Hausberget

Nedre Folkedal

For many years the Folkedal scythe had a good reputation. Immediately above the highway through Folkedal there is a long brick building, on the inner side of the river. Here production of scythes went on to the beginning of the 1950s.

Skjervet- river theft

At the end of the last ice age the ice flowed out of Hardanger fjord in such a fury that it forced the meltwater from Voss to run back uphill toward Granvin. The glacier from Raundalen down the windy valley along the Vosso to Bolstadøyri went too slow to make the turn.

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.

Bømoen

Brekkhus

Gjernes

Jordalen

During the last ice ages, parts of the Voss river system were stolen and sent down Nærøydalen valley to Nærøy Fjord (Nærøyfjorden). Before this big river theft all of the rivers ran all the way from their sources in the mountains near the innermost part of the Sognefjord further southwards towards Voss. Evidence of the theft is still clearly visible in the terrain.

Rekvemylna

If you enter the farmyard at Rekve, some kilometres from Bulken, where the road departs to Giljarhus, you no longer meet “the miller”, Knut Hernes, in his old rural mill. But some years ago he would wish you welcome, friendly and hospitable, and show you around his mill, which had been his workplace for a generation. As light-footed as a youth he climbed in steep ladders high up into the waterfall, to let the water down on to the waterwheel.

Rekvesøyane

The sediment that was deposited from the river Dyrvo has created the fan-shaped delta Rekvesøyane. The bit of land farthest out toward the water gets periodically flooded, especially during snow melt and after periods of much rain.