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the main shock of the 2004 indian ocean earthquake produced a maximum ground acceleration of about 7.6 g, which is equivalent to the force of about one-third of a g-force (1 g is equal to 9.8 m/s2). the maximum ground acceleration is measured to the east of the hypocenter.
figure 1. four seismograms for the m=7.5 2004 sumatra-andaman earthquake. the first shows the record of the larger 2004 indian ocean earthquake (m=9.1) that occurred near the same time. the second is from the 2004 sumatra-andaman earthquake. the third is from the m=8.6 northern sumatra earthquake. the fourth is from a m=7.5 earthquake in western australia (blue arrow). after the m=9.1 indian ocean earthquake, the three offshore sumatran earthquakes were all well offshore and the local tsunami was much less than that produced by the 2004 indian ocean earthquake. note that the m=7.5 earthquake in australia was very distant from any coast and produced a small tsunami. the m=8.6 sumatra-andaman earthquake occurred at a depth of 5 km and ruptured through the trench, producing a large tsunami with massive vertical displacement.
the m=7.5 sumatra-andaman earthquake is a normal fault rupture. the slip from the sumatra-andaman earthquake is much smaller than that of the 2004 indian ocean earthquake. the rupture from the sumatra-andaman earthquake did not reach the trench, so it ruptured through the subduction zone. most of the energy from the 2004 indian ocean earthquake was transferred offshore to the trench. in contrast, the three aftershocks offshore sumatra released little energy and only a small fraction of the energy of the 2004 indian ocean earthquake. this is shown in figure 2.
the main shock of the 2004 indian ocean earthquake produced a maximum ground acceleration of about 7.6 g, which is equivalent to the force of about one-third of a g-force (1 g is equal to 9.8 m/s2). the maximum ground acceleration is measured to the east of the hypocenter. figure 1. four seismograms for the m=7.5 2004 sumatra-andaman earthquake. the first shows the record of the larger 2004 indian ocean earthquake (m=9.1) that occurred near the same time. the second is from the 2004 sumatra-andaman earthquake. the third is from the m=8.6 northern sumatra earthquake. the fourth is from a m=7.5 earthquake in western australia (blue arrow). after the m=9.1 indian ocean earthquake, the three offshore sumatran earthquakes were all well offshore and the local tsunami was much less than that produced by the 2004 indian ocean earthquake. note that the m=7.5 earthquake in australia was very distant from any coast and produced a small tsunami. the m=8.6 sumatra-andaman earthquake occurred at a depth of 5 km and ruptured through the trench, producing a large tsunami with massive vertical displacement. the m=7.5 sumatra-andaman earthquake is a normal fault rupture. the slip from the sumatra-andaman earthquake is much smaller than that of the 2004 indian ocean earthquake. the rupture from the sumatra-andaman earthquake did not reach the trench, so it ruptured through the subduction zone. most of the energy from the 2004 indian ocean earthquake was transferred offshore to the trench. in contrast, the three aftershocks offshore sumatra released little energy and only a small fraction of the energy of the 2004 indian ocean earthquake. this is shown in figure 2. 5ec8ef588b
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