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Fossen cliff

Fossen Bratte

07.12.2018 - 09:36

The steep drop by Fossen cliff has been the biggest challenge for those who wished to make a road over Kvamskogen through the years. Leave the car by the monument on the old road and take a walk down to the bend by the waterfall that Bergen-folk call "The bridal veil". Why is there a waterfall just here?

Gneiss.

Frøland- Liarostunnel

16.06.2018 - 17:24

Soft shapes in the hard mountain.

Grasdalen

12.03.2018 - 13:08

Gullbotnen

Gullbotnen

07.12.2018 - 10:32

A barren belt where almost nothing grows, runs through the forest on the east slope of Gullbotnen. But, along the west side of the main road there is a fertile zone that flourishes with several finicky plant types. The contrasts arise from the extreme variations in the nutrient content of the bedrock.

Notaholmen, Samnanger

Notaholmen

16.06.2018 - 17:28

The fishnet shed at Notaholmen stands as a reminder of the days when people used to row out on the fjord to set their nets. On Notaholmen the nets were dried, repaired and tanned. And it was a great advantage to store them in a place inaccessible for rats and mice.

Innarsøyane toward Holmengrå.

Innarsøyene

31.03.2018 - 17:09

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

Smedholmen, Fitjar

Smedholmen

30.03.2018 - 20:10

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.

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