Strong earthquake M 6.1 struck near east coast of Honshu, Japan

strong-earthquake-m-6-1-struck-near-east-coast-of-honshu-japan

A strong earthquake M 6.1 struck near east coast of Honshu, Japan on May 18, 2013 at 05:48 UTC. Epicenter of the earthquake was located 50 km (31mi) NE of Namie, Japan and 61 km (38mi) ESE of Watari, Japan at coordinates 37.761°N 141.454°E. USGS recorded depth of the earthquake at 41.5 km (25.8 mi) whereas EMSC reported depth at 60 km and same magnitude as USGS.

JMA is reporting M 5.9 earthquake at depth of 50 km.

According to GDACS, this earthquake can have a low humanitarian impact based on the magnitude and the affected population and their vulnerability.

There are about 3 010 000 people living within 100 km radius of the earthquake.

honshu earthquake intensity

Earthquake intensity map. Credits: USGS

Tectonic summary by USGS

Seismotectonics of Japan and Vicinity

Japan and the surrounding islands straddle four major tectonic plates: Pacific plate; North America plate; Eurasia plate; and Philippine Sea plate. The Pacific plate is subducted into the mantle, beneath Hokkaido and northern Honshu, along the eastern margin of the Okhotsk microplate, a proposed subdivision of the North America plate. Farther south, the Pacific plate is subducted beneath volcanic islands along the eastern margin of the Philippine Sea plate. This 2,200 km-long zone of subduction of the Pacific plate is responsible for the creation of the deep offshore Ogasawara and Japan trenches as well as parallel chains of islands and volcanoes, typical of Circumpacific island arcs. Similarly, the Philippine Sea plate is itself subducting under the Eurasia plate along a zone, extending from Taiwan to southern Honshu that comprises the Ryukyu Islands and the Nansei-Shoto trench.

Subduction zones at the Japanese island arcs are geologically complex and produce numerous earthquakes from multiple sources. Deformation of the overriding plates generates shallow crustal earthquakes, whereas slip at the interface of the plates generates interplate earthquakes that extend from near the base of the trench to depths of 40 to 60 km. At greater depths, Japanese arc earthquakes occur within the subducting Pacific and Philippine Sea plates and can reach depths of nearly 700 km. Since 1900, three great earthquakes occurred off Japan and three north of Hokkaido. They are the M8.4 1933 Sanriku-oki earthquake, the M8.3 2003 Tokachi-oki earthquake, the M9.0 2011 Tohoku earthquake, the M8.4 1958 Etorofu earthquake, the M8.5 1963 Kuril earthquake, and the M8.3 1994 Shikotan earthquake. More information on regional seismicity and tectonics

Featured image:  ©2013 TerraMetrics, Map Data ©2013 Google

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