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![Fossen cliff](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/sam_11.jpg?itok=VQQxhF23)
Fossen Bratte
The steep drop by Fossen cliff has been the biggest challenge for those who wished to make a road over Kvamskogen through the years. Leave the car by the monument on the old road and take a walk down to the bend by the waterfall that Bergen-folk call "The bridal veil". Why is there a waterfall just here?
![Frøland power station and lake Frøland.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/sam_4.jpg?itok=7O9c4Igu)
Frøland
Much rain, a steep drop and nearness to Bergen meant that the power-making potential of the Samnanger water system was exploited early. Samnanger was thus one of the first power-producing municipalities in western Norway. With its subsequent expansion and new power stations, about 400 gigawatts of electricity per hour were produced on average each year. This is enough to meet the energy needs of 25,000 households.
![Gneiss.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/sam_25.jpg?itok=1PhE0wUc)
![Soft shapes in the hard mountain.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/samnanger.jpg?itok=TBH6DVLU)
![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.
![Curvy scours in the bedrock (](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/sund_23.jpg?itok=fisI_JUk)
Golta- Gneiss
Over thousands of years, autumn storms and strong land-driving winds have cleaned the bare rocks of Golta. The waves can beat far in over land and make it dangerous to walk along the shoreline. When the storms have calmed, the results of their work comes into view.
![Toftestallen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/bo_13.jpg?itok=zrSHKUwq)
Toftestallen
The large coastal waves that crash down on the islands west in the sea gather their energy from storms and winds all the way out in the North Atlantic Ocean. The most common place of origin is nonetheless the North Sea. When these waves break over the skerries and islets along the shore, or on the rocky outermost islands, their energy is released. This takes the form of turbulence in the water and sea spray up on land. Can the enormous energy contained in the waves be exploited?
![The power station at Gåssand, Os](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_237-1-1.jpg?itok=kDd6e2yS)
Gåssand
The 28th November 1914 was a day to remember for the Os inhabitants. This was the day they could turn the switch on the wall and have electric light in their houses. It was like opening the door on the future when the power station at Gåssand was put into operation.
![Lyse Monastery, reconstruction](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh-239_lysekloster.jpg?itok=bc_kHrFJ)
![Os station](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/kvh_236-3_0.jpg?itok=3kDX3WjZ)