A study of ancient coral reefs in Indonesia revealed the slowest earthquake ever recorded

The NTU Asian School of the Environment team that was behind the study of ancient coral reefs in Indonesia (LR) includes: Associate Professor Emma Hill, PhD student Rishav Malik and Associate Professor Aaron Meltzner. Credit: NTU Singapore

Researchers at Nanyang Technological University of Singapore (NTU Singapore) found a slow-moving earthquake that lasted 32 years – the slowest on record – that ultimately led to the catastrophic Sumatra earthquake of 1861.

The NTU research team says their study highlights potential missing or misconfigured factors in today’s global earthquake risk assessments.

Slow-moving earthquakes or slow-slip events refer to a type of prolonged and extended stress release phenomenon in which the Earth’s tectonic plates slide against each other without causing major vibration or damage to the Earth. It usually involves movements ranging from a few centimeters per year to centimeters per day.

The NTU team made a surprising discovery while studying historical sea levels using ancient coral reefs called microatolls on Simeulue Island, located off the coast of Sumatra. Small coral particles grow sideways and higher, and are natural registers of changes in sea level and land elevation, through their visible growth patterns.

Using data from microatolls and combining them with simulations of Earth’s tectonic plate movement, the NTU team found that from 1829 until the Sumatra earthquake in 1861, the southeastern island of Simolo was sinking into the sea faster than expected.

The NTU team said this slow slide event was a gradual process that eased pressure on the shallow region where two tectonic plates met. However, this pressure was transferred to the nearby deeper part, culminating in the massive 8.5 magnitude earthquake and tsunami in 1861, which resulted in massive damage and loss of life.

The discovery marks the longest slow-slide event ever recorded and will change world views of the timescale and mechanisms of the phenomenon, says the NTU team. Scientists previously believed that slow slip events only occur over hours or months, but NTU research shows that in reality they can last for decades without causing the catastrophic tremors and tsunamis seen in historical records.

The study’s lead author, Rishav Malik, PhD. Thanks to the long spans of ancient coral reefs, we were able to investigate and find answers to the secrets of the past. The method we adopted in, ”said a student at NTU Asian School of the Environment. This paper will also be useful for future studies of other subduction zones – places prone to earthquakes, tsunamis and volcanic eruptions. Thus our study can contribute to better assessments of future risks. ”

“When we first found these coral reefs more than a decade ago, we learned from their growth patterns that something strange was going on as they were growing,” said Associate Professor Aaron Meltzner, co-author of the Earth Observatory in Singapore at NTU University. Now we’re finally a viable explanation. .

The results, published in the peer-reviewed journal Nature Geoscience in May, led the authors to suggest that current earthquake risk assessments may ignore the ongoing slow slip events in the observations, and thus not properly consider the likelihood of slow slip events. To cause earthquakes and tsunamis in the future.

A possible ‘slow-moving’ earthquake is ongoing on Ingano Island

The shallow portion of the subduction zone lies further from the ground under kilometers of water, is usually “quieter” and does not produce many earthquakes. Its remote location also makes it difficult for land-based scientific tools to discover activities and for scientists to understand what is going on.

Therefore, many scientists have tended to interpret the “quietness” of the shallow part of the subduction zone as meaning that the tectonic plates beneath it are sliding steadily and undamaged.

Although this may be true in some cases, the NTU study found that this slip is not as stable as assumed and can occur in slow slip events.

“Because these slow slip events are so slow, we might miss them because the current automated recordings are generally only 10 years old,” Reshaf said in detail in their findings.

He added, “If a similar behavior is observed that leads to earthquakes elsewhere, this process may eventually be recognized as a precursor to an earthquake.”

Utilizing their research methodology, the NTU team also highlighted a potential ongoing slow slide event on the island of Enggano, Indonesia, located about 100 kilometers (60 miles) southwest of Sumatra.

As Professor Meltzner said, “If our findings are correct, then this means that communities living near this Indonesian island are likely to face higher risks from tsunamis and earthquakes than previously thought. This indicates that risk models and mitigation strategies need to be done. Update. ”

Earthquake and tsunami risks from subduction zones may be higher than current estimates. More information: Rishav Mallick et al, Sunda megathrust long-lived shallow slow slip events, Nature Geoscience (2021). DOI: 10.1038 / s41561-021-00727-y provided by Nanyang Technological University

Quote: Study of ancient coral reefs in Indonesia reveals slowest earthquake ever recorded (2021, May 12) Retrieved May 12, 2021 from https://phys.org/news/2021-05-ancient-corals-indonesia-reveals -slowest.html

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