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.

Bondhusdalen

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.

Dale

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.

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.

Hjølmo

In the steep hillside in Hjølmodalen, a small side valley from Øvre Eidfjord (Upper Eidfjord), which has been a key entrance to the Hardanger Plateau, the hamlet of old farmhouses still lie clustered together. The yard is empty today, some of the houses are used in the summer, but the grass grows round all the corners.

Kjeåsen

High up above the fjord, at a height of 600m lie the two holdings at Kjeåsen. Today you can drive there by car, through a new tunnel that the power engineers in Sima have drilled. Until 1974 the only road went up the steep hillside, along iron bolted ladders across dizzying rocks – a road for the strong at heart.

Melderskin

MELDERSKIN - ONCE A NUNATAK? Melderskin, the towering and majestic landmark at Rosendal, rises 1462 metres above sea level. The top area is smooth, but slightly inclined. Geologists think that the area is a remnant of a weakly undulating landscape, that originated near the sea, long before the Ice Age set in.

Måbø

Måbø is the uppermost farm in Måbødalen. This narrow and steep mountain valley has been one of the routes from the fjord communities up to the mountain plateau from times immemorial. We are not certain of the meaning of the name Måbø. Perhaps it has its origin in an Old Norse male name Mávi, from the name for seagull, már. The last syllable “bø” means farm. Today Måbø gives us a compact close-up of the subsistence economy: the small farm with the clearance piles, stone walls and a lane that guided the animals into the yard, at the foot of the great mountain expanse.

Måbødalen- geology

The old pack road had 1500 steps, where cars today gas through the mountain. The time of this hard work is over, and of getting used to the steep terrain, as well; only the view from the top is much the same as before. Vøringsfossen in summer is one of Western Norway’s biggest natural wonders. It marks the transition between the older, open part of the Sysendalen valley and the younger, narrow and winding valley of Måbødalen.