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![Bordalsgjelet](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/voss_33.jpg?itok=xPd4kUeG)
Bordalsgjelet
Deep down between the stone polished phyllite bedrock in Bordalsgjelet canyon, there is a cascading river. In close cooperation with hard polishing stones, the water has carved into the bedrock for thousands of years - and is still doing so today.
![Bømoen toward the north.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/voss_52.jpg?itok=mV3IWyRp)
![Fadnesskaret](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/voss_17.jpg?itok=DJXiHJma)
![The rock painting “running dog”](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_352-4.jpg?itok=nlTkE3N6)
![Strandvollen ved Hallaråker. Siggjo in the background](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/halleraker_1.jpg?itok=lQl0voUI)
![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.
![Lønaøyane](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/voss_45.jpg?itok=2ZdPPcna)
Lønaøyane
The Strandaelvi river is forever protected from the development of hydropower. The Lønaøyane islands – which comprise the delta furthest north in Lake Lønavatnet - are a part of this water system. In 1995 the level of protection for the Lønaøyne islands was strengthened to that of a nature preserve because of the rich birdlife in this wetland.
![Slopes above the Kårdal boarding house](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/voss_22.jpg?itok=Fvt_DoMF)
![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.
![Rekvesøyane](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/voss_23.jpg?itok=AaNmW0ie)
Rekvesøyane
The sediment that was deposited from the river Dyrvo has created the fan-shaped delta Rekvesøyane. The bit of land farthest out toward the water gets periodically flooded, especially during snow melt and after periods of much rain.