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Dwelling house and store from the Øystese hamlet.

Øystese- Kvam rural museum

07.12.2018 - 14:52

The chest from Sekse, painted by Gunnar Årekol in 1813.

Årekol

27.05.2018 - 15:30

The trade center at Årbakka, Tysnes

Årbakka- The trading center

30.03.2018 - 20:26

Baldellia

Ådlandsvatnet

19.06.2018 - 16:39

Plants that grow in and beside water have to be prepared for marked and rapid changes in their living conditions. They must be able to tolerate living under water without drowning, and getting totally dried out without whithering. Many swamp plants are well adapted to these kinds of changes.

Fishing in Flagafossen in the 1930s

Vosso

24.01.2019 - 14:46

There is probably no bigger salmon to be found in the whole wide world than in Vosso. The average size varies from season to season of course, but for many years this fish has had an average weight of over 10 kilograms. Thumping big ones of 30 kg. have been fished from the river, but one must go back to the 1940s for the last salmon of this size last that was caught.

Pump house for the Vossevangen water works.

Vossavangen

24.01.2019 - 14:18

Xylograph of the shipyard, Bergen

Verftet

19.02.2019 - 14:12

Today the name “Verftet” is linked to both a district and conglomeration of buildings lying protected by Fredriksberg castle. The original shipyard was founded in the 1780s by Georg Brunchorst and Georg Vedeler. It was called Gerogenes Verft (the shipyards of the Georgs), and here ships were both built and repaired in the years after 1786.

Vicarage Alley during the big flood on the 28th of September, 1917.

Vangsvatnet

19.06.2018 - 18:10

The guesthouse settlement at Utne around 1900.

Utne

27.05.2018 - 15:29

When sergeant Peder Larsen Børsem from Strandebarm was “demobilised” in 1721, following the large Nordic War, he married the Bergen lady Elisabeth Schrøder and settled as innkeeper at Utne with a letter of privilege from the county governor dated 29 October 1722.

From Upper Musland toward Geitadalen.

Ulvanosa

04.01.2019 - 11:02

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.

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