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The rock carvings at Bakko.

Bakko

26.05.2018 - 11:18

Everyone knows the famous painting by Tidemand & Gude “Brudeferden i Hardanger” (The Wedding Party in Hardanger) one of the great icons in the National Gallery. Some have, in a humorous lack of respect for this masterpiece linked the concept of “bride’s passage” to another pictorial presentation in Hardanger. This is found on the farm Bakko in Herand, carved in the rock by an unknown artist around 3,000 years ago.

Bergesfjellet

Bergesfjellet

12.03.2018 - 13:17

Kjerringafjellet

Bergsdalen

13.12.2018 - 15:03

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.

Bjørsvik

Bjørsvik

24.06.2018 - 15:41

The industrial settlement Bjørsvik

Glacier fall at Bondhusbreen.

Bondhusdalen

19.12.2018 - 19:25

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 - 12:00

Buardalen and Buarbreen before 1880.

Buardalen Valley

24.06.2018 - 15:34

Buarbreen glacier was one of the first destinations during the period of increasing tourism in Odda in the 1800s. Foreigners came by the thousands, mostly Englishmen and Germans, to the magnificent landscape in front of the glacier. Back at the hotel in Odda they could enjoy drinks containing ice from the glacier.

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.

Flatekvål

Eksingedalen- landscape

13.12.2018 - 17:06

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 - 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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