University of Bergen- Remove Small landforms filter Small landforms
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Sålesnes
Jondal has one of the country’s oldest slate quarries. Roof tiles have been extracted here since the end of the 1700s, but the quarry is much older. Kvernurdi is mentioned in a diploma in 1421, when Bård Sigurdsson at Torsnes became the owner through a settlement. Already then it must have been customary to cut millstones here.
Mosnes
The permanently-protected Mosneselva River, with its meltwater from Folgefonna, runs out into Åkra Fjord by the roadless and uninhabited Mosnes. Those who once lived here were forced to surrender to the ravages of Nature. In the autumn of 1962 there was a flood so great that the people were driven from their farms.
Måge
Steatite is a type of stone that is abundant in Hardanger. There are large steatite deposits in the mountain below Folgefonna. These deposits are visible both in Krossdalen in Jondal, at Kveitno in Odda and at Måge in Ullensvang. There are many traces of steatite quarrying in Hardanger, and one of the largest fields is in the hillside above Måge.
Einstapevoll- slates
“On the country of Wallestrand…the rock almost everywhere appears to be of a slate-like substance, be it at the seashore, on the farms or in their distant fields”.
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.
