Saturday, July 09, 2011 at 07:57:12 PM (CDT) - Central Daylight (Chicago)
The USGS reports a 7.0 magnitude earthquake off the eastern coast of Honshu, Japan on on July 09, 2011 at 07:57:12 PM (CDT) - Central Daylight (Chicago).
According to the shake map the severity was a level IV or "Light". As with the previous less severe 5.6 Magnitude quake on 7/7/2011 no damage was reported, although a tsunami warning was issued. Per the following AP article:
The earthquake caused visible shaking as per the following Reuters video:
Date: Saturday Jul. 9, 2011 10:44 PM ET
TOKYO — A strong earthquake with a magnitude of 7.1 hit Japan's northeastern coast on Sunday, prompting a tsunami warning for the area still recovering from a devastating quake and killer wave four months ago.
Residents in coastal areas were warned to evacuate, but there were no immediate reports of damage.
The quake hit at 9:57 local time (0057 GMT), and a warning of a tsunami was issued for most of the northeastern coastline. The epicenter of the quake was in the Pacific Ocean off the coast of Japan's main island, Honshu, at a depth of about 6 miles (10 kilometres).
Japanese officials predicted the quake could generate tsunami of up to 20 inches (50 centimetres), but the initial waves were only about 4 inches (10 centimetres).
Japan's northeastern coastline was devastated by an earthquake and tsunami on March 11 that left nearly 23,000 dead or missing and touched off a nuclear crisis at a badly damaged facility in Fukushima.
Officials said there were no reports of abnormalities at the Fukushima plant caused by Sunday's quake. Airports in the area were also functioning normally.
Japan is one of the world's most earthquake-prone countries. Dozens of strong aftershocks have been felt since the March 11 disaster, which measured a 9.0 magnitude and was the strongest in Japanese history.
Sunday's quake registered 4 on the Japanese scale of 7, meaning it was felt as moderately strong. Because of the damage from the March quake and tsunami, however, many buildings in the area are structurally weak and seawalls have been destroyed, making the region more vulnerable to relatively weaker quakes.