- Remove Small landforms filter Small landforms
- Remove Museum filter Museum
- Remove Late glacial filter Late glacial
- Remove Metamorphic rocks filter Metamorphic rocks
- Remove Meland, frå 2020 del av nye Alver kommune. filter Meland, frå 2020 del av nye Alver kommune.
- Remove Vaksdal filter Vaksdal
- Remove Farm sites filter Farm sites
- Remove Sveio filter Sveio
- Remove Bedrock filter Bedrock
Eldsfjellet
The eclogites in western Norway were formed when Precambrian basement rocks were squeezed and pressed down under great pressure deep under the Caledonian mountain chain. The process may well have triggered some of the deepest earthquakes the world has ever known. The clearest traces of this drama are found in and around Mt. Eldsfjellet, in peaceful Meland.
Bergsdalen
The mountains of western Norway are lovely to wander in. In Cambro-Silurian time it was the mountain itself that wandered. The mountain, or more correctly the bedrock, first moved eastward, then back a bit westward again. All this rocking back and forth in the mountains ended about 400 million years ago.
Einstapevoll- slates
“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”.