- 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 Fjell, frå 2020 del av nye Øygarden kommune filter Fjell, frå 2020 del av nye Øygarden kommune
- Remove Faults filter Faults
Haganes
The gneiss landscape west and north of Bergen viewed in profile can remind us of a saw blade of the kind that has long, slanted sides that get broken off shorter transverse sides. It has taken several hundred million years to file this saw blade, an enduring interplay between various geological processes.
Landro
Landro has been the largest estate on Sotra, including 15 farms with reasonable conditions for agriculture. Their boathouses have had an excellent harbour in Landrovågen. Landro thus has been a good basis for the combination of agriculture and fishing.
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.
Fitjarøyane
If we study the group of islands south of Selbjørns Fjord from the air or on a sea map, we will notice that many of the islands are elongated and lie systematically in rows. The islands are divided by long sounds, for example Trollosen, Nuleia and Hjelmosen, which are oriented in a south-southeast to north-northwesterly direction.
Bordalsgjelet
Deep down between the stone polished phyllite bedrock in Bordalsgjelet canyon, there is a cascading river. In close cooperation with hard polishing stones, the water has carved into the bedrock for thousands of years - and is still doing so today.
Teigdalen
It is not surprising that there are several folk tales connected to the large and unusual scree deposit that is found at Langeland, uppermost in Teigdalen. It is said that folk have been taken into the mountains by these stone blocks and have come back and told about how the wood nymphs live. It is also said that packs of thieves hid here in the old days, both themselves and the treasures they had stolen.
Krokavatnet
On Sunday the 29th of January, 1989, at 17:38 o'clock, Etna shook. The earthquake, with its epicentre ca. 9 kilometres south of Etne centre, had a strength of 4.2 on the Richters scale. This could be felt over large parts of West Land, especially in the areas around Åkra, Etne, Hardanger Fjord and Sauda Fjord. The earthquake was the largest that has ever been measured in Hordaland.