Chilean Quake Likely Shifted Earth’s Axis, NASA Scientist Says

By Alex Morales

March 1 (Bloomberg) — The earthquake that killed more than 700 people in Chile on Feb. 27 probably shifted the Earth’s axis and shortened the day, a National Aeronautics and Space Administration scientist said.

Earthquakes can involve shifting hundreds of kilometers of rock by several meters, changing the distribution of mass on the planet. This affects the Earth’s rotation, said Richard Gross, a geophysicist at NASA’s Jet Propulsion Laboratory in Pasadena, California, who uses a computer model to calculate the effects.

“The length of the day should have gotten shorter by 1.26 microseconds (millionths of a second),” Gross, said today in an e-mailed reply to questions. “The axis about which the Earth’s mass is balanced should have moved by 2.7 milliarcseconds (about 8 centimeters or 3 inches).”

The changes can be modeled, though they’re difficult to physically detect given their small size, Gross said. Some changes may be more obvious, and islands may have shifted, according to Andreas Rietbrock, a professor of Earth Sciences at the U.K.’s Liverpool University who has studied the area impacted, though not since the latest temblor.

Santa Maria Island off the coast near Concepcion, Chile’s second-largest city, may have been raised 2 meters (6 feet) as a result of the latest quake, Rietbrock said today in a telephone interview. He said the rocks there show evidence pointing to past earthquakes shifting the island upward in the past.

‘Ice-Skater Effect’

“It’s what we call the ice-skater effect,” David Kerridge, head of Earth hazards and systems at the British Geological Survey in Edinburgh, said today in a telephone interview. “As the ice skater puts when she’s going around in a circle, and she pulls her arms in, she gets faster and faster. It’s the same idea with the Earth going around if you change the distribution of mass, the rotation rate changes.”

Rietbrock said he hasn’t been able to get in touch with seismologists in Concepcion to discuss the quake, which registered 8.8 on the Richter scale.

“What definitely the earthquake has done is made the Earth ring like a bell,” Rietbrock said.

The magnitude 9.1 Sumatran in 2004 that generated an Indian Ocean tsunami shortened the day by 6.8 microseconds and shifted the axis by about 2.3 milliarcseconds, Gross said.

The changes happen on the day and then carry on “forever,” Benjamin Fong Chao, dean of Earth Sciences of the National Central University in Taiwan, said in an e-mail.

“This small contribution is buried in larger changes due to other causes, such as atmospheric mass moving around on Earth,” Chao said.

To contact the reporter on this story: Alex Morales in London at amorales2@bloomberg.net.
Last Updated: March 1, 2010 14:11 EST

Tags: Alex Morales, British Geological Survey, Computer Model, Concepcion Chile, David Kerridge, Earth Axis, Earth Hazards, Earth S Axis, Earth Science, Earth Sciences, Earthquake, Earthquakes, Geophysicist, Indian Ocean Tsunami, Jet Propulsion Laboratory, Kilometers, Liverpool University, Magnitude 9, Microseconds, Nasa Scientist, National Aeronautics And Space, National Aeronautics And Space Administration, Quake, Richard Gross, Richter Scale, Rotation Rate, Santa Maria Island, Sumatra, Temblor, Tsunami

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Scientists Drill a Mile Into Active Deep Sea Fault Zone

Scientists Drill a Mile Into Active Deep Sea Fault Zone

  • 7:27 pm  |
  • Categories: Earth Science

riser-pipe

In the first deep sea drilling expedition designed to gather seismic data, scientists have successfully drilled nearly a mile beneath the ocean floor into one of the world’s most active earthquake zones.

Researchers aboard the drilling vessel Chikyu — meaning “planet Earth” in Japanese — used a special technology called riser drilling to penetrate the upper portion of the Nankai Trough, an earthquake zone located about 36 miles southeast of Japan. By collecting rock samples and installing long-term monitoring devices, the geologists hope to understand how stress builds up in subduction zones like Nankai, where the Philippine Sea plate plate is sliding beneath the island of Japan.

riserRiser drilling involves encasing a deep sea drill in a giant metal tube, called a riser, that extends from the ship down to the drilling site, effectively bolting the ship to the sea floor. The researchers circulate lightly pressurized mud down through the drilling tube and back up through the riser.

“One of the key benefits is the pressurized mud keeps the wall rock from collapsing on the drilling pipe, which allows you to drill deeper and with better control,” geologist Timothy Byrne of the University of Connecticut wrote in an e-mail. “For example, nearly perfectly vertical holes or steeply inclined holes can be drilled,” wrote Byrne, who co-led the project.

Using a riser also makes it easier to send core samples and cuttings, or small chips of rock collected during drilling, back up to the surface.

The Nankai Trough last ruptured twice in 1944 and 1946, generating earthquakes greater than magnitude 8 that shook the region and caused deadly tsunamis. Since then, the two plates have continued to move, but the boundary between them has been locked, causing pressure to build.

“We know that a locked fault is not a quiet thing, but we don’t quite understand why,” said geologist Kelin Wang of the Geological Survey of Canada, who was not involved in the research. “When we understand what is meant by locking, we can understand how energy is building up for the next event.”

The Nankai project is part of an international effort called the Integrated Ocean Drilling Program, designed to investigate a variety of scientific questions through drilling. The IODP chose to drill for seismic data in Nankai because of the region’s history of recent earthquakes and the accessible location of the rupture zone. The drilling is not powerful enough to trigger an earthquake.

What is learned in Japan will help scientists understand other earthquake-prone plate boundaries, such as the Cascadia subduction zone, which extends along the Pacific coast from British Columbia to Northern California

“For us in North America, the good news is that the Nankai subduction zone is strikingly similar to ours,” Wang said. Both zones are hotter and accumulate more sediment than average. “By studying Nankai, we North Americans can actually benefit pretty directly from the project. It’s almost as if we are drilling our own subduction zone, because we’ll see a lot of the same things.”

The first drilling and sampling operations in Nankai began on May 12 and are expected to conclude on August 1. After the initial drilling stage, scientists lowered various gauges and logging instruments into the hole to measure temperature, stress, water pressure and rock permeability. Once they gather enough data, the scientists will prepare the hole for future installation of long-term monitoring equipment.

See Also:

Image 1: Riser aboard Chikyu vessel, JAMSTEC/IODP. Image 2: D. Sawyer, JOI/USSAC/IODP. Video: JAMSTEC/IODP.

Tags: Core Samples, Drilling Pipe, Drilling Vessel, E Mail, Earth Science, Earthquake Zone, Earthquake Zones, Fault Zone, Giant Metal, Metal Tube, Nankai Trough, Philippine Sea Plate, Planet Earth, Rock Samples, Sea Drilling, Seismic Data, Special Technology, Subduction Zones, Timothy Byrne, University Of Connecticut

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Massive Fake Quake Will Shake 6-Story Condo

Massive Fake Quake Will Shake 6-Story Condo

  • 5:23 pm  |
  • Categories: Earth Science

quakesim

A massive simulated earthquake will rock a six-story wooden condominium to the brink of collapse

Tuesday, during one of the largest shake-table experiments undertaken to date.

The simulation, which will be webcast live July 14 at 11 a.m. EDT on the National Science Foundation website, is designed to test how a mid-rise wood-frame building would stand up to shaking from an earthquake around magnitude 7.5.

“We’re taking it to an earthquake level that’s associated with being on the verge of collapse,” said civil engineer Michael Symans of Rensselaer Polytechnic Institute, who helped design the test building. “We don’t expect it to collapse, but we expect it to be very vulnerable to a strong aftershock that could cause it to collapse.”

The 23-unit condo building currently sits on the world’s largest shake table, a 50-by-60-foot structure in Miki, Japan. The table will simulate the motions of the 1994 earthquake in Northridge, California, amplified about 1.5 times. Sensors on each floor of the building will record motion and detect internal damage, generating valuable data about how wooden structures perform in a quake.

Although wooden buildings are cheaper and faster to construct than those made of steel, very few mid-rise structures in the United States are currently built of wood. “Even in seismically vulnerable parts of the West Coast, there just isn’t much of an understanding of how taller wood structures will behave under ground shaking,” Symans said. “It might be desirable to build in wood, but at this point that’s not an option from a building-code point of view, partially because we just don’t know what will happen in an earthquake.”

The test marks the final experiment in a four-year collaboration called the Network for Earthquake Engineering Simulation Wood project, funded by a $1.4 million grant from NSF and donated materials from the industrial manufacturer Simpson Strong-Tie.

The project’s first experiment subjected a two-story wooden house to a magnitude 6.7 earthquake, which severely damaged the structure. The engineers determined that homes built to current building standards might not topple during a large earthquake, but they’d likely never be livable again.

For the current test, they experimented with new design principles meant to help the condominium withstand shaking.

“Basically, what happens during an earthquake in multiple-story building is something called a ’soft story,’” said civil engineer John van de Lindt of Colorado State University, who led the condo design. “It’s not as stiff as the story above it, and the earthquake demands more stiffness from the lower story. This can develop into a pancake collapse, which damages the building and can kill people.”

The new design distributes the stiffness vertically throughout the height of the building, van de Lindt said, to reduce the chance of a soft-story collapse.

On June 30 and July 6, engineers subjected the condo to preliminary testing, seen in the video below.

In the two smaller earthquake simulations, the building sustained very little damage. “So far, it looks like it’s working like a charm,” he said. “If there were families living in this condo, they wouldn’t even have to move out.”

Tuesday’s quake may be a different story. Numerical models predict a 3 percent drift, which means that each story of the building will shift over about three inches — enough to cause significant damage, but not enough to cause collapse. The only way to validate the computer models is to do a full-scale simulation, and that’s something that’s never been done before on such a large building.

“The reality is that we really don’t know what will happen,” Symans said.

See Also:

Image: Simspon-Strong Tie.

Tags: Brink Of Collapse, Civil Engineer, Earth Science, Earthquake Engineering, Foundation Website, Frame Building, Leggett, Mid Rise, National Science Foundation, Northridge California, Rensselaer Polytechnic Institute, Rise Structures, Shake Table, Story Condo, Table Experiments, Unit Condo, Wood Frame, Wood Structures, Wooden Buildings, Wooden Structures

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SARYCHEV PEAK VOLCANO

Perfect timing. On June 12th, just as Russia’s Sarychev Peak volcano was erupting for the first time in 20 years, the International Space Station flew directly overhead. Astronauts had their camera ready and snapped one of the most dramatic Earth-science photos ever taken from space:

Researchers are studying this rare photo to learn about the early stages of powerful volcanic eruptions. A few phenomena stand out:

(1) The volcano erupted with such force, the plume actually punched through the atmosphere. Note how clouds around the volcano have parted in a circular ring–that is a result of a shock wave produced by the upward blast. (2) The plume is a mixture of brown ash and white steam. A “dirty thunderstorm” complete with lightning could be in progress within the roiling cloud. (3) The smooth white bubble on top of the plume is probably a mass of water condensing from air shoved upward by the rising ash column. If so, it is akin to the iridescent pileus clouds sometimes featured on spaceweather.com.

If you’re not amazed yet, try this: Put on a pair of red-blue stereo glasses and behold the eruption in 3D. The anaglyph was created by graphic artist Patrick Vantuyne of Belgium. No stereo glasses? A cross-eyed version is also available.

Tags: Anaglyph, Ash Column, Astronauts, Brown Ash, Circular Ring, Earth Science, Graphic Artist, International Space Station, Perfect Timing, Phenomena, Pileus Clouds, Plume, Rare Photo, Science Photos, Shock Wave, Space Researchers, Stereo Glasses, Thunderstorm, Volcanic Eruptions, Volcano

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