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Boat builder Magnus Trå tests the stability of the newly built four-ored boa

Strandebarm

27.05.2018 - 14:57

The cross church from 1710

Ulvik church

27.05.2018 - 15:54

Sketch showing the process of formation of an esker.

Langavassfjellet

29.03.2018 - 11:35

Moraine ridges, Fruo.

Fruo

26.05.2018 - 11:21

At Fruo, nature has built its own little "Chinese wall ". Some kilometers south of the Vøringsfossen waterfall, there are a number of moraine ridges, the longest and most notable of their kind in Hordaland.

The Eidfjord terrace as seen from Lægreid, presumably in the early 1900s.

Hæreid- geology

28.11.2018 - 20:13

The Eidfjord terrace is a gigantic ridge that reaches up more than one hundred metres from the city centre in Eidfjord. It serves as a powerful natural monument left behind by the ice when it retreated.

From Valldalen

Valldalen

29.03.2018 - 11:59

Valldalen or Valdalen, the name that the locals used in past times, had been a permanent settlement for a long time, and later the biggest mountain-farm valley in western Norway. Since that time there have been many changes: Most of the fields are no longer in use. Bjørkeskogen, a birch forest that had grown in the valley for thousands of years, took more and more over. And in the valley bottom, the Valldals dam now keeps the artificially large Valldalsvatnet Lake in place.

From Helland toward the end of the valley with the Skrikjo waterfall.

Opedal

03.12.2018 - 13:53

The waterfall at the top of Tokagjelet

Tokagjelet

03.12.2018 - 09:55

There is a sharp transition between the wide valley at Kvamskogen and the narrow Tokagjelet. The transition is no less dramatic when we come out of the crooked tunnels far down in the canyon, and the open Steinsdalen valley spreads out before us. The canyon both separates and joins together different epochs in western Norway's history.

Rindarne moraine

29.03.2018 - 11:56

Skjervet toward the east. Jørdre Farm up to the left.

Skjervet- river theft

02.12.2018 - 20:59

At the end of the last ice age the ice flowed out of Hardanger fjord in such a fury that it forced the meltwater from Voss to run back uphill toward Granvin. The glacier from Raundalen down the windy valley along the Vosso to Bolstadøyri went too slow to make the turn.

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