Great Flood of 1844

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The Great Flood of 1844 yielded the biggest water discharge in recorded history of the Missouri River and Upper Mississippi River in North America. The adjusted economic impact was not as great as subsequent floods because of the small population in the region at the time. The flood devastation was particularly widespread since the region had few levees at the time, so the waters were able to spread far from the normal banks. The highest mortality rates included the Wyandot Indians, with 100 deaths from the diseases after the flood in the vicinity of what became Kansas City, Kansas.

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Earlier in 1844, "by the first of May", the Mississippi River's banks overflowed and "By the 6th, the people of St. Louis began to be severly alarmed", until the water level lowered. However, "a succession of violent rain storms commenced on the 3rd of June" and by June 12, the riverbanks overflowed and people evacuated. The floods receded on June 28, and the crisis ended by the middle of July. [1]

The flood formed a large sandbar in front of the Wayne City Landing at Independence, Missouri, causing settlers to go further west to Westport Landing, which resulted in significant local economic and cultural impact. [2] Independence had been the trailhead for several key emigrant trails, prior to 1846, both the Santa Fe Trail and one alternative eastern starting branch of the Oregon Trail. After the Mexican–American War treaty of 1848, the Oregon Trail's trailhead became a trailhead of the California Trail and an alternative beginning for the Mormon Trail.

In 1850, the United States Congress passed the Swamp Land Act providing land grants to build stronger levees.

The flood is the highest recorded for the Mississippi River at St. Louis. The discharge was 1,300,000 cubic feet per second (37,000 m3/s) in 1844, while 782,000 cu ft/s (22,100 m3/s) in 1951 and 1,030,000 cu ft/s (29,000 m3/s) in 1993.

Other floods

This USGS exhibit shows flood crest levels at Westport Landing on the Missouri River at what later became Kansas City. KC-floods.jpg
This USGS exhibit shows flood crest levels at Westport Landing on the Missouri River at what later became Kansas City.

Over time, channeling and levee construction have altered how floods affect various areas along the Missouri River. For example, here is a comparison of flood data at and associated impacts on the area that became Kansas City for three big floods since the early 19th century.

See also

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References

  1. Gould, Emerson W. (1889). Fifty Years on the Mississippi; Or, Gould's History of River Navigation. Nixon-Jones Printing Company. pp. 247–248.
  2. Jackson County 175th Anniversary Timeline Archived 2010-12-17 at the Wayback Machine
  3. Report upon the physics and hydraulics of the Mississippi river. Andrew Atkinson Humphreys, Henry Larcom Abbot, 1867, Govt. Printing Office (available on Google Books).