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.

Halne

At Halnefjorden, a few hundred metres east of Halne mountain lodge, lie the remains of two stone sheds – Halnelægeret. Some generations ago the cattle drovers stopped here in the summer; they were the cowboys of their time. But Halnelægeret already had a long history before the cattle drovers came.

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.

Langavassfjellet

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.

The village of Etne

Much of the sand and gravel that the town of Etne is built on was laid down at the end of the Ice Age and is evidence of melting glaciers and roaring meltwater rivers. The uncompacted material in the big terraces leave their unmistakeable mark on the wide elongated valleys.

Støle church

The stone church at Støle may have been built around 1160 probably as a private chapel for the mighty Stødle clan. It is likely that it was Erling Skakke, the king’s representative and father of king Magnus Erlingsson, who built the church.

Skånevik- moraine

In Skånevik there are marks left from the ice edge that advanced during the thousand-year cold spell (Younger Dryas) that marked the end of the Ice Age roughly 11 500 years ago. The glacier first proceeded out into Åkra Fjordand and around Vannes and thereafter sent an arm in toward Skånevik. Here, the glacier lay down an end moraine up against the mountainside.