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Fosnstraumen
At the southern end of the bridge between Radøy and Fosnøy archaeologists found an unusual Stone Age settlement. There was a thick “cultural layer” here with the remains of the waste dumps of a hunting people. The place was called Kotedalen. Here they came, one group after the other, and settled for some weeks, some months, or maybe years before they went on, leaving the settlement deserted. Time after time it happened. At least 16 settlement phases have been identified, stretching over 5,500 years.
Finne
Peter Bonde, who owned Finne towards the end of the 1200s, had a jumping stag in his family emblem. This stag is the origin for the heraldic blazon of Voss. Peter Bonde and his descendants acquired possession of many farms and farm parts; the so-called Finne properties became some of the largest land properties in the country.
Oppheim
In the slope above Oppheim church lies the old vicarage at OPPHEIM. If you stroll up the road from the church you will arrive in a farmyard marked by traces of building style and living traditions from the Middle Ages.
Ringheim
The farm Ringheim by Lundarvatnet is amongst the largest in Voss. It is divided into eight units and four cadastral numbers: Store Ringheim, Indre Ringheim, Nedre Ringheim and Vetle Ringheim. The farm Lund, from which Lundarvatnet takes its name, must have been a part of Ringheim, and the farms Gjerde and Tròdo (Trå) must formerly have been separated from Ringheim. The name Ringheim indicates that it stems from early times.
Fossen Bratte
The steep drop by Fossen cliff has been the biggest challenge for those who wished to make a road over Kvamskogen through the years. Leave the car by the monument on the old road and take a walk down to the bend by the waterfall that Bergen-folk call "The bridal veil". Why is there a waterfall just here?
Gullbotnen
A barren belt where almost nothing grows, runs through the forest on the east slope of Gullbotnen. But, along the west side of the main road there is a fertile zone that flourishes with several finicky plant types. The contrasts arise from the extreme variations in the nutrient content of the bedrock.