GLOF is low-frequency event, but it often causes enormous loss and damage of life, property and human environment in downstream regions. The economic losses caused by GLOF are much higher than the project costs to early consolidate moraine dam and release flood waters. Glacial lake outbursts can be very difficult and expensive to control, but regional exposure and vulnerability of exposed elements downstream can be reduced by improving adaptation capacity and risk management level.

Landslides have large negative economic and societal impacts, including loss of life and damage to infrastructure. Slope stability assessment is a vital tool for landslide risk management, but high levels of uncertainty often challenge its usefulness. Uncertainties are associated with the numerical model used to assess slope stability and its parameters, with the data characterising the geometric, geotechnic and hydrologic properties of the slope, and with hazard triggers (e.g., rainfall).

A large earthquake and tsunami took place in February 2010, affecting a significant part of the Chilean coast (Maule earthquake (Mw = 8.8). Dichato (37° S), a small town located on Coliumo Bay, was one of the most devastated coastal places and is currently under reconstruction. Therefore, the risk factors which explain the disaster at that time as well as perceived restoration 6 years after the event were analyzed in the present paper. Numerical modeling of the 2010 Chile tsunami with four nested grids was applied to estimate the hazard.