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From Russia Today:
An earthquake of 7.3 magnitude has hit 231 miles (371 kilometers) east of Japan’s Honshu Island with tremors felt in Tokyo. The quake prompted an evacuation at the devastated Fukushima Daiichi plant and sent tsunami fears across 5 prefectures.
The quake struck at a depth of 10 kilometers at 17:10 GMT, 320 kilometers southeast of Ishinomaki in Miyagi Prefecture, according to the US Geological Survey. Strong tremors could be felt on Japan’s main Honshu Island, as well as on the northern island of Hokkaido.
From Fox News:
A magnitude 7.3 earthquake hit the Fukushima region of Japan Saturday morning, according to the U.S. Geological Survey.
The quake hit Japan’s east coast at 2:10 a.m. Tokyo time, near the crippled Fukushima nuclear site. The tremor was felt in Tokyo, some 300 miles away.
Japan’s emergency agencies declared a tsunami warning for the area.
Oct 25, 2013 at 2:31p ET (h/t Anonymous tips): 7.3-magnitude quake rocks Japan […] An earthquake of magnitude 7.3 struck early Saturday morning off Japan’s east coast, the U.S. Geological Survey said. Japan’s emergency agencies declared a tsunami warning for the region that includes the crippled Fukushima nuclear site. […] NHK reported that Tokyo Electric Power Co., the operator of the Fukushima plant, ordered workers near the coast to move to higher ground. […]
Oct. 25, 2013: The October 25, 2013 M 7.3 earthquake offshore of Honshu, Japan occurred as the result of normal faulting in the shallow oceanic crust of the Pacific plate. The earthquake occurred outboard (east) of the Japan Trench, which marks the seafloor expression of the subduction zone plate boundary between the Pacific and North America plates, and is immediately up-dip of the source region of the March 2011 M 9.0 Tohoku earthquake. […] The location, depth, and focal mechanism of the October 25 2013 event are consistent with normal faulting rupture near the outer-arc high of the Japan Trench. In this region, normal faulting is encouraged by both the bending of the Pacific plate as it enters the subduction zone, and by stresses transferred from the locked subduction thrust interface to the west. Since the March 2011 Tohoku earthquake, two large events of M 7.7 and M 7.3 have occurred in the vicinity of the October 25, 2013 earthquake. […]