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Elias Fiigenschoug’s painting of Halsnøy monastery , 1656

Halsnøy Monastery

19.06.2018 - 16:12

Halsnøy Monastery is situated in the midst of the lush fjord country in Sunnhordland, on one of the old spits, or “necks”, that has given name to the island. Gently sloping fields lead down to the sea on both sides, in the south towards the Kloster Fjord, to the north towards the sheltered Klostervågen.

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.

Klosteret

12.06.2018 - 19:10

A zone with nuggets from the inner earth.

Drøna

12.03.2018 - 13:01

Vinnesholmen, Fusa

Vinnesholmen

21.11.2018 - 19:25

Sysendammen

Sysendammen

18.03.2018 - 07:59

Nils Hertzberg watercolour of “Spånheimsklosteret”

Sponheim

27.05.2018 - 15:52

The smallholding Træet, Askøy

Træet

30.03.2018 - 08:56

Frøland power station and lake Frøland.

Frøland

18.03.2018 - 08:03

Much rain, a steep drop and nearness to Bergen meant that the power-making potential of the Samnanger water system was exploited early. Samnanger was thus one of the first power-producing municipalities in western Norway. With its subsequent expansion and new power stations, about 400 gigawatts of electricity per hour were produced on average each year. This is enough to meet the energy needs of 25,000 households.

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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