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![Fra Blåmanen mot Vardegga og Ulriken.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/vidden.jpg?itok=8VZJtCoS)
![Langavatnet, Åsane (Svein Nord)](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/berg_6_cmyk_0.jpg?itok=EdtUxacZ)
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.
![Huglo](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/stord_27.jpg?itok=9cCQ5yAR)
Huglo
The majority of Huglo is bare rock. A bit of dwarf pine forest is the only vegetation able to put down roots. Along the west- and east sides, to the contrary, the landscape is unusually green and lush. The reason lies both in the bedrock and in the ice that covered the area 12 000 years ago.
![Svartediket med Vidden i bakgrunnen (Helge Sunde)](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/304/isdalen_endret_til_rgb.jpg?itok=WdgQVjEL)
Isdalen
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.