December 16

Mount Fuji Begins Its Last Major Eruption

170718th CenturyDisasterEast Asiahighexpanded detail

The Hōei eruption of Mount Fuji began on December 16, 1707, and unleashed one of Japan’s most significant volcanic events in centuries, scattering ash across eastern Honshu without producing lava flows.

Summary

In the early 18th century, Japan under the Tokugawa shogunate experienced relative stability after earlier periods of warfare, but natural disasters posed ongoing threats to agriculture and population centers. Mount Fuji, a sacred and prominent volcano on Honshu island, had been dormant for centuries prior. On December 16, 1707, during the Hoei era, the volcano erupted explosively from a new vent on its southeastern flank, ejecting vast quantities of ash, pumice, and scoria in a Plinian-style event. The eruption continued intermittently until February 1708, blanketing eastern Japan with ash layers up to several feet thick in places and triggering landslides. Immediate effects included respiratory issues, crop failures, and famine across affected regions, though no direct lava flows occurred.

Context

Japan in the early 18th century enjoyed relative peace under the Tokugawa shogunate, which had consolidated power after the turbulent Sengoku period and established a centralized feudal system centered in Edo. Mount Fuji, revered in Shinto and Buddhist traditions and visible from the capital, had shown no major activity for centuries, though minor seismic signals occasionally reminded residents of its presence in the tectonically active Ring of Fire. The broader society depended heavily on agriculture in the provinces surrounding the volcano, making any disruption to farmland a potential crisis for food security and social stability.

What Happened

On December 16, 1707, during the fourth year of the Hōei era, explosive activity commenced from new vents on Mount Fuji’s southeastern flank, ejecting plumes of ash, pumice, and scoria high into the atmosphere in a Plinian-style eruption. The event unfolded over several days, beginning with an initial earthquake and ejection of cinders that soon gave way to more intense discharges of rock and finer material; three distinct vents, later numbered 1 through 3, opened in succession. Ash drifted eastward, reaching the city of Edo roughly 100 kilometers away within hours and accumulating several centimeters thick in places, while provinces such as Izu, Kai, Sagami, and Musashi experienced heavier falls. The eruption continued intermittently through the winter, powered in part by the mixing of different magma types, and ceased on February 24, 1708.

Aftermath

Immediate effects centered on widespread agricultural damage as volcanic ash smothered fields and stunted crop growth across eastern Japan. Farmers in affected areas attempted to clear debris, but heavy rains in the following summer washed ash into rivers such as the Sakawa, creating temporary dams that later burst and triggered destructive floods and landslides on the Ashigara plain. Starvation followed in many communities, with the loss of harvests compounding respiratory difficulties from lingering ash; no precise death toll exists, but famine claimed numerous lives in the Fuji region and beyond.

Legacy

The Hōei eruption remains Mount Fuji’s last confirmed major activity, shaping Japanese understanding of volcanic hazards and prompting greater attention to land management and disaster preparedness in subsequent centuries. Its distinctive crater on the southeastern slope, now accessible via hiking trails, serves as a tangible reminder, while the event continues to inform modern geological monitoring and risk assessments for the densely populated Kanto region. Artistic depictions, including later works by Hokusai, further embedded the eruption in cultural memory of the volcano’s power.

Why It Matters

The Hoei eruption demonstrated the volcanic risks even to seemingly stable landscapes and prompted long-term changes in land use and disaster awareness in Japan. It remains the most recent confirmed activity at Mount Fuji, influencing geological studies and hazard planning for one of the world's most iconic volcanoes into the modern era.

Related Questions

Why is the 1707 eruption called the Hōei eruption?

It occurred during the fourth year of the Hōei era in the Japanese calendar and created a new crater area later named Mount Hōei.

Did the eruption produce lava flows?

No; it was an explosive Plinian event that released only ash, pumice, and scoria without surface lava.

How far did the ash travel?

Ash reached Edo (modern Tokyo) about 100 kilometers away, with measurable deposits in several surrounding provinces.

What role did earthquakes play?

The 1707 Hōei earthquake, occurring weeks earlier, is thought to have helped mobilize magma by altering stresses beneath the volcano.

Has Mount Fuji erupted since 1708?

No confirmed major eruptions have occurred; a few unverified reports exist, but 1707–1708 remains the last verified event.

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Sources

  1. Hōei eruption, Wikipedia. Accessed 2026-07-07.
  2. Dec 16, 1707 CE: Most Recent Eruption of Mount Fuji, National Geographic. Accessed 2026-07-07.
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