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The Halsnøy Boat

19.06.2018 - 16:25

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.

Troldhaugen, Bergen

Troldhaugen

29.03.2018 - 22:49

A zone with nuggets from the inner earth.

Drøna

12.03.2018 - 13:01

Drageidkanalen, Fusa

Drageid canal

20.03.2018 - 18:05

Turøyvarden, Fjell

Turøyvarden

29.03.2018 - 19:08

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.

Pilot vessel at Fedje.

Fedje traffic office

19.05.2018 - 19:54

Lindås locks at the beginning of the 1900s.

Spjutøy

16.06.2018 - 18:51

At Spjutøy and Straumsosen there are three entrances from Lurefjorden to the fjord basin inside. Right up the end of the 1800s the ferry could not reach further than to Mølna at Spjutøy. At Skallestraumen there was a bark mill driven by the powerful tidal current in the sound. Here was also a store, a bakery and a hostelry place around the middle of the 1800s.

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