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Hidden Slippery Clay on Seafloor May Have Worsened Devastating 2011 Japan Tsunami, New Research Finds

Thick layer of clay created a weak spot, intensifying quake'

Hidden Slippery Clay on Seafloor May Have Worsened Devastating 2011 Japan Tsunami, New Research Finds
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Japan - Ekhbary News Agency

Hidden Slippery Clay on Seafloor May Have Worsened Devastating 2011 Japan Tsunami, New Research Finds

A significant layer of slippery clay beneath the ocean floor may have played a crucial role in intensifying the devastating tsunami that struck Japan in 2011 following a magnitude 9.1 earthquake. New scientific findings suggest this clay formation created a critical weak point, thereby amplifying the seismic event's impact and the subsequent tsunami's destructive power. The research, published in the journal *Science*, offers a compelling explanation for why the 2011 Tohoku earthquake and tsunami were so exceptionally destructive.

The 2011 Tohoku earthquake and tsunami remain one of Japan's most catastrophic natural disasters, causing immense loss of life and widespread devastation. While the magnitude of the earthquake was immense, the sheer scale of the resulting tsunami had puzzled scientists. This latest study, led by geophysicists from the Australian National University, proposes a geological mechanism that sheds new light on the event.

According to the research, the clay layer, which could be as thick as 30 meters (98 feet), was situated along the fault line responsible for the earthquake. This geological feature is described as a "mechanical weak point" due to its low-friction properties. Dr. Ron Hackney, a geophysicist at the Australian National University and director of the Australian and New Zealand International Scientific Drilling Consortium, explained the significance: "It's low-friction, so that clay is weak. It can slip very easily." This characteristic significantly altered the dynamics of the earthquake rupture.

During the seismic event, the slippery nature of the clay layer likely caused the fault to rupture with less side-to-side, or strike-slip, motion than would be expected for an earthquake of this magnitude. The researchers theorize that this reduced horizontal displacement concentrated the energy release into an upward thrust. This vertical motion is believed to have been exceptionally large, potentially lifting the seafloor by 50 to 70 meters (164 to 230 feet) over an area spanning approximately 500 kilometers (310 miles). It is this dramatic upward surge of the seafloor that directly generated the colossal tsunami wave, which inundated an estimated 561 square kilometers (217 square miles) of Japanese coastline.

To gather evidence for their hypothesis, an international team of researchers, aboard the scientific drilling vessel *Chikyu*, conducted direct drilling operations into the fault zone in 2024. After penetrating 7,000 meters (23,000 feet) below the ocean surface and an additional 1,000 meters (3,300 feet) below the seafloor, they successfully retrieved sediment cores from within the fault and from the Pacific Plate. Analysis of these samples revealed the presence of a thick, viscous clay layer that had been slowly accumulating over an estimated 130 million years. As the Pacific Plate subducts beneath Japan, this clay layer is compressed, effectively squeezing the overlying continental rocks and creating the identified weak point.

The study suggests that similar clay layers might exist in other subduction zones globally. There is existing evidence pointing to their potential presence near Sumatra, Indonesia, the site of a devastating magnitude 9.1 earthquake and tsunami on December 26, 2004. However, the geological composition of fault zones in other seismically active regions, such as the Kamchatka Peninsula, remains less understood.

These findings have significant implications for earthquake and tsunami preparedness. As Earth scientists become increasingly adept at predicting earthquake magnitudes and shaking intensity, understanding the role of specific seafloor geology, like these clay layers, can refine early warning systems. Improved predictions of seafloor displacement and subsequent tsunami behavior could lead to more accurate and timely warnings, potentially saving countless lives in future mega-disasters.

Keywords: # Japan tsunami # Tohoku earthquake 2011 # seafloor clay # subduction zone # earthquake science # tsunami warning # geological weak point