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Bordalsgjelet

Bordalsgjelet

13.01.2019 - 13:52

Deep down between the stone polished phyllite bedrock in Bordalsgjelet canyon, there is a cascading river. In close cooperation with hard polishing stones, the water has carved into the bedrock for thousands of years - and is still doing so today.

Bømoen toward the north.

Bømoen

12.01.2019 - 16:32

Fadnesskaret

Fadnesskaret

31.03.2018 - 20:07

The rock painting “running dog”

Gjøstein

13.03.2018 - 21:23

Strandvollen ved Hallaråker. Siggjo in the background

Hallaråker

19.05.2018 - 20:27

The soil tongues below Jomfrunuten.

Jomfrunuten

03.12.2018 - 14:13

Freezing and thawing are processes that influence plant cover, move enormous blocks, stretche long mounds of earth, break open bedrock and create patterns in stone and earth.

Lønaøyane

Lønaøyane

31.03.2018 - 19:10

The Strandaelvi river is forever protected from the development of hydropower. The Lønaøyane islands – which comprise the delta furthest north in Lake Lønavatnet - are a part of this water system. In 1995 the level of protection for the Lønaøyne islands was strengthened to that of a nature preserve because of the rich birdlife in this wetland.

Slopes above the Kårdal boarding house

Mjølfjell

22.01.2019 - 13:49

Glacial river plain at Lake Klevavatnet.

Rallarvegen

04.12.2018 - 14:30

They rest there, all as one, the silent witnesses of Western Norway's saga of creation: Precambrian basement, phyllite and thrust sheet. In the end came the glaciers and sculptured the vast landscape. Along the ground or on the horizon, from bicycle or on foot - the landscape tells its story - and it tells it clearer on Rallarvegen than many other places.

Rekvesøyane

Rekvesøyane

29.03.2018 - 11:53

The sediment that was deposited from the river Dyrvo has created the fan-shaped delta Rekvesøyane. The bit of land farthest out toward the water gets periodically flooded, especially during snow melt and after periods of much rain.

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