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Bergesfjellet

Bergesfjellet

12.03.2018

Kjerringafjellet

Bergsdalen

13.12.2018

The mountains of western Norway are lovely to wander in. In Cambro-Silurian time it was the mountain itself that wandered. The mountain, or more correctly the bedrock, first moved eastward, then back a bit westward again. All this rocking back and forth in the mountains ended about 400 million years ago.

Glacier fall at Bondhusbreen.

Bondhusdalen

19.12.2018

The Bondhus area in Maruanger has been a magnet for tourists ever since the stream of tourists to Norway's west coast began in the middle of the 1800s. The magnificent landscape with the "ice trail" up to Bondhusvatnet Lake, the ice falls from Bondhusbreen glacier and Keisarstigen trail up to Folgefonna are still popular tourist attractions.

Botnavatnet

Botnavatnet

29.03.2018

Cirque in Dyrdal in Lindås

Dyrdal

13.12.2018

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.

Flatekvål

Eksingedalen- landscape

13.12.2018

Eksingedalen alternates between wide, flat flood plains with good farmland, and narrow passages with waterfalls where the roads cling to the mountainsides. The alternations in the landscape are a result of the sculpturing work by glaciers over several ice ages, and the deposition of the glacial river deposits when the last glacier finally melted back.

Eclogite bedrock at Ådnefjellet.

Eldsfjellet

13.12.2018

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.

Section from a sea map from the Danish Sea Map Archive from 1798, drawn by Poul Løvernørn.

Fitjarøyane

18.06.2018

If we study the group of islands south of Selbjørns Fjord from the air or on a sea map, we will notice that many of the islands are elongated and lie systematically in rows. The islands are divided by long sounds, for example Trollosen, Nuleia and Hjelmosen, which are oriented in a south-southeast to north-northwesterly direction.

Rosemåling

Frette

06.03.2019

Gjønavatnet and Kikedalen

Gjønavatnet and Kikedalen

16.06.2018

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