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From Upper Musland toward Geitadalen.

Ulvanosa

04.01.2019 - 11:02

Some mountains have rounded shapes, while others have steep slopes and sharp edges. Ulvanosa (1246 mos.) has both. The forms reflect the type of bedrock below, and the forces that were in effect when they were formed.

Garnes station

Garnes

12.06.2018 - 19:16

«Den Trondhjemske postvei»

Munkebotn

12.06.2018 - 19:18

A zone with nuggets from the inner earth.

Drøna

12.03.2018 - 13:01

Vinnesholmen, Fusa

Vinnesholmen

21.11.2018 - 19:25

Vegane gjennom den tronge og bratte Måbødalen

Måbødalen- road construction

26.05.2018 - 11:33

Workers

Lussand-roadwork

26.05.2018 - 11:43

The road along the north side of the Hardanger fjord - between Øystese and Eide in Granvin – was literally built “by hand”. The construction work started in February 1933, and on 9 October 1937 Crown Price Olav opened the stretch of road between Øystese and Ålvik at Fyksesund bridge.

The smallholding Træet, Askøy

Træet

30.03.2018 - 08:56

The bridge at Mørkhølen

Mørkhølen

13.12.2018 - 08:48

Geologists from all over the world come to study the veined bedrock (the dark stripe in the picture) at Spildepollen.

Spildepollen

07.12.2018 - 10:55

The oceanic crust of the North Sea was subjected to a lot of stretching both in Permian and Triassic times, and later in the Jurassic. This stretching resulted in the North Sea collapsing in and also to large faults forming west of Hordaland and on the mainland. Austefjorden in Sund follows one of these faults.

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