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![Holo](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/304/holo_farger.jpg?itok=s9d9djnZ)
Holo
I Kvassdalen var det aktiv stølsdrift med mjølking av kyr og geitehald nokre år inn i vårt tusenår, og slik hadde det vore i meir enn to hundre år. Såleis har dalen ikkje fått gro til med kratt og skog, men er open og lys. Fortsett er det beiting av kyr og sauer.
![Olavskrossen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_346-3.jpg?itok=xw-nvaa7)
![Lydvaloftet](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_345-4.jpg?itok=Y0Vdd9zs)
![The iron bars found at Rambjørg.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_319-2.jpg?itok=Kl9g7nMT)
![Door](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_319-4.jpg?itok=-5nryjpy)
![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.
![Bordalsgjelet](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/voss_33.jpg?itok=xPd4kUeG)
Bordalsgjelet
Deep down between the stone polished phyllite bedrock in Bordalsgjelet canyon, there is a cascading river. In close cooperation with hard polishing stones, the water has carved into the bedrock for thousands of years - and is still doing so today.
![Cirque in Dyrdal in Lindås](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/mas_22.jpg?itok=YmoL_BEr)
Dyrdal
If you journey along Austfjorden, you at the same time turn the pages of time back through Ice Age history. The landforms show how the landscape has developed gradually as the glaciers have grown - and melted again - in several episodes: from small cirques, we see innermost at Dyrdal, to larger fjords, like at Mas fjord further out.
![The combination building at Nordvik.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_250-2.jpg?itok=CxcVlWaV)