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![Hallingskeid](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_360-4_0.jpg?itok=jjyCUd7C)
![The soil tongues below Jomfrunuten.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/ulvik_36.jpg?itok=aOfkkEth)
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.
![Glacial river plain at Lake Klevavatnet.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/ulvik_32.jpg?itok=duW0R_ur)
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.
![The cross church from 1710](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_359-3_0.jpg?itok=a4Vem1vB)
![Typical landscape in Geitaknottane Nature Preserve](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvam_38.jpg?itok=nBAhBLqi)
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, 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.
![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.