During the last five decades since 1968, Elbasani zone in Albania is dominated by low seismicity. This fault has evidenced some seismological phenomena. It a transversal active with normal and strike-slip faults characterized low-velocity layers. From instrumental seismicity this area have been located 1831 seismic events, magnitude ML > 1.1 Richter 3 of them 5.0. Recently on May 19, 2014, m...