VOLUME 4/3 x Pi x r^(3), r=1, = 4.2 m^(3), and Mass 4.2 x 2.4 = 10 (tons). Rocks moved by Ice and water may one day continue further down and result in a rockfall.or making a natural dam and result in a new hazard...All photos reserved

Mudslide, the Triggering area. Water accumulation due to heavy precipitation resulted in a slide picking up rocks and trees all the way down to farmlands. All photos reserved

Mudslide September 2019, seen from above, the gate through the forrest. All photos reserved

The power of a mudslide, the danger and hazard. From Vikøy, Kvam. All photos reserved

Mudslide in combination with rockslide, can be extreme hazardous. Water sampling  reduces  friction,  and gravity forces become greater than the friction forces.

A sudden happening, like water or snow sampling  in  a local area of heavy mud layers,  or rocks slipping away, can be the triggering event that makes the mudslide escalate downhill. Mean terrain angle of chance for slide, is mainly  37-38 degrees. 

From Rembesdal Lake, below the Icefall of Hardangerjøkul Icecap. photo NRK

GEOHAZARDS  is a common part of  Hardanger daily life.

Floods in rivers, snow and mud avalanches  and rockfalls are the dominating geohazards.

Roads are damaged and closed, from time to time. 

Jøkulhlaups were events of larger extent in previous periods,, and certainly Simadal valley in Eidfjord was often prone to floods due to the Hardangerjøkul melting and extreme accumulation of precipitation.

Mitigations like dams and tunnels, has changed the risk. 

The years 1895  and  1936  are well known for these events,  the jøkulhlaups, followed by huge floods in the valley river,  damaging farms and farmlands, roads,  bridges  and houses..

By luck, no one got lost..

 

In 1936,  in August,  a natural dam broke in front of Demmevatn Lake to the northwest of the Icefall, above Rembesdal Lake. Water from intensive summer melting suddenly made its way through  and below the ice  and flooded into the  lake and further with the Simadal Valley river . The entire valley bottom was reshaped....

This happened on a warm summer day with  clear sky. People escaped from the rising flood.

Later,    Rembesdal Lake has been  regulated and water draining tunnels   from the Demmevatn made larger , to ensure limited meltwater build up.