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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.
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.
Osa
At the bottom of the Osa fjord there is a cultural landscape marked by great contrasts; the wide terraces and the river delta at the fjord contrast with the steep hillsides in the background, where Norddalen leads up to the mountain. There are two farms here. Osa and Sævartveit – the farm at the river mouth and the hollow by the sea.
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.
Botnen
Fyksesundet and Botnagrenda present a fine experience of the landscape and cultural history; a geographically isolated local settlement with extensive cultural contact with the outside world.
Nes
The farm Nes lies directly inside Mundheim on a forested headland in the fjord between Mundheimsvika and Bondesundet, a farm with an attractive and well-kept cultural landscape.
Steinsdalsfossen
Øvsthusfossen, or Steinsdalsfossen waterfall, as it is called today, attracts tourists by the thousands, and always has done as long as there have been tourists in Norway, since the early 1800s.