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Innarsøyane toward Holmengrå.

Innarsøyene

31.03.2018 - 17:09

Kræmmerholmen photographed in early 1900.

Kræmmerholmen

16.06.2018 - 18:44

Kræmmerholmen is one of the old privileged trading posts. From the 1600s all trading in West Norway took place in Bergen, and the farmers were obliged to travel into town in order to sell their produce and buy what they needed. In Bergen City Privilege of 1702 the merchants in the city were allowed to establish “Trading posts in the countryside”. The owner had to have residency in Bergen and the trading post was to be run by an assistant. In this way the city retained financial control of those living in the districts, and not least with buying and selling of fish.

Aksnesholmane

Aksnesholmane

26.05.2018 - 16:30

There are especially many seabirds inwards along the fjords of western Norway. There are not many islets, either, so if the birds want to nest, it is not always easy to find good sites. At Aksnesholmane there is an impressive colony of gulls, and the locality has been protected since 1923.

Bruosen

Bru

26.05.2018 - 16:33

Bruosen is one of the few river harbours in the county. As landing place for the churchgoers, this place and the boatshed environment follow a tradition that goes back to the Middle Ages, but the country store of today is much younger.

Fykse

Fykse

29.03.2018 - 11:55

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.

Rockslide at Mundheim in the spring of 1997

Mundheim

26.05.2018 - 16:36

At Mundheim there is a dangerous stretch of the highway. The mountainside has given way several times in this area. Typically, it happens in the spring, when the frost has loosened its grip.

Sandven hotel

Sandven

26.05.2018 - 16:39

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.