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![Gildrehola](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/awfawf.jpg?itok=2AAfbxlk)
![Gjuvsland (Svein Nord)](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/navn.jpg?itok=npdQFont)
![Halsnøy](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvi_15.jpg?itok=mn2F8JKB)
Halsnøy
Hadde ikkje Hardangerfjordbreen mot slutten av istida rykt fram over fjordbotnen, ville Halsnøy ikkje eksistert som éi øy, men som mange småøyar. Breen skuva framfor seg så mykje leire frå havbotnen at Brattåsen, Toftåsen, Landåsen og Svartaberg vart samla i eitt landområde.
![Maters Fjord with Holmedalsberget in the background.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvi_37.jpg?itok=mDDqfdul)
Holmedalsberget
If you want to be on your own for a long day in a magnificent deciduous forest in demanding terrain, then HOLMESDALSBERGET is the right place. This is a big forested area by Matres Fjord in the southwestly part of Kinnherad. Here, we find one of the largest deciduous forests in Hordaland. The forest stretches over several kilometres.
![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.
![Langhaugane, Ulvanosa in the background.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvi_38.jpg?itok=bdNUBUC5)
![Møkjedalen (Bjørn Moe)](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvi_22.jpg?itok=iPMTpA3a)
![Skorpo (Svein Nord)](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvi_49.jpg?itok=i4VQIqsW)
Skorpo
Skorpo - Polished by glaciers and meltwater
![Tveita](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/nvh_260_tveitabotn_2_150.jpg?itok=qnyU8yR3)
![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.