How did the Fukushima tsunami affect the economy?
The disaster disrupted supply chains and trade, with industrial production dropping sharply in the following months. Many of Japan’s nuclear power reactors were shut down for safety checks following the nuclear emergency at the Fukushima Dai-ichi plant, causing electricity shortages in some areas of East Japan.
What was the impact of the Tohoku earthquake?
Land fall – some coastal areas experienced land subsidence as the earthquake dropped the beachfronts in some places by more than 50 cm. Damage – 332,395 buildings, 2,126 roads, 56 bridges and 26 railways were destroyed or damaged. 300 hospitals were damaged and 11 were totally destroyed.
What were the long term effects of the Tohoku earthquake?
The mean rate of increase in disability prevalence in coastal (14.7%) and inland (10.0%) disaster areas was higher than in non-disaster areas (6.2%) (P < 0.001). During the 3 years after the earthquake, the increase of disability prevalence from before the GEJE continued to be higher in the disaster-stricken areas.
Who responded to the 2011 Japan earthquake?
Following the 2011 Tōhoku earthquake and tsunami, Japan received messages of condolence and offers of assistance from a range of international leaders. According to Japan’s foreign ministry, 163 countries and regions, and 43 international organizations had offered assistance to Japan as of September 15, 2011.
What were the causes of the Tohoku earthquake?
The earthquake was caused by the rupture of a stretch of the subduction zone associated with the Japan Trench, which separates the Eurasian Plate from the subducting Pacific Plate.
Where was the epicenter of the Tohoku earthquake?
The 9.1-magnitude (Mw) undersea megathrust earthquake occurred on 11 March 2011 at 14:46 JST (05:46 UTC) in the north-western Pacific Ocean at a relatively shallow depth of 32 km (20 mi), with its epicenter approximately 72 km (45 mi) east of the Oshika Peninsula of Tōhoku, Japan, lasting approximately six minutes.
How bad is a 4.5 earthquake?
Events with magnitudes greater than 4.5 are strong enough to be recorded by a seismograph anywhere in the world, so long as its sensors are not located in the earthquake’s shadow. The following describes the typical effects of earthquakes of various magnitudes near the epicenter.