- Remove Small landforms filter Small landforms
- Remove Thrust sheets filter Thrust sheets
- Remove Maritime environments filter Maritime environments
- Remove Seabirds filter Seabirds
- Remove Monastery filter Monastery
- Remove Fitjar filter Fitjar
- Remove Iron age filter Iron age
- Remove Voss, frå 2020 del av nye Voss herad. filter Voss, frå 2020 del av nye Voss herad.
- Remove Eidfjord filter Eidfjord
- Remove Coniferous forests filter Coniferous forests
- Remove Cultural landscapes filter Cultural landscapes
![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.
![Byrkjehaugen, Voss](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_344-2.jpg?itok=aHQ6m2N7)
Byrkjehaugen
On the farm Bø, close to the highway between Bulken and Voss lies Byrkjehaugen, one of the largest burial mounds in West Norway. Originally it was around 50m across and 5m high, but following the excavation in 1908 and chipping off by both railway and road construction, the cross-section has shrunk to 37m and the height to 4m. All the same, it is an impressive burial monument for the passing traveller to see.
![The mountainside in Sysendalen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/eid_28.jpg?itok=aOUhxIsm)
Sysendalen
If you are lucky you can find 9000-year-old pine stumps on Hardangervidda. Since that time, the tree line has continuously declined. But now, it is on its way back up again.
![Skytjedalen in Eidfjord.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/011.jpg?itok=YAgcsVmd)
![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.
![Voss Spruce Toward Istad](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/voss_50.jpg?itok=YKDZ42oi)
Vossagran
How did the spruce tree get to Voss? Did the seed or small spruce plants get help from people, for example, to make it here unscathed? Nobody knows.
![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)
![Smedholmen, Fitjar](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_219-_bu.jpg?itok=RVN_WnRB)