Understanding Earthquakes and Their Impacts: Part I
Ed. Note: This is the first of a two-part blog focusing on the science and aftermath of earthquakes. Part I focuses on the science of a high-magnitude earthquake and whether one could happen in the United States. Tomorrow, Part II will focus on What We Can Do About It.
Part I: Could a 9.0 Happen Here?
Four deadly earthquakes in just over a year—Haiti, Chile, New Zealand, and now Japan—have provided sudden reminders of the tectonic forces active beneath our feet. Perhaps more importantly, they serve as reminders that disasters resulting from those earthquakes are not the work of nature alone. Even in the face of such giant forces, societal decisions before and after an earthquake can have a major impact on the amount of damage, lives lost, and other outcomes. So while scientists and engineers share in society’s obligation to help the victims, we have an additional responsibility to learn from these events and share lessons that can be applied to vulnerable communities—not only abroad, but also here in the United States.
To make those wise decisions requires some basic geology. Most people know that the crust of the Earth is broken into about a dozen major sections, or plates, (and a number of smaller ones) that slowly move against one another. And when plates collide, the rock material in the collision zone is strained and eventually either breaks or slips along the boundary, causing an earthquake. Less widely appreciated is that the largest earthquakes occur along plate boundary zones where one plate is driven down beneath another. Most of these “subduction zones” are located around the rim of the Pacific Ocean in what is known as the Ring of Fire, so called because these regions are also particularly prone to volcanic eruptions.
As it turns out, Japan sits on or near the intersection of four of these plates, with the ensuing high risk from earthquakes and volcanoes. The magnitude-9.0 earthquake that occurred on March 11, 2011, was the largest to have struck Japan since seismic recording began 130 years ago and was the fourth-largest earthquake ever recorded worldwide, releasing approximately 1,000 times the energy of the Haiti earthquake of January 2010. In that light it is remarkable that the damage and loss of life was not far greater than it was—a tribute to Japan’s sizable and science-based investments in strict building codes, public preparedness, and earthquake and tsunami early warning systems. In particular, the current estimates of lives lost just from the shaking of this giant earthquake number in the low hundreds. More on this in Part Two of this blog, which we’ll post tomorrow. But it’s important to remember that even as nations begin the humbling process of rethinking certain assumptions about earthquake potential, nuclear safety, and tsunami protection, we must also use the lessons of what went right to redouble ongoing efforts to build resilient communities.
Is this really a problem that the United States has to worry about? The short answer is yes. According to the U.S. Geological Survey, 39 U.S. states have moderate-to-high earthquake hazard, as well as Puerto Rico, the U.S. Virgin Islands, Guam, and the Marianas Islands. These states include the ones people think of along the West Coast, but also ones in the Mountain West, the Central United States (where we are this year commemorating the bicentennial of a series of magnitude-7 earthquakes that struck the Mississippi Valley in 1811-12), and the East, where magnitude-7 earthquakes have struck as recently as the 1880s. Over all, annualized earthquake losses in the U.S. are estimated at $5.3 billion.
That figure could be dwarfed, of course, in the event of a magnitude-9 earthquake. And while the exact location, timing, or intensity of earthquakes cannot be predicted, the U.S. West Coast has two subduction zones—the type of plate boundary that is off the coast of Honshu, Japan—capable of magnitude-9 earthquakes. One is offshore of southern Alaska and the other is offshore a length of the Pacific Northwest coast stretching from Vancouver, BC, to Northern California—a region known as “Cascadia.” Earthquakes in southern Alaska produced major tsunamis in 1946, 1957, 1964, and 1965. The Cascadia zone last ruptured in 1700 and has an average recurrence interval of 500-600 years. The subduction zone in the eastern Caribbean has generated magnitude-8 earthquakes as recently as 1946. The 30-year probability of a magnitude-7 or greater earthquake in California is 94%, a number that fortunately drops to 4% for magnitude-8 or greater. Clearly, when it comes to a giant U.S. temblor, it is not a question of “if” but of “when.”
Tomorrow: What We Can Do About It
Tammy Dickinson is a Senior Policy Analyst at the White House Office of Science and Technology Policy
David Applegate is Senior Science Advisor for Earthquake & Geologic Hazards at the US Geological Survey