Fig. 6From: Effusive crises at Piton de la Fournaise 2014–2015: a review of a multi-national response modelLava flow paths forecast by DOWNFLOW for the May 2015 eruption for noise levels (Δh) of 0.8 m and 2.5 m on the shaded relief of the same DEM used to run DOWNFLOW. The slope taken down the steepest descent path was that sent to LMV for initialization of FLOWGOBack to article page