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.

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.

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

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.

Holmeknappen

If you come by sea to Bergen and come up the Herdle Fjord, the yellow ochre marine shed at Holmeknappen is a well known landmark to starboard as you come close to the little shore settlement. In olden days Holmenknappen served important functions as a centre for a wide hinterland of the surrounding farms, warehouse, landing point, country store and later a steamer quay, a hotel (1896) and a dairy (1909). But today Holmeknappen is no longer a focal point. Transport and commercial routes have changed the old pattern