Fig. 13

Comparison of the Q-LavHa simulation from the lowermost fissure of the 2002 eruption carried out on the SRTM DEM acquired in 2000 (A) and the TanDEM-X DEM acquired in 2012 (B), both at 30m spatial resolution. The topography of the 2002 lava flow (outlined in black), is present in the TanDEM X DEM but not in the SRTM DEM. Although differences can be noted between the simulation in the central and especially in the most distal part of the flow, the general areas susceptible to lava flow invasion remain very similar