New Fault Zone found under Los Angeles, page 1
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Topic started on 4-4-2003 @ 05:53 PM by dragonrider
Newfound L.A. Fault Threatens Major Quake

Stefan Lovgren
for National Geographic News
April 3, 2003



Between the sun and the stars, Los Angeles sometimes seems like paradise. But life in the City of Angels comes at a price: earthquakes.
Now the threat of "the big one" may be greater than previously feared. Researchers have identified a buried fault that may have caused at least four large-magnitude earthquakes in the past 11,000 years and is still active.

Known as the Puente Hills Blind Thrust System, the fault is three to 17 kilometers (2 to 11 miles) deep and extends for almost 50 kilometers (31 miles) from northern Orange County, through Los Angeles, up to Beverly Hills.


Earthquakes pose a constant threat to California. A recently identified fault found beneath the Los Angeles basin suggests the threat to the city is greater than previously thought.


"In terms of location, it couldn't be much worse," said James Dolan, a professor at University of Southern California's department of Earth sciences, who led the study. "Downtown L.A. is sitting on top of this thing."

Paleoseismologists have previously pinpointed the locations, magnitudes, and dates of ancient earthquakes, but never in so-called blind thrust faults. These are faults that don't extend to the surface of the Earth. Scientists have in fact debated if such faults exist beneath Los Angeles. The new study shows they both exist and could pose a credible earthquake hazard.

Earthquakes New and Old

The researchers received help for their study from an unexpected source: the oil industry. Companies like Texaco, which have spent millions of dollars on geologic drilling research in California, provided scientists with invaluable research data.

Using that information and high-resolution seismic reflection data, Dolan and colleagues drilled 15 bore holes, up to 40 meters (130 feet) deep, to study sediment layers overlying the hidden fault. What they found was subtle folding of the sediments revealing a history of ancient earthquakes.

The study shows the occurrence of at least four earthquakes with a magnitude of 7.2 to 7.5 on the Richter scale during the past 11,000 years. Perhaps most importantly, the 6.0-magnitude Whittier Narrows earthquake occurred in 1987 along a segment of Puente Hills, demonstrating that the fault system remains active and dangerous.

Squeezing L.A.

Geodetic studies show that Los Angeles is contracting. The northern point of the L.A. basin is moving closer to the southern point. "L.A. is being squeezed from north to south at about 4 to 5 millimeters [0.15-0.2 inch] per year," said Dolan.

This shortening, part of which is happening on top of recognized fault systems, literally bends the rock in the ground. The process stores energy, and when this energy exceeds the strength of the system, the fault breaks, triggering an earthquake.

Scientists believe that up to half of the energy stored in this process could be released on the Puente Hills fault.

"The good news is that major earthquakes along this fault are very infrequent, it may not happen again for thousands of years," said Dolan. "The bad news is that it could be very strong when it does happen."

An earthquake with a magnitude of about 7.5 on the Richter scale probably occurred on the Puente Hills fault 7,000 to 8,000 years ago. That means it was 15 times stronger than the 1994 earthquake that hit Northridge, north of Los Angeles, and killed 51 people.

The Northridge earthquake, which measured 6.7 on the Richter scale, caused U.S $44 billion in economic damage and is the largest natural disaster in U.S. history.

The tremblor proved that an earthquake smaller in magnitude can cause greater damage than a more powerful earthquake. The shaking in Northridge was some of the worst ever felt.

Bowl of Jello

In bigger earthquakes, shaking lasts longer and is felt over a larger area. There is a difference in frequency content between small and large earthquakes. Small earthquakes have higher frequency energy and can be particularly harmful to homes. Big earthquakes have low frequency energy and may cause more damage to large structures like skyscrapers.

What makes Los Angeles particularly vulnerable to any earthquake is that part of the basin the city is built on is filled with weak sediments. "The fault will pump energy directly into the basin and cause it to shake like a bowl of Jello," said Dolan.

Mexico City has a similar problem. That city was severely damaged in a 1985 earthquake, even though the epicenter lay in far-away Acapulco.

Establishing what kind of earthquakes could happen is critical for seismic hazard zoning, emergency response, and risk mitigation strategies.

"You want to find out as much as you can about the threat," said Dolan. "That gives you a batter chance to prepare for it."

The main challenge is to build earthquake-proof structures. As seismologists are fond of saying, "Earthquakes don't kill people, buildings do."

A summary of the research appears in the current issue of Science, the journal of the American Association for the Advancement of Science.


reply posted on 5-4-2003 @ 03:36 PM by dragonrider
If you asked me that a couple of years ago, I would have said the Oakland Earthquake was the big one... The rocks associated with the San Andreas are highly fractured, and many geologists believe that they are so highly fractured to be incapable of storing sufficient energy to cause an earthquake significantly greater than about 7.5.

That was before I started looking into the newer theories regarding quake swarms and blind thrust faults. (Yes, I am a geologist, but I am NOT a seismologist. I am trained in petroleum geology, and seismology is sort of a hobby if anything for me). This new data looks like this previously unknown fault zone could store much more energy than the San Andreas, resulting in much worse damage.

The one seismic zone I can think of that would be equivalent would be the New Madrid Seismic Zone, located along the western boundaries of Kentucky and Tennessee. The last time this fault zone was active was in 1811. Although we have no solid proof of just how bad that quake was, it was estimated to be 9+ on the richter scale (higher than anything currently measured). It is known to have made the entire Mississippi river run backwards, and buried 2 towns under it.

My personal suspicion is that sometime in the next 5-10 years, something very large is going to cut loose on the west coast. I also suspect (granted I have no hard evidence for this, just a hunch) that such activity will be linked to volcanic activity in the Washington/Oregon area. I think that we are going to have a massive eruption with Mt. Ranier shortly, and it may trigger something very large....


reply posted on 10-4-2003 @ 10:21 PM by dragonrider
Astrocreep:

I can certainly understand your concern with the lakes in West KY. I would also be very concerned with Memphis TN to your south. I dont know about flooding potential there, but it is a very built up metro area, with a large population. If something around a 8 or 9 Richter hit, there would likely be massive loss of life there.

I have also read a couple of articles about splaying faults associated with the NMSZ. There is an older and largely inactive fault zone to the the north and west near Illinois/Chicago. A couple of theories are that these splaying faults might connect up to the fault zone near Chicago: if the big one rips loose, it could transmit enough seismic energy along these faults to seriously affect Chicago as well.

Your surface readings using GPS or laser sounds pretty interesting. They do the same thing in the pacific northwest on suspect mountains (there is a bit of interest in Mt. Ranier, which I sort of think is the next one to explode). I agree, such activities are of limited use, and mainly only useful in a Mt St. Helens type of scenario, where you are monitoring the swelling or shifting of a known slope. For the NMSZ they would likely do much better with buried monitoring points using stress/strain meters, temperature, dialectric, ect. Unfortunately, these are all very expensive prospects, which is why I suspect they are trying to run surface measurements instead.

As far as survivability, the tight hard clays are better than the sand/silt (the most dangerous areas by far), but I would prefer to be on good solid limestone if at all possible. If this were an option for you, I would seriously consider relocation to an area with a solid concrete foundation on solid limestone. Also, I would avoid any areas on top of or immediately under any slope greater than 15 degrees.
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