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![From a soapstone quarry at Lykling](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/nvh_268_lykling_kleber_2_150.jpg?itok=F7bjH3TA)
![Skredhaugen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_392-2.jpg?itok=yDgN2ZD4)
![A “chest piece” from Bu museum.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_392-3.jpg?itok=OmJbReR9)
![The quartz quarry in the mountainside above Kvalvikane](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/ull_27.jpg?itok=zyI9-mbt)
Kvalvikane
In Ålvik quartz has long been used to produce ferro-silicon. The quartz was collected from the other side of the fjord, from the mountainside above Kvalvikane.
![Smedholmen, Fitjar](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_219-_bu.jpg?itok=RVN_WnRB)
![Liarbø, Fitjar](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_216-3_liarbo216a.jpg?itok=4A2LYm0f)
![The old limestone quarry is today rebuilt and become Moster Amfi.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_206-3a.jpg?itok=US4hTVFq)
![The hayshed in Håvik, Bømlo](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/hus.jpg?itok=Z7aBNCrm)
![Urangsvågen-Rubbestadneset](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/bo_51.jpg?itok=TOAhYhRU)
Urangsvågen-Rubbestadneset
In 1868 the first stone workers came to Rubbestadneset to take out the granite for the Skoltegrunns Pier, predecessor of the Skoltegrunns wharf in Bergen. Later granite was also taken out from the area, around Innværs Fjord and UransvågenN. The activity probably peaked around 1900, with over 40 men at work. 15 years later, it was finished.
![Siggjo from the south. (Svein Nord)](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/bo_52.jpg?itok=ZLhD-gho)
Siggjo
Siggjo is a cone-shaped, volcano-like mountaintop in the part of Hordaland where one finds the best preserved volcanic rocks. The rock types originate from one or several volcanoes that spewed out glowing lava and ash. But, the shape of the mountain, as it appears today, formed later and by completely different forces.