• Nynorsk
  • English

Universitetet i bergen logoUniversity of Bergen

Search form

Search form

Toward Støle and Sørheim, 1920.

The village of Etne

18.12.2018 - 20:39

Much of the sand and gravel that the town of Etne is built on was laid down at the end of the Ice Age and is evidence of melting glaciers and roaring meltwater rivers. The uncompacted material in the big terraces leave their unmistakeable mark on the wide elongated valleys.

Boat engines, Norwegian Engine Museum in Skånevik

Skånevik- Norwegian engine museum

25.04.2018 - 21:25

Botnavatnet

Botnavatnet

29.03.2018 - 12:00

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.

Today there are only a few farmers that grow potatoes in Fitjar.

Fitjar- potatoes

19.12.2018 - 18:18

The deep agricultural soils in Fitjar are found especially in the area between Lake Storavatnet and Breivika. The many stonewalls in the area reflect that the earth probably was full of stones and stone blocks. The stones that couldn't be dug out had also a function: they stored heat that helped to grow potatoes.

Strandflat and scree by land

Landa

19.06.2018 - 16:06

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.

Den flate terrassen på moreneryggen på garden Tjedla viser kor høgt havet stod på slutten av den siste istida.

Skånevik- moraine

06.03.2019 - 14:58

In Skånevik there are marks left from the ice edge that advanced during the thousand-year cold spell (Younger Dryas) that marked the end of the Ice Age roughly 11 500 years ago. The glacier first proceeded out into Åkra Fjordand and around Vannes and thereafter sent an arm in toward Skånevik. Here, the glacier lay down an end moraine up against the mountainside.

Foglefonna and Sandvikedalen with Hardangerjøkulen in the distance.

Mosnes

12.03.2019 - 15:46

The permanently-protected Mosneselva River, with its meltwater from Folgefonna, runs out into Åkra Fjord by the roadless and uninhabited Mosnes. Those who once lived here were forced to surrender to the ravages of Nature. In the autumn of 1962 there was a flood so great that the people were driven from their farms.