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.

Vikøy

Through Adolph Tidemand’s detailed close-ups of smokehouses in Kvam, the vicarage in Vikøy, where he lived during his painting trips through Hardanger, has obtained a central position in the Norwegian national romanticism.

Røldal

The stave church in Røldal was one of the key pilgrimage churches in West Norway. The church was probably built between 1250 and 1350, and in the high Middle Ages Røldal was the most important destination for pilgrims in the country beside the Nidaros cathedral. It was the crucifix that attracted people to midnight mass on midsummer night. That was when it excreted its miraculous sweat.

Ullensvang church

Ullensvang church, situated beside the vicarage, in idyllic surroundings on the headland just inside Lofthus municipality, is mentioned for the first time in written sources in 1309. At that time the present Gothic stone church must have been new. Judging by the style in the western portal and the eastern chancel windows, the church must have been built around 1300 or just before, probably by builders from Bergen influenced by the English Gothic style.

Lyse chapel

The small white-painted chapel with the red brick tiled roof just south of the monastery ruins at Lyse was built in 1663 as a local chapel for the monastery estate, following the takeover of the property by the District Recorder (Stiftskriver) Niels Hanssøn Schmidt two years previously. The chapel, with its harmonic proportions, lies in the cultural landscape beside the grand monastery estate, witness to a time gone by. But even today, there is a tradition of high mass on the 2nd day of Ascension in Lyse Chapel.

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.

Hårteigen

Hårteigen, «the grey signpost», as the name suggests, is a landmark for mountain hikers on the western plateau. The piece of mountain is also a monument for the mighty rock layers that once covered the entire plateau.