University of Bergen- Remove Small landforms filter Small landforms
- Remove Fjell, frå 2020 del av nye Øygarden kommune filter Fjell, frå 2020 del av nye Øygarden kommune
- Remove Cultural landscapes filter Cultural landscapes
- Remove Ulvik filter Ulvik
- Remove Kvam filter Kvam
- Remove Conservation area filter Conservation area
- Remove Large landforms filter Large landforms
- Remove Os, frå 2020 del av nye Bjørnafjorden kommune filter Os, frå 2020 del av nye Bjørnafjorden kommune
- Remove Meland, frå 2020 del av nye Alver kommune. filter Meland, frå 2020 del av nye Alver kommune.
- Remove Sedimentary rocks filter Sedimentary rocks
- Remove Masfjorden filter Masfjorden
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
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.
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
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.
Løno
Small boat folk in Hordaland know where Løno is. As do many seabirds. With the big ocean at its back and a wide, weather beaten strait ahead of it, Løno is one of Hordaland’s most isolated and exposed recreational areas. The islands west of Sotra are some of the county’s most stable nesting localities for seabirds.
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.
Dyrdal
If you journey along Austfjorden, you at the same time turn the pages of time back through Ice Age history. The landforms show how the landscape has developed gradually as the glaciers have grown - and melted again - in several episodes: from small cirques, we see innermost at Dyrdal, to larger fjords, like at Mas fjord further out.
Raunøya
The sea birds discovered it long ago. Raunøya and the surrounding islands are the most beautiful places in Masfjorden.
Eldsfjellet
The eclogites in western Norway were formed when Precambrian basement rocks were squeezed and pressed down under great pressure deep under the Caledonian mountain chain. The process may well have triggered some of the deepest earthquakes the world has ever known. The clearest traces of this drama are found in and around Mt. Eldsfjellet, in peaceful Meland.
Husebø
When the Corncrake returned to Nordhordland, it came as no surprise that Husebø was the place it chose. Here, remnants of the old cultural landscape are still in good condition. And the Corncrake is not alone in appreciating this.
