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.

Dalseid- Eidslandet road construction

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.

Bolstad

The village at Bolstadøyri acquired its structure around the middle of the 1800s, but from the old days there has been a meeting place here; court location and trading post. The guesthouse place stems from the second half of the 17th century, and in the previous century Bolstadøyri was one of the largest rural trading posts in Nordhordland.

Brekkhus

Hamlagrø

The type of underlying rock can be decisive for how many different types of plants are found in an area. In the area around Hamlagrø-lake the diversity is especially obvious. The geological conditions change much here within a short distance.

Stalheimskleiva

From the oldest times on record in Norway one of the most important traffic arteries between west and east Norway has passed across Bolstad – Voss – Stalheim – Gudvangen and Lærdal. The post road between Oslo and Bergen was established here 1647, but in Stalheimskleiva there was only a packhorse track right up to the 1840s. Wheeled transport and carts were in little use in the mountains in West Norway up to that time.