- 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 Ulvik filter Ulvik
- Remove Vernacular arts filter Vernacular arts
- Remove Large landforms filter Large landforms
- Remove Bømlo filter Bømlo
- Remove Granvin, frå 2020 del av nye Voss herad filter Granvin, frå 2020 del av nye Voss herad
![Potholes](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/gra_31.jpg?itok=W2LZyIpN)
![](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_366_x.jpg?itok=bWyHW2Im)
Kjerland
On the farms Kjerland and Røynstrond, east of the river that flows into the fjord, we find many decorative painters who belong to the so-called sòlekistemålarane in Hardanger: Knut and Mikkjel Røynstrand and Johannes Jonsson Kjærland.
![The contrast between phyllite and Precambrian basement is clearly visible at Lussand.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/gra_27.jpg?itok=knbu7uIk)
Lussand- geology
Hardangerfjorden kløyver Hordaland i to. Den etter måten rettlinja fjorden skjer seg liksom på skeive inn i landet. Ikkje som Sognefjorden og Nordfjord – dei krokar og buktar seg innover meir eller mindre vinkelrett på kysten. Hardangerfjordens utforming har røter 400 millionar år tilbake i tida, då den veike sona i fjellet, der isen seinare tok grådig for seg, vart danna. Denne sona stig på land ved Lussand.
![Skjervet toward the east. Jørdre Farm up to the left.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/gra_32.jpg?itok=HGK8HMBs)
Skjervet- river theft
At the end of the last ice age the ice flowed out of Hardanger fjord in such a fury that it forced the meltwater from Voss to run back uphill toward Granvin. The glacier from Raundalen down the windy valley along the Vosso to Bolstadøyri went too slow to make the turn.
![The soil tongues below Jomfrunuten.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/ulvik_36.jpg?itok=aOfkkEth)
Jomfrunuten
Freezing and thawing are processes that influence plant cover, move enormous blocks, stretche long mounds of earth, break open bedrock and create patterns in stone and earth.
![Glacial river plain at Lake Klevavatnet.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/ulvik_32.jpg?itok=duW0R_ur)
Rallarvegen
They rest there, all as one, the silent witnesses of Western Norway's saga of creation: Precambrian basement, phyllite and thrust sheet. In the end came the glaciers and sculptured the vast landscape. Along the ground or on the horizon, from bicycle or on foot - the landscape tells its story - and it tells it clearer on Rallarvegen than many other places.
![Nils Hertzberg watercolour of “Spånheimsklosteret”](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_362-2.jpg?itok=tMjpbmV9)
![Bergesfjellet](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/bo_31.jpg?itok=i9o6PSWe)
![The lobster park in Espevær](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/bomlo_39.jpg?itok=QWK2IaA7)
![Siggjo from the south. (Svein Nord)](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/bo_52.jpg?itok=ZLhD-gho)
Siggjo
Siggjo is a cone-shaped, volcano-like mountaintop in the part of Hordaland where one finds the best preserved volcanic rocks. The rock types originate from one or several volcanoes that spewed out glowing lava and ash. But, the shape of the mountain, as it appears today, formed later and by completely different forces.