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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.
Frøystein
The farm Frøystein by the Ulvik fjord is commonly called Fryste. In 1614 the name was written Frøstemb – an obvious Danish influence – and the form Frøsten was used up until the land register in 1886 and 1907. It is probable that the name of the farm originally was Frystvin; a vin-name. Thus it has no connection with neither Frøy (Norse fertility god) nor stein (stone).
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.
Rallarvegen
They rest there, all as one, the silent witnesses of Western Norway's saga of creation: Precambrian basement, phyllite and thrust sheet. In the end came the glaciers and sculptured the vast landscape. Along the ground or on the horizon, from bicycle or on foot - the landscape tells its story - and it tells it clearer on Rallarvegen than many other places.
Ulvik-village
The ice cap that covered the land during each of the 40 past ice ages over the past 2 million years of Earth's history pressed down the crust of the earth - like a finger on a rubber ball. And when the ice finally loosened its grip 11,000 years ago, the earth's crust rose again, most where the ice was thickest, least where it was thin, quickly in the beginning, and later more slowly. To this day, the land in the inner part of Norway continues to rise by perhaps one millimetre per year. By and large, however, the crust in Hordaland has again reached equilibrium after the weight of the ice was removed.
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.
Einstapevoll- the farm
Einstapevoll (from einstape: “bregne” (fern)) lies on the west side of the Tittelsnes peninsula. Up to 1831 the farm was a vicarage belonging to Stord parish. The priests had leasing rights. Land rent and other fees from the farm was part of their salaries.