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Reconstruction sketch of the yard at Høybøen, Fjell

Høybøen

12.06.2018 - 20:00

In connection with the planned developments in the oil sector at Vindenes around 1980, excavations were carried out under the auspices of Bergen Historical Museum. Exceptionally interesting traces of an old farm at Høybøen then came to light. These were the remnants of a farm where there had been two houses containing several rooms.

The bridge at Mørkhølen

Mørkhølen

13.12.2018 - 08:48

The combination building at Nordvik.

Nordvik

16.06.2018 - 17:27

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.

Lyngoksen

Lyngoksen

31.03.2018 - 19:54

Drawing: longhouse, Sætre

Sætre

16.06.2018 - 18:35

The old communal hamlet before 1910.

Dale farm

18.06.2018 - 20:10

The Dale farm lies well situated on the gravel by the river, below the mountain Beitelen. But a few stone throws further north, on the wide expanse behind the houses, there has been an older farmstead. Here there have been found a number of cooking hollows, pole holes, an old road and traces of something believed to have been a palisade. Finds from this oldest farmstead may be dated to the time of the migrations, 400-600 years A.D.

The road Stamnes-Eidslandet

Dalseid- Eidslandet road construction

25.04.2018 - 20:57

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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