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![The delta at the outflow of Storelvi in Granvinsvatnet.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/gra_1.jpg?itok=er1kEGup)
Granvinsvassdraget
After the ice age, Granvin Fjord reached all the way up under Skjervsfjossen waterfall. Just a thousand years later, as a result of the rising of the land after the ice melted, this whole inner part of the fjord freed itself of the sea and became Granvinsvatnet lake. In spite of this rise in elevation, this waterway is still navigable for fish: Sea trout have wandered into Granvinsvatnet in more recent times and evolved to become freshwater trout. And salmon and sea trout made the journey 13 kilometres up the Storelvi river.
![Potholes](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/gra_31.jpg?itok=W2LZyIpN)
![Skjervet toward the east. Jørdre Farm up to the left.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/gra_32.jpg?itok=HGK8HMBs)
Skjervet- river theft
At the end of the last ice age the ice flowed out of Hardanger fjord in such a fury that it forced the meltwater from Voss to run back uphill toward Granvin. The glacier from Raundalen down the windy valley along the Vosso to Bolstadøyri went too slow to make the turn.
![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)
![Notaholmen, Samnanger](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_250_zz.jpg?itok=XSNGpegF)
Notaholmen
The fishnet shed at Notaholmen stands as a reminder of the days when people used to row out on the fjord to set their nets. On Notaholmen the nets were dried, repaired and tanned. And it was a great advantage to store them in a place inaccessible for rats and mice.
![Grunnosen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/austr_17.jpg?itok=YXEI98_B)
![The marine use environment on Krossøy, Austrheim](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_306-1.jpg?itok=G4q9_8h8)
Krossøy
Furthest north in the island community Rongevær, at the entrance to Fensfjorden, lies Krossøy. Belonging to the farm are the islands of Krossøy, Husøy, Kårøy, Lyngkjerringa, Søre Kjerringa, Rotøy and Kuhovet. All of them have been inhabited. On Krossøy itself today there are four holdings. The marine use environment here is one of the best preserved along the West Norwegian coast.