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![Sunde, Kvinnherad](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_194_xxx.jpg?itok=7zdyKxkc)
Sunde
In 1852 Haktor Thorsen erected two large warehouses on one of his farms in Sunde and started trading and salting herring. This was the start of an industrial adventure that made Sunde into one of the first industrial communities in Kvinnherad.
![From Rubbestadneset.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/kvh_205_wartsila_150.jpg?itok=nem7PIQE)
![Nils Hertzber’s watercolour from 1829 gives us an impression of the burial site with the menhirs at Årbakkesanden.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_222-1-1.jpg?itok=iSlCbTy_)
Årbakka- The prehistoric site
The prehistoric site at Årbakkasanden with menhirs and burial mounds has been visited, described and illustrated by many learned researchers through the last 350 years. All the same, we still know very little of this unique cultural monument.
![Glacier fall at Bondhusbreen.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvi_41.jpg?itok=R53rfaSZ)
Bondhusdalen
The Bondhus area in Maruanger has been a magnet for tourists ever since the stream of tourists to Norway's west coast began in the middle of the 1800s. The magnificent landscape with the "ice trail" up to Bondhusvatnet Lake, the ice falls from Bondhusbreen glacier and Keisarstigen trail up to Folgefonna are still popular tourist attractions.
![From Ingahogg.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/kvinnherad.jpg?itok=dmrfeaRp)
Ingahogg
At nearly 1000 metres over sea level, on the north side of INGAHOGG mountain, the remains of a soapstone quarry have been discovered. It is said, according to the Sagas, that Inga collected the big soapstone that lies in front of the Åkra Church from here.
![From Upper Musland toward Geitadalen.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvi_48.jpg?itok=PG7RknzF)
Ulvanosa
Some mountains have rounded shapes, while others have steep slopes and sharp edges. Ulvanosa (1246 mos.) has both. The forms reflect the type of bedrock below, and the forces that were in effect when they were formed.
![Rosemåling](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/304/frette.jpg?itok=NK9-3KWy)
![Foglefonna and Sandvikedalen with Hardangerjøkulen in the distance.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/etne_40.jpg?itok=QkNKWy9j)
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.
![Einstapevoll](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/sveio-11.jpg?itok=kzXzvNHZ)
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”.
![Bautastein, Straumen gard (Svein Nord)](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/304/bautastein_straumen.png?itok=cLMyr1H7)