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![Glacial river plain at Lake Klevavatnet.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/ulvik_32.jpg?itok=duW0R_ur)
Rallarvegen
They rest there, all as one, the silent witnesses of Western Norway's saga of creation: Precambrian basement, phyllite and thrust sheet. In the end came the glaciers and sculptured the vast landscape. Along the ground or on the horizon, from bicycle or on foot - the landscape tells its story - and it tells it clearer on Rallarvegen than many other places.
![Ulvikapollen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/ulvik_13.jpg?itok=ufHTN52m)
Ulvikapollen
When the lush beach area innermost in Ulvikapollen was protected, the bird life was instrumental to the decision. The plant diversity is just as impressive. In Hordaland sea meadows such as this are rare small in size - they are more common in coastal environments.
![The Haugsdal delta](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/mas_4.jpg?itok=70eU9NoY)
Haugsdalen
Early in the 1900s there were much larger salt water deltas in Hordaland. But, essentially all of the larger river deltas got filled in and regulated for use in industry during the last century. Now, there is only Haugsdals delta left.
![Bergesfjellet](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/bo_31.jpg?itok=i9o6PSWe)
![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.
![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.
![Rimbareidtjørna](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/fi_15.jpg?itok=TrTU29bZ)
Rimbareid- Vestbøstad
At nesting time you cannot avoid hearing the calls of the curlew or the snipe along the narrow road through the cultural landscape from Rimbareid to Vestbøstad. And on late summer evenings, the intense song of the sedge warbler rings out over the two characteristic tarns in the area.
![From Hamlagrøhornet one sees a division between the fertile phyllite and the naked Precambrian basement rock types in the landscape](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/voss_55.jpg?itok=WKuDCDHt)
Hamlagrø
The type of underlying rock can be decisive for how many different types of plants are found in an area. In the area around Hamlagrø-lake the diversity is especially obvious. The geological conditions change much here within a short distance.
![Lønaøyane](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/voss_45.jpg?itok=2ZdPPcna)
Lønaøyane
The Strandaelvi river is forever protected from the development of hydropower. The Lønaøyane islands – which comprise the delta furthest north in Lake Lønavatnet - are a part of this water system. In 1995 the level of protection for the Lønaøyne islands was strengthened to that of a nature preserve because of the rich birdlife in this wetland.
![Slopes above the Kårdal boarding house](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/voss_22.jpg?itok=Fvt_DoMF)