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![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.
![Glacier fall at Bondhusbreen.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvi_41.jpg?itok=R53rfaSZ)
Bondhusdalen
The Bondhus area in Maruanger has been a magnet for tourists ever since the stream of tourists to Norway's west coast began in the middle of the 1800s. The magnificent landscape with the "ice trail" up to Bondhusvatnet Lake, the ice falls from Bondhusbreen glacier and Keisarstigen trail up to Folgefonna are still popular tourist attractions.
![Gjuvsland (Svein Nord)](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/navn.jpg?itok=npdQFont)
![From Upper Musland toward Geitadalen.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvi_48.jpg?itok=PG7RknzF)
Ulvanosa
Some mountains have rounded shapes, while others have steep slopes and sharp edges. Ulvanosa (1246 mos.) has both. The forms reflect the type of bedrock below, and the forces that were in effect when they were formed.
![Fra Blåmanen mot Vardegga og Ulriken.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/vidden.jpg?itok=8VZJtCoS)
![Langavatnet, Åsane (Svein Nord)](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/berg_6_cmyk_0.jpg?itok=EdtUxacZ)
Åsane
Most associate Åsane with ridges, naturally enough (the Norwegian word for "ridge" is "Ås"). A lesser noticed trait in the landscape are the unusual flat areas that lie between the ridges. The Dalselva River, which was channeled at the end of the 1950s, runs down only 2.5 metres from Lake Langavatnet by Vågsbotn to Flatevad, where it goes over into rapids by Fossekleiva. The layers of gneiss stand nearly vertically, and the mountain surface is so even that one might think it had been planed with a planer.
![The combination building at Nordvik.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_250-2.jpg?itok=CxcVlWaV)
![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.
![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)
![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.