The quake, which lasted about 100 seconds, bears little resemblance to the catastrophic 9.1 magnitude quake that struck the same region in December 2004. Yesterday’s quake was marked predominantly by ‘strike-slip’ motion – meaning that two sections of Earth’s crust rubbed against each other horizontally rather than one piece thrusting up over or down under another. The absence of vertical motion accounts for why the quake did not generate a major tsunami. Nevertheless, this quake has generated some provocative scientific. http://blogs.nature.com
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