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Bergesfjellet

Bergesfjellet

12.03.2018 - 13:17

Bjellandsvatnet (Bjørn Moe)

Bjellandsvatnet

06.05.2019 - 09:44

Lake Bjellandsvatnet is one of the richest wetland areas in Sveio. But, everything has its limit, and the supply of nutrients can be too much. This is what was about to happen in Lake Bjellandsvatnet.

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.

A zone with nuggets from the inner earth.

Drøna

12.03.2018 - 13:01

Potholes by the Koldals River

Eikelandsosen

29.03.2018 - 11:29

"So many and such big potholes as are found at Eikelandsosen, we don't see other places in western Norway, and as beautifully polished as the mountainside is along the river up to Koldal , one would look a long time to see anywhere else. There is much to dazzle a geologist's eyes. If only these features could bring others the same joy!"

Eio

Eio

18.03.2019 - 09:21

A silled lake at Ekse

Eksingedalen- hydropower development

13.12.2018 - 16:56

Water discharge at the outlet of the Ekso into Eidsfjord was halved after the big hydropower development in the mountainous area between Modalen and Eksingedalen and further southward toward Evanger in the 1960s, 70s and 80s. In an attempt to amend the changed environmental conditions in the waterway the developer built 35 small dams in the river.

Ekso ved Eidslandet, Eidsfjorden i bakgrunnen

Ekso

21.03.2019 - 15:46

In the late 1800s, Ekso was known among the nobility in England as having among the best salmon rivers. In summer the Lords could haul in big fish of up to 25 kg. In return, the townsfolk were paid for fishing rights, lodging and local assistance.

Whitefish

Engesundsvatnet

31.03.2018 - 21:17

Espevik

Espevik

03.01.2019 - 15:26

220 million years ago, glowing hot molten rock masses intruded into fractures in the earth's crust in the outer parts of Hordaland. Some of these are believed to have reached the surface and formed lava flows, which since have been eroded away by wind and weather. But, most of these flows solidified into diabase sills before they got to the surface.

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