Herandsholmen

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.

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.

Granvinsvassdraget

After the ice age, Granvin Fjord reached all the way up under Skjervsfjossen waterfall. Just a thousand years later, as a result of the rising of the land after the ice melted, this whole inner part of the fjord freed itself of the sea and became Granvinsvatnet lake. In spite of this rise in elevation, this waterway is still navigable for fish: Sea trout have wandered into Granvinsvatnet in more recent times and evolved to become freshwater trout. And salmon and sea trout made the journey 13 kilometres up the Storelvi river.

Kjerland

On the farms Kjerland and Røynstrond, east of the river that flows into the fjord, we find many decorative painters who belong to the so-called sòlekistemålarane in Hardanger: Knut and Mikkjel Røynstrand and Johannes Jonsson Kjærland.

Kongstun

In the Middle Ages the farmers were under obligation to transport state officials. The bishops were entitled to 18 horses when they travelled about on visitations, and the king could requisition free transport.

Bergensbanen

Already at the beginning of the 1870s demands were made that there had to be a railway connection between Bergen and East Norway. The first section between Bergen and Voss was finished in 1883. The route alternatives further on were many: Lærdal-Valdres, Aurland-Geiteryggen, Raundalen-Finse and Ulvik-Finse. Following a long dispute, an agreement was finally reached that the middle route alternative, Raundalen- Myrdal- Finse, was the best alternative. In 1894 the government passed a resolution that the Bergen railway should be built, but only the section Voss-Taugevatn. This was a political gamble in order to make the rest of the country participate in the plans. In 1898 it was approved that the railway be continued eastwards from Taugevatn to Oslo. This high mountain project was one of the most challenging railway projects in Europe. The Bergen railway was to be built across a mountain plateau without roads.

Bergensbanen- snow measurements

Opponents of the Bergen Railway used the snow argument for all it was worth. During the debate in Parliament before the decision about the route was reached in 1894, fears of snowfalls of over 20 metres were presented.

Trail toward Kyrkjedøri

Roughly 550 million years ago, what is now Finse lay at the bottom of the sea - the remains of mud and clay that were deposited in this sea have ended up on the roofs of Norway. Also the thrust sheet from the continental collision has found its way to Finse, after a several hundred kilometre-long, trek through the mountains, that took several tens of millions of years to complete.

Ulvikapollen

When the lush beach area innermost in Ulvikapollen was protected, the bird life was instrumental to the decision. The plant diversity is just as impressive. In Hordaland sea meadows such as this are rare small in size - they are more common in coastal environments.