Contact: Knut van der Wel
The Research Council of Norway
Named Åknesremna (the Åknes Rift), the crack is located at an elevation of about 800 metres above sea level in Møre & Romsdal County. It is widening by three to 10 centimetres each year. Researchers know that this can only mean one thing: a landslide is imminent - and this won't be the first time.
Tidal waves in Norway
Norway has experienced several huge tidal waves along the coastline and in the fjords. The best known disaster is the Tafjord slide that occurred in 1934. Parts of the mountainside simply dropped off, causing a 64-metre high tidal wave to wash about 200 metres inland. It completely wiped out the villages of Tafjord and Fjøra in Møre & Romsdal County.
Can happen again
Researchers are painfully aware that disasters like that can happen again. Consequently, they want to do everything they can to ensure the earliest possible warnings as there will be no time to spare. They have calculated that if the Åknesremna were to break off, the tidal wave would reach Geiranger just ten minutes later! In other words, every second will count.
A state-of-the-art surveillance system records the tiniest little movement in the mountain. Using lasers, radar and GPS, the mountain is studied carefully. There is even a weather station that provides continuous weather reports from the area. It is important to keep an eye on the wind, precipitation and temperature.
Unfortunately, these steep mountainsides are not very easily accessible. For that reason, eight helicopter pads have been built in the mountain highlands. Helicopters convey people and equipment to where they are needed. There are also two bunkers where the researchers have provisions, electricity and sleeping accommodations.
Automatic early warning
It is particularly important to keep an eye on the systems of cracks, or fractures as they are called. From experience, researchers know that the level of activity increases as a landslide becomes imminent. In a manner of speaking, when the mountain gets very active, it sends out its own early warning. By constant monitoring, researchers therefore believe that they can predict a slide least one day in advance.
Surveying and monitoring are not limited to the mountainsides. To be prepared as well as possible in the event of a landslide, it is also important know a great deal about the seabed in the fjords. Such knowledge makes it possible to calculate how high the waves can be, and how quickly they will travel up the fjord. By mapping the shore zone, scientists can figure out how far waves will wash up on shore.
Breaking the waves
Scientists have vast amounts of data from readings and from disasters as a result of past slides and floods. Computers allow them to use the data to simulate what would happen if there were to be a landslide. They can predict where the tidal wave will peak, and where it will be most dangerous.
This information is especially important for municipalities, so that they can prevent building and construction, etc., in dangerous locations. This enables them to avoid the type of disasters that have struck this and other areas so many times before.