Study Finds Ice Age Sediment Makes Coastal Louisiana Sink
A recent article in the Geophysical Research Letters entitled, Post-glacial sediment load and subsidence in coastal Louisiana by Erik R. Ivins, Roy K Dokka, and Ronald G. Blom concluded that heavy sediment deposited in the Mississippi River delta at the end of the last ice age has caused coastal Louisiana in the Mississippi River delta to sink. This process is expected to continue for hundreds of years. The process will likely cause the area in question to subside over three feet in the next two hundred years.
The sinking of this land will likely be compounded by a general sea level rise from global warming. These factors will make the area more vulnerable to hurricanes and tropical storms. Of course, the hurricanes and tropical storms will then themselves do further damage to the coastal wetlands.
News Accounts related to this research paper can also be found at;
Associated Press: Sediment Make New Orleans Sink - February 1, 2008
Erich P Rapp
