A magnitude 8.7 earthquake rattled northern Sumatra, Indonesia, on March 28, 2005, at 11:09 p.m., local time. At least 330 people are dead, but Indonesian officials expect the toll to soar over 2,000. The earthquake was centered 160 kilometers southeast of the 9.0 quake that triggered the devastating December 26,2004, tsunami, between the islands of Simeulue and Nias. The most severe damage appears to be on Nias, where large parts of the city Gunungsitoli were destroyed.
The United States Geological Survey reports that the March 28 quake occurred on the same fault that triggered the December 26 earthquake, probably as a result of stress placed on the fault by the first quake. The above map shows the locations of both earthquakes off the northwest coast of Sumatra. The March 28 earthquake occurred in a section of the fault just south of the part of the fault that slipped on December 26. The last time this section of fault moved was in 1861, when a large earthquake triggered a fatal tsunami.
As the image illustrates, the earthquakes occurred just east of the Sunda Trench, the deep underwater canyon where the Australia Plate is being pulled under the Sunda Plate. The plates, giant sections of the Earth’s crust, float on a layer of soft rock, propelled by convection currents beneath them. The Australia plate moves about five centimeters northeast in relation to the Sunda plate every year. As the Australia plate has crumbled under the Sunda plate, a number of faults have developed in the Sunda plate, including the thrust fault that produced both the December 26 and March 28 quakes.
According to the Pacific Tsumani Warning Center, sea level readings taken after the March 28 earthquake show that a small tsunami was generated, but there have been no reports of damage. Why did the 9.0 earthquake generate a massive tsunami compared to the small wave that came out of the most recent earthquake? By USGS estimates, both earthquakes occurred about 30 kilometers (18.6 miles) beneath the Earth’s surface, but the March 28 quake was much smaller and probably didn't displace the same amount of earth as the December 26 quake.
The contrast in ocean depths between the Australia Plate and the Pacific Plate near the Solomon islands reveals the subduction of the former beneath its northeastern neighbor. This subduction was responsible for the 7.2-magnitude quake on January 4, 2010.