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![Hana](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/berg_56.jpg?itok=xl5rWX0M)
![Nils Hertzberg watercolour of “Spånheimsklosteret”](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_362-2.jpg?itok=tMjpbmV9)
![Boatshed](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_335-3.jpg?itok=egD0W5wD)
![The Ostra chests are easily recognisable with their characteristic style.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_327-1.jpg?itok=x-fr2TBj)
Mjøsvågen
Around Mjøsvågen here is still a compact marine use area. Some of the buildings are common boathouses, but most of them also house small enterprises and workshops. This is where the farmers from Øvsthus, Mjøs, Hole and other farms have supplemented their meagre incomes as smiths, brass moulders, clog makers, chest builders and decorative painters.
![Ystebøtræet, Radøy](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_301-1.jpg?itok=mqbwhdA8)
![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.
![Working with roof slates in the slate quarry at Nordheim around the year 1900](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/voss_29.jpg?itok=AFazwPkE)
Nordheim
"And here these endless kingdoms and these toils for a rich working life far and wide have lain and slept for a hundred thousand years! Right up until the Voss Railway came in 1883 and woke them, like the prince in the fairytale who awakened the Sleeping Beauty."
![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)
![Skreien](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/vaksdal_21.jpg?itok=H25GT68d)
![Kjerringafjellet](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/vaksdal_31.jpg?itok=iFmhzSNw)
Bergsdalen
The mountains of western Norway are lovely to wander in. In Cambro-Silurian time it was the mountain itself that wandered. The mountain, or more correctly the bedrock, first moved eastward, then back a bit westward again. All this rocking back and forth in the mountains ended about 400 million years ago.