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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?
![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)
![The defensive refuge at Borgåsen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh-etne-2_img_1.jpg?itok=9l2JAuTi)
Borgåsen
In Etne there are no less than four defensive refuges. They are all situated in strategic positions, so that they have served as places of refuge and protection for central parts of the district
![Toward Støle and Sørheim, 1920.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/terassen.jpg?itok=1OuuZEj5)
The village of Etne
Much of the sand and gravel that the town of Etne is built on was laid down at the end of the Ice Age and is evidence of melting glaciers and roaring meltwater rivers. The uncompacted material in the big terraces leave their unmistakeable mark on the wide elongated valleys.
![Rock inscriptions at Helgaberget.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh-etne-3_img_1.jpg?itok=HCOBcyqm)
Helgaberget
Helgaberget – the holy hill – is a little rocky crag which thrusts itself a few metres above the terraced surface of Støle. The surface of the rock is strewn with figures inscribed in the rock and it was, as far as one can judge, a cult centre in the Bronze Ages. The name could indicate that the tradition of holiness can have lasted for almost 3,000 years.
![Den flate terrassen på moreneryggen på garden Tjedla viser kor høgt havet stod på slutten av den siste istida.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/304/skanevik_endret_til_rgb.jpg?itok=KfKszhQ9)
Skånevik- moraine
In Skånevik there are marks left from the ice edge that advanced during the thousand-year cold spell (Younger Dryas) that marked the end of the Ice Age roughly 11 500 years ago. The glacier first proceeded out into Åkra Fjordand and around Vannes and thereafter sent an arm in toward Skånevik. Here, the glacier lay down an end moraine up against the mountainside.
![Foglefonna and Sandvikedalen with Hardangerjøkulen in the distance.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/etne_40.jpg?itok=QkNKWy9j)
Mosnes
The permanently-protected Mosneselva River, with its meltwater from Folgefonna, runs out into Åkra Fjord by the roadless and uninhabited Mosnes. Those who once lived here were forced to surrender to the ravages of Nature. In the autumn of 1962 there was a flood so great that the people were driven from their farms.
![Lona in April](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/sam_19.jpg?itok=cZuecxsb)
Lona
One does not need much imaginationto see that where the river bends down in Røssebotnen, there has once been a lake. The landscape tells this - more clearly than any book.