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Dale farm
The Dale farm lies well situated on the gravel by the river, below the mountain Beitelen. But a few stone throws further north, on the wide expanse behind the houses, there has been an older farmstead. Here there have been found a number of cooking hollows, pole holes, an old road and traces of something believed to have been a palisade. Finds from this oldest farmstead may be dated to the time of the migrations, 400-600 years A.D.
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.
Eksingedalen- landscape
Eksingedalen alternates between wide, flat flood plains with good farmland, and narrow passages with waterfalls where the roads cling to the mountainsides. The alternations in the landscape are a result of the sculpturing work by glaciers over several ice ages, and the deposition of the glacial river deposits when the last glacier finally melted back.