Deadly Indonesian Quake Was a Rare ‘Superfast’ Event – Jet Propulsion Laboratory

NASA

Last September’s major earthquake near Palu City
on the Indonesian island of Sulawesi was a rare supershear event, a new study
has found. Fewer than 15 of these superfast-moving, extra-powerful earthquakes have
ever been identified.

In these events the rupture, or propagating crack,
moves along a fault extremely rapidly, causing the up-and-down or side-to-side waves that shake the ground
– called seismic shear waves – to pile up and intensify. The result is much stronger
shaking than in a slower quake.

Researchers at UCLA; NASA’s Jet Propulsion
Laboratory in Pasadena, California; and other institutions analyzed high-spatial-resolution
observations of the seismic waves caused by the devastating temblor, along
with satellite radar and optical images,to
characterize the speed, timing and extent of the magnitude
7.5 Palu earthquake that occurred on Sept. 28, 2018. They calculated
that the quake ruptured at a steady speed of 9,171 mph (14,760 kph), with the
main shock continuing for almost a minute. Earthquakes typically rupture at
about 5,600 to 6,700 mph (9,000 to 10,800 kph). Processing the satellite
images, the researchers found that the two sides of the 93-mile-long (150-kilometer-long)
fault slipped by about 16 feet (5 meters) – a surprisingly large amount.

“Understanding
how faults rupture in large earthquakes will help improve seismic hazard models
and help earthquake engineers design buildings and other infrastructure to
better withstand possible future earthquake shaking,” said JPL’s Eric Fielding,
a co-author of the new study published today in
Nature Geoscience.

A rupturing fault creates several kinds of waves in the
ground, including shear waves that spread out at 7,900 mph (12,700 kph). In a supershear earthquake, the fast-moving rupture overtakes
the slower shear waves propagating in front of it and pushes them together into
bigger, more powerful waves. “The intense shaking [that results] is
similar to the sonic boom associated with a supersonic jet,” said Lingsen
Meng, a professor at UCLA and co-author of the report.

The consistent speed of the Palu rupture was surprising,
considering the nature of the fault itself. Previously studied supershear earthquakes occurred on
faults that were remarkably straight, offering few obstacles to the earthquakes’
motion. Satellite images of the Palu fault, however, revealed that it had at
least two large bends. The rupture maintained a steady speed around these bends.

That challenges
scientists’ models of earthquake rupture, according to senior corresponding
author Jean-Paul Ampuero of the Universite? Co?te d’Azur in Nice, France. However,
Ampuero said, these models were developed for idealized faults in homogeneous
material. “Real faults are surrounded by rocks that have been fractured
and softened by previous earthquakes,” he said. “In theory, speeds
that would be unexpected in intact rocks can happen in damaged rocks.”

The
scientists analyzed synthetic aperture radar data from the Japan Aerospace
Exploration Agency’s ALOS-2 satellite; optical image data from the Copernicus
Sentinel-2A and -2B satellites, operated by the European Space Agency; and optical
images from the Planet Labs PlanetScope satellite constellation, managed by
Planet Labs in San Francisco. Both space agencies and Planet Labs reprogrammed their
satellites immediately after the quake to acquire more images of central
Sulawesi island to help with research, allowing the team to produce a
comprehensive analysis.

The study is
titled “Early and Persistent Supershear Rupture of the 2018 Magnitude 7.5
Palu Earthquake.”

News Media Contact

Esprit Smith
Jet Propulsion Laboratory, Pasadena, California
818-354-4269
Esprit.smith@jpl.nasa.gov

Stuart Wolpert
UCLA
310-206-0511
swolpert@stratcomm.ucla.edu

Written by Carol Rasmussen
NASA’s Earth Science News Team

2019-015

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