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Fjøsanger

Fjøsanger

05.12.2018 - 13:49

Fjøsanger is known among ice age researchers from around the world. Under an excavation in 1975-77, geologists from the University of Bergen found layers from the last interglacial, ca. 115 000 to 130 000 years old.

Garnes station

Garnes

12.06.2018 - 19:16

«Den Trondhjemske postvei»

Munkebotn

12.06.2018 - 19:18

“The Trondheim post road” from Gaulen, Lindås.

Isdalstø

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.