June 14, 2006 navbardiscovery.comDiscovery ChannelTLCAnimal PlanetTravel ChannelDiscovery Health ChannelDiscovery Store
Discovery Channel rule
Discovery Channel
free newsletter
site search
Discovery News Brief

send to a friend
printer friendly version
rss headline feed | xml

Map of Landslide Area
Map of Landslide Area

New Orleans Sits Atop Giant Landslide
small text
large text

March 31, 2006 — New Orleans is at the top end of what looks like a gigantic, slow-moving landslide, according to geologists who have been carefully studying the ground movements in the area.

Amid news that rebuilding the city's levees will cost substantially more than projected, the discovery of a much wider, older cause for the area's rapid subsidence flies in the face of years of policies that have pinned the blame on human activities for most of the area's gradual sinking below sea level.

The pumping of groundwater, levee building, and oil and gas extraction have carried the blame so far, but what's being called "tectonic" subsidence appears to account for 73 percent of all sinking from 1969 to 1971 and 50 percent from 1971 to 1977.

"Not only is southern Louisiana sinking, it's sliding," said geologist Roy Dokka of Louisiana State University.


Like a smaller landslide on the side of a hill, the huge Southern Louisiana landslide has a "headwall" where the slide is breaking away and a "toe" out in the Gulf where the debris from the slide is piling up, Dokka explained. The only difference from a traditional landslide is that this one is far, far larger and it's buried under lots of wet sediments, so it requires very accurate survey measurements to detect it.

Dokka obtained that data by re-examining decades of geodetic survey data from the National Oceanic and Atmospheric Administration (NOAA) in the area and calibrated it with the more stable Global Positioning System.

With that he was able to detect movements in the ground that were not visible to surveyors who used less reliable benchmarks like the more changeable sea level. He also used data from some very deep wells to see how much the land has been compacting from the removal of water and petroleum – a common cause of subsidence.

His conclusion was that while there are certainly local subsidence effects from the over-pumping of groundwater and the river levees keeping sediments from reaching wetlands, these things are sitting atop a much larger block of earth that's been sliding into the Gulf of Mexico for eons. Dokka published a paper on his work in the April issue of Geology.

"Here it's subsidence that's occurring deep in the Earth," said Dokka.

As a result, there are faults along which the motion is taking place. One such fault, the Michoud Fault, runs right through New Orleans and is essentially the place where the sliding section of earth is breaking away.

The huge downward slide of the Mississippi Delta is pretty much what current geological theories would predict, said geologist Art Berman, who writes about such matters for the Houston Geological Society and works as a petroleum geologist in the Gulf of Mexico.

"We're at the margin of an active basin," said Berman. "There's 50,000 feet of sediment in the Gulf of Mexico that's pretty young."

All that sediment has weighed down the crust of the Earth there and caused it to sink.

"This is probably pretty common in areas like this worldwide," Dokka said.

Get More News:
14 Jun 2006   Upside-Down Sensors Doomed Craft
14 Jun 2005   Surface Snares Water Like Beetle Back
14 Jun 2005   Rare Rhino Captured on Film
14 Jun 2005   Alberto: More Good Than Harm?
13 Jun 2006   Database to Analyze Horse Speak
13 Jun 2006   Study: Polar Bears Turning to Cannibalism
13 Jun 2006   Study: Sperm Have Sense of Smell

news main

Pictures: Roy Dokka/Geology |
Contributers: Larry O'Hanlon |

By visiting this site, you agree to the terms and conditions
of our Visitor Agreement. Please read. Privacy Policy.
Copyright © 2006 Discovery Communications Inc.

Discovery Beyond Sweepstakes

The leading global real-world media and entertainment company.

May We Suggest