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Sculptures in the bedrock

Herand- geologi

11.12.2018 - 14:12

Hereiane. Jonahornet in the background.

Hereiane

26.05.2018 - 16:24

At Hereiane on warm summer days one you can walk barefoot up the hill from the fjord all the way up to 400 metres elevation. The naked, furrowed bedrock often causes travellers who see it from the north side of the fjord to wonder. Why does it look like this, and why is there so little that grows here? It is a long way to the heavy metal industry in Ålvik and Odda, and there hasn’t been a forest fire in modern times.

Skytjedalen in Eidfjord.

Skytjedalen

03.01.2019 - 14:57

Sysendammen

Sysendammen

18.03.2018 - 07:59

Potholes

Hausberget

31.03.2018 - 21:20

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.

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.

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.

Kvamskogen, toward the north.

Kvamskogen

02.12.2018 - 20:57

The different bedrock types that got shoved in over Hordaland in Cambro-Silurian times still remain, layer by layer, almost like a cake. But at Kvamskogen the cake has been turned upside down.

Vesoldo

Vesoldo

27.05.2018 - 15:02

Folds are to be found everywhere in the remains of the Caledonian mountain chain. Some were formed during the collision with Greenland, others stem from the time when the mountain chain collapsed. Few can compare with the giant fold that remains in the mountain area around Tørvikenuten, Vesoldo and Hellefjellet.

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