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The Hopland mills around 1940.

Kvernhusvågen

30.03.2018 - 09:08

Statue of Magnus Erlingsson by the Town Hall in Etne.

Støle

19.05.2018 - 20:53

High above the sea and the beach flats, on one of the wide terraces shaped by the sea and the ice, lies the farm Støle (Stødle). The Old Norse name of Studla is derived from studill “support, shelf”. As far back as Viking times Støle has been a chieftain’s farm, a good farm on the plains formed by the moraine masses.

The wheelhouse at Hovdanes, Tysnes

Hovdanes

30.03.2018 - 20:24

Nils Hertzberg watercolour of “Spånheimsklosteret”

Sponheim

27.05.2018 - 15:52

King Sverre in the snowstorm in the Voss Mountains, 1870.

Sverrestigen

19.06.2018 - 17:48

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.

The mill in Kvernapollen

Kvernapollen

16.06.2018 - 18:29

When the workers came to Kollsnes to start on the work with the landing for the gas terminal from the Troll field in the North Sea, they found the ruins of an old farm mill at Kvernapollen.

Ask- The king's estate

12.06.2018 - 16:56

The saw tooth pattern is clearly visible from Skora Mountain southwards toward Tellnes and Skogsvågen.

Haganes

12.06.2018 - 19:59

The gneiss landscape west and north of Bergen viewed in profile can remind us of a saw blade of the kind that has long, slanted sides that get broken off shorter transverse sides. It has taken several hundred million years to file this saw blade, an enduring interplay between various geological processes.

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