Reppadalen

The unusual bog landscape, with enormous peat deposits surrounded by steep mountainsides, makes Reppadalen in Arna an exciting, but little visited tour destination for most of Bergen's inhabitants. Those who live in Arna, however, know to make the most of its beautiful natural splendour.

Vidden

Åsane

Most associate Åsane with ridges, naturally enough (the Norwegian word for "ridge" is "Ås"). A lesser noticed trait in the landscape are the unusual flat areas that lie between the ridges. The Dalselva River, which was channeled at the end of the 1950s, runs down only 2.5 metres from Lake Langavatnet by Vågsbotn to Flatevad, where it goes over into rapids by Fossekleiva. The layers of gneiss stand nearly vertically, and the mountain surface is so even that one might think it had been planed with a planer.

Blomvågen

"One of the big scientific sensations", was the title in the Bergens Times newspaper on the 22nd of November, 1941. It was the geologist Isal Undås who had been interviewed by the newspaper. He thought that he had discovered a 120 000 year old whale bone, remains of life from before the last Ice Age.

Tjeldstømarka

There is no place in Hordaland where there are so many over-wintering song swans as in Tjeldstømarka. And there are few places in the county that have had this birdfowl as a guest for as long.

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.

Dale farm

The Dale farm lies well situated on the gravel by the river, below the mountain Beitelen. But a few stone throws further north, on the wide expanse behind the houses, there has been an older farmstead. Here there have been found a number of cooking hollows, pole holes, an old road and traces of something believed to have been a palisade. Finds from this oldest farmstead may be dated to the time of the migrations, 400-600 years A.D.

Eksingedalen- landscape

Eksingedalen alternates between wide, flat flood plains with good farmland, and narrow passages with waterfalls where the roads cling to the mountainsides. The alternations in the landscape are a result of the sculpturing work by glaciers over several ice ages, and the deposition of the glacial river deposits when the last glacier finally melted back.

Hana

Høvik