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.

Brekkhus

Evanger

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.

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?

Frøland- Liarostunnel

Gjernes

Grasdalen

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.

Hamlagrø

The type of underlying rock can be decisive for how many different types of plants are found in an area. In the area around Hamlagrø-lake the diversity is especially obvious. The geological conditions change much here within a short distance.

Holo

I Kvassdalen var det aktiv stølsdrift med mjølking av kyr og geitehald nokre år inn i vårt tusenår, og slik hadde det vore i meir enn to hundre år. Såleis har dalen ikkje fått gro til med kratt og skog, men er open og lys. Fortsett er det beiting av kyr og sauer.