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![Blanks for bowls and ladles](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_231-4.jpg?itok=EnFHKTo-)
Eidsbøen
Where the school and the sports facility lie at Eidsbøen there was previously a bog surrounded by small hillocks. More than 1000 years ago this was a holy place, where the dead were buried.
![Hallingskeid](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_360-4_0.jpg?itok=jjyCUd7C)
![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.
![Hallstatt sword](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_360-2x.jpg?itok=4HquQz9B)
![On the trail toward Kyrkjedøri, a half hour walk from Finse station, we find these small ridges](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/ulvik_12.jpg?itok=gpoawGzE)
Trail toward Kyrkjedøri
Roughly 550 million years ago, what is now Finse lay at the bottom of the sea - the remains of mud and clay that were deposited in this sea have ended up on the roofs of Norway. Also the thrust sheet from the continental collision has found its way to Finse, after a several hundred kilometre-long, trek through the mountains, that took several tens of millions of years to complete.
![Fossil scree](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/ulvik_10.jpg?itok=4OVfBQkN)
![Skerries with a long history](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/auste_15.jpg?itok=MU10Q3lW)
Møkstrafjordøyane
The sea keeps the bedrock in the outer skerries smooth and clean. When the bedrock is also varied and interesting, the setting is perfect for a discovery tour of these bare-faced outcrops.