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![Bjørsvik](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/lindas_11_1.jpg?itok=vyYie0Yy)
Bjørsvik
The industrial settlement Bjørsvik
![Tufted Ducks](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/lindas_7.jpg?itok=g_0kvi80)
![The sites show the longhouse, a smaller “old folk’s house” and a hayshed.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/3151.jpg?itok=c_m0Rz1s)
Lurekalven
Lurekalven is an unpopulated island of heather moor which is a part of the wilderness belonging to the five farms on Ytre Lygra. Between the two islands there is only a small sound. As late as the 1920s, milking cows were rowed over the sound from Lygra in summer – a form of farming that was adapted to the coastal landscape.
![Romarheimsdalen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/lindas_33.jpg?itok=VKAH_TBc)
![The geology along Oster Fjord and further eastward, in cross-section and on the surface. (Haakon Fossen)](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/304/stall_english.png?itok=1uke2PrO)
Stall
The Bergen Arcs have an unusually sharp boundary to the bedrock in the east. Geologists think that this was caused by movements in the earth's crust during the Devonian Period. Then, the Bergen Arcs on the Lindås peninsula sank a whole 10 kilometres in relation to the Precambrian basement gneisses on the east side of Fens Fjord and Aust Fjord.
![Vollom](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/lindas_14.jpg?itok=RhEa2l84)
Vollom
On Vollom, northwest of Seim, we find the only natural beech forest in Western Norway, which is also the most northerly of its type in the world. Beech grows also many other places in the county, but these trees are totally lacking in history compared with those of Vollomskogen Forest.
![Nedre Helland](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/mo_1.jpg?itok=J9xuc7pb)
Nedre Helland- skred
Many still remember when the avalanche struck Nedre Helland, on the 14th of August, 1953 14:30 o'clock. All of the buildings at one of the farms and the main house on the neighbouring farm were destroyed. The one woman who was inside a building escaped, frightened but unharmed. The same with the others who lived at Nedre Helland; everyone was a safe distance from the avalanche.
![Mo with the Otterstad farm in the background early in the 1900s.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_329-1_0.jpg?itok=JUVMdLHq)
Otterstad
Tthe Otterstad farms lie in the innermost part of Mofjorden, on the northwest side of the river. The row of stave-built boatsheds that belong to the farm were probably constructed a little after the middle of the 1800s. Both here and on the Mo side, the boatsheds were important storage places at the seashore; wood and other farm products intended for the town; corn and merchandise in return.
![Otterstadstølen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/mo_4.jpg?itok=yFY5zoII)
Otterstadstølen
Otterstadstølen lies in an idyllic grassy plain surrounded by rich forest, but also with high mountains close by. The mountainsides are steep and typical of this part of the county. The same cannot be said about the forest. This spruce forest has been able to develop freely for hundreds of years. Otherwise in the county, only Voss has spruce forest.
![Steinslandsvatnet](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/nv_466.jpg?itok=Wx0aw3W7)