- Remove Small landforms filter Small landforms
- Remove Basement rocks filter Basement rocks
- Remove Nordhordland filter Nordhordland
- Remove Large landforms filter Large landforms
- Remove Voss (tidl. kommune) filter Voss (tidl. kommune)
- Remove Quarries filter Quarries
- Remove Tourism filter Tourism
- Remove Farm sites filter Farm sites
![The longhouse at Førland](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_304-2.jpg?itok=ZjuFC_Ry)
![The extended farm dwelling at Hopland](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_304-1.jpg?itok=ird44EKf)
Hopland
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](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_305-1s.jpg?itok=b8MlF38y)
![Isdalstunet, Lindås](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_312-isdal.jpg?itok=xIVDv9Tm)
Isdal
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](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_314-2s.jpg?itok=HHEx49Ww)
![Lurøyane](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/lindas_26.jpg?itok=20iNP_Fs)
![Barn with stone end wall](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_321-5.jpg?itok=3i5jhWB2)
![Cirque in Dyrdal in Lindås](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/mas_22.jpg?itok=YmoL_BEr)
Dyrdal
If you journey along Austfjorden, you at the same time turn the pages of time back through Ice Age history. The landforms show how the landscape has developed gradually as the glaciers have grown - and melted again - in several episodes: from small cirques, we see innermost at Dyrdal, to larger fjords, like at Mas fjord further out.
![The “Bualoft” at Kjetland from the 1600s or 1700s.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_319-1.jpg?itok=P91sL-0S)
![Eclogite bedrock at Ådnefjellet.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/meland_21.jpg?itok=W8PmuPzd)
Eldsfjellet
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.