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March 1875 Southeast tornado outbreak

Weather event in the United States From Wikipedia, the free encyclopedia

March 1875 Southeast tornado outbreak
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The March 1875 Southeast tornado outbreak was a devastating event that struck the Southern United States from March 19–20, 1875. It produced least 19 tornadoes were recorded, with seven that rated F4 by tornado expert Thomas P. Grazulis. Georgia bore the brunt of the destruction and fatalities, with two tornado families causing most of the damage. These families followed parallel paths, 12 to 15 mi (19 to 24 km) apart, through Georgia and South Carolina, consisting of multiple long-tracked and intense tornadoes.

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The deadliest tornado of the outbreak, an F4 that killed 28–42 people in and around Sparta, Georgia, and Edgefield, South Carolina, on March 20. Another F4 tornado on a similar path may have caused up to 30 additional fatalities. Overall, the outbreak resulted in at least 96 deaths, 377 injuries, and $650,000 in damages - a staggering toll for the time.[1][nb 1][nb 2][nb 3]

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Confirmed tornadoes

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The ratings for these tornadoes were done by tornado expert Thomas P. Grazulis and are not official ratings.

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  • Note: Some of the events listed as individual tornadoes were probably tornado families.[1]

March 19 event

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March 20 event

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Sparta, Georgia/Edgefield, South Carolina

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A massive F4 carved a 75 miles (121 km) path of destruction through parts of Georgia and South Carolina, with a width ranging from 300 yards (270 m) to over 1 mile (1.6 km). The tornado first struck northwest of Sparta, Georgia, in Hancock County, destroying numerous farms and claiming four lives, three of whom were on a single farm. Remarkably, a door hinge from the farmhouse was found embedded 3 inches (7.6 cm) deep in a tree over a 14 mi (0.40 km) away.

In Warren County, at least six people died, including one at a church west of Warrenton. The pastor credited the survival of most congregants to the pews, which shielded them from falling timbers. The tornado continued through Camak, where 39 of the town's 40 homes were either damaged or obliterated. McDuffie County reported at least seven fatalities, potentially as many as 9, primarily among residents of small cabins.

Columbia County may have experienced up to 20 deaths, although only eight deaths were confirmed. In Appling at least four people perished, with reports suggesting as many as eight may have died on a single plantation. After crossing the state line into Edgefield County, South Carolina, the tornado caused comparatively less destruction. though six farms and plantations were destroyed, and three fatalities were recorded. The tornado finally dissipated south of Edgefield.

The death toll from this tornado is officially listed at 28, though uncertainties place the number as high as 42.[13]

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Notes

  1. An outbreak is generally defined as a group of at least six tornadoes (the number sometimes varies slightly according to local climatology) with no more than a six-hour gap between individual tornadoes. An outbreak sequence, prior to (after) the start of modern records in 1950, is defined as a period of no more than two (one) consecutive days without at least one significant (F2 or stronger) tornado.[2]
  2. The Fujita scale was devised under the aegis of scientist T. Theodore Fujita in the early 1970s. Prior to the advent of the scale in 1971, tornadoes in the United States were officially unrated.[3][4] While the Fujita scale has been superseded by the Enhanced Fujita scale in the U.S. since February 1, 2007,[5] Canada used the old scale until April 1, 2013;[6] nations elsewhere, like the United Kingdom, apply other classifications such as the TORRO scale.[7]
  3. Historically, the number of tornadoes globally and in the United States was and is likely underrepresented: research by Grazulis on annual tornado activity suggests that, as of 2001, only 53% of yearly U.S. tornadoes were officially recorded. Documentation of tornadoes outside the United States was historically less exhaustive, owing to the lack of monitors in many nations and, in some cases, to internal political controls on public information.[8] Most countries only recorded tornadoes that produced severe damage or loss of life.[9] Significant low biases in U.S. tornado counts likely occurred through the early 1990s, when advanced NEXRAD was first installed and the National Weather Service began comprehensively verifying tornado occurrences.[10]
  4. All dates are based on the local time zone where the tornado touched down; however, all times are in Coordinated Universal Time and dates are split at midnight CST/CDT for consistency.
  5. Prior to 1994, only the average widths of tornado paths were officially listed.[11]

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