Arnatveit

On the farm of Arnatveit, high up on the slope above the highway, an old smokehouse remains standing in the courtyard of the main farm property, in the place of the old common courtyard. Today this farm lies at the outskirts of a large housing estate. Most of the farmland of the other farm properties has been sold to benefit the city’s need of sites for the new community of Arna.

Bergenhus

Bergsdalen

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.

Bryggen

In the 1300s Bergen was a trading centre of European dimension. The town is thought to have had around 7000 inhabitants and was the largest and most important in the country. In a European context it was an average size town. At this time the most tightly built town area was still mostly east of Vågen from Holmen in the north to Vågsbotn in the south. Already in medieval times, latest in the 1340s, this area was called Bryggen.

Dalseid- Eidslandet road construction

Domkirken

Dyrdal

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.

Eikelandsosen

"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!"

Eksingedalen- landscape

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.

Eldsfjellet

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.