- Remove Small landforms filter Small landforms
- Remove Cultural landscapes filter Cultural landscapes
- Remove Ulvik filter Ulvik
- Remove Kvam filter Kvam
- Remove Austrheim filter Austrheim
- Remove Burial mounds filter Burial mounds
- Remove Thrust sheets filter Thrust sheets
- Remove Quarries filter Quarries
- Remove Chieftains and royal lines filter Chieftains and royal lines
- Remove Railroad filter Railroad
![Rotating snowplough](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_361-_2.jpg?itok=uZtECxjV)
Bergensbanen
Already at the beginning of the 1870s demands were made that there had to be a railway connection between Bergen and East Norway. The first section between Bergen and Voss was finished in 1883. The route alternatives further on were many: Lærdal-Valdres, Aurland-Geiteryggen, Raundalen-Finse and Ulvik-Finse. Following a long dispute, an agreement was finally reached that the middle route alternative, Raundalen- Myrdal- Finse, was the best alternative. In 1894 the government passed a resolution that the Bergen railway should be built, but only the section Voss-Taugevatn. This was a political gamble in order to make the rest of the country participate in the plans. In 1898 it was approved that the railway be continued eastwards from Taugevatn to Oslo. This high mountain project was one of the most challenging railway projects in Europe. The Bergen railway was to be built across a mountain plateau without roads.
![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.
![The soil tongues below Jomfrunuten.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/ulvik_36.jpg?itok=aOfkkEth)
Jomfrunuten
Freezing and thawing are processes that influence plant cover, move enormous blocks, stretche long mounds of earth, break open bedrock and create patterns in stone and earth.
![Osa and the Osa fjord](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_360xxx.jpg?itok=YQCQAW0y)
Osa
At the bottom of the Osa fjord there is a cultural landscape marked by great contrasts; the wide terraces and the river delta at the fjord contrast with the steep hillsides in the background, where Norddalen leads up to the mountain. There are two farms here. Osa and Sævartveit – the farm at the river mouth and the hollow by the sea.
![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.
![Nils Hertzberg watercolour of “Spånheimsklosteret”](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_362-2.jpg?itok=tMjpbmV9)
![Traces of the dwellings and activity in the quarry.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/nvh_464_takskifer_ulvik_2_150.jpg?itok=tTKVd-vg)
![Lyngoksen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/austr_16.jpg?itok=FU0ZNly2)
![Botnagrenda](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_369-_2.jpg?itok=9FLr126Z)
Botnen
Fyksesundet and Botnagrenda present a fine experience of the landscape and cultural history; a geographically isolated local settlement with extensive cultural contact with the outside world.
![Kvamskogen, toward the north.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvam_45.jpg?itok=fafg-yeC)
Kvamskogen
The different bedrock types that got shoved in over Hordaland in Cambro-Silurian times still remain, layer by layer, almost like a cake. But at Kvamskogen the cake has been turned upside down.