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Toward Støle and Sørheim, 1920.

The village of Etne

18.12.2018 - 20:39

Much of the sand and gravel that the town of Etne is built on was laid down at the end of the Ice Age and is evidence of melting glaciers and roaring meltwater rivers. The uncompacted material in the big terraces leave their unmistakeable mark on the wide elongated valleys.

Etne and the Etne delta around 1900.

Etnedeltaet

18.06.2018 - 20:23

During the latter half of the 1900s the big natural river deltas on Westland disappeared. Until the 1980s there was still a small, but significant remnant of the original river delta from the Etneelva river, but today most of this, too, is industrial land.

Langfoss (Alf Adriansen)

Langfoss

29.03.2018 - 11:48

Boat engines, Norwegian Engine Museum in Skånevik

Skånevik- Norwegian engine museum

25.04.2018 - 21:25

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

Jordalsgjelet

Jordalen

13.01.2019 - 17:22

During the last ice ages, parts of the Voss river system were stolen and sent down Nærøydalen valley to Nærøy Fjord (Nærøyfjorden). Before this big river theft all of the rivers ran all the way from their sources in the mountains near the innermost part of the Sognefjord further southwards towards Voss. Evidence of the theft is still clearly visible in the terrain.

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.

The mighty scree by Langeland Farm

Teigdalen

19.06.2018 - 17:53

It is not surprising that there are several folk tales connected to the large and unusual scree deposit that is found at Langeland, uppermost in Teigdalen. It is said that folk have been taken into the mountains by these stone blocks and have come back and told about how the wood nymphs live. It is also said that packs of thieves hid here in the old days, both themselves and the treasures they had stolen.

Vosso between Evangervatnet and Bolstadfjorden.

The Vosso river network

07.12.2018 - 15:22

The Vosso is Hordaland's main artery, she has never run more richly than in our times, and no other river in western Norway carries so much water. The increase in the amount of water comes mainly from hydropower development, due to the transfer of water from other water systems. Climate change can also be a reason that the Vosso carries more water than before.

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