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Botnagrenda

Botnen

26.05.2018 - 16:32

Fyksesundet and Botnagrenda present a fine experience of the landscape and cultural history; a geographically isolated local settlement with extensive cultural contact with the outside world.

The soil tongues below Jomfrunuten.

Jomfrunuten

03.12.2018 - 14:13

Freezing and thawing are processes that influence plant cover, move enormous blocks, stretche long mounds of earth, break open bedrock and create patterns in stone and earth.

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.

Nestunet by Nesvatnet.

Nes

13.12.2018 - 08:30

The farm Nes lies directly inside Mundheim on a forested headland in the fjord between Mundheimsvika and Bondesundet, a farm with an attractive and well-kept cultural landscape.

Osa and the Osa fjord

Osa

01.05.2018 - 17:06

At the bottom of the Osa fjord there is a cultural landscape marked by great contrasts; the wide terraces and the river delta at the fjord contrast with the steep hillsides in the background, where Norddalen leads up to the mountain. There are two farms here. Osa and Sævartveit – the farm at the river mouth and the hollow by the sea.

Romarheimsdalen

Romarheimsdalen

29.03.2018 - 11:38

The geology along Oster Fjord and further eastward, in cross-section and on the surface. (Haakon Fossen)

Stall

11.12.2018 - 14:43

The Bergen Arcs have an unusually sharp boundary to the bedrock in the east. Geologists think that this was caused by movements in the earth's crust during the Devonian Period. Then, the Bergen Arcs on the Lindås peninsula sank a whole 10 kilometres in relation to the Precambrian basement gneisses on the east side of Fens Fjord and Aust Fjord.

The potato cellar at Verastunet is still in good condition.

Verås

19.05.2018 - 19:58