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Burial mounds from the Bronze Age at Skarvaberget, Sydnes

Sydnes

19.05.2018 - 20:59

Klokkarvatnet

Kalandsvatnet and Klokkarvatnet

03.08.2018 - 12:30

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

Årstad in the 1890s

Årstad

12.06.2018 - 17:18

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.

The boathouses at Svåsand.

Svåsand

26.05.2018 - 16:28

Down by the fjord at Svåsand, close to the main highway, there is a long row of boathouses, one of the well-preserved, older boathouse locations along the Hardanger fjord. It is the farms at Svåsand that have their boathouses here, four main farms with origins far back in time.

Blanks for bowls and ladles

Eidsbøen

13.03.2018 - 20:58

Where the school and the sports facility lie at Eidsbøen there was previously a bog surrounded by small hillocks. More than 1000 years ago this was a holy place, where the dead were buried.

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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