Tveit

Vesoldo

Folds are to be found everywhere in the remains of the Caledonian mountain chain. Some were formed during the collision with Greenland, others stem from the time when the mountain chain collapsed. Few can compare with the giant fold that remains in the mountain area around Tørvikenuten, Vesoldo and Hellefjellet.

Øystese- Kvam rural museum

Bu

Huse

The farm Huse is situated on a broad terrace in the valley above the church and the commons ground in Kinsarvik. Huse is one of the largest farms in Kinsarvik. The house from the Middle Ages, still standing at Huse today, probably from the middle of 1200, is joined on to a house in the Swiss style from around 1890. This house, with a smoke-vent in the roof, bears witness of a grand old farm and of the chieftain’s power in early medieval times.

Årekol

Ulven

In the region of Ulven phyllite occurs with Hordaland's youngest fossils, and a beautiful quartz conglomerate. The phyllite and conglomerate got squeezed into the bottom of an ancient oceanic crust, made of gabbro and greenstone, in the heart of the Caledonide mountain chain.

Sandviksfjellet

On Sandviksfjellet there are old boulders that have been made into mountains. The stones have been stretched out or squeezed together between huge slabs of rock, during slow, but powerfulprocesses of transport. This conglomerate shows, in quite a special way, the enormous powers that were active during the collision between Norway and Greenland over 400 million years ago.

Frette

Møkstrafjordøyane

The sea keeps the bedrock in the outer skerries smooth and clean. When the bedrock is also varied and interesting, the setting is perfect for a discovery tour of these bare-faced outcrops.