Olai Årskog donated the farm with all its contents of tools and interior decoration, for museum purposes.

Espevik

Espevik

03.01.2019 - 15:26

220 million years ago, glowing hot molten rock masses intruded into fractures in the earth's crust in the outer parts of Hordaland. Some of these are believed to have reached the surface and formed lava flows, which since have been eroded away by wind and weather. But, most of these flows solidified into diabase sills before they got to the surface.

Pages