- Remove Small landforms filter Small landforms
- Remove Maritime environments filter Maritime environments
- Remove Seabirds filter Seabirds
- Remove Monastery filter Monastery
- Remove Fitjar filter Fitjar
- Remove Avalanches and rock falls filter Avalanches and rock falls
- Remove Etne filter Etne
- Remove Voss, frå 2020 del av nye Voss herad. filter Voss, frå 2020 del av nye Voss herad.
- Remove Railroad filter Railroad
- Remove Tourism filter Tourism
- Remove Thrust sheets filter Thrust sheets
- Remove Vaksdal filter Vaksdal
- Remove Coniferous forests filter Coniferous forests
- Remove Bømlo filter Bømlo
Bergsdalen
The mountains of western Norway are lovely to wander in. In Cambro-Silurian time it was the mountain itself that wandered. The mountain, or more correctly the bedrock, first moved eastward, then back a bit westward again. All this rocking back and forth in the mountains ended about 400 million years ago.
Hisøya
"I am going to prove to you that I am right". That is what the idealist and county doctor Christian Heitmann is supposed to have said in the early 1890s. He sat together with the parish priest, Kullmann, at Heitmann's home in Stord and discussed whether the islands in western Norway could have been forested or not. The priest thought that the area was too barren and weather-beaten for forest to have been able to grow so far out in the sea. But, Heitmann was sure he was right. He challenged the scepticism and set off to work.
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.
Skogafjellet
You have to travel to Scotland in order to find pine forests similar to those at Bømlo. The nearness to the sea has contributed in different ways to shaping one of the westernmost pine forests in Norway.
Urangsvågen-Rubbestadneset
In 1868 the first stone workers came to Rubbestadneset to take out the granite for the Skoltegrunns Pier, predecessor of the Skoltegrunns wharf in Bergen. Later granite was also taken out from the area, around Innværs Fjord and UransvågenN. The activity probably peaked around 1900, with over 40 men at work. 15 years later, it was finished.