Gildrehola

Skorpo

Skorpo - Polished by glaciers and meltwater

Fjøsanger

Fjøsanger is known among ice age researchers from around the world. Under an excavation in 1975-77, geologists from the University of Bergen found layers from the last interglacial, ca. 115 000 to 130 000 years old.

Salhus

Salhus has been a connecting point for sea travellers far back in time. The name probably derives from the Old Norse word sáluhús, “house for travellers”. The name may indicate that this was a place for an inn even in the Middle Ages. The place is eminently situated in the route to and from Bergen. For travellers coming by boat from Sogn and Nordhordland, Salhus is the last stop before Bergen. Travellers from the communities in Voss also came this way earlier when they were going to Bergen

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

Grasdalen

Bolstad

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.

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.

Fleischers Hotel