Dalseid- Eidslandet road construction

Straume- maritime environment

Kvalvågen

Sætre

Førland

Landsvik

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.

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.

Gullbrå

From written sources we know that the farm Gullbrå was in use early in the 1600s. The Apostolic church in Bergen owned land here that it rented out, but even early in the 1600s some of the land was in private ownership. Eksingedalen then belonged to Modalen parish, which was under Hamre parish. In 1723 the Apostolic church still had properties here, and Ivar and Lars were farmers.