How the 2011 Earthquake Shifted Japan Eastward: A Geological Perspective

Just 15 minutes after the powerful magnitude 9 Tohoku earthquake struck Japan on March 11, 2011, nearly all of the country shifted eastward by approximately half a centimeter. This seismic shift resulted from incredibly strong seismic waves that traveled 5,800 kilometers deep into the Earth and then rebounded to the surface.

While a 5-millimeter shift may seem trivial amid the devastation, it is crucial to understand that it occurred over a staggering distance of 3,000 kilometers. This distance is nearly seven times the length of the main rupture line of the earthquake, marking it as the largest recorded slip of its kind.

Notably, the unique timing and pattern of this event are significant. According to Park Sun Young of the University of Chicago, “No typical earthquake dynamics occurred at that precise moment, and a similar 5-millimeter eastward shift occurred almost simultaneously throughout most of Japan.”

The alterations were remarkable, extending not just from north to south but throughout the entire nation and even affecting the surrounding oceans.

“It’s not merely a singular ‘edge’ moving,” Park explained. “The eastward shift is widespread across Japan, particularly where GPS stations are present. With a similarly high density of sensors on the ocean floor, we could ascertain more precisely how widespread this offshore movement is. However, on land, this shift is observable almost universally across Japan.”

By analyzing extensive GPS and seismic data collected during the disaster, Park and his colleagues investigated how such massive shifts were instigated and why the rupture transpired 15 minutes post the main shock.

Earthquakes typically generate waves that penetrate deep into the Earth and reflect off its core; however, these waves usually lose strength by the time they resurface. In the Tohoku event, the main shock was so powerful that, despite the weakening of the original wave, it remained robust enough to induce tremors nationwide, as four adjacent tectonic plates moved synchronously.

“We surmise that the intense shaking from the initial Tohoku earthquake weakened the plate boundaries, rendering them more prone to movement when these nuclear reflection waves reached them,” states Professor Park.

This incident highlights a newly identified post-earthquake rupture mechanism, suggesting a need for awareness of potential seismic hazards from waves that travel deeper and over much larger distances following significant earthquakes, potentially triggering additional seismic events.

Further research is essential to understand the implications of this phenomenon in other global regions susceptible to similar seismic vulnerabilities, as noted by Robin Lee from the University of Canterbury, New Zealand.

“This illustrates that major earthquakes can instigate widespread delayed faulting within minutes and across a significantly larger area than previously expected,” Lee stated.