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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.

Drawing: longhouse, Sætre

Sætre

16.06.2018 - 18:35

Hellisøy lighthouse, Fedje

Hellisøy

16.06.2018 - 18:43

Hellisøy lighthouse was lit for the first time in 1855. The characteristic red cast-iron tower with two white belts is 33m high and a light height of 46m above high tide.

Holmengrå

Holmengrå

07.12.2018 - 12:45

Holmengrå is the only place in Hordaland where we find traces of the abrasion that is supposed to have transformed Western Norway from a Himalaya-like high mountain landscape during the earth's Paleozoic Era, to a flat lowlands terrain during the Mezosoic Era. Just 400 million years ago, large and small stones plummeted down from the high mountains. Some of these stones became incorporated into the conglomerate bedrock on Holmengrå.

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

Barn with stone end wall

Andviki

19.05.2018 - 19:59

The “Bualoft” at Kjetland from the 1600s or 1700s.

Kjetland

17.06.2018 - 16:34

Eclogite bedrock at Ådnefjellet.

Eldsfjellet

13.12.2018 - 09:04

The eclogites in western Norway were formed when Precambrian basement rocks were squeezed and pressed down under great pressure deep under the Caledonian mountain chain. The process may well have triggered some of the deepest earthquakes the world has ever known. The clearest traces of this drama are found in and around Mt. Eldsfjellet, in peaceful Meland.

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