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.

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.

Skytjedalen

Sysendammen

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.

Dale power station

In 1923 Bergenshalvøens Kommunale Kraftselskap (BKK) expropriated large areas for power plants and development of hydropower started soon afterwards. Dale power station with the two first aggregates, each of 14 MW was put into operation on 17 November 1927. In the supply reservoir in Storefossen 5152 cubic metres of concrete were cast, and a modern and well-equipped power station was built.

Eksingedalen- hydropower development

Water discharge at the outlet of the Ekso into Eidsfjord was halved after the big hydropower development in the mountainous area between Modalen and Eksingedalen and further southward toward Evanger in the 1960s, 70s and 80s. In an attempt to amend the changed environmental conditions in the waterway the developer built 35 small dams in the river.

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.