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Klokkarvatnet

Kalandsvatnet and Klokkarvatnet

03.08.2018 - 12:30

The Boat Hall at the Horda Museum houses 26 clinker-built, open wooden boats

Horda Museeum

19.06.2018 - 18:39

Kalandsvika Bay in the eastern part of Kalandsvatnet

Kalandsvika

12.06.2018 - 19:32

There is little to say about the opportunity for surveying from the bird observation tower in Kalandsvika: 155 different bird species have been sighted in the Kalands water shed. Take your binoculars and visit the tower in late spring - early summer or during the winter half of the year. If you are lucky, you might get to see a rare bird species.

Fra Blåmanen mot Vardegga og Ulriken.

Vidden

07.12.2018 - 14:19

Svartediket med Vidden i bakgrunnen (Helge Sunde)

Isdalen

06.03.2019 - 18:12

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.

Fjellsiden

Fjellsiden

31.03.2018 - 14:58

Møllendal graveyard is the winter home of the urban crows in Bergen. Those that do not want to stay overnight in the graveyard, perch in the lush deciduous trees at Fjellsiden.

Nygårdsparken in the 1920s.

Nygårdsparken

31.03.2018 - 14:59

Byparken

07.12.2018 - 14:01

It isn't true that hungry students have hunted down basking ducks in the city park Byparken in their spring fervour, as rumours may have it. But, it is not unusual to see students throw themselves over the park's wild birds, and hold on to them tight. They ring the birds. Because of this, we know quite a lot about the birds in Byparken.

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.