- Remove Quarns and mills filter Quarns and mills
- Remove Coniferous forests filter Coniferous forests
- Remove Large landforms filter Large landforms
- Remove Avalanches and rock falls filter Avalanches and rock falls
- Remove Basement rocks filter Basement rocks
- Remove Faults filter Faults
- Remove Sunnhordland filter Sunnhordland
Bondhusdalen
The Bondhus area in Maruanger has been a magnet for tourists ever since the stream of tourists to Norway's west coast began in the middle of the 1800s. The magnificent landscape with the "ice trail" up to Bondhusvatnet Lake, the ice falls from Bondhusbreen glacier and Keisarstigen trail up to Folgefonna are still popular tourist attractions.
Ingahogg
At nearly 1000 metres over sea level, on the north side of INGAHOGG mountain, the remains of a soapstone quarry have been discovered. It is said, according to the Sagas, that Inga collected the big soapstone that lies in front of the Åkra Church from here.
Ulvanosa
Some mountains have rounded shapes, while others have steep slopes and sharp edges. Ulvanosa (1246 mos.) has both. The forms reflect the type of bedrock below, and the forces that were in effect when they were formed.
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.