The Next Great Earthquake

March 22, 2007
The Next Great Earthquake
Subduction Zones (blue curves) and tectonic boundaries (brown curves) with filled circles showing locations of known earthquakes of M7.5 or greater since 1900. Credit: Rensselaer Polytechnic Institute/Robert McCaffrey

The 2004 Sumatra-Andaman earthquake and resulting tsunami are now infamous for the damage they caused, but at the time many scientists believed this area was unlikely to create a quake of such magnitude. In the March 23 issue of the journal Science, a geophysicist from Rensselaer Polytechnic Institute urges the public and policy makers to consider all subduction-type tectonic boundaries to be “locked, loaded, and dangerous.”

“Seismologists have long tried to determine which subduction boundaries are more likely than others to break,” says Robert McCaffrey, professor of earth and environmental sciences at Rensselaer. “Yet, the great earthquake of 2004 ruptured a segment that was thought to be among the least likely to go.”

On Dec. 26, 2004, the earth beneath the Indian Ocean buckled and ruptured, unleashing one of the largest earthquakes in recorded history. Shockwaves from the magnitude 9.2 (M9) quake created a wall of rushing water that devastated communities up to 1,000 miles away.

M9 earthquakes typically occur at a specific type of tectonic boundary called a subduction zone, where one plate is gently slipping underneath another plate, which causes friction, cracking, and lifting of the plates. An M9 earthquake can be created by only 20 meters of slip between two converging plates — less then the length of an 18-wheeler truck — but its effects can be global in their impact.

Slips of this length only occur every 200 to 1,000 years or more at a particular boundary, leaving no reliable historic records to track their frequency, McCaffrey notes. Complete records are only available going back 100 years. Scientists had widely accepted that the age and speed of the subducting plate is important in creating M9 earthquakes, based primarily on support from this 100-year historical record.

But this narrow understanding put the Sumatran subduction zone in a very low risk category. McCaffrey suggests that such limited records are incapable of mapping a trend in geological events that could be several centuries or more apart.

Geologists also focused on the temperature of subduction zones, indicating that temperature at the plate convergence region plays a strong role in the strength of a resulting earthquake. These thermal considerations place the Andaman subduction zone in the high-magnitude class, but one pitfall with this type of classification is that it characterizes some subduction zones as being incapable of producing an M9.

“[The day of the quake], Earth gave us a stark reminder of the important difference between improbability and impossibility,” McCaffrey says. “Our understanding of where and when the next great earthquake will happen is in its infancy at best. We have not had enough time to decipher M9 behavior.”

In creating new public policy, McCaffrey urges officials to consider all subduction zones as lethal. “Several are near densely populated land areas, and the potential impacts of shaking and tsunamis cannot be overstated,” he says.

When crafting warning systems, policy makers should always remember that an earthquake even hundreds of miles removed can create a tsunami capable of widespread destruction, McCaffrey says. Therefore warning systems need to be created with input and support from many countries, in addition to educational outreach to coastal communities. “These systems need to be strong and they need to be maintained over the long term because we have no way of knowing when the next great earthquake will hit,” he says.

“We can never forget what happened,” McCaffrey continues. “Now is the time to use the knowledge that we have gained and work to save lives should another M9 hit tomorrow or hundreds of years from now. Many didn’t know about tsunamis before the quake; we must make sure that now they never fail to remember their destructive force.”

McCaffrey’s research focuses on plate motion, crustal deformation, and seismology. He is currently researching the movement of tectonic plates using global positioning systems (GPS). Among his many research projects, he has used GPS to track the movement of tectonic plates in and around Indonesia and Sumatra since 1989 and noted that the subduction zone was steadily squeezing the island of Sumatra, loading the system for an earthquake. No one predicted how soon and how big the earthquake would be. McCaffrey later explained the build-up to the earthquake as a time when one plate stuck against its counterpart. The energy and pressure built and the system cracked, causing the now historical M9.

Source: Rensselaer Polytechnic Institute

Explore further: Understanding Earthquakes

Related Stories

Understanding Earthquakes

December 20, 2005

Rensselaer campus regulars may not be aware of it, but earthquakes frequently surge through the basement of the Jonsson Engineering Center, the seemingly placid engineering building overlooking the school’s football field. ...

Recommended for you

Cities and monuments switch off for Earth Hour

March 26, 2017

The Empire State Building and United Nations headquarters in New York joined other iconic buildings and monuments around the world plunging into darkness for sixty minutes on Saturday to mark Earth Hour and draw attention ...

Land-based microbes may be invading and harming coral reefs

March 24, 2017

A new study suggests that coral reefs—already under existential threat from global warming—may be undergoing further damage from invading bacteria and fungi coming from land-based sources, such as outfall from sewage ...

Managing bushfires for safety and biodiversity

March 24, 2017

People have long used planned fires as a tool to open up access to hunting grounds, to encourage new plant growth, and to cultivate plants for cooking, heating and spiritual purposes.


Please sign in to add a comment. Registration is free, and takes less than a minute. Read more

Click here to reset your password.
Sign in to get notified via email when new comments are made.