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The longhouse at Førland

Førland

21.11.2018 - 19:36

The extended farm dwelling at Hopland

Hopland

03.01.2019 - 15:24

The farmhouses at holding No. 15 at Hopland are built together to form a long, continuous building, with dwelling house, hayshed and cowshed built in one row. There have been many such joined structures in the coastal communities, but today there are few remaining. If we travel to the other side of the North Sea, to the Faeroes, Shetland and the Orkney Islands, we find corresponding features in the older building traditions. We find ourselves in a large North Atlantic cultural area.

The marine use environment on Krossøy, Austrheim

Krossøy

16.06.2018 - 18:32

Furthest north in the island community Rongevær, at the entrance to Fensfjorden, lies Krossøy. Belonging to the farm are the islands of Krossøy, Husøy, Kårøy, Lyngkjerringa, Søre Kjerringa, Rotøy and Kuhovet. All of them have been inhabited. On Krossøy itself today there are four holdings. The marine use environment here is one of the best preserved along the West Norwegian coast.

The Hopland mills around 1940.

Kvernhusvågen

30.03.2018 - 09:08

Drawing: longhouse, Sætre

Sætre

16.06.2018 - 18:35

Bjørsvik

Bjørsvik

24.06.2018 - 15:41

The industrial settlement Bjørsvik

Isdalstunet, Lindås

Isdal

16.06.2018 - 18:48

Isdal one of the few clustered settlements left in the Hordaland communities, after the extensive changes taking place around the turn of the former century, which broke up the shared farms and the old intermixture of strips. The old, low houses are situated in a compact enclosure, which is very noticeable in the landscape when you travel the main road north from Knarrvik.

The longhouse at Litleoksa

Litleoksa

16.06.2018 - 18:48

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.

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