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Lussand- geology
Hardangerfjorden kløyver Hordaland i to. Den etter måten rettlinja fjorden skjer seg liksom på skeive inn i landet. Ikkje som Sognefjorden og Nordfjord – dei krokar og buktar seg innover meir eller mindre vinkelrett på kysten. Hardangerfjordens utforming har røter 400 millionar år tilbake i tida, då den veike sona i fjellet, der isen seinare tok grådig for seg, vart danna. Denne sona stig på land ved Lussand.
Storegraven
The first mention of Granvin church in written sources is in 1306, but the church location must be far older than this. The farm Storegraven is centrally situated at Granvinsvatnet, by the important traffic artery between Hardanger and Voss, where the road takes off to Ulvik.
Jomfrunuten
Freezing and thawing are processes that influence plant cover, move enormous blocks, stretche long mounds of earth, break open bedrock and create patterns in stone and earth.
Rallarvegen
They rest there, all as one, the silent witnesses of Western Norway's saga of creation: Precambrian basement, phyllite and thrust sheet. In the end came the glaciers and sculptured the vast landscape. Along the ground or on the horizon, from bicycle or on foot - the landscape tells its story - and it tells it clearer on Rallarvegen than many other places.
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.