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.

Holmen

HOLMEN AND THE KØLLE FAMILY Holmen lies by the fjord, innermost in Ulvikpollen. Originally this was a small smallholding or coast dweller’s place belonging to the farm Håheim. Major Johan Henrik Palludan obtained leasehold for a part of Holmen in 1773, and erected a grand house, as he was the head of Nordre Hardangerske kompani. In 1806 Mrs Palludin sold Holmen to the somewhat eccentric theologian Kristian Kølle, and thus the Kølle family came to Ulvik. Today the Kølle house in Holmen is gone, today it is the residence of the principal of the State horticultural school that occupies the ground – a villa in the dragon style from the turn of the previous century.

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.

Sponheim

Smedholmen

Bordalsgjelet

Deep down between the stone polished phyllite bedrock in Bordalsgjelet canyon, there is a cascading river. In close cooperation with hard polishing stones, the water has carved into the bedrock for thousands of years - and is still doing so today.

Hamlagrø

The type of underlying rock can be decisive for how many different types of plants are found in an area. In the area around Hamlagrø-lake the diversity is especially obvious. The geological conditions change much here within a short distance.

Mjølfjell

Nordheim

"And here these endless kingdoms and these toils for a rich working life far and wide have lain and slept for a hundred thousand years! Right up until the Voss Railway came in 1883 and woke them, like the prince in the fairytale who awakened the Sleeping Beauty."