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![Hana](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/berg_56.jpg?itok=xl5rWX0M)
![Stend station in 1935](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/kvh_266-2.jpg?itok=A5MyGZka)
![Håbrekke farm](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/bru.jpg?itok=oPLcku2-)
![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)
![“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.
![Skytjedalen in Eidfjord.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/011.jpg?itok=YAgcsVmd)
![The quartz quarry in the mountainside above Kvalvikane](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/ull_27.jpg?itok=zyI9-mbt)
Kvalvikane
In Ålvik quartz has long been used to produce ferro-silicon. The quartz was collected from the other side of the fjord, from the mountainside above Kvalvikane.
![The contrast between phyllite and Precambrian basement is clearly visible at Lussand.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/gra_27.jpg?itok=knbu7uIk)
Lussand- geology
Hardangerfjorden kløyver Hordaland i to. Den etter måten rettlinja fjorden skjer seg liksom på skeive inn i landet. Ikkje som Sognefjorden og Nordfjord – dei krokar og buktar seg innover meir eller mindre vinkelrett på kysten. Hardangerfjordens utforming har røter 400 millionar år tilbake i tida, då den veike sona i fjellet, der isen seinare tok grådig for seg, vart danna. Denne sona stig på land ved Lussand.
![Finse Mountain](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/ulvik_27.jpg?itok=YBAj4Xpc)
Bergensbanen- snow measurements
Opponents of the Bergen Railway used the snow argument for all it was worth. During the debate in Parliament before the decision about the route was reached in 1894, fears of snowfalls of over 20 metres were presented.
![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.