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![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.
![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.
![The mill in Kvernapollen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_287-3.jpg?itok=bugwrxNl)
Kvernapollen
When the workers came to Kollsnes to start on the work with the landing for the gas terminal from the Troll field in the North Sea, they found the ruins of an old farm mill at Kvernapollen.
![Toftestallen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/bo_13.jpg?itok=zrSHKUwq)
Toftestallen
The large coastal waves that crash down on the islands west in the sea gather their energy from storms and winds all the way out in the North Atlantic Ocean. The most common place of origin is nonetheless the North Sea. When these waves break over the skerries and islets along the shore, or on the rocky outermost islands, their energy is released. This takes the form of turbulence in the water and sea spray up on land. Can the enormous energy contained in the waves be exploited?
![The power station at Herlandsfossen, Osterøy](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_327-4.jpg?itok=UYh1p6Mj)
![The power station at Gåssand, Os](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_237-1-1.jpg?itok=kDd6e2yS)
Gåssand
The 28th November 1914 was a day to remember for the Os inhabitants. This was the day they could turn the switch on the wall and have electric light in their houses. It was like opening the door on the future when the power station at Gåssand was put into operation.
![This little mountain in the picture sticks up because the layers are tilted on their sides.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/oygard_21.jpg?itok=ugcTumKb)