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Lysøen, Os

Lysøen

27.03.2019 - 12:54

Lysøen, this fairytale castle with its Russian-inspired onion dome on the corner turret, stands as a reminder of the diversity of the period called Historicism and a monument to a versatile artist; a key figure in the Norwegian National Romanticism.

Nordåsvatnet (Helge Sunde)

Nordåsvatnet

12.06.2018 - 17:13

The Post-war Era came to Fana with its population growth and modern sanitary equipment. This had nearly catastrophic consequences for Nordåsvatnet as a recreational area. After the runoff water got re-directed to deeper water, and later also to the fjord outside, Lake Nordås won back both its swimming guests and its sports fishermen.

Store Lungegårdsvannet

Store Lungegårdsvannet

12.06.2018 - 17:14

Troldhaugen, Bergen

Troldhaugen

29.03.2018 - 22:49

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

Skogseidsvatnet

Skogseidvatnet

31.03.2018 - 15:01

Lake Skogseidvatnet is the most famous fishing lake in Hordaland, with good stocks of both char and trout. There is fishing here throughout the year: with a net in the autumn, through the ice in winter, and with a fishing rod in the summer.

Vinnesholmen, Fusa

Vinnesholmen

21.11.2018 - 19:25

Vinnesleira

Vinnesleira

06.12.2018 - 11:03

Bays that are shallow far out into the sea, with fine sand and clay, are rare in Hordaland. Where they are found, the reason is usually that the edge of the glacier made smaller advances or stopovers when it calved back at the end of the last Ice Age. This is what happened at Vinnesleira.

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