Agastølen

Whoever wanders the mountain plateau will form time to time hit upon old mountain summer farms, with solid old stone sheds, half sunk into the ground; a building tradition that has roots into prehistoric times. When we have been satiated with untouched Nature, it is somewhat comforting to come upon the old mountain chalets - they represent a type of human encroachment that we not only accept, but appreciate. They arouse a feeling of recognition and are a distinct witness to how people in the rural communities have made use of even the most remote resources.

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.

Heggjagarden

The transport exchange on the farm Vik in Eidfjord was an important part of the communication network in older times. This is where people secured transport by boat out in the fjord, those travelling across the mountain from east and down into Måbødalen. The transport exchange was situated at “Wiige grund”. Today the highway cuts through the farmyard; the main farmhouse from the 1800s lies on the upper side of the road, the large sea-house, with a bakery in former times, lies close to the fjord.

Måbødalen- road construction

Sysendammen

Hallingskeid

Jomfrunuten

Freezing and thawing are processes that influence plant cover, move enormous blocks, stretche long mounds of earth, break open bedrock and create patterns in stone and earth.

Ulvik church

Hernar

Hernar is a small group of islands northwest of Seløy, an old outlying harbour on the western route. This is where ships were lying in wait for favourable weather before heading out west, and this is where the ships from the western Isles came in. Hjeltefjorden is proof of this. The fjord is named after the people from Hjaltland (Shetland).

Toftestallen

The large coastal waves that crash down on the islands west in the sea gather their energy from storms and winds all the way out in the North Atlantic Ocean. The most common place of origin is nonetheless the North Sea. When these waves break over the skerries and islets along the shore, or on the rocky outermost islands, their energy is released. This takes the form of turbulence in the water and sea spray up on land. Can the enormous energy contained in the waves be exploited?