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Grunnosen

Grunnosen

31.03.2018 - 17:07

Pilot vessel at Fedje.

Fedje traffic office

19.05.2018 - 19:54

Innarsøyane toward Holmengrå.

Innarsøyene

31.03.2018 - 17:09

Bjørsvik

Bjørsvik

24.06.2018 - 15:41

The industrial settlement Bjørsvik

Tufted Ducks

Eikangervågen

31.03.2018 - 17:09

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.

Cirque in Dyrdal in Lindås

Dyrdal

13.12.2018 - 08:58

If you journey along Austfjorden, you at the same time turn the pages of time back through Ice Age history. The landforms show how the landscape has developed gradually as the glaciers have grown - and melted again - in several episodes: from small cirques, we see innermost at Dyrdal, to larger fjords, like at Mas fjord further out.

The south side of Raunøya.

Raunøya

31.03.2018 - 21:11

The sea birds discovered it long ago. Raunøya and the surrounding islands are the most beautiful places in Masfjorden.

Door

Trodalen

17.06.2018 - 16:37

Eclogite bedrock at Ådnefjellet.

Eldsfjellet

13.12.2018 - 09:04

The eclogites in western Norway were formed when Precambrian basement rocks were squeezed and pressed down under great pressure deep under the Caledonian mountain chain. The process may well have triggered some of the deepest earthquakes the world has ever known. The clearest traces of this drama are found in and around Mt. Eldsfjellet, in peaceful Meland.

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