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The contrast between phyllite and Precambrian basement is clearly visible at Lussand.

Lussand- geology

30.11.2018 - 12:16

Hardangerfjorden kløyver Hordaland i to. Den etter måten rettlinja fjorden skjer seg liksom på skeive inn i landet. Ikkje som Sognefjorden og Nordfjord – dei krokar og buktar seg innover meir eller mindre vinkelrett på kysten. Hardangerfjordens utforming har røter 400 millionar år tilbake i tida, då den veike sona i fjellet, der isen seinare tok grådig for seg, vart danna. Denne sona stig på land ved Lussand.

Storegraven and Granvin church

Storegraven

26.05.2018 - 11:46

The first mention of Granvin church in written sources is in 1306, but the church location must be far older than this. The farm Storegraven is centrally situated at Granvinsvatnet, by the important traffic artery between Hardanger and Voss, where the road takes off to Ulvik.

Glacial river plain at Lake Klevavatnet.

Rallarvegen

04.12.2018 - 14:30

They rest there, all as one, the silent witnesses of Western Norway's saga of creation: Precambrian basement, phyllite and thrust sheet. In the end came the glaciers and sculptured the vast landscape. Along the ground or on the horizon, from bicycle or on foot - the landscape tells its story - and it tells it clearer on Rallarvegen than many other places.

Nils Hertzberg watercolour of “Spånheimsklosteret”

Sponheim

27.05.2018 - 15:52

The cross church from 1710

Ulvik church

27.05.2018 - 15:54

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.