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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.

Skytjedalen in Eidfjord.

Skytjedalen

03.01.2019 - 14:57

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.

The smallholding Træet, Askøy

Træet

30.03.2018 - 08:56

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.

Fra Blåmanen mot Vardegga og Ulriken.

Vidden

07.12.2018 - 14:19

Vinnesholmen, Fusa

Vinnesholmen

21.11.2018 - 19:25

Ystebøtræet, Radøy

Ystebøtræet

18.06.2018 - 20:08

Langavatnet, Åsane (Svein Nord)

Åsane

05.12.2018 - 18:44

Most associate Åsane with ridges, naturally enough (the Norwegian word for "ridge" is "Ås"). A lesser noticed trait in the landscape are the unusual flat areas that lie between the ridges. The Dalselva River, which was channeled at the end of the 1950s, runs down only 2.5 metres from Lake Langavatnet by Vågsbotn to Flatevad, where it goes over into rapids by Fossekleiva. The layers of gneiss stand nearly vertically, and the mountain surface is so even that one might think it had been planed with a planer.

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