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![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.
![«Parti af Stømsnæs ved Bergen».](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/askoy_6_0.jpg?itok=KmaRpfwP)
![Fantasy drawing of the animal life that reigned when the Bjorøy layer was deposited during the younger part of the Jurassic Period.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/nv_35.jpg?itok=VWoic2L9)
Vatlestraumen
There are coal bits hidden in the sand under Vatlestraumen. These remains from a geological layer from the Jurassic Period were discovered when the undersea Bjorøy Tunnel was built in 1994. Oil- and gas reservoirs in the Troll Field in the sea west of Hordaland are from the same time. It is, nonetheless, quite surprising to find bedrock from dinosaur time inside of the outer islands of western Norway. On the Scandinavian mainland north of Denmark, there are only a very few places where one f inds rock from this time in earth history.
![Fossen cliff](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/sam_11.jpg?itok=VQQxhF23)
Fossen Bratte
The steep drop by Fossen cliff has been the biggest challenge for those who wished to make a road over Kvamskogen through the years. Leave the car by the monument on the old road and take a walk down to the bend by the waterfall that Bergen-folk call "The bridal veil". Why is there a waterfall just here?
![Gneiss.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/sam_25.jpg?itok=1PhE0wUc)
![Soft shapes in the hard mountain.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/samnanger.jpg?itok=TBH6DVLU)
![The mill that belonged to Johan Steinegger in Kvalvågen in Lindås, an attempt to exploit the difference in tides](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/austr_5.jpg?itok=-8B2oviO)
![Holmengrå](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/fedje_18.jpg?itok=sUXXEBb1)
Holmengrå
Holmengrå is the only place in Hordaland where we find traces of the abrasion that is supposed to have transformed Western Norway from a Himalaya-like high mountain landscape during the earth's Paleozoic Era, to a flat lowlands terrain during the Mezosoic Era. Just 400 million years ago, large and small stones plummeted down from the high mountains. Some of these stones became incorporated into the conglomerate bedrock on Holmengrå.
![“Prospectus of Frekhaug”. J.F.L.Dreier, 1812](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_295-3.jpg?itok=aGf5ib0l)
Frekhaug
Frekhaug has been a large farm with well-off owners through many generations. The main house, a two storey building with a hipped roof, must have been erected about 1780.