University of Bergen5 results
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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.
Last changed: 03.01.2019 | Content type: Place
Kvamskogen
02.12.2018 - 20:57
The different bedrock types that got shoved in over Hordaland in Cambro-Silurian times still remain, layer by layer, almost like a cake. But at Kvamskogen the cake has been turned upside down.
Last changed: 02.12.2018 | Content type: Place
