Ystås

Kjerland

On the farms Kjerland and Røynstrond, east of the river that flows into the fjord, we find many decorative painters who belong to the so-called sòlekistemålarane in Hardanger: Knut and Mikkjel Røynstrand and Johannes Jonsson Kjærland.

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.

Ulvanosa

Some mountains have rounded shapes, while others have steep slopes and sharp edges. Ulvanosa (1246 mos.) has both. The forms reflect the type of bedrock below, and the forces that were in effect when they were formed.

Melderskin

MELDERSKIN - ONCE A NUNATAK? Melderskin, the towering and majestic landmark at Rosendal, rises 1462 metres above sea level. The top area is smooth, but slightly inclined. Geologists think that the area is a remnant of a weakly undulating landscape, that originated near the sea, long before the Ice Age set in.

Bondhusdalen

The Bondhus area in Maruanger has been a magnet for tourists ever since the stream of tourists to Norway's west coast began in the middle of the 1800s. The magnificent landscape with the "ice trail" up to Bondhusvatnet Lake, the ice falls from Bondhusbreen glacier and Keisarstigen trail up to Folgefonna are still popular tourist attractions.

Gjerde

Tveito

Skorven

Øvre Folkedal

Folkedal, which today is like a small “detour” from the main highway, was in the Middle Ages centrally situated in one of the most important roads between Hardanger and Voss. This is the road that Olav Haraldsson travelled in 1023, when he came from the royal farm at Avaldsnes for a meeting with the Voss inhabitants about the new belief. The road passes across the mountain pasture Krossaset and down Bordalen to Vangen.