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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.

Einstapevoll

Einstapevoll- slates

06.05.2019 - 09:53

“On the country of Wallestrand…the rock almost everywhere appears to be of a slate-like substance, be it at the seashore, on the farms or in their distant fields”.

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.

From a soapstone quarry at Lykling

Lykling- soapstone

22.08.2018 - 15:58

The old limestone quarry is today rebuilt and become Moster Amfi.

Moster amfi

18.06.2018 - 20:18

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.

From Rubbestadneset.

Rubbestadneset

18.06.2018 - 20:20

Siggjo from the south. (Svein Nord)

Siggjo

18.06.2018 - 20:21

Siggjo is a cone-shaped, volcano-like mountaintop in the part of Hordaland where one finds the best preserved volcanic rocks. The rock types originate from one or several volcanoes that spewed out glowing lava and ash. But, the shape of the mountain, as it appears today, formed later and by completely different forces.

Ramnagjelet, Ulvik

Ulvik-village

04.12.2018 - 15:45

The ice cap that covered the land during each of the 40 past ice ages over the past 2 million years of Earth's history pressed down the crust of the earth - like a finger on a rubber ball. And when the ice finally loosened its grip 11,000 years ago, the earth's crust rose again, most where the ice was thickest, least where it was thin, quickly in the beginning, and later more slowly. To this day, the land in the inner part of Norway continues to rise by perhaps one millimetre per year. By and large, however, the crust in Hordaland has again reached equilibrium after the weight of the ice was removed.

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