TAU Analysis of October 7 Ground Motions Reveals Seismic Signatures of Hamas Murderers

Photo Credit: Abed Rahim Khatib / Flash 90

Hamas's Ezzedine al Qassam Brigades terrorist rides a bulldozer near the Israeli border fence.

A groundbreaking study in the field of forensic seismology, conducted by Tel Aviv University researchers, has identified the seismic signature of Hamas forces’ movement before the October 7th attack. Researchers from the Department of Geophysics at Tel Aviv University’s Porter School of the Environment and Earth Sciences and Sackler Faculty of Exact Sciences recently analyzed data recorded at three seismic stations in southern Israel. The findings reveal that on the morning of October 7th, approximately half an hour before the deadly terrorist assault, the stations recorded weak but widespread human-induced seismic noise. The researchers attribute these anomalous seismic amplitudes to the unusual movement of heavy vehicles within the Gaza Strip heading toward organizational points along the Israeli border up to 20 minutes before the ground barrier breach.

Findings from the research. / Tel Aviv University

The researchers explain that forensic seismology is often used to monitor conventional and nuclear explosions. However, this is the first time in history that weak ground motions resulting from preparations for a terrorist attack have been identified by analyzing the characteristics of seismic noise induced by vehicular traffic. They believe the discovery demonstrates the potential usage of seismic-based sensing technology to provide early warnings of terrorist activity. However, they emphasize that the identification of these movements in Gaza was conducted retrospectively, months after the attack.

The study, led by Dr. Asaf Inbal of the Department of Geophysics at Tel Aviv University’s Porter School of the Environment and Earth Sciences and Sackler Faculty of Exact Sciences, was published in The Seismic Record, a journal of the Seismological Society of America (Forensic Seismic Evidence for Precursory Mobilization in Gaza Leading to the October 7 Hamas Attack).

October 7th was a MASSACRE.

Never forget.@MichaelRapaport was at the Gaza border, where the fence was broken down on Oct. 7, and heard from @GrishaConsult who recounts what happened that horrific day. pic.twitter.com/fw13tG8Bvk

— Embassy of Israel to the USA (@IsraelinUSA) November 5, 2024

Dr. Inbal explains: “The Israeli Geological Survey operates a nationwide network of dozens of highly sensitive seismometers that continuously monitor ground motions. This network is primarily designed to detect and locate earthquakes and provide warnings of strong ground shaking caused by large-magnitude seismic events. However, three stations in the network—located in Amazia, Ktsiot, and Yatir, between 30 and 50 kilometers from Gaza—recorded unusual seismic noise levels early on the morning of October 7th, 2023. This noise can be attributed with confidence to the vehicular activity in Gaza as Hamas terrorists gathered for the attack. The time frame was between 6:00 and 6:30 AM before the rocket fire began. The likelihood that the recorded signals originated from Gaza is over 99.9%.”

Although the seismometers are designed to detect extremely weak ground motions, Dr. Inbal points out that the ability to link the seismic noise to Gazan vehicle movements was facilitated by the quiet background seismic noise levels that prevailed in southern Israel during the early hours of that Saturday morning, which coincided with the holiday of Simchat Torah.

At least 3 Humvee armored vehicles belonging to the Israel Defense Forces were seized as trophies by the Al-Qassam Brigades (the military wing of Hamas) and taken to the Gaza Strip pic.twitter.com/urbv5KUSkk

— S p r i n t e r (@SprinterFamily) October 7, 2023

“The motions recorded near the seismometers were in the range of tens of nanometers per second, whereas the minimum ground motion detectable by humans is several millimeters per second,” explains Dr. Inbal. “The characteristics of the noise originating from Gaza and captured by the Israeli stations are fundamentally different from those recorded at the same stations on previous Saturdays during those hours. We analyzed three years of data from the Israeli station trio recorded in the same time frame as the one leading up to the attack. We found no instance of a Saturday morning when correlated amplitudes were recorded at all three stations for over 10 minutes.”

“It’s important to note that these stations are widely spaced, with each station primarily sensitive to seismic noise generated by nearby human activity. For instance, the distance between Ktsiot and Amazia is about 80 kilometers, and on previous Saturdays, there was no correlation between the data recorded at these stations,” Dr. Inbal adds. “On the morning of the attack, when local activity near the stations was minimal, we found unique widespread seismic amplitudes, which monotonically increased with time approaching the attack. No known natural or human source on the Israeli side could have generated seismic signals with a distribution and intensity similar to those attributed to Hamas movements. Although the outdoor music festival near Re’im generated some seismic noise, our analysis shows that this noise does not match the strength or location of the noise sources recorded by the Israeli seismic network on October 7th.”

The analysis indicates the seismic noise detected began at 6:00 AM and intensified as the attack approached. Occasionally, the noise contained short bursts strong enough to pinpoint their source and track their progress. The location and intensity of these sources in Gaza suggest vehicle movements advancing southward and northward within Gaza, from Rafah in the south to the Erez crossing in the north, during the 30 minutes leading up to the attack.

“We have good resolution along Salah al-Din Road, a major thoroughfare crossing Gaza from Rafah in the south to Beit Lahia in the north,” says Dr. Inbal. “We can confirm with high certainty that their forces moved along this route at speeds of 25 to 50 km/h. Observations from stations dozens of kilometers from Gaza’s border indicate convoys of heavy vehicles such as bulldozers and trucks carrying operatives. Three minutes before the attack began, we detected noise sources reaching the northern end of Gaza near Beit Lahia and the southern end near Khan Yunis. At the same time, we continued receiving signals from central Gaza, near Nuseirat. We know the assault began almost simultaneously along the entire border, so these seismic observations provide further evidence of the extensive deployment of Hamas forces, likely enabling the simultaneous breach of the ground barrier.”

Dr. Inbal concludes: “This development results from five years of seismological research aimed at characterizing seismic noise generated by human activities. I hope this new knowledge will lead to the expanded use of such tools for both security and industrial purposes. We see graduates of the Department of Geophysics at Tel Aviv University playing a leading role in scientific and technological advancements, and we are confident that in the future, multi-purpose seismic-sensing technologies will be more widely used in various fields that impact our daily lives.”