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The Halsnøy Boat

19.06.2018

From Upper Musland toward Geitadalen.

Ulvanosa

04.01.2019

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.

A zone with nuggets from the inner earth.

Drøna

12.03.2018

Drageidkanalen, Fusa

Drageid canal

20.03.2018

Turøyvarden, Fjell

Turøyvarden

29.03.2018

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

Spildepollen

07.12.2018

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

Lindås locks at the beginning of the 1900s.

Spjutøy

16.06.2018

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.

Manger

Manger

18.06.2018

Mangerite is a rock type that was first made famous in a treatise by the Bergen geologist Carl Fredrik Kolderup in 1903. The rock type got its name from the place where it was found, and has made the Mangerud name well known around the world, at least among geologists.

Two of the rowlocks which have been found in the bogs Mangersnes, Radøy

Mangersnes

18.06.2018

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