Its course has changed many times and it will eventually change its path again. There are several factors that contribute to the change in courses of the Mississippi River. The main factor is energy. The Mississippi is a very curvy, knowns as meandering, river.
There are several factors that contribute to the change in courses of the Mississippi River. The main factor is energy. The Mississippi is a very curvy, knowns as meandering, river.
Floods are becoming more frequent, longer, and higher — even though average annual rainfall in the Mississippi drainage basin has been almost flat since 1940. It has flooded every other year on average since 1972 vs. once every six and a half years 1940-72.
In the lower portion of the Mississippi, the river moves very slowly. It's a broad, shallow river. As the water moves basically south towards the Gulf of Mexico, it encounters bends.
about once every 1,000 yearsThe Changing Courses of the Mississippi River Before the extensive levee system that “trained” our river to stay in one place, the Mississippi changed course about once every 1,000 years.
Many of these abandoned meanders provide important marshland wildlife habitat. The last major change to the river's course in the Vicksburg area occurred in 1876. On April 26 of that year, the Mississippi River suddenly changed courses, leaving Vicksburg high and dry.
The fact that the Mississippi River ran backwards after the massive New Madrid earthquake of 1811 is now the stuff of legend, but did you know that it's run backwards at least twice since?
One of the world's most powerful earthquakes changed the course of the Mississippi River in Missouri and created Reelfoot Lake in Tennessee while shaking parts of Arkansas, Kentucky, Illinois and Ohio.
The Mississippi River has changed course to the Gulf every thousand years or so for about the last 10,000 years. Gravity finds a shorter, steeper path to the Gulf when sediments deposited by the river make the old path higher and flatter. It's ready to change course again.
Left to their own devices, rivers change course over time, and the Mississippi is no exception. Geologists surmise that the Mississippi changed course numerous times over the past 10,000 years, wandering across a roughly 320-kilometer (200-mile) range along the Gulf Coast.
Between December 16, 1811, and late April 1812, a catastrophic series of earthquakes shook the Mississippi Valley. Towns were destroyed, an 18-mile-long lake was created and even the Mississippi River temporarily ran backwards.
The storm surge ahead of Hurricane Isaac made the Mississippi River run backwards for 24 hours. US Geological Survey (USGS) instruments at Belle Chasse in Louisiana recorded the flow of the river, finding it running in reverse on Tuesday.
The force of the land upheaval 15 miles south of New Madrid, drowned the inhabitants of an Indian village; turned the river against itself to flow backwards; devastated thousands of acres of virgin forest; and created two temporary waterfalls in the Mississippi.
Abstract. Since its admission into the Union in 1817, Mississippi has had only four earthquakes of intensity V or greater within its borders.
Earthquake CatalogDate and timeMag DepthMap2019-11-05 00:27:14 -06:00 (Nov 5, 2019 06:27 GMT)2.1MapSunday, October 20, 2019 GMT (1 quake)2019-10-20 17:14:32 -06:00 (Oct 20, 2019 23:14 GMT)2.4 7.7 kmMapSunday, October 6, 2019 GMT (1 quake)28 more rows
There were no significant confirmed earthquakes in or near Mississippi in the past 24 hours. Look up quakes in the past 30 days!
The Mississippi River has changed course to the Gulf every thousand years or so for about the last 10,000 years. Gravity finds a shorter, steeper path to the Gulf when sediments deposited by the river make the old path higher and flatter. It’s ready to change course again.
The higher the hill, the greater the “head” or force driving the flow. Floods on the Mississippi raise the water level inside the levees and increase this force. Floods are becoming more frequent, longer, and higher — even though average annual rainfall in the Mississippi drainage basin has been almost flat since 1940.
The lower Mississippi, though, isn't straight. Because it's moving slowly and meandering, there are bends up and down it. Human beings have liked to cut channels between pieces of the river in order to cut down on the river miles in a given trip. The Mississippi silts up.
Sometimes, when a river overflows its banks, it can reach a new channel that provides a more direct pathway to wherever the river wants to go. If that happens, the new channel can become the main channel. If the Mississippi were allowed to do what it wanted, what is now the Atchafalaya River would become the new ending of the Mississippi. Again, in a purely natural world, that would be a six of one, half dozen of the other situation. But now human systems depend on the Mississippi remaining roughly as it was in 1900 when we started to build massive amounts of infrastructure.
The 1993 flood was the most costly Mississippi flood in US history. Below, you can see raw footage from the 1927 flood courtesy of the Internet Archive and Army Corps of Engineers. The Mississippi moves. Rivers change course, as you can see in the beautiful map below, which shows the river's meanderings.
That's a flood. Like all other rivers, pretty much, the Mississippi floods. Before humans built stable settlements, you could move away from the water, but if your town happens to sit near a river, you're stuck. The river is going to want to flood and you're going to want to stop it. That's the tension of the river.
By the time of the great 1927 flood, there were 1500 miles of levees, and that was only the beginning. It was the Flood Control Act of 1928 and various addenda that would create and refine the Mississippi River and Tributaries project, which is managed by the Army Corps of Engineers.
John McPhee locates the beginning of the problem with the Mississippi way back at the founding of New Orleans. By 1724, a decree to build levees had already been promulgated. Things have only gotten worse since then. By 1812, there were already hundreds of miles of levee along the west bank.
26,000 square miles were inundated and 600,000 people displaced.
Did you ever hear the saying, "it's easier to get the Mississippi to change its course than get a stubborn child to change his mind"? I guess whoever made this one up didn't know that the Mississippi actually does change its course about every thousand years or so.
How could a river change its course? Actually, the whole process is due to silt. Every year, erosion from farm fields and building projects washes millions of tons of soil into streams and rivers.
Over the past eight thousand years, the Mississippi's main channel has become clogged up and changed course at least seven times. Under natural conditions the city of New Orleans should now be underwater, but this has been prevented by the Army Corps of Engineering's spending millions of dollars to prevent the Mississippi from changing course.
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