the risk of a Tsunami is much less.
http://earthquake.usgs.gov/recenteqsww/Quakes/usaxay.htmThis earthquake occurred near the western boundary of the aftershock zone of the devastating December 26th, 2004 earthquake. The aftershock zone of the December 26th earthquake continues to be active and forms a crescent-shaped region extending about 1200 km north of Sumatra, Indonesia. The recent event was a strike-slip earthquake in the Burma plate near its boundary with the India plate. Strike-slip earthquakes generate horizontal motion across a fault. This is unlike the motion caused by the December 26th earthquake that was the result of thrust-faulting on the interface of the India plate and the Burma plate, in which the India plate thrust beneath the overriding Burma plate. Given the different mechanisms, the recent event did not occur on the same fault that caused the Great Sumatra-Andaman Islands earthquake. However, the two earthquakes are almost certainly related. A great earthquake can trigger earthquake activity on faults that are distinct from the main-shock fault plane, and separated from it by tens or even hundreds of kilometers. A magnitude 7.2 earthquake is considered a major earthquake, however the size of this recent earthquake pales in comparison to the December 26th earthquake. A 7.2 strike-slip earthquake typically ruptures a 15 km by 80 km patch along a fault, whereas the December, 2004 earthquake ruptured a patch of fault about 1200 km long and 200 km wide.