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Gneiss.

Frøland- Liarostunnel

16.06.2018 - 17:24

Soft shapes in the hard mountain.

Grasdalen

12.03.2018 - 13:08

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.

Øvre Kvernes

Kvernes

01.09.2020 - 15:45

Håkons Hall, Domkirken Church, Bergen Børs Stock Exchange, Permanenten and other well known buildings in Bergen are decorated with soapstone from Øvre Kvernes. The quarry is a big hole in the mountainside by the cliff just east of the farm buildings.

From Kvitingen nature preserve.

Kvitingen

16.06.2018 - 17:26

Few other places in Hordaland, or even the whole country, get as much rain as in the Samnanger mountains. The mountains here simply attract wetness. The weather station on Kvitingen has continuous measurements all the way back to 1900, and the measurements have documented several records for the county. The station is therefore much used as a reference for the rainfall in western Norway.

Boat engines, Norwegian Engine Museum in Skånevik

Skånevik- Norwegian engine museum

25.04.2018 - 21:25

Frostrøyk i Osdalføret.

Søfteland

04.12.2018 - 18:37

If you drive between Søfteland and Ulven on a clear spring morning, or an evening in late autumn, you are advised to be careful on the turns. The temperature on the road can fall to under 0 °C here long before other places in the municipality. On clear, still nights the earth's surface chills quite a bit. In exposed areas a layer of cold air develops very near the ground and the road surface can easily chill to below freezing.

Geologist William Helland-Hansen examining a quartz conglomerate in the Ulven Syncline on one of the hills by the north west end of Lake Ulvenvatnet.

Ulven

03.01.2019 - 15:16

In the region of Ulven phyllite occurs with Hordaland's youngest fossils, and a beautiful quartz conglomerate. The phyllite and conglomerate got squeezed into the bottom of an ancient oceanic crust, made of gabbro and greenstone, in the heart of the Caledonide mountain chain.