- Remove Thrust sheets filter Thrust sheets
- Remove Granvin, frå 2020 del av nye Voss herad filter Granvin, frå 2020 del av nye Voss herad
- Remove Kvam filter Kvam
- Remove Samnanger filter Samnanger
- Remove Road constructions filter Road constructions
![The contrast between phyllite and Precambrian basement is clearly visible at Lussand.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/gra_27.jpg?itok=knbu7uIk)
Lussand- geology
Hardangerfjorden kløyver Hordaland i to. Den etter måten rettlinja fjorden skjer seg liksom på skeive inn i landet. Ikkje som Sognefjorden og Nordfjord – dei krokar og buktar seg innover meir eller mindre vinkelrett på kysten. Hardangerfjordens utforming har røter 400 millionar år tilbake i tida, då den veike sona i fjellet, der isen seinare tok grådig for seg, vart danna. Denne sona stig på land ved Lussand.
![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, 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).
![Gneiss.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/sam_25.jpg?itok=1PhE0wUc)
![Gullbotnen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/sam_18.jpg?itok=dlJQCo79)
Gullbotnen
A barren belt where almost nothing grows, runs through the forest on the east slope of Gullbotnen. But, along the west side of the main road there is a fertile zone that flourishes with several finicky plant types. The contrasts arise from the extreme variations in the nutrient content of the bedrock.
![The bridge at Mørkhølen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/kvh_249_morkholen_bru_150_0.jpg?itok=3UvMvfAf)
![Kvamskogen, toward the north.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvam_45.jpg?itok=fafg-yeC)
Kvamskogen
The different bedrock types that got shoved in over Hordaland in Cambro-Silurian times still remain, layer by layer, almost like a cake. But at Kvamskogen the cake has been turned upside down.
![The waterfall at the top of Tokagjelet](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvam_49.jpg?itok=OJAJPjRK)
Tokagjelet
There is a sharp transition between the wide valley at Kvamskogen and the narrow Tokagjelet. The transition is no less dramatic when we come out of the crooked tunnels far down in the canyon, and the open Steinsdalen valley spreads out before us. The canyon both separates and joins together different epochs in western Norway's history.
![Vesoldo](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/nv_465.jpg?itok=0QTt1JUj)
Vesoldo
Folds are to be found everywhere in the remains of the Caledonian mountain chain. Some were formed during the collision with Greenland, others stem from the time when the mountain chain collapsed. Few can compare with the giant fold that remains in the mountain area around Tørvikenuten, Vesoldo and Hellefjellet.
![Øvre Kvernes](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/sam_17.jpg?itok=RsNY3AA3)
Kvernes
Håkons Hall, Domkirken Church, Bergen Børs Stock Exchange, Permanenten and other well known buildings in Bergen are decorated with soapstone from Øvre Kvernes. The quarry is a big hole in the mountainside by the cliff just east of the farm buildings.