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Last and largest New Madrid earthquake

When
1812–1813
Where
Epicenter near New Madrid, Missouri Territory; New Madrid and surrounding fissures
Episodes
2

The final and largest shock of the New Madrid sequence struck near New Madrid on 7 February 1812, at 09:45 UTC (3:45 am local time). Sources give conflicting magnitude estimates—M 7.4–8.6 in one account and about 7.5 in another—so the figure remains contested. The town lay in Missouri Territory, not yet the state of Missouri.

Episodes

  1. 7 February 1812 · Epicenter near New Madrid, Missouri TerritoryFinal and largest New Madrid shock

    A major earthquake struck near New Madrid, Missouri, at 3:45 am local time on 7 February 1812, with contested magnitude estimates.

  2. 1813 · New Madrid and surrounding fissuresDepopulation and fissures at New Madrid

    By 1813, fissures scarred both sides of the river near New Madrid, and the town's population had fallen from about 1,000 to roughly 300.

Background and detail

Background. The New Madrid fault system produced a series of intense intraplate earthquakes beginning 16 December 1811, with further large shocks in January and February 1812. Four of the largest earthquakes in recorded North American history, with moment magnitudes estimated at 7 or greater, occurred within this three-month period.

The February Shock. On 7 February 1812 at 09:45 UTC (3:45 am local time), an earthquake struck with its epicenter near New Madrid. One source estimates its moment magnitude at 7.4–8.6, while another gives about 7.5; the largest estimate exceeds 8, but the figures are not reconciled across sources.

Aftermath and Population. Eliza Bryan of New Madrid, Missouri Territory, wrote an eyewitness account in March 1812. A Methodist chaplain traveling with Andrew Jackson's 1813 Natchez Expedition recorded that fissures near New Madrid looked awful on both sides of the river, that the earth continued to shake at times, and that the town's population had fallen from roughly 1,000 before the earthquakes to about 300, as many alarmed residents departed.

Longer-Term Evidence. Hundreds of aftershocks followed over several years. Dendrochronology on old bald cypress in Reelfoot Lake recorded fractures and rapid growth after inundation, while cypress in the St. Francis sunklands showed slowed growth in the half century after 1812—signals interpreted as evidence of the 1811–12 series.

People involved

Sources

  1. 1811–1812 New Madrid earthquakes Wikipedia, revision of 2026-09-30
  2. New Madrid seismic zone Wikipedia, revision of 2026-06-30

Machine-drafted from the cited Wikipedia passages and checked by a reviewing model, not by a human editor. Every passage cites the revision it was written from; dates and places follow those passages.