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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.
Kvamskogen
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.
Tangarås
From his loft window on the doctor’s farm at Tangarås the young Hans Ernst Kinck had a view of the fjord and the Mauranger mountains. The fjord settlements in West Norway made a strong impression on the young boy when his family moved from Setesdal, from “the stifling mystique of the ballad”, to Strandebarm in 1876. The new district doctor bought the old captain’s farm at Tangarås, which had for some time been a military head farm after Håbrekke further into the settlement.
Vesoldo
Folds are to be found everywhere in the remains of the Caledonian mountain chain. Some were formed during the collision with Greenland, others stem from the time when the mountain chain collapsed. Few can compare with the giant fold that remains in the mountain area around Tørvikenuten, Vesoldo and Hellefjellet.
