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![Hereiane. Jonahornet in the background.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/jondal_19.jpg?itok=zuuwq9tu)
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.
![Cross-leaved heath (Akvarell: Miranda Bødtker)](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/auste_3.jpg?itok=LlH8ouMq)
![Gneiss.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/sam_25.jpg?itok=1PhE0wUc)
![Gullbotnen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/sam_18.jpg?itok=dlJQCo79)
Gullbotnen
A barren belt where almost nothing grows, runs through the forest on the east slope of Gullbotnen. But, along the west side of the main road there is a fertile zone that flourishes with several finicky plant types. The contrasts arise from the extreme variations in the nutrient content of the bedrock.
![Slåttene](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/sam_14.jpg?itok=TPx2vADn)
![Fykse](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvam_31.jpg?itok=d1pn9Mw8)
![Kvamskogen, toward the north.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvam_45.jpg?itok=fafg-yeC)
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.
![Rockslide at Mundheim in the spring of 1997](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvam_3.jpg?itok=M0w_nyFl)
Mundheim
At Mundheim there is a dangerous stretch of the highway. The mountainside has given way several times in this area. Typically, it happens in the spring, when the frost has loosened its grip.
![Vesoldo](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/nv_465.jpg?itok=0QTt1JUj)
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.
![Skerries with a long history](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/auste_15.jpg?itok=MU10Q3lW)
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.