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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.
Tokagjelet
There is a sharp transition between the wide valley at Kvamskogen and the narrow Tokagjelet. The transition is no less dramatic when we come out of the crooked tunnels far down in the canyon, and the open Steinsdalen valley spreads out before us. The canyon both separates and joins together different epochs in western Norway's history.
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.
Møkstrafjordøyane
The sea keeps the bedrock in the outer skerries smooth and clean. When the bedrock is also varied and interesting, the setting is perfect for a discovery tour of these bare-faced outcrops.