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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.

Main mine shaft in Valaheigruva mine.

Varaldsøy- mining

19.06.2018 - 16:13

There is still a lot of ore in the abandoned mines on Varaldsøy Island. If today's prices and availability of ore continue, it is doubtful whether the mines will resume operation. But, the pyrite is there, if the market should return. On Varaldsøy Island one finds at least nine mines and prospect pits, that for the most part date back to the latter part of the 1800s.

At lake Gaupåsvatnet.

Gaupås

19.05.2018 - 19:24

Troldhaugen, Bergen

Troldhaugen

29.03.2018 - 22:49

A zone with nuggets from the inner earth.

Drøna

12.03.2018 - 13:01

Sysendammen

Sysendammen

18.03.2018 - 07:59

Amateur geologist Torgeir Garmo at work taking out crystals from the rock.

Ågotnes- crystals

12.03.2018 - 13:07

Road cuts and blast areas are a joy to rock collectors, even if the disturbance to nature is ever so disfiguring. These are the best kinds of places to hunt for crystals, which otherwise are removed by weather and wind. In the Ågotnes area there are especially many beautiful crystals to be found.

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.

Section of the lid of the chest painted around 1830, by Nils Johannesson Tveiterås

Tveit

16.06.2018 - 17:28

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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