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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).
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.
Færavåg
The main house at Færavåg was built in 1599. History tells us that a German came to Færavåg and built the house. He divided the land between his two sons. They in turn divided it between their two sons, thus there were four equal holdings on the farm. And it is said that all households lived in the same house. They each stayed in their own corner around the fire in the middle of the floor.
Nedrevåge
Vågsbygdo was severely hit by landslides and rock falls in the decades around 1700, in addition, the rivers transported masses of loose sediment, both large stones and gravel. A lot of what slid down from the Vågsliene (slopes at Våg) collected in Neravåge. It was so bad that the damage “never again can be remedied or restored”, it was said in 1670.
