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A flight from Praia a Mare to Castrovillari in Southern Italy shows a map of the ground deformation occurred between 2012 and 2014. These results are from Italian National Research Council (CNR), Italian National Institute for Geophysics and Volcanology (INGV) and Italian Department of Civil Protection. The study shows that during the long seismic swarm occurred in the Pollino area between 2010 and 2014 the earthquakes were accompanied by an aseismic slow slip of the interested faults. This contributes to release of a part of tectonic deformation that would be otherwise associated with earthquakes and could explain why, compared to the rest of the Apennines, larger magnitude earthquakes were relatively less frequent in the past in the Pollino area. The complete study is published on Scientific Reports and can be freely accessed from the following link: http://www.nature.com/articles/s41598... Video in Italiano: • Mappa di deformazione del Pollino (Calabri...