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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)
![Slåttene](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/sam_14.jpg?itok=TPx2vADn)
![Tysse](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_248-3.jpg?itok=wR1WPlx6)
Tysse
As early as 1862 Svein L.Røsseland started a country store and lodging house at Ytre Tysse, and later on he became steamship agent and the first post office manager in Samnanger. However, the decisive change came when F.Mathiessen started A/S Samnanger Uldvarfabrik (woollen factory) in 1886.
![Grunnosen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/austr_17.jpg?itok=YXEI98_B)
![Leirvågen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/austr_10.jpg?itok=DGquSLwq)
Leirvågen
A marsh is a grassy meadow that is strongly influenced by salt from the sea. This type of nature is abundant in Denmark, among other places. The flatlands along the river that run out by Leirvågen, are the municipalities' largest marsh. At spring tide, these flatlands are flooded underwater for several hundred metres in over land.
![Lyngoksen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/austr_16.jpg?itok=FU0ZNly2)
![Etne and the Etne delta around 1900.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/etne_2.jpg?itok=bfLAQc7X)
Etnedeltaet
During the latter half of the 1900s the big natural river deltas on Westland disappeared. Until the 1980s there was still a small, but significant remnant of the original river delta from the Etneelva river, but today most of this, too, is industrial land.
![Strandflat and scree by land](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/fi_14.jpg?itok=4i8IcPpe)