1811–1812 New Madrid earthquakes

Coordinates: 36°24′N 89°36′W / 36.4°N 89.6°W / 36.4; -89.6
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1811–1812 New Madrid earthquakes
The Great Earthquake at New Madrid, a 19th-century woodcut from Devens' Our First Century (1877)
1811–1812 New Madrid earthquakes is located in Missouri
1811–1812 New Madrid earthquakes
1811–1812 New Madrid earthquakes is located in Tennessee
1811–1812 New Madrid earthquakes
1811–1812 New Madrid earthquakes is located in the United States
1811–1812 New Madrid earthquakes
UTC time1811-12-16 08:15:00
 1811-12-16 13:15:00
 1812-01-23 15:00:00
 1812-02-07 09:45:00
USGS-ANSSComCat
 ComCat
 ComCat
 ComCat
Local date16 December 1811
 16 December 1811
 23 January 1812
 7 February 1812
Local time02:15
 08:15
 09:00
 03:45
Magnitude 
 Mw  7.5[1]
 Mw  7.0[2]
 Mw  7.3[3]
 Mw  7.5[4]
Max. intensityXII (Extreme)
AftershocksMw  6.3,[5] 6.3,[6] 6.1[7] & 6.3[8]
CasualtiesUnknown[9]
New Madrid fault and earthquake-prone region considered at high risk today

The 1811–1812 New Madrid earthquakes (/ˈmædrɪd/) were a series of intense intraplate earthquakes beginning with an initial earthquake of moment magnitude 7.2–8.2 on December 16, 1811, followed by a moment magnitude 7.4 aftershock on the same day. Two additional earthquakes of similar magnitude followed in January and February 1812. They remain the most powerful earthquakes to hit the contiguous United States east of the Rocky Mountains in recorded history.[10][11][12] The earthquakes, as well as the seismic zone of their occurrence, were named for the Mississippi River town of New Madrid, then part of the Louisiana Territory and now within the U.S. state of Missouri.

The epicenters of the earthquakes were located in an area that at the time was at the distant western edge of the American frontier, only sparsely settled by European settlers. Contemporary accounts have led seismologists to estimate that these stable continental region earthquakes were felt strongly throughout much of the central and eastern United States, across an area of roughly 50,000 square miles (130,000 km2), and moderately across nearly 3 million km2 (1 million sq mi). The 1906 San Francisco earthquake, by comparison, was felt moderately over roughly 6,200 sq mi (16,000 km2). The New Madrid earthquakes were interpreted variously by American Indian tribes, but one consensus was universally accepted: the powerful earthquake had to have meant something. For many tribes in Tecumseh's pan-Indian alliance, it meant that Tecumseh and his brother the Prophet must be supported.[13]

Events

The many more aftershocks include one magnitude 7 aftershock to the December 16, 1811, earthquake which occurred at 6:00 UTC (12:00 am local time) on December 17, 1811, and one magnitude 7 aftershock to the February 7, 1812, earthquake which occurred on the same day at 4:40 UTC (10:40 pm local time).[12] Susan Hough, a seismologist of the United States Geological Survey, has estimated the earthquakes' magnitudes as around magnitude 7.[16]

Eyewitness accounts

Linnean Society, was on the Mississippi on the night of December 15, 1811, and describes the tremors in great detail in his Travels in the Interior of America in the Years 1809, 1810 and 1811, published in 1817:[17]

After supper, we went to sleep as usual: about ten o'clock, and in the night I was awakened by the most tremendous noise, accompanied by an agitation of the boat so violent, that it appeared in danger of upsetting ... I could distinctly see the river as if agitated by a storm; and although the noise was inconceivably loud and terrific, I could distinctly hear the crash of falling trees, and the screaming of the wild fowl on the river, but found that the boat was still safe at her moorings. By the time we could get to our fire, which was on a large flag in the stern of the boat, the shock had ceased; but immediately the perpendicular banks, both above and below us, began to fall into the river in such vast masses, as nearly to sink our boat by the swell they occasioned ... At day-light we had counted twenty-seven shocks.

Eliza Bryan[18] in New Madrid, Territory of Missouri, wrote the following eyewitness account in March 1812:

On the 16th of December, 1811, about two o'clock, a.m., we were visited by a violent shock of an earthquake, accompanied by a very awful noise resembling loud but distant thunder, but more hoarse and vibrating, which was followed in a few minutes by the complete saturation of the atmosphere, with sulphurious vapor, causing total darkness. The screams of the affrighted inhabitants running to and fro, not knowing where to go, or what to do—the cries of the fowls and beasts of every species—the cracking of trees falling, and the roaring of the Mississippi— the current of which was retrograde for a few minutes, owing as is supposed, to an irruption in its bed— formed a scene truly horrible.

John Reynolds, the fourth governor of Illinois, among other political posts, mentions the earthquake in his biography My Own Times: Embracing Also the History of My Life (1855):[19]

On the night of the 15th of December, 1811, an earthquake occurred, that produced great consternation amongst the people. The centre of the violence was in New Madrid, Missouri, but the whole valley of the Mississippi was violently agitated. Our family all were sleeping in a log cabin, and my father leaped out of bed crying aloud "the Indians are on the house" ... We laughed at the mistake of my father, but soon found out it was worse than the Indians. Not one in the family knew at the time that it was an earthquake. The next morning another shock made us acquainted with it, so we decided it was an earthquake. The cattle came running home bellowing with fear, and all animals were terribly alarmed on the occasion. Our house cracked and quivered, so we were fearful it would fall to the ground. In the

the church bell in Cahokia sounded by the agitation of the building. It is said the shock of an earthquake was felt in Kaskaskia
in 1804, but I did not perceive it. The shocks continued for years in Illinois, and some have experienced it this year, 1855.

The Shaker diarist Samuel Swan McClelland described the effects of the earthquake on the Shaker settlement at West Union (Busro), Indiana, where the earthquakes contributed to the temporary abandonment of the westernmost Shaker community.[20]

Geologic setting

Reelfoot Rift

The underlying cause of the earthquakes is not well understood, but modern faulting seems to be related to an ancient geologic feature buried under the Mississippi River

igneous rocks formed from magma that was being pushed towards the surface. The resulting rift system failed to split the plate, but has remained as an aulacogen
(a scar or weak zone) deep underground.

More than 4,000 earthquakes have been reported in the New Madrid Seismic Zone since 1974.

In recent decades, minor earthquakes have continued.[21] The epicenters of over 4,000 earthquakes can be identified from seismic measurements since 1974, originating from the seismic activity of the Reelfoot Rift. Forecasts for the next 50 years estimate a 7-10% chance of a major earthquake like those of 1811–1812, and a 25-40% chance of a quake of magnitude 6 or greater.[22]

In a report filed in November 2008, the U.S.

transportation systems, and other vital infrastructure.[23]

Aftermath

The quakes caused extensive changes to the region's topography. Subsidence, uplift, fissures, landslides and riverbank collapses were common. Trees were uprooted by the intense shaking; people drowned when subsided land flooded. Reelfoot Lake was formed in Tennessee by subsidence of 1.5 meters to 6 meters in some places. Lake St. Francis in eastern Arkansas was expanded by subsidence, with sand and coal being ejected from fissures in the adjacent swamps as water levels rose by 8 to 9 meters. Waves on the Mississippi River caused boats to wash ashore; river banks rose, sand bars were destroyed, and some islands completely disappeared.[24] Sand blows occurred in Missouri, Tennessee, and Arkansas, covering farmland.

Tilted trees following the New Madrid Earthquakes.

The continuous underlying rock mass, uninterrupted by fractures or faults, conducted the seismic waves from the earthquakes over great distances, with perceptible ground shaking as far away as Canada.[25] Intense effects were widely felt in Illinois, Arkansas, Tennessee, Kentucky and Missouri.

The number of people who died is unknown; as a frontier area, the region was sparsely populated, and communications and records were poor. The predominantly wooden buildings resisted collapse,[25] though the intense shaking caused many chimneys to fall, wood structures to crack, and trees to fall on buildings,[24] particularly in the epicentral area during the first earthquake on December 16, 1811.[24]

Rated at VII on the Mercalli Intensity Scale, the New Madrid earthquakes remain the strongest recorded North American earthquakes east of the Rocky Mountains.[24][25] The earthquakes strengthened the Shawnee prophet Tenskwatawa after the defeat at the Battle of Tippecanoe and the destruction of Prophetstown, with local Native Americans seeing it as a vindication of his teachings.[26]

Gallery

Subsidence of Reelfoot Lake in Tennessee. The subsidence was between 4.9 and 19.6 feet.
  • Reelfoot Rift and NMSZ
    Reelfoot Rift and NMSZ
  • Damage-range comparison between a moderate New Madrid zone earthquake (1895, magnitude 6.8), and a similar Los Angeles event (1994, magnitude 6.7).
    Damage-range comparison between a moderate New Madrid zone earthquake (1895, magnitude 6.8), and a similar Los Angeles event (1994, magnitude 6.7).

See also

References

  1. ^ "M 7.5 - Northeastern Arkansas (New Madrid Seismic Zone)". USGS. Retrieved December 30, 2023.
  2. ^ "M 7.0 - Western Tennessee (New Madrid Seismic Zone)". earthquake.usgs.gov. USGS. Retrieved March 23, 2022.
  3. ^ "M 7.3 - North of New Madrid, Missouri (New Madrid Seismic Zone)". USGS. Retrieved December 30, 2023.
  4. ^ "M 7.5 - Western Tennessee (New Madrid Seismic Zone)". USGS. Retrieved December 30, 2023.
  5. ^ "M 6.3 - Near New Madrid, Missouri (New Madrid Seismic Zone)". earthquake.usgs.gov. USGS. Retrieved June 8, 2021.
  6. ^ "M 6.3 - Near New Madrid, Missouri (New Madrid Seismic Zone)". earthquake.usgs.gov. USGS. Retrieved June 8, 2021.
  7. ^ "M 6.1 - Near Memphis, Tennessee". earthquake.usgs.gov. USGS. Retrieved June 8, 2021.
  8. ^ "M 6.3 - Near Marked Tree, Arkansas". earthquake.usgs.gov. USGS. Retrieved June 8, 2021.
  9. ^ O.W. Nuttli (1974). "The Mississippi Valley earthquakes of 1811 and 1812". Earthquake Information Bulletin (USGS). 6 (2). United States: U.S. Geological Survey: 8–13. Retrieved June 8, 2021.
  10. ^ "U.S. Geological Survey: Largest Earthquakes in the United States". Archived from the original on December 13, 2016. Retrieved August 28, 2017.
  11. ^ a b c d Historic Earthquakes New Madrid Earthquakes 1811–1812 USGS Archived June 8, 2011, at the Wayback Machine
  12. ^ a b c d e f g h The Enigma of the New Madrid Earthquakes of 1811–1812. Johnston, A. C. & Schweig, E. S. Annual Review of Earth and Planetary Sciences, Volume 24, 1996, pp. 339–384. Available on SAO/NASA Astrophysics Data System (ADS)
  13. . (Page numbers may be for a different printing.)
  14. ^ "Summary of 1811-1812 New Madrid Earthquakes Sequence". United States Geological Survey. October 2, 2019. Retrieved June 8, 2021.
  15. ^ National Earthquake Information Center. "M 7.8 - Western Tennessee (New Madrid Seismic Zone)". United States Geological Survey. Retrieved June 8, 2021.
  16. ^ Richard A. Lovett, Quake analysis rewrites history books, Nature News, April 29, 2010.
  17. .
  18. ^ Letter of Eliza Bryan found in Lorenzo Dow's Journal, Published By Joshua Martin, Printed By John B. Wolff, 1849, p. 344. Accessed September 17, 2009. Archived 2009-09-21.
  19. ^ Reynolds, John (1855). My own times: embracing also the history of my life. B. H. Perryman and H. L. Davison. p. 125. Retrieved July 10, 2011.
  20. ^ Diary of Samuel Swan McClelland, in "Shakers of Eagle and Straight Creeks," Shakers of Ohio: Fugitive Papers Concerning the Shakers of Ohio, with unpublished manuscripts, J. P. MacLean, ed. Columbus, Ohio, 1907.
  21. ^ "USGS Release: Scientists Update New Madrid Earthquake Forecasts". Usgs.gov. January 13, 2003. Retrieved November 8, 2008.
  22. ^ Carey Gillam (November 20, 2008). "Government warns of 'catastrophic' U.S. quake". Reuters. Retrieved February 25, 2012.
  23. ^ a b c d "Summary of 1811-1812 New Madrid Earthquakes Sequence". www.usgs.gov. Retrieved November 26, 2021.
  24. ^ a b c "New Madrid earthquakes of 1811–12 | United States | Britannica". www.britannica.com. Retrieved November 26, 2021.
  25. ^ Cozzens, Peter (2021). The Warrior and the Prophet: The Epic Story of the Brothers Who Led the Native American Resistance.

Further reading

External links

  • The Enigma of the New Madrid Earthquakes of 1811–1812. Johnson, A.C. and Schweig, E.S. (1996) Annual Review of Earth and Planetary Sciences, Volume 24, pp. 339–384. SAO/NASA Astrophysics Data System (ADS)
  • The Introduction to The Lost History of the New Madrid Earthquakes by Conevery Bolton Valencius.
  • The New Madrid Fault Zone (NMFZ) Archived December 19, 2008, at the Wayback Machine (links to maps, history, predictions, etc. from the Arkansas Center for Earthquake Education)
  • Steamboat Adventure: The New Madrid Earthquakes (dozens of contemporary accounts of the earthquake, provided by Hanover College)
  • USGS, Summary of 1811-1812 New Madrid Earthquake Sequence, at https://www.usgs.gov/natural-hazards/earthquake-hazards/science/summary-1811-1812-new-madrid-earthquakes-sequence?qt-science_center_objects=0#qt-science_center_objects
  • [2] The "Hard Shock:" The New Madrid Earthquakes. The History Guy

36°24′N 89°36′W / 36.4°N 89.6°W / 36.4; -89.6