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![Vøringsfossen waterfall and the Upper Måbødalen Valley, as seen from the viewpoint at Hotel Fossli.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/eid_27.jpg?itok=N8nsqBs2)
Måbødalen- geology
The old pack road had 1500 steps, where cars today gas through the mountain. The time of this hard work is over, and of getting used to the steep terrain, as well; only the view from the top is much the same as before. Vøringsfossen in summer is one of Western Norway’s biggest natural wonders. It marks the transition between the older, open part of the Sysendalen valley and the younger, narrow and winding valley of Måbødalen.
![Vegane gjennom den tronge og bratte Måbødalen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_407-1.jpg?itok=jN0RFHBc)
![Rembesdalsskåka and the lower part of Demmevatnet, from Tresnuten. Demmevass cabin is visible to the left in the picture.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/nv_491.jpg?itok=eg8SNPfS)
Simadalen
On the 10th of August, 1937, over half of the agricultural land in Simadalen was submerged by the river. The damage to roads and houses was also catastrophic. This was the most destructive flood ever recorded in Hordaland.
![Skytjedalen in Eidfjord.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/011.jpg?itok=YAgcsVmd)
![Sysendammen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/eid_37.jpg?itok=ibwv5qBG)
![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.
![Workers](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_369-3.jpg?itok=8KobiG8l)
Lussand-roadwork
The road along the north side of the Hardanger fjord - between Øystese and Eide in Granvin – was literally built “by hand”. The construction work started in February 1933, and on 9 October 1937 Crown Price Olav opened the stretch of road between Øystese and Ålvik at Fyksesund bridge.
![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.
![Skjervet, approx. 1900](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_364-1.jpg?itok=1x6DvMWY)
Skjervet- road construction
The road between Eide in Granvin and Voss is one of the oldest roads mentioned in the Middle Ages. In a diploma from 1343 from Voss regarding distribution of road works, we also find mention of the road to Angr (the Granvin fjord).
![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.