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![The long house at Golta, Sund](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_276-1.jpg?itok=qlke6iyO)
Golta- Long house
In the years between the wars a major registration of houses and house costumes, house construction methods, fireplaces and forms of housing clusters was started in West Norway – an ambitious mapping of everything that came under the name “Registration of Culture and Geography in West Norway”. One of the places of which material was gathered in 1938 was an old multi-room house at Golta; new and interesting material for the researchers from the Historical Museum, but well known within the local building tradition through several generations.
![Goltasund bridge and Goltasundet](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/kvh_276_goltasundet_150.jpg?itok=1CBSE3io)
Goltasundet
For generations the land-seine was the most important tool for catching herring and mackerel, and therefore a suitable casting bay was worth its weight in gold. Goltasundet (the Golta sound) on Golta was such a place. Here the herring often drifted in and fantastic casts might be made here.
![The Salting shed at Trælevika.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_275-4.jpg?itok=20MdCbWg)
![The lobster park in Espevær](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/bomlo_39.jpg?itok=QWK2IaA7)
![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)
![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)
![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.
![The eider population at Bømlo has increased sharply during the last decade.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/fuuugler.jpg?itok=gor6FPw4)
![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.
![Oyster farmer Alf-Roald Sætre of the Espevik dam](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/tysnes_6.jpg?itok=Qe16WF4L)