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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.

Sketch showing the process of formation of an esker.

Langavassfjellet

29.03.2018 - 11:35

Gneiss.

Frøland- Liarostunnel

16.06.2018 - 17:24

Gullbotnen

Gullbotnen

07.12.2018 - 10:32

A barren belt where almost nothing grows, runs through the forest on the east slope of Gullbotnen. But, along the west side of the main road there is a fertile zone that flourishes with several finicky plant types. The contrasts arise from the extreme variations in the nutrient content of the bedrock.

Notaholmen, Samnanger

Notaholmen

16.06.2018 - 17:28

The fishnet shed at Notaholmen stands as a reminder of the days when people used to row out on the fjord to set their nets. On Notaholmen the nets were dried, repaired and tanned. And it was a great advantage to store them in a place inaccessible for rats and mice.

Ådland

13.12.2018 - 08:31

Ådland, innermost in the Samnanger Fjord is an old church centre and transport centre; a nodal point in the transport from sea to land. The white painted church standing today, was built in 1851, but there were two older churches here in former centuries.

Garnets at Vågenes

Vågenes

18.06.2018 - 20:08

On Vågenes, on one of the prominences out toward Eitrevågen, one finds garnets in anorthosite. The garnets are both older, and not least bigger, than average.

Ystebøtræet, Radøy

Ystebøtræet

18.06.2018 - 20:08

The main house at Nedrevåge, Tysnes

Nedrevåge

19.06.2018 - 17:44

Vågsbygdo was severely hit by landslides and rock falls in the decades around 1700, in addition, the rivers transported masses of loose sediment, both large stones and gravel. A lot of what slid down from the Vågsliene (slopes at Våg) collected in Neravåge. It was so bad that the damage “never again can be remedied or restored”, it was said in 1670.

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