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![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.
![Boat bow of oak shaped like an animal head.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_223-4.jpg?itok=6Y1lzt5t)
![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.
![Finnesloftet drawn by Peter A.Blix in 1888.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_345-1s.jpg?itok=_7csw4kW)
Finne
Peter Bonde, who owned Finne towards the end of the 1200s, had a jumping stag in his family emblem. This stag is the origin for the heraldic blazon of Voss. Peter Bonde and his descendants acquired possession of many farms and farm parts; the so-called Finne properties became some of the largest land properties in the country.
![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.
![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.
![Lydvaloftet](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_345-4.jpg?itok=Y0Vdd9zs)
![Storsetehilleren/Matrehola](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_319-3.jpg?itok=VSiOpI2L)
Matrehola
On a large gravel terrace in Matredalen (the Matre valley), a couple of kilometres from the coastal settlement Matre, lies Storseterhilleren, at the end of a large stone block that came rushing down from the mountain. The Matre river runs just over 100 metres to the east of the cave.
![The Mølster farm in the interim war period.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_347-1.jpg?itok=rxJ5QKba)