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Stone quarry in Kollevågen, 1922

Hanøy

12.06.2018 - 16:56

Shelduck.

Herdleflaket

05.12.2018 - 10:11

Spring, summer and autumn, there is bird life on Valen, and the tidal zone is especially attractive. Out on Herdlaflaket, you see ducks and other diving birds all year round, but most in winter.

The smallholding Træet, Askøy

Træet

30.03.2018 - 08:56

Bjørsvik

Bjørsvik

24.06.2018 - 15:41

The industrial settlement Bjørsvik

Tufted Ducks

Eikangervågen

31.03.2018 - 17:09

The sites show the longhouse, a smaller “old folk’s house” and a hayshed.

Lurekalven

07.12.2018 - 18:51

Lurekalven is an unpopulated island of heather moor which is a part of the wilderness belonging to the five farms on Ytre Lygra. Between the two islands there is only a small sound. As late as the 1920s, milking cows were rowed over the sound from Lygra in summer – a form of farming that was adapted to the coastal landscape.

Burning heath

Lygra

16.06.2018 - 18:50

The heath landscape on outer Lygra, Utluro and Lurekalven will in future become part of a landscape protection area, to be maintained through traditional activities with year-round outdoor sheep, grazing and burning. The West Norwegian heath country belongs to a large North Atlantic coastal landscape stretching from the Bay of Biscay to the Lofoten islands.

The potato cellar at Verastunet is still in good condition.

Verås

19.05.2018 - 19:58

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.

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.

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