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Fruo
At Fruo, nature has built its own little "Chinese wall ". Some kilometers south of the Vøringsfossen waterfall, there are a number of moraine ridges, the longest and most notable of their kind in Hordaland.
Hæreid- geology
The Eidfjord terrace is a gigantic ridge that reaches up more than one hundred metres from the city centre in Eidfjord. It serves as a powerful natural monument left behind by the ice when it retreated.
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.
Langavassmyrane
The Ruff lek on Langvassmyrane is the only known phenomenon of its kind on Hardangervidda. Every year it attracts hens from the whole plateau. The marsh is also the richest wetland in the county. This green oasis is located in a rocky moraine landscape a few hours walking distance south of Dyranut.
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.
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.