- Remove Quarns and mills filter Quarns and mills
- Remove Nordhordland filter Nordhordland
- Remove Large landforms filter Large landforms
- Remove Hydro power filter Hydro power
Bjørsvik
The industrial settlement Bjørsvik
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.
Hummelfossen
As early as 1906 the Matre and Haugsdal waterway was bought up by the businessman Blauuw from Bergen; the first “waterfall speculator” in the Matre area. He immediately resold it to Fr. Hiorth, who transferred all the rights to the company Matrefaldene in 1908. Behind A/S Matrefaldene were German interests, Badische Anilin und Sodafabrik, which wanted to start production of saltpetre fertilizer with nitrogen and electricity.
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.
Stølsheimen
The large mountain area between Modalen, the Voss communities and Sogn is one of the finest mountain pasture areas in West Norway. In older times this area was called Steinslandsheimen, in our times it has acquired the name Stølsheimen. Power development and protection interests have been opposed here. The core area of Stølsheimen has now been protected as a landscape protection area, while some of the oldest mountain farms have been flooded. A register in the 1970s comprised almost 40 mountain farm settlements in the central area of Stølsheimen, belonging to Modalen, Høyanger and Vik municipalities.
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.