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Great Kantō Earthquake

1923 megathrust earthquake in Japan

  • 21 min read
  • 8 chapters
The current bridge was built in 1911. It withstood the Kanto Earthquake in 1923.
urbzoo · CC BY 2.0

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Through Earthquake and Plate tectonics

The event was a complex disaster, with modern research indicating it consisted of three consecutive shocks in the span of several minutes. The initial megathrust event in Kanagawa Prefecture was followed three minutes later by a magnitude 7.2 earthquake centered beneath Tokyo Bay, and two minutes after that by a magnitude 7.3 shock in Yamanashi Prefecture. Fires, exacerbated by strong winds from a nearby typhoon, spread rapidly through the densely populated urban areas, accounting for the majority of the devastation and casualties. The death toll is estimated to have been between 105,000 and 140,000 people, including tens of thousands who went missing and were presumed dead. Over half of Tokyo and nearly all of Yokohama were destroyed, leaving approximately 2.5 million people homeless. The disaster triggered widespread social unrest, including the Kantō Massacre, in which ethnic Koreans and others mistaken for them were murdered by vigilante groups based on false rumors.

In the aftermath, the Japanese government declared martial law and undertook extensive relief and restoration efforts. The earthquake prompted ambitious plans for the reconstruction of Tokyo, aiming to create a modern, resilient imperial capital under the leadership of Home Minister Gotō Shinpei. However, these plans were often met with political contestation, financial constraints, and local resistance, leading to a reconstruction that, while significantly improving infrastructure, fell short of the grandest visions. The disaster also fueled debates about national identity, modernity, and societal values, with many commentators interpreting the event as a divine punishment for perceived moral decline and advocating for spiritual and social regeneration.

The Great Kantō Earthquake remains a pivotal event in modern Japanese history, profoundly impacting urban planning, disaster preparedness, and social consciousness. 1 September is commemorated annually in Japan as Disaster Prevention Day.

Earthquake and immediate impact

The Kantō region of eastern Japan is prone to major earthquakes due to its location near complex tectonic plate boundaries. The 1923 earthquake occurred when the Philippine Sea Plate subducted beneath the Okhotsk Plate (sometimes considered part of the North American Plate) along the Sagami Trough. The initial shock, occurring at 11:58:32 JST on 1 September 1923, was a complex event. Modern analysis indicates a dual rupture on a broad trench-type fault: the first rupture occurred near Odawara in Kanagawa Prefecture, some 100 km (62 mi) southwest of Tokyo, followed about ten seconds later by a second shock on the other side of Sagami Bay near the Miura Peninsula. This was followed minutes later by two major aftershocks: a magnitude 7.2 earthquake beneath northern Tokyo Bay at 12:01, and a magnitude 7.3 earthquake in Yamanashi Prefecture at 12:03. Survivor accounts consistently describe these three distinct seismic events.

The earthquake immediately toppled structures, crushed people, and caused widespread panic. Survivor accounts describe an initial period of stunned silence followed by a frantic rush as people tried to reunite with family and salvage belongings. Engineer Mononobe Nagao recalled the earth shaking "back and forth for what seemed like 15 seconds", followed by violent vertical convulsions that knocked people to the ground. Writer Tanaka Kōtarō described the sound as akin to a giant "blackening whirlwind" churning up the earth from "deep underground".

Fires and pandemonium

Within 30 minutes of the first tremor, more than 130 major fires broke out across Tokyo, particularly in the densely populated eastern and northeastern sections. These fires were fueled by overturned charcoal braziers used for midday meals, leaking gas from ruptured lines, and flammable debris from collapsed wooden buildings. Strong winds, associated with a typhoon passing off the coast, fanned the flames, creating massive firestorms that swept through the city. The air temperature in some areas reached 46 °C (115 °F).

The combination of ongoing aftershocks and rapidly spreading fires led to pandemonium. Millions of residents attempted to flee, often carrying their possessions, which clogged the already damaged streets and bridges. Kawatake Shigetoshi described being trapped in a "wave of people" in eastern Tokyo, unable to move as fires approached from multiple directions. Many sought refuge in open spaces, such as parks and the grounds surrounding the Imperial Palace, but these areas quickly became overcrowded. Waterways like the Sumida River also became congested with boats as people tried to escape by water, only to face sparks and burning debris falling from the sky. The disaster quickly overwhelmed Tokyo's infrastructure and its capacity for an orderly evacuation.

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