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Garnes station

Garnes

12.06.2018 - 19:16

Stend station in 1935

Stend station

12.06.2018 - 19:19

Fra Blåmanen mot Vardegga og Ulriken.

Vidden

07.12.2018 - 14:19

Langavatnet, Åsane (Svein Nord)

Åsane

05.12.2018 - 18:44

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 - 14:03

Vinnesholmen, Fusa

Vinnesholmen

21.11.2018 - 19:25

The smallholding Træet, Askøy

Træet

30.03.2018 - 08:56

Os station

Os station

16.06.2018 - 16:01

The monks leave their mark at Lysekloster

Lysekloster- The monks and nature

15.05.2018 - 13:34

Lysekloster was the largest agricultural property in the country when it was phased out during the Reformation in 1537. In its prime this cloister encompassed two-thirds of all the farms in Os. The monks introduced and cultivated new plant species and it was probably they who stocked the waters with fish not indigenous to the area. This legacy from the Middle Ages has left a lasting mark.

From the mountainous rocks just below Sandvikshytte cabin on Sandviksfjellet.

Sandviksfjellet

06.03.2019 - 15:22

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.

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