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.

Årstad

Alrekstad (later Årstad) is the birthplace of Bergen. The estate was an estate for Harald Hårfagre and several of his descendants: Eirik Blodøks, Håkon den gode og Olav Tryggvason. These first kings moved with their courts and guardsmen from estate to estate. From these estates the king ruled the country.

Årskog

Årskog farm is situated in a typical coastal landscape in a gentle terrain that slopes down from the outlying heaths down towards the fjord. The farm steading exists as it was in the 1800s. In 1980 the two brothers, Lars and Olai Årskog donated the farm with all its contents of tools and interior decoration, for museum purposes.

Ådlandsstova

The Ådland house is one of the biggest medieval houses still existing in West Norway. It is constructed from unusually large, hard fir wood, beautifully oval-cut. One story links the cottage to the Gildeskålbakken at Orninggård (Lower Ådland); thus indicating that the cottage has been the medieval banqueting hall. The building has been dated back to the 13-1400s by carbon dating.

Vågsbunnen

Vågsbotn was the name of the innermost part of the eastern part of town from Auta-almenning (today’s Vetrlidsalmenning), skirting the bottom of Vågen to Allehelgenskirken (All Saints’ Church) (at the present Allehelgensgate). In early medieval times Vågen reached almost all the way to Olavskirken (the Cathedral). It was a relatively wide bay inside the premonitory where Korskirken was built. The area was therefore much shorter than what is known as Vågsbunnen today.

Vidden

Vargavågen

Undarheim

Ulven camp

Ulvanosa

Some mountains have rounded shapes, while others have steep slopes and sharp edges. Ulvanosa (1246 mos.) has both. The forms reflect the type of bedrock below, and the forces that were in effect when they were formed.