A global Android smartphone-based earthquake detection and early warning system detects seismic activity in real time and delivers effective alerts, rivaling traditional seismic networks. The system, which harnesses the power of existing smartphones, has collected voluntary feedback through user surveys, indicating that 85% of recipien...
A recent study analyzed seismic waveform data from a tsunami earthquake (Mw 8.3-8.5) that occurred off the British South Sandwich Islands in 2021. The team found a combination of directional variation in rupture propagation and slow slip events contributing to long-duration shaking, differing from conventional models.
Researchers analyzed seismic waveform data to reveal a complex source process with multiple rupture episodes. The study found that the earthquake exhibited unconventional rupture behavior, with asymmetric ruptures propagating in both north and south directions.
Researchers detected a slow slip earthquake in Japan's Nankai Fault, behaving like a tectonic shock absorber. The event revealed fluids are a key ingredient for slow earthquakes and confirmed that the fault releases pent-up energy harmlessly.
A powerful earthquake struck Myanmar, causing widespread collapse of vulnerable buildings that led to majority of deaths and destruction. The report calls for adopting modern seismic building codes and prioritizing retrofitting of existing structures.
A new laboratory earthquake model connects the microscopic real contact area between fault surfaces to earthquake occurrences, offering insights into earthquake mechanics and potential prediction. Continuous monitoring of physical properties could provide new tools for short-term systems and reliable prediction.
Researchers mapped electron density in the ionosphere and observed unique 3D wave patterns after the 2024 Noto Peninsula Earthquake, showing earthquakes generate waves from multiple points along the entire fault line. The study provides new insights into how earthquakes affect the upper atmosphere.
A new near-real-time prediction model for earthquake-triggered landslides has been developed, utilizing a global database of 398,698 mapped events and cutting-edge deep learning. The model achieves spatial accuracy exceeding 82% and can generate probability maps of landslide occurrence in under one minute.
A magnitude 7.7 earthquake struck central Myanmar on March 28, 2025, causing 4,900 fatalities and widespread destruction. The event exposed weaknesses in urban planning, preservation, and disaster preparedness, emphasizing the need for reconciliation with seismic resilience.
Researchers found that socially and economically marginalized groups face higher earthquake risk due to housing conditions, income, language, and race. Governments can design more inclusive emergency response strategies by integrating social vulnerability measures into disaster-risk assessments.
Researchers have discovered that the Wasatch Fault's shallow dipping angle at depth may lead to stronger, more intense shaking at the surface, increasing the risk of injury and destruction. The scientists found that the fault rocks themselves are weaker due to past deformation, priming the fault for future failure.
A team of researchers from the University of Tokyo used simulations to create a detailed 3D model of a fault, which helped them understand how different parts of a fault contribute to uplift during an earthquake. The study revealed that fault geometry is a critical factor in determining the impact of earthquakes on land.
A recent study by Virginia Tech researchers found that a major earthquake could expand the coastal floodplain by 35-116 square miles, affecting thousands of residents and properties. The impact would be most severe in southern Washington, northern Oregon, and northern California.
Advanced signal detectors have a low success rate detecting underground nuclear tests when seismic signals from nearby earthquakes overlap. Researchers found that even sophisticated multi-channel correlation detectors can only identify explosions with a 37% success rate, contrasting with a 97% success rate without earthquake interference.
Researchers are extending the earthquake history of northeastern North America by analyzing Native American place names and languages, revealing regular seismic activity and past large earthquakes. The study found that words for earthquake exist in several tribes' languages, suggesting a repetitive phenomenon.
Researchers analyzed sediment cores from four lakes in Guatemala, revealing the distinct direction of ground shaking during a magnitude 7.5 earthquake that devastated the country in 1976. The unusual pattern showed thicker deposits at the end of the fault rupture, indicating directional shaking.
A study by Christie Rowe and Alex Hatem found that faults are typically branching networks of fault strands, making them hundreds of meters wide. This suggests that significant parts of the broad array of fractures can be activated in a single earthquake.
Researchers at KAUST developed a highly accurate 3D dynamic model to better anticipate large earthquakes. The model provides a more accurate understanding of strong shaking during the Turkiye earthquake, enabling information for future seismic hazard assessments.
Researchers found that strong ground acceleration within a stepover geometry can launch boulder-sized rocks briefly defying gravity. The study suggests stronger shaking in the area nearest to the fault around stepovers and complex fault geometries should be accounted for in ground motion predictions.
The March 28 magnitude 7.7 Myanmar earthquake ruptured over 400 kilometers of the Sagaing fault, causing severe ground shaking and infrastructure damage. Seismologists shared early analyses of the event's fault properties, highlighting a supershear rupture and widespread triggering by dynamic stresses.
This study used high-resolution satellite data to rapidly assess coseismic surface ruptures caused by the 2023 Türkiye earthquake doublet. The research found separate rupture zones for each earthquake and highlighted seismic hazard risks for specific fault segments, including the Malatya Fault and East Anatolian Fault Zone.
A Kobe University study found that temperature at the plate interface predicts earthquake type, while a specific plate shape causes a seismic gap. Water released from rock transformation explains slow slip events and tectonic tremors, reducing stress between plates.
A new study by Reichman University and the Geological Survey of Israel found that the Israeli public prioritizes faster earthquake warnings over accuracy. Injuries from early warnings were negligible compared to damage without warnings.
A Rice University researcher is working to fortify buildings in Haiti against future earthquakes with cost-effective retrofitting solutions. The study, recently published in Earthquake Spectra, explores five techniques to improve seismic performance, including steel braces and reinforced concrete jacketing.
The study found the main shock and aftershocks concentrated at a depth of 12 km with high consistency across multiple methods, indicating a reverse thrust event with a small dextral strike-slip component. Historical GPS observations and geological surveys revealed the earthquake was triggered by Lajishan Fault activity.
Researchers forecast shaking damage from crustal earthquake scenarios in Mexico City, with varying levels of damage depending on the region's underlying geology. The study modeled earthquakes up to magnitude 5.5 and found that one- to two-story buildings received the most damage, particularly in areas with soft lakebed sediments.
Researchers found a correlation between solar heat and seismic activity, suggesting that incorporating solar activity predictions into detailed Earth temperature models can improve earthquake forecasts. This study sheds light on the role of solar heat in triggering earthquakes, potentially providing a more accurate prediction method.
Researchers found that foliated rocks along a fault line exhibit anisotropic properties, causing uneven strength and contributing equally to earthquake generation. This discovery suggests that the properties of rocks may play a significant role in seismic activity.
A Japanese research team investigated the connection between housing damage from the Great East Japan Earthquake and all-cause mortality. The study found no significant relationship between the two, suggesting that public health efforts may have suppressed mortality rates.
Researchers used Synthetic Aperture Radar satellites to quantify off-fault damage and surface displacement caused by the two 2023 earthquakes. The study suggests that off-fault damage can reach up to five kilometers from the fault, contradicting previous estimates.
Researchers used a remote seismic station to detect and characterize an earthquake swarm in American Samoa, producing a new catalog of events. The technique employed, combining single-station data with deep-learning models, can be useful in sparse monitoring regions.
Researchers found evidence that repeated earthquakes like the 2024 Noto Peninsula earthquake shaped the region's topography. The study used satellite radar images to measure displacements caused by the earthquake, resulting in over 4m of uplift and emergence of new terraces along the northern coast.
A recent study published in Seismica journal has debunked claims that a magnitude 4.5 earthquake in Iran was a covert nuclear weapons test. The researchers analyzed seismic signals from the event and concluded that it was caused by natural geological forces, contradicting widespread misinformation on social media and news outlets.
Researchers developed a new algorithm that combines fibre optic data with traditional seismometer measurements to improve earthquake detection. The approach works well even in noisy environments and can be applied to any fibre network, enabling more detailed and effective seismic monitoring networks.
A team of researchers re-examined the aftershock sequence of the 2015 Bonin Islands earthquake and found no evidence for a record-breaking deep aftershock in the lower mantle. Instead, they discovered a distribution of aftershocks compatible with a 12-kilometer olivine sliver that sheds light on how deep earthquakes can occur.
If the Summerville phenomenon is an earthquake light, it might be that shallow earthquakes in the area released water-soluble gases like radon or methane, which were then ignited by static electricity or rock movement. Gas detectors could potentially test this hypothesis.
The university has patented a novel energy dissipation device using sand to protect buildings from earthquake damage. The device absorbs and dissipates seismic energy through specially designed containers filled with granular materials like sand.
A recent Colorado State University study demonstrates that climate change can affect earthquake frequency, as glaciers recede and slip along faults increases. This suggests that earthquake activity could increase as glaciers melt, impacting hazard assessment and seismology.
Scientists have developed a new technique to study faults, which can improve earthquake forecasts by determining the origins and directions of past rupture events. By analyzing curved scratches left on the fault plane, researchers can pinpoint where earthquakes start and spread, providing valuable insights for modeling future scenarios.
Researchers are on the trail of the 2011 mega earthquake's causes through deep-sea drilling. They aim to determine properties and processes in subduction zones, which can contribute to tsunamis.
The study discovered significant alterations in the region's state of stress and deformation following the 1975 Kalapana earthquake. The researchers found that Kīlauea's south flank experienced greater displacement prior to the earthquake, pointing to changes in mechanical properties influencing seismic activity.
A new study finds that reducing the depth of wastewater injection can decrease seismic activity, lending further support to this approach. The research suggests that regulatory efforts to backfill some injection wells with cement and reduce volumes have been effective in lowering Oklahoma's induced earthquake rate.
Baise's research has spanned earthquake site response, liquefaction, site characterization, regional wave propagation, ground motions models and earthquake damage assessment. She uses data-driven approaches to learn from observational data and was an early adopter of machine learning methods in model development.
A machine learning model predicts soil behavior during earthquakes, identifying areas vulnerable to liquefaction and providing contour maps for safer construction sites. The study uses geological data to create detailed 3D maps of soil layers, improving prediction accuracy by 20%.
A magnitude 4.8 earthquake in New Jersey triggered widespread alarm, but surprisingly, the epicenter showed minimal damage, while distant areas like NYC and Virginia experienced stronger shaking. An analysis of Lg waves revealed a previously unmapped fault with complex strike-slip motion and thrust, affecting regional hazard assessments.
Researchers have long believed that rock friction follows a simple relationship with temperature, but a new study published in PNAS suggests otherwise. The study reveals that different underlying mechanisms affect the frictional resistance of faults, which could improve earthquake hazard assessments and forecasts.
Researchers studied the 4.8-magnitude Tewksbury earthquake, which surprised millions with its strong shaking reports despite minimal damage near the epicenter. The study found that the rupture direction may have funneled the shaking away from the epicenter and toward the northeast.
A study found that a significant increase in plate-derived water beneath Arima Hot Springs occurred before the 1995 Kobe earthquake, potentially weakening the fault and triggering the quake. This phenomenon is similar to increased chloride ions and radon in groundwater, which have been reported as precursors to earthquakes.
Researchers propose that branch faults serve as 'on-ramps' for rupture on more mature main faults, leading to large earthquakes. The hypothesis is based on observations of past 25 years of magnitude 7.8 or larger continental transform earthquakes, which all originated on a branch fault.
A study found increased menstrual irregularities in women living in areas affected by the 2023 earthquake in Turkey. Risk factors included post-traumatic stress symptoms, chronic diseases, and smoking.
A new study examines the relationship between the 2024 M7.6 Noto Hanto earthquake and a preceding earthquake swarm in Japan's Noto Peninsula. The research highlights the importance of monitoring seismic swarms and understanding fluid migration patterns to enhance predictive models for future seismic events.
Researchers from Kyushu University have identified a link between fault strength and earthquake magnitude, suggesting that stronger faults are more likely to produce large earthquakes. The study analyzed seismic activity at over 1,000 locations and estimated the stress field and characterized faults as strong or weak.
Five boulders in northern New York and Vermont provide limits on earthquake shaking intensity. The age of the rock formations indicates how long it's been since a region experienced that level of shaking.
Researchers identified abnormal seismic activity three months before two major quakes in Alaska and California. The detection method uses machine learning to analyze datasets derived from earthquake catalogs.
Researchers questioned the Cascadia subduction zone's earthquake record, finding that turbidite layers showed no better correlation than random chance. The study suggests a need for further research on turbidite layers and their connection to past earthquakes.
A rare 'dual-initiation' mechanism led to Japan's violent Noto earthquake, which killed over 280 people and damaged 83,000 homes. The quake began simultaneously at two points on the fault, encircling a barrier and breaking it, releasing intense energy.
A novel negative-stiffness isolation device has been developed to provide multidirectional negative stiffness and energy dissipation, effectively mitigating earthquake impacts. The device's advanced design enhances seismic protection by offering a robust solution for safeguarding buildings in earthquake-prone areas.
Researchers from USU and international partners will investigate how earthquake energy accumulates and releases on major strike-slip faults. The project aims to improve earthquake hazard models and provide educational opportunities in Earth sciences.
Researchers tested GNSS data for rapid landslide prediction and found near real-time prediction possible within 40 minutes, according to Chen and colleagues. The study highlighted the importance of continuous monitoring and improved prediction models for regions susceptible to landslides.
Researchers applied sub-daily GPS to measure the spatial and temporal evolution of early afterslip following the 2010 Mw 8.8 Maule earthquake, revealing a nearly 10% reduction in coseismic displacement overestimation. The study enhances seismic hazard assessment and contributes to improving early warning systems.