Scientists used a study on the Tanlu Fault to demonstrate that self-similar fractal stress is better suited for characterizing the sources of destructive scenario earthquakes. The research found that this approach aligns more closely with observed earthquake phenomena.
Researchers analyzed historical shaking data from past earthquakes, including CHIMP data, to find that hazard maps for California and other countries predicted higher shaking than observed. The discrepancy was due to conversion equation issues between map values and intensity data.
The USGS considers sharing aftershock forecasts internationally to help people affected by earthquakes, but raises concerns about scientific sovereignty and cultural barriers. Research suggests that people value the information, but there are challenges to expanding it for public consumption.
Researchers at the Universiteit van Amsterdam triggered mini-earthquakes in a lab by applying a small seismic wave to a granular material. The study shows that these events can be understood using laboratory-scale frictional experiments, and its findings are relevant for understanding remote earthquake triggering in larger faults.
Researchers have found evidence of a multifault network at subduction interfaces, contradicting the long-held concept of a single main fault. This discovery has significant implications for modeling earthquakes and predicting risks, which could lead to improved forecasts and mitigation strategies.
Recent advancements in AI and IoT have improved earthquake prediction by identifying patterns in historical seismic data. However, limitations such as computational complexity, data quality, and interpretability remain, requiring a comprehensive approach to integrate diverse datasets.
A team of researchers identified a significant Mw7.5 earthquake in Japan as exhibiting characteristics of a 'seismic dragon king', demonstrating predictability. The study analyzed data from the Japan Meteorological Agency's focal mechanism catalogue using the load-unload response ratio (LURR) method.
The EQFL measurement calculates earthquake-related fatalities as a ratio to the country's population size, revealing Ecuador, Lebanon, Haiti, Turkmenistan, Iran, and Portugal have experienced the greatest impact. Smaller countries suffer more from earthquake fatalities due to their larger proportion of their population.
Researchers created detailed maps of a major continental earthquake using drones and field surveys. The study shows the rupture sequence started slowly on the Africa/Arabia plate boundary, then exploded at the Arabia/Anatolia boundary, activating the East Anatolian fault system.
The new USGS National Seismic Hazard Model shows nearly 75% of the US is at risk for damaging earthquakes, with a color-coded map highlighting areas most prone to shaking. The model identifies over 500 additional faults that could produce damaging quakes, updating the landscape of earthquake research.
Researchers used USGS source modeling and InSAR satellite data to analyze the 6.8 Al Haouz earthquake in Morocco, finding a compact source with slip between 15-35 km deep, deeper than expected for earthquakes in this region.
A panel of experts concluded that the November 2022 Peace River earthquake sequence in Alberta, Canada was likely induced by human activity. The study used questionnaires created to distinguish natural from induced earthquakes, and gathered data on fluid injection information and past regional seismicity.
Researchers analyzed seismic data from the region since 2014, detecting a 8-month long crustal seismicity transient suggesting a preparation process before the M 7.8 Kahramanmaraş earthquake. This highlighted high and increasing seismic hazard in the area.
Researchers used airborne lidar technology to create a map of over 1,000 deep-seated landslides in the Puget Lowlands. The study found strong evidence of the last major Seattle Fault earthquake, estimated to be magnitude 7-7.5, and potential traces of older earthquakes.
A 15th-century Hebrew prayer book has revealed a previously unknown earthquake affecting the Marche region in central Italy. The note describes an intense shaking event causing severe damage and partial collapse of buildings, with epicenter similarities to a 1799 sequence.
A new study demonstrates how unused telecommunications fiber optic cables can be transformed for offshore Earthquake Early Warning (EEW) systems. Researchers used a 50-kilometer cable to sample seismic data at 8,960 channels and achieved an approximate three-second improvement in EEW alert times compared to onshore DAS arrays.
Soil liquefaction, a destructive phenomenon during earthquakes, is redefined by this groundbreaking study. Liquefaction can now be understood to occur in drained conditions with low seismic-energy density levels, triggered by seismic shaking facilitating interstitial fluid flow within the soil.
The 1923 Kantō earthquake sparked devastating fires that killed 90% of Tokyo's population, making it one of the deadliest natural disasters in history. The study highlights the importance of fire prevention and response as part of earthquake mitigation plans for regions with strong seismic shaking and wood-framed buildings.
Researchers have created a new model using deep learning to forecast aftershocks, outperforming the current ETAS model on larger datasets. The Recurrent Earthquake foreCAST (RECAST) model demonstrates better performance and computational efficiency.
A new methodology, developed by USGS researchers, integrates earthquake-induced ground failures with ground shaking hazards to provide a comprehensive forecast for pipeline damage. This approach is crucial for identifying potential damage in buried gas pipelines covering hundreds of kilometers.
A team of scientists at Caltech used a section of fiber optic cable to measure the intricate details of a magnitude 6 earthquake, pinpointing four individual asperities that led to the rupture. The study demonstrates the potential of distributed acoustic sensing technology to improve our understanding of earthquake physics.
Decades of seismic data reveal that central Utah's earthquake 'swarms' are more common than other types of sequences, with 80% of sequences being swarms. The study also found that these swarms exhibit heterogeneous behavior across different locations in the region.
Researchers found evidence of a precursory phase of fault slip occurring two hours before large earthquakes, using global GPS time-series data from nearly 100 major quakes worldwide. The study suggests that many large earthquakes start with a precursory phase of slip or represent the tail end of a longer process.
Researchers found a hierarchical rupture growth through a complex fault network, promoting and halting rupture growth. The earthquakes' source areas developed a network of faults with bends, steps, and branches, leading to irregular rupture evolution and diverse triggering behaviors.
A study examined the seismic performance of 12 hospitals in Turkey's southcentral region, finding that base-isolated structures performed better than fixed-base ones during the 2023 earthquakes. The report provides valuable insights for policymakers and engineers to enhance hospital resilience and disaster response strategies.
The February 2023 Türkiye earthquakes were a devastating doublet, with two large aftershocks occurring within nine hours of each other. The first mainshock ruptured the East Anatolian Fault (EAF) bilaterally over 350 kilometers, creating surface fault offsets of more than six meters.
Satellite imagery revealed a rupture zone of approximately 75 km in length, with surface features showing a gradual widening and decrease in horizontal dislocations. The study found secondary hazards such as liquefaction mainly occurring in low-lying terrain.
Researchers at the University of Otago have discovered a new area of coastal uplift in Rarangi, Marlborough, using laser mapping and kelp genetics. The study provides new insights into Aotearoa's landscapes and recent earthquake impacts.
The study found that the Tanlu Fault Zone underwent episodic dextral strike-slip movement in late Cenozoic, with the Banquan Basin serving as a record of this process. The movement was linked to the evolution of the pull-apart basin and surrounding faults.
Faults in Ridgecrest, California were sensitive to solid earth tidal stresses before the July 2019 earthquake sequence. Researchers found a strong signal of tidal modulation after 2018, but it's unclear if it triggered the earthquake. The study suggests that tidal stresses may be an indicator of upcoming earthquakes.
Research shows that Mexico City hospitals follow well-established earthquake early warning (EEW) protocols, which have significantly reduced the risk of injuries to staff and patients. The protocols include protective actions such as evacuation procedures, drop-cover-hold, and turning off equipment, with reinforced drills helping to pr...
Researchers found tsunami deposits in a coastal mangrove pond that suggest a massive magnitude 8.7 or larger earthquake triggered the tsunami, potentially impacting both Caribbean and Atlantic coasts of Puerto Rico. The discovery provides valuable insights into seismic risk in the region.
A new report by the USGS and FEMA estimates that earthquakes cost the nation an average of $14.7 billion annually in building damage and associated losses. The report's updated estimate is twice the previous annual figure due to increased building value and improved hazards analysis.
Residents in affected communities emphasized the need for more tailored information, including aftershock forecasts and tsunami risk maps. The study highlights the importance of effective risk communication and community engagement to promote preparedness and safety.
An international team, led by Eric Sandvol from the University of Missouri, aims to better understand the makeup of the earthquake zone and surrounding areas. The team plans to deploy 250 seismometers around the East Anatolian fault to study energy waves produced by earthquakes.
Researchers have discovered a unique underwater spring in the Pacific Northwest that could provide insights into earthquake hazards. The Pythia's Oasis seep is sourced from water 2.5 miles beneath the seafloor at the plate boundary, regulating stress on the offshore fault.
Researchers have developed a way to quickly detect and assess glacial valley landslides in coastal Alaska, which can trigger dangerous local tsunamis. They use seismic data to pinpoint landslide events and estimate their volume, aiming to develop an operational detection tool for tsunami centers.
A recent study determined that the magnitude of a February 2023 Turkish earthquake is the largest ever recorded in its history. The researchers used a novel method to measure the event's moment magnitude, which yielded results higher than previously reported ones.
A study by Revathy Parameswaran and colleagues compared ground motion and magnitude estimates from satellite and seismic records for the 2021 Chignik earthquake. The researchers found that GNSS and strong-motion acceleration seismic data can be used interchangeably or jointly for rapid magnitude or ground motion estimation.
A new approach uses crowdsourced data from affected people to estimate earthquake impact within 10-20 minutes, potentially aiding early disaster management. The system analyzes 'felt intensity' reports, providing a basis for quickly assessing the severity of damage.
A new statistical model based on a global database of public reports can identify an earthquake as high- or low-impact within minutes. The researchers used over 1.5 million felt reports from 10,000 earthquakes to develop the model, which was able to provide impact results for 393 global events in 10 minutes.
Researchers at the University of Texas at Austin have discovered a frictional phenomenon that governs how quickly faults heal after an earthquake. This discovery could help scientists understand when and how violently faults move, providing valuable new insights into the causes and potential for large earthquakes.
A new study by Brown researchers reveals that changes in tectonic plate thickness impact the location of the Denali Fault, a major strike-slip fault. The findings provide key insights into how geological faults behave as they deepen, shedding light on earthquake hazards.
Researchers at Northwestern University developed a new earthquake probability model that considers the specific order and timing of previous earthquakes. This allows for more accurate forecasting and explains why earthquakes sometimes come in clusters.
Researchers used seafloor video and carbon dating to determine that an underwater landslide scar is too old to be associated with the 1918 earthquake and tsunami. Instead, they propose a rupture of a two-segment fault along the eastern wall of the Mona Rift as the source of the tsunami.
The University of Texas at El Paso will establish a national Center for Collective Impact in Earthquake Science, addressing low-probability but high-impact earthquake risk and community needs. Researchers aim to develop leading-edge earthquake research projects and integrate diversity into their work.
Researchers at Kyoto University have found that the Tohoku earthquake may have occurred upon a complete stress release, with data suggesting normal faults in both sedimentary formations above and below the plate boundary fault. This discovery provides insights into how fault slipping contributed to the devastating tsunami.
The study found that earthquake-accelerated landslides (EALs) can maintain accelerated motion for a long time after the earthquake, causing particularly serious human casualties in seismically active areas. Satellite radar observations detected and investigated EALs in Central Italy, leading to the first ever complete EAL inventory.
A team of researchers from Cornell University has developed a method to study delayed earthquake triggering in laboratory settings. They found that the speed and strength of 'creep fronts' are sensitive to fault stress levels from previous earthquakes, which could potentially serve as local stress meters for predicting seismic events.
A new study found that edge waves and the short continental shelf contributed to the prolonged duration of the tsunami. The researchers used strong motion, GNSS, satellite, and tide gauge data to model the earthquake and learn more about the tsunami's behavior in Acapulco Bay.
Scientists have found that the tectonic stress in Japan's Nankai subduction zone is less than expected, contradicting predictions of a major buildup of pent-up energy. The research suggests that the fault may not be as unstable as thought, but still requires further investigation and long-term monitoring.
A new analysis by Devin McPhillips reveals that the recurrence interval for earthquakes along some California faults may be 16% longer than previously estimated. This is due to the incorporation of event likelihood, a variable quantifying how likely it is that a past earthquake is real and unique.
Seismologists have identified hundreds of thousands of microearthquakes along previously unknown fault structures in Oklahoma and Kansas, allowing them to map and measure earthquake clusters. The study found that nearly a 5% chance that a cluster would host a magnitude 4 or larger earthquake within a year if it reached a certain length...
Researchers found the Tonga tsunami reached 90 meters in height, outperforming previous tsunamis like 2011 Japan tsunami. The event emphasized the need for improved detection systems, as volcano-based tsunamis are currently 30 years behind earthquake-based event monitoring tools.
Researchers at the University of Illinois used single calcite crystals with varying surface roughness to simplify the physics of fault movement. The study found that friction can increase or decrease with sliding velocity depending on mineral types and environment, providing a fundamental understanding of rate-and-state equations.
A University of California San Diego study finds that importers highly dependent on Japan increased total imports of those products after the 2011 earthquake, intensifying offshoring rather than reshoring. Global supply chains are difficult to untangle following a crisis, and firms opt for offshore production to keep costs down.
Researchers in China have developed new techniques for monitoring and predicting earthquake precursors using satellite observation and ground-based methods. These methods include earth resistivity, magnetotelluric, geomagnetic, and geoelectric field observations, as well as EM radiation and satellite observation.
Seismologists analyzed historical accounts of the 1860 Jour de Pâques earthquake sequence, which may have released strain in a key fault zone. The analysis suggests that two large events occurred in 1860, one magnitude 6.0-6.4 and another 6.6-6.9, releasing built-up stress before recent earthquakes.
A new approach based on deep learning AI detects weak gravitational signals, or PEGS, generated by large-mass motion in megaquakes. This allows for real-time tracking of earthquake growth after a magnitude 8 event.
Researchers simulated earthquakes in a lab and found that fine-grained gravel formed at fault boundaries can trigger powerful ruptures, contrary to previous beliefs about stable faults. The study used high-pressure and shear simulations to show that rock gouge weakens friction between plates, leading to intermittent slip.