By Julia Whitty| Fri May. 13, 2011 2:24 PM PDT
Sediment-laden water pours into the Gulf of Mexico from the Mississippi and Atchafalaya Rivers. Credit: Norman Kuring, Ocean Color Team.
As you can see from the image above, a lot more than water comes down a river. The Mississippi and its distributary, the Atchafalaya River, carry an average of 230 million tons of soil into the Gulf of Mexico every year. On flood years, the total runs a lot higher.
That's going to cause downstream problems this year... all the way downstream to the ocean. But before we go there, let's take a quick look at how the system works.
Credit: USGS.
The graphic above shows sediment concentration and sediment discharge for major US rivers. The giant half-circle in the Gulf represents the Mississippi/Atchafalaya discharge. Why are the two rivers bundled together? Because they're really the same river: the parentheses bracketing a 100-mile-wide delta.
Mississippi delta switching during the past 4,600 years. Credit: Wikimedia Commons.
Before 1927's epic flood, the Mississippi was free to wander the delta, whiplashing between courses whenever a huge flood year like this one pushed it over its banks—a process known as delta switching. In the above image you can see some of its historical courses and when it ran them.
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