- Remove Quarns and mills filter Quarns and mills
- Remove Basement rocks filter Basement rocks
- Remove Civil servant dwellings and manors filter Civil servant dwellings and manors
- Remove Faults filter Faults
- Remove Tourism filter Tourism
- Remove Mountain plants filter Mountain plants
- Remove Sedimentary rocks filter Sedimentary rocks
![The mill in Kvernapollen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_287-3.jpg?itok=bugwrxNl)
Kvernapollen
When the workers came to Kollsnes to start on the work with the landing for the gas terminal from the Troll field in the North Sea, they found the ruins of an old farm mill at Kvernapollen.
![The mill that belonged to Johan Steinegger in Kvalvågen in Lindås, an attempt to exploit the difference in tides](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/austr_5.jpg?itok=-8B2oviO)
![The Hopland mills around 1940.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_304-3.jpg?itok=ZvabRlGu)
![Holmengrå](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/fedje_18.jpg?itok=sUXXEBb1)
Holmengrå
Holmengrå is the only place in Hordaland where we find traces of the abrasion that is supposed to have transformed Western Norway from a Himalaya-like high mountain landscape during the earth's Paleozoic Era, to a flat lowlands terrain during the Mezosoic Era. Just 400 million years ago, large and small stones plummeted down from the high mountains. Some of these stones became incorporated into the conglomerate bedrock on Holmengrå.
![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
![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.
![“Prospectus of Frekhaug”. J.F.L.Dreier, 1812](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_295-3.jpg?itok=aGf5ib0l)
Frekhaug
Frekhaug has been a large farm with well-off owners through many generations. The main house, a two storey building with a hipped roof, must have been erected about 1780.
![Hana](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/berg_56.jpg?itok=xl5rWX0M)
![Skreien](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/vaksdal_21.jpg?itok=H25GT68d)