Alvøen

Alvøen is one of the oldest industrial places in Norway. As early as the 1620s a gunpowder mill was built here. The place itself was well situated for industrial activity, lying only 100 m from the waterfall, which provided power for the mill, and a good harbour wherefrom the products were shipped. The success of the gun-powder mill varied in the 1600s and 1700s, but what made Alvøen best known was its paper production.

Bergesfjellet

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.

Bondhusdalen

The Bondhus area in Maruanger has been a magnet for tourists ever since the stream of tourists to Norway's west coast began in the middle of the 1800s. The magnificent landscape with the "ice trail" up to Bondhusvatnet Lake, the ice falls from Bondhusbreen glacier and Keisarstigen trail up to Folgefonna are still popular tourist attractions.

Botnavatnet

Bryggen

In the 1300s Bergen was a trading centre of European dimension. The town is thought to have had around 7000 inhabitants and was the largest and most important in the country. In a European context it was an average size town. At this time the most tightly built town area was still mostly east of Vågen from Holmen in the north to Vågsbotn in the south. Already in medieval times, latest in the 1340s, this area was called Bryggen.

Damsgård

As a fairytale castle Damsgård Hovedgård lies on the slope rising up from the Puddefjord. The old connection between the farm and the sea, as we see it on Dreier’s prospectus from 1810, has been broken up by roads and encroachments in the building mass. But the main building itself is a central monument in Norwegian architecture from the 1700s – one of the finest representatives for the rococo period, with a magnificent and rich décor both in its interior and exterior.

Dyrdal

If you journey along Austfjorden, you at the same time turn the pages of time back through Ice Age history. The landforms show how the landscape has developed gradually as the glaciers have grown - and melted again - in several episodes: from small cirques, we see innermost at Dyrdal, to larger fjords, like at Mas fjord further out.

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.

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.