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![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)
![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
![Tufted Ducks](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/lindas_7.jpg?itok=g_0kvi80)
![The sites show the longhouse, a smaller “old folk’s house” and a hayshed.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/3151.jpg?itok=c_m0Rz1s)
Lurekalven
Lurekalven is an unpopulated island of heather moor which is a part of the wilderness belonging to the five farms on Ytre Lygra. Between the two islands there is only a small sound. As late as the 1920s, milking cows were rowed over the sound from Lygra in summer – a form of farming that was adapted to the coastal landscape.
![Burning heath](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh-315-1.jpg?itok=ppNzj4Tv)
Lygra
The heath landscape on outer Lygra, Utluro and Lurekalven will in future become part of a landscape protection area, to be maintained through traditional activities with year-round outdoor sheep, grazing and burning. The West Norwegian heath country belongs to a large North Atlantic coastal landscape stretching from the Bay of Biscay to the Lofoten islands.
![The potato cellar at Verastunet is still in good condition.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/kvh_316_veras_potetkjeller_150.jpg?itok=BG46uTxF)
![Toward Støle and Sørheim, 1920.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/terassen.jpg?itok=1OuuZEj5)
The village of Etne
Much of the sand and gravel that the town of Etne is built on was laid down at the end of the Ice Age and is evidence of melting glaciers and roaring meltwater rivers. The uncompacted material in the big terraces leave their unmistakeable mark on the wide elongated valleys.