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![Gjuvsland (Svein Nord)](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/navn.jpg?itok=npdQFont)
![The circular buckle from Hatteberg, Kvinnherad](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_198-2_0.jpg?itok=Nx0pe53v)
![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.
![Møkjedalen (Bjørn Moe)](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvi_22.jpg?itok=iPMTpA3a)
![The dwelling house at Rød, Kvinnherad](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_195-2.jpg?itok=0KnxvR7P)
Rød
In 1969 Sigurd and Margreta Dønhaug donated a collection of around 170 historical cultural objects to Kvinnherad municipality. They wanted their gift to become the start of a farm collection in Uskedalen. And that is what happened.
![Burial mounds from the Bronze Age at Skarvaberget, Sydnes](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/kvh_193_sydnes_gravhaug_150.jpg?itok=Fyg1S_87)
![Tveita](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/nvh_260_tveitabotn_2_150.jpg?itok=qnyU8yR3)
![Hauga House at Tveito, Kvinnherad](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_195-4.jpg?itok=i7qSkBTz)
![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.