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Langavassmyrane looking towards Langavatn.

Langavassmyrane

26.05.2018 - 11:30

The Ruff lek on Langvassmyrane is the only known phenomenon of its kind on Hardangervidda. Every year it attracts hens from the whole plateau. The marsh is also the richest wetland in the county. This green oasis is located in a rocky moraine landscape a few hours walking distance south of Dyranut.

Notaholmen, Samnanger

Notaholmen

16.06.2018 - 17:28

The fishnet shed at Notaholmen stands as a reminder of the days when people used to row out on the fjord to set their nets. On Notaholmen the nets were dried, repaired and tanned. And it was a great advantage to store them in a place inaccessible for rats and mice.

Slåttene

Slåttene

31.03.2018 - 19:53

Ådland

13.12.2018 - 08:31

Ådland, innermost in the Samnanger Fjord is an old church centre and transport centre; a nodal point in the transport from sea to land. The white painted church standing today, was built in 1851, but there were two older churches here in former centuries.

The marine use environment on Krossøy, Austrheim

Krossøy

16.06.2018 - 18:32

Furthest north in the island community Rongevær, at the entrance to Fensfjorden, lies Krossøy. Belonging to the farm are the islands of Krossøy, Husøy, Kårøy, Lyngkjerringa, Søre Kjerringa, Rotøy and Kuhovet. All of them have been inhabited. On Krossøy itself today there are four holdings. The marine use environment here is one of the best preserved along the West Norwegian coast.

Leirvågen

Leirvågen

16.06.2018 - 18:34

A marsh is a grassy meadow that is strongly influenced by salt from the sea. This type of nature is abundant in Denmark, among other places. The flatlands along the river that run out by Leirvågen, are the municipalities' largest marsh. At spring tide, these flatlands are flooded underwater for several hundred metres in over land.

Lyngoksen

Lyngoksen

31.03.2018 - 19:54

Leech (Jan Rabben)

Flakkavågen

19.06.2018 - 17:19

The main house at Nedrevåge, Tysnes

Nedrevåge

19.06.2018 - 17:44

Vågsbygdo was severely hit by landslides and rock falls in the decades around 1700, in addition, the rivers transported masses of loose sediment, both large stones and gravel. A lot of what slid down from the Vågsliene (slopes at Våg) collected in Neravåge. It was so bad that the damage “never again can be remedied or restored”, it was said in 1670.

Onarheim

19.06.2018 - 17:45

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