Folgefonna

The glacier is not only white – it is full of colour. The colours have several sources: glacial flour, desert dust, or living algae. And the light refraction in the ice creates cool, bluish nuances – a masterpiece of the interaction between cold and light.

Hereiane

At Hereiane on warm summer days one you can walk barefoot up the hill from the fjord all the way up to 400 metres elevation. The naked, furrowed bedrock often causes travellers who see it from the north side of the fjord to wonder. Why does it look like this, and why is there so little that grows here? It is a long way to the heavy metal industry in Ålvik and Odda, and there hasn’t been a forest fire in modern times.

Indre Vikane

Svåsand

Down by the fjord at Svåsand, close to the main highway, there is a long row of boathouses, one of the well-preserved, older boathouse locations along the Hardanger fjord. It is the farms at Svåsand that have their boathouses here, four main farms with origins far back in time.

Halne

At Halnefjorden, a few hundred metres east of Halne mountain lodge, lie the remains of two stone sheds – Halnelægeret. Some generations ago the cattle drovers stopped here in the summer; they were the cowboys of their time. But Halnelægeret already had a long history before the cattle drovers came.

Simadalen

On the 10th of August, 1937, over half of the agricultural land in Simadalen was submerged by the river. The damage to roads and houses was also catastrophic. This was the most destructive flood ever recorded in Hordaland.

Skytjedalen

Sysendammen

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.

Hallingskeid