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![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.
Litlandsvatnet
Large quantities of nickel ore have been mined from Litlandsvatnet, between Lonevågen and Hosanger. The discovery was made in 1875. During the period of operation from 1882 to 1945, 4170 tonnes of pure nickel were extracted from 462 000 tonnes of ore, a large production by Norwegian standards.
![The sites show the longhouse, a smaller “old folk’s house” and a hayshed.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/3151.jpg?itok=c_m0Rz1s)
Lurekalven
Lurekalven is an unpopulated island of heather moor which is a part of the wilderness belonging to the five farms on Ytre Lygra. Between the two islands there is only a small sound. As late as the 1920s, milking cows were rowed over the sound from Lygra in summer – a form of farming that was adapted to the coastal landscape.
![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.
![Manger](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/radoy_25.jpg?itok=2_lft7Ih)
Manger
Mangerite is a rock type that was first made famous in a treatise by the Bergen geologist Carl Fredrik Kolderup in 1903. The rock type got its name from the place where it was found, and has made the Mangerud name well known around the world, at least among geologists.
![Two of the rowlocks which have been found in the bogs Mangersnes, Radøy](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_301-3.jpg?itok=UOKNndXl)
![](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/berg_12_0.jpg?itok=hv7XxFE6)
![Storsetehilleren/Matrehola](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_319-3.jpg?itok=VSiOpI2L)
Matrehola
On a large gravel terrace in Matredalen (the Matre valley), a couple of kilometres from the coastal settlement Matre, lies Storseterhilleren, at the end of a large stone block that came rushing down from the mountain. The Matre river runs just over 100 metres to the east of the cave.
![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)