- Remove Boats and seafaring filter Boats and seafaring
- Remove Vernacular crafts filter Vernacular crafts
- Remove Thrust sheets filter Thrust sheets
- Remove Coniferous forests filter Coniferous forests
- Remove Sediments filter Sediments
- Remove Road constructions filter Road constructions
![Two of the rowlocks which have been found in the bogs Mangersnes, Radøy](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_301-3.jpg?itok=UOKNndXl)
![Garnets at Vågenes](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/radoy_6.jpg?itok=atL5iY_1)
Vågenes
On Vågenes, on one of the prominences out toward Eitrevågen, one finds garnets in anorthosite. The garnets are both older, and not least bigger, than average.
![Kjerringafjellet](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/vaksdal_31.jpg?itok=iFmhzSNw)
Bergsdalen
The mountains of western Norway are lovely to wander in. In Cambro-Silurian time it was the mountain itself that wandered. The mountain, or more correctly the bedrock, first moved eastward, then back a bit westward again. All this rocking back and forth in the mountains ended about 400 million years ago.
![The road Stamnes-Eidslandet](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_336_zzz.jpg?itok=HOHn9Gl1)
Dalseid- Eidslandet road construction
![Flatekvål](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/vaksdal_29.jpg?itok=FmtrpVtP)
Eksingedalen- landscape
Eksingedalen alternates between wide, flat flood plains with good farmland, and narrow passages with waterfalls where the roads cling to the mountainsides. The alternations in the landscape are a result of the sculpturing work by glaciers over several ice ages, and the deposition of the glacial river deposits when the last glacier finally melted back.
![Bergesfjellet](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/bo_31.jpg?itok=i9o6PSWe)
![Strandvollen ved Hallaråker. Siggjo in the background](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/halleraker_1.jpg?itok=lQl0voUI)
![The green Hisøya Island](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/bomlo_45.jpg?itok=QgN_C4RW)
Hisøya
"I am going to prove to you that I am right". That is what the idealist and county doctor Christian Heitmann is supposed to have said in the early 1890s. He sat together with the parish priest, Kullmann, at Heitmann's home in Stord and discussed whether the islands in western Norway could have been forested or not. The priest thought that the area was too barren and weather-beaten for forest to have been able to grow so far out in the sea. But, Heitmann was sure he was right. He challenged the scepticism and set off to work.
![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.
![Bergesvatnet Lake with Skogafjellet to the left.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/bo_49.jpg?itok=kEQx0X4t)
Skogafjellet
You have to travel to Scotland in order to find pine forests similar to those at Bømlo. The nearness to the sea has contributed in different ways to shaping one of the westernmost pine forests in Norway.