Måbødalen- geology

The old pack road had 1500 steps, where cars today gas through the mountain. The time of this hard work is over, and of getting used to the steep terrain, as well; only the view from the top is much the same as before. Vøringsfossen in summer is one of Western Norway’s biggest natural wonders. It marks the transition between the older, open part of the Sysendalen valley and the younger, narrow and winding valley of Måbødalen.

Skytjedalen

Sysendammen

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.

Holmeknappen

If you come by sea to Bergen and come up the Herdle Fjord, the yellow ochre marine shed at Holmeknappen is a well known landmark to starboard as you come close to the little shore settlement. In olden days Holmenknappen served important functions as a centre for a wide hinterland of the surrounding farms, warehouse, landing point, country store and later a steamer quay, a hotel (1896) and a dairy (1909). But today Holmeknappen is no longer a focal point. Transport and commercial routes have changed the old pattern

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.

Dale power station

In 1923 Bergenshalvøens Kommunale Kraftselskap (BKK) expropriated large areas for power plants and development of hydropower started soon afterwards. Dale power station with the two first aggregates, each of 14 MW was put into operation on 17 November 1927. In the supply reservoir in Storefossen 5152 cubic metres of concrete were cast, and a modern and well-equipped power station was built.

Eksingedalen- hydropower development

Water discharge at the outlet of the Ekso into Eidsfjord was halved after the big hydropower development in the mountainous area between Modalen and Eksingedalen and further southward toward Evanger in the 1960s, 70s and 80s. In an attempt to amend the changed environmental conditions in the waterway the developer built 35 small dams in the river.

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.

Moastølen