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Elm - and lime tree

Andvikedalen

31.03.2018 - 19:56

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.

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.

Bronze keys and remains of a wooden stick from Døso.

Døso

16.06.2018 - 14:11

Blanks for bowls and ladles

Eidsbøen

13.03.2018 - 20:58

Where the school and the sports facility lie at Eidsbøen there was previously a bog surrounded by small hillocks. More than 1000 years ago this was a holy place, where the dead were buried.

Potholes by the Koldals River

Eikelandsosen

29.03.2018 - 11:29

"So many and such big potholes as are found at Eikelandsosen, we don't see other places in western Norway, and as beautifully polished as the mountainside is along the river up to Koldal , one would look a long time to see anywhere else. There is much to dazzle a geologist's eyes. If only these features could bring others the same joy!"

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.

Fana church, Bergen

Fana church

22.10.2019 - 17:00

In the Middle Ages the stone church in Fana was a place for pilgrimage, containing a miraculous silver crucifix that could heal the sick. A hill to the west of the church is still called Krykkjehaugen (the crutch hill); according to belief this is where the sick threw away their crutches. Perhaps this church, lying where it does at the old half county boundary , also held a special position in relation to the district churches in the county.

Fjøsanger road

19.05.2018 - 19:23

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