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The village at Bolstadøyri acquired its structure around the middle of the 1800s, but from the old days there has been a meeting place here; court location and trading post. The guesthouse place stems from the second half of the 17th century, and in the previous century Bolstadøyri was one of the largest rural trading posts in Nordhordland.
Evanger (from Old Norse ålvangr, “vang”, “voll” (field) where the horses may graze) is the place where the river from Vangsvatnet, the Voss watercourse, runs out into Evangervatnet. From here Teigdalen valley runs to the north, towards Eksingedalen, and from here there is a short distance to Bergsdalen in the south.
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.
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.
From the oldest times on record in Norway one of the most important traffic arteries between west and east Norway has passed across Bolstad – Voss – Stalheim – Gudvangen and Lærdal. The post road between Oslo and Bergen was established here 1647, but in Stalheimskleiva there was only a packhorse track right up to the 1840s. Wheeled transport and carts were in little use in the mountains in West Norway up to that time.
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.
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.