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Garnes station

Garnes

12.06.2018

Stend station in 1935

Stend station

12.06.2018

Fra Blåmanen mot Vardegga og Ulriken.

Vidden

07.12.2018

Langavatnet, Åsane (Svein Nord)

Åsane

05.12.2018

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.

Gjønavatnet and Kikedalen

Gjønavatnet and Kikedalen

16.06.2018

Vinnesholmen, Fusa

Vinnesholmen

21.11.2018

The smallholding Træet, Askøy

Træet

30.03.2018

Os station

Os station

16.06.2018

From the mountainous rocks just below Sandvikshytte cabin on Sandviksfjellet.

Sandviksfjellet

06.03.2019

On Sandviksfjellet there are old boulders that have been made into mountains. The stones have been stretched out or squeezed together between huge slabs of rock, during slow, but powerfulprocesses of transport. This conglomerate shows, in quite a special way, the enormous powers that were active during the collision between Norway and Greenland over 400 million years ago.

Svartediket med Vidden i bakgrunnen (Helge Sunde)

Isdalen

06.03.2019

The valley on the inside of the Svartediks dam, a five minutes' bus ride from Bergen centre, is often referred to by Bergen folk as Isdalen ("Ice Valley") - justifiably, since the area could have been described in textbooks for its ice-carved land forms. The glacier's polishing over ca. 40 ice ages has created a magnificient landscape. The original ice valley climbs up behind Ulriken at the end of Svartediket.