On Monday 6 February, at 4.17 a.m., a 7.8 magnitude earthquake struck Turkey and Syria. Earthquakes in this part of the world are common, but the magnitude of this one is clearly impressive: to find an earthquake this strong on this fault, you have to go back to 1114. Ten minutes after the strongest quake, a 6.7 magnitude aftershock occurred near the epicentre and other aftershocks continue to occur in an area stretching over 350 kilometres from eastern Turkey to the Syrian border. These 'aftershocks', the earthquakes that occur after a major earthquake, are expected and their statistical behaviour is well known. More surprisingly and dramatically, a second earthquake of magnitude 7.5 occurred at 13:24 local time, further north. This earthquake is not an aftershock: according to the first data processed live by the major international seismological agencies, it occurred on an east-west fault cutting the main rupture. We do not yet have all the information provided by satellite...