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Stordfjella mountain towards the south.

Kattnakken–Stovegolvet

19.06.2018 - 16:33

The highest mountainous area on Stord, including Kattnakken, Midtfjellet and Stovegolvet, has more in common with the mountainous terrain on the mainland than in the low coastal landscape of Sunnhordland. The volcanic bedrock together with the erosive powers of nature has resulted in a unique plateau landscape.

Tveitafoss Hydroelectric power station

Kinso

31.03.2018 - 19:16

The spotted trout

Krækkjavassdraget

31.03.2018 - 15:04

Few other animal species on Hardangervidda have been as much the focus of scientific research as the spotted trout. The spotted trout is considered to be a genetic variant of brown trout. It lives in parts of the Krækkjav water system. Otherwise, on a world scale, this species is only found in a small area in Kaukasus, and possibly also in a lake in Rondane.

Sketch showing the process of formation of an esker.

Langavassfjellet

29.03.2018 - 11:35

Langhaugane, Ulvanosa in the background.

Langhaugane

03.01.2019 - 16:52

Lona in April

Lona

27.03.2019 - 13:48

One does not need much imaginationto see that where the river bends down in Røssebotnen, there has once been a lake. The landscape tells this - more clearly than any book.

Lyngholmen

13.03.2018 - 21:20

Manger

Manger

18.06.2018 - 20:06

Mangerite is a rock type that was first made famous in a treatise by the Bergen geologist Carl Fredrik Kolderup in 1903. The rock type got its name from the place where it was found, and has made the Mangerud name well known around the world, at least among geologists.

Rosendals Mountain (Jan Rabben)

Melderskin

12.03.2019 - 15:35

MELDERSKIN - ONCE A NUNATAK? Melderskin, the towering and majestic landmark at Rosendal, rises 1462 metres above sea level. The top area is smooth, but slightly inclined. Geologists think that the area is a remnant of a weakly undulating landscape, that originated near the sea, long before the Ice Age set in.

Slopes above the Kårdal boarding house

Mjølfjell

22.01.2019 - 13:49

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