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Geitaknottane
Many travellers between Mundheim and Gjermundshamn are captivated by the expansive view toward Øynefjord, Varaldsøy and Folgefonna. The barren pine forest on the slopes on the upper-side of the road is not seen by many. Who would think that this area is home to rare species of plants and animals, creatures who have made their homes here for thousands of years?
Kvamskogen
The different bedrock types that got shoved in over Hordaland in Cambro-Silurian times still remain, layer by layer, almost like a cake. But at Kvamskogen the cake has been turned upside down.
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.
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.
Vangdal
At Salthamaren in Vangdalsberget it is thought that salt was burned some time in history, and deep layers of coal in the ground show that fire has been made up here several times. But they were hardly salt-burners, the first people who stopped here. Some of them carved figures into the rock. On top of the rocky outcrop, furthest out on the cliff, a group of Stone Age hunters carved animal figures. More than 1,500 years later Bronze Age farmers drew ship figures at the foot of the rock. Both these works of art - some of the oldest in Hordaland – are still visible, carved in the rock at Salthamaren.
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.