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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.
Ånuglo
Take a tour to Ånuglo on a warm summer's day. You can anchor up in Skipavågen and go exploring along the beach. Or, you can find giant holly trees and ivy inland on the island. If you take a trip to the small farms on the west side - one of which is still in operation - you can experience colourful flower meadows from a time most dream of, but few can still remember.
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.
Yddal
Yddal is one of the biggest and finest pine forest areas in the county. The rich forest resources provided an important foundation for the settlement of Yddal. Up until about the 1950s, there were three farms here. Where the lumberjacks couldn't get to, the trees grew very big and can be over 300 years old.
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.
Vinnesleira
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.