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Large submarine earthquakes that occurred worldwide in a 1-year period (June 2013 to June 2014) – a contribution to the understanding of tsunamigenic potential

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Figure 1. Locations of the epicenters (red dots), event number (given in Table 1), date of occurrence and magnitudes of submarine earthquakeevents of Mw >= 6.7 that were analyzed during a 1-year period from June 2013 to June 2014.
Figure 2. Earthquake events which occurred in the west Pacific source zone: (a) overview of the source zone; location of the epicenters (redstars), focal mechanisms (red beach balls), and subduction zones (yellow lines) for: (b) the Okhotsk-Russia normal faulting event, (c) theAlaska thrust fault event, (d) the Honshu normal faulting event, (e) the Philippine reverse faulting event, and (f) six events, four around thePapua New Guinea, their focal mechanisms: three are normal faulting and one is thrust faulting, and two near the Solomon Island, their focalmechanisms: a strike–slip and a reverse faulting.
Figure 3. Earthquake events which occurred in the east Pacific source zone: (a) overview of the source zone; (b) location of the Californiaand Mexico events (red stars), their focal mechanism: thrust faulting and strike–slip faulting, respectively (red beach ball), the subductionzone (yellow line) and the spreading centers (red lines); (c) location of four events: the Peru event and three events in northern Chile (redstars), their focal mechanisms are thrust faulting (red beach ball), and the subduction zone (yellow line).
Figure 4. Earthquake events which occurred in the South Atlantic Ocean source zone: (a) overview of the source zone; (b) location of fiveevents: three around Scotia Plate, one near the Falkland Island and another one near Bouvet Island, their focal mechanisms are strike–slipfaulting (red beach ball), the subduction zone (yellow line), the transforms (magenta lines), the active spreading center and fracture zones(red lines).
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