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Potholes

Hausberget

31.03.2018 - 21:20

Klokkarvatnet

Kalandsvatnet and Klokkarvatnet

03.08.2018 - 12:30

Sculptures in the bedrock

Herand- geologi

11.12.2018 - 14:12

Skårsvatnet

Skårsvatnet

26.05.2018 - 23:34

In September, 1901, a load of golden orfe fish was transported from Preussen to Bergen for stocking of Nygårdspark. One of the originators of the project was the well known doctor Klaus Hanssen. Thirteen years later, Hansen was called to help. Would he please come to Øystese to assist the district doctor Peter Munch Søergaard in his attempt to combat tuberculosis in the village? Hanssen came - and had in his suitcase living "goldfish" from Nygårdsparken.

The soil tongues below Jomfrunuten.

Jomfrunuten

03.12.2018 - 14:13

Freezing and thawing are processes that influence plant cover, move enormous blocks, stretche long mounds of earth, break open bedrock and create patterns in stone and earth.

Bordalsgjelet

Bordalsgjelet

13.01.2019 - 13:52

Deep down between the stone polished phyllite bedrock in Bordalsgjelet canyon, there is a cascading river. In close cooperation with hard polishing stones, the water has carved into the bedrock for thousands of years - and is still doing so today.

Hellandsfossen

Hellandsfossen

31.03.2018 - 21:13

Lonelva

Lonelva

18.06.2018 - 20:02

It is said that the salmon populations with the largest and the smallest salmon in the world both come from the waters that run out into the fjord system around Osterøy. Vosso is supposed to have the largest spawning salmon to be found in any river, whereas Lonelva is said to have the smallest.

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.

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