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![Potholes by the Koldals River](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/fokllk.jpg?itok=MZgPWao9)
Eikelandsosen
"So many and such big potholes as are found at Eikelandsosen, we don't see other places in western Norway, and as beautifully polished as the mountainside is along the river up to Koldal , one would look a long time to see anywhere else. There is much to dazzle a geologist's eyes. If only these features could bring others the same joy!"
![Gjønavatnet and Kikedalen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/nvh_320_kikedalen_150.jpg?itok=mWd_BFbm)
![Hammarsland, Fusa](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_244-3.jpg?itok=yFuY5P-3)
![The man from Holmefjord](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_246-7.jpg?itok=XaoETJFZ)
Holmefjord
Even though we know of several hundred burial places from the Stone Age in Hordaland, we do not often hit on the Stone Age Man himself. But there are a few.
![Vinnesleira](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/fusa_3.jpg?itok=XFQuYzaF)
Vinnesleira
Bays that are shallow far out into the sea, with fine sand and clay, are rare in Hordaland. Where they are found, the reason is usually that the edge of the glacier made smaller advances or stopovers when it calved back at the end of the last Ice Age. This is what happened at Vinnesleira.
![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.
![Osa and the Osa fjord](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_360xxx.jpg?itok=YQCQAW0y)
Osa
At the bottom of the Osa fjord there is a cultural landscape marked by great contrasts; the wide terraces and the river delta at the fjord contrast with the steep hillsides in the background, where Norddalen leads up to the mountain. There are two farms here. Osa and Sævartveit – the farm at the river mouth and the hollow by the sea.
![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.
![Ulvikapollen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/ulvik_13.jpg?itok=ufHTN52m)
Ulvikapollen
When the lush beach area innermost in Ulvikapollen was protected, the bird life was instrumental to the decision. The plant diversity is just as impressive. In Hordaland sea meadows such as this are rare small in size - they are more common in coastal environments.