Articles tagged with Seismology
New seismic data gathered by Stanford University researchers provides the first west-to-east view of the subsurface where India and Asia collide. The study suggests two competing processes are operating beneath the collision zone: movement of one tectonic plate under another, as well as thinning and collapse of the crust.
Researchers at ETH Zurich propose an alternative theory for the formation of the Alps, suggesting that the mountains were uplifted by the subduction of the Eurasian plate beneath the Adriatic microplate. This new model simulates the processes leading to the formation of the Alps and explains the observed seismicity in the region.
A recent study used OBS data to clarify the formation mechanism of the Double-peak seamount in the Northwest Sub-basin (NWSB) of the South China Sea (SCS). The survey revealed a high velocity layer at the bottom of the crust, indicating possible in-situ mantle serpentinization or lower crust magma underplating. The study enriches the d...
A magnitude 5 earthquake near Le Teil in southern France revealed unexpected surface rupture and ground displacement, reactivating the ancient La Rouvière fault. The event raised concerns about seismic risk in France and Western Europe, with potential for other faults producing similar surface ruptures.
A team of scientists installed an optical seismometer on La Soufrière de Guadeloupe volcano's summit to monitor gas and steam eruptions. The instrument collects data that will be combined with other observations to better understand the volcano's explosive potential.
Researchers have matched seismic signals with aurora displays in Alaska, offering a new way to study magnetic fluctuations. By combining data from all-sky cameras and seismometers, scientists can better understand the link between solar winds and the Earth's magnetic field.
The study reveals an 'inchworm-like' slip evolution of supershear rupture along the Palu-Koro fault, showcasing the effect of complex fault geometry on rupture propagation. This phenomenon may have significant implications for assessing future earthquake impacts and related disasters.
A recent study found that COVID-19 lockdowns led to a 50% global reduction in human-caused seismic noise, with the most pronounced effects seen in densely populated areas. This 'anthropause' phenomenon has provided a unique opportunity for researchers to better distinguish between human and natural seismic noise.
Researchers found a significant link between well depth and seismic probability, suggesting that deeper wells are more likely to trigger earthquakes. The study also revealed that the type of fluid used in hydraulic fracturing, including gel vs. slickwater operations, may affect seismic activity.
Researchers have discovered ancient volcanic activity and subtle, unusual movements in the Earth's surface in the Eifel region of Germany, suggesting a greater risk to northwestern Europe. The study suggests that the region is an active volcanic system with significant seismic activity.
Researchers at Kyushu University analyzed data from NASA's InSight lander to determine the sources of different types and frequencies of Martian microtremors. The study found that low-frequency P-waves were related to changes in wind and solar irradiation, while higher-frequency ambient noises were dominated by lander vibration.
A typhoon-induced event altered the frequency and location of earthquakes in Taiwan by changing crustal stress levels. This study suggests that surface processes can trigger seismicity, highlighting a new connection between tectonics and external factors in earthquake hazard assessment.
A new study maps over 22,000 tremors to recreate the complex three-dimensional structure of a fault zone in southern California. The research reveals that dynamic pressure changes from natural fluid injections controlled the evolution of an earthquake swarm in the region.
A four-year-long earthquake swarm near Cahuilla, California was driven by a naturally occurring injection of underground fluids, revealing complex conditions for fluid flow within the fault zone. The study provides new insights into seismic processes and brings closer concrete explanations for how earthquake swarms start and terminate.
A team of geoscientists used seismic anisotropy to create high-resolution, 3D images of mantle flows in a subduction region. The images revealed fragmented tectonic plates and complex mantle flow patterns.
Researchers have created a new map revealing the Earth's mantle at a depth of 3,000 kilometers by analyzing thousands of seismic waves collected over 30 years. The map shows hot and dense regions below Hawaii and French Polynesia.
Researchers at University of Alaska Fairbanks found that seismic surveys can cause long-lasting scars on the tundra, affecting its hydrology and habitat. The study emphasizes the need for more data on seismic exploration impacts and better weather records to minimize damage in the Arctic Refuge.
A new method for creating digital replicas of rock samples is being developed by geoscience researchers at the University of Texas at Austin. This technique allows scientists to learn about rock samples without touching them and can be used to calculate important rock properties such as permeability and electrical conductivity.
A new study proposes a model for the formation of diamond-bearing kimberlites in Northern Alberta, which was caused by the movement of an ancient slab of oceanic rocks. The research combines geophysical imaging, geochronological dating and plate motion calculation to explain how diamonds came to Earth's surface.
Researchers discovered new variants of feldspar stable under extreme pressure conditions, potentially altering seismologic signatures and plate dynamics. The high-pressure polymorphs were formed through severe geometrical distortions in the tetrahedral framework.
Researchers from Los Alamos National Laboratory have developed a new technique that separates industrial noise from natural seismic signals using cloud computing. The approach allows for large-scale seismic analysis ten times faster than traditional methods and has the potential to transform the field of seismology.
Scientists have measured the velocity of seismic waves in iron-sulfur alloys thought to comprise Mars' core, providing crucial information about the planet's internal structure. This study simulates the Martian core's composition and origin, helping researchers compare observations with Martian space probes.
A recent study used fiber optic cables to capture seismic signatures of the Rose Parade, capturing the vibrations of marching bands and floats. The technique, called distributed acoustic sensing (DAS), revealed distinct signals from the parade, including harmonic frequencies corresponding to even-stepping marching bands.
NASA scientists have developed a new seismometer system called SUBLIME to measure moonquakes and map the Moon's interior. The system will alert astronauts to seismic events and provide an early-warning system, with the long-term goal of establishing a network of seismic stations.
The Stanford study develops a calculation of the risk that shaking triggered by a given project will be felt in surrounding communities. The authors propose setting yellow-light thresholds approximately two magnitude units below the red light to reduce nuisance-level shaking.
The study presents a comprehensive view of tectonic stresses acting on North America, offering regional clues about subsurface behavior. The findings have implications for understanding and mitigating induced seismicity, particularly in areas targeted for energy exploration.
Researchers have found that fault segments connected at depth can influence earthquake risk and magnitude. A study suggests that a rapid decay in slip at the edge of a fault segment indicates a connection below the surface.
Researchers propose that rocks colliding inside a fault zone during an earthquake produce high-frequency vibrations, which could help explain puzzling seismic patterns and predict quake damage. The new explanation suggests smoother faults with rounded internal structures may produce less damaging quakes.
Researchers at MIT have developed a machine learning method to fill in the missing low-frequency seismic waves in human-generated seismic data, allowing for more accurate mapping of underground structures. The technique was trained on simulated earthquakes and used to infer missing frequencies from new input data.
Researchers analyzed Marsquakes from InSight mission, finding moderate seismic activity intermediate between Earth and the Moon. The data revealed geological layers within the planet and identified areas of high geological activity, guiding future missions searching for potential life.
Seismologists have recovered nearly 40-year-old seismic data tapes from the 1980 Mount St. Helens eruption, providing a near-continuous sequence of activity leading up to the May 18th event. The data analysis suggests no significant change in seismic signals that would have hinted at an imminent major eruption.
A high-resolution catalog of earthquakes from the 2019 Ridgecrest sequence reveals complex rupturing and crosscutting fault structures. The catalog helps researchers understand the triggering and evolution of the sequence, shedding light on the physics and processes involved.
Researchers at Kazan University are developing advanced aerial drones with devices such as detectors and special cameras to enhance geological surveys. The goal is to analyze upper strata of rocks, evaluate hydrocarbon potential, and improve forest planning and soil analysis.
A new study has recalculated the magnitude of the Great Lisbon Earthquake from 8.5 to 9.0 to 7.7 using macroseismic data from Portugal, Spain, and Morocco. The analysis suggests that the earthquake's epicenter was offshore the southwestern Iberian Peninsula and may have involved faulting onshore.
Researchers at BP partner with ORNL to tackle the challenge of managing large seismic datasets, which can reach half a petabyte in size. The Adaptable I/O System (ADIOS) provides a flexible way to describe data, allowing for efficient compression and processing.
Researchers propose a new theory that iron particles fall from the molten outer core and accumulate on the inner core, creating piles up to 200 miles thick. This phenomenon could help explain seismic wave anomalies and provide insights into the Earth's interior composition and behavior.
Researchers at GEOMAR Helmholtz Centre for Ocean Research Kiel identify Volcano F as the origin of a large pumice raft drifting towards Australia. The team used satellite images and seismic data to confirm the connection between the volcano and the floating rocks.
A floating array of sensors in the Pacific Ocean will provide a comprehensive view of Earth's interior, offering insights into buoyancy, viscosity, density, and temperature of the deep mantel plume. The array will help scientists understand the plate-tectonic cycle that gives us energy and reveals the potential barriers for material fl...
Scientists are exploring the use of fiber optic cables as earthquake sensors due to their potential for accurate seismic data collection. Distributed Acoustic Sensing (DAS) technology uses internal flaws in fibers to detect changes in temperature, strain, or vibrations caused by seismic waves.
A new study from the University of British Columbia found that vivid images are more effective than statistical data in conveying earthquake risk. The researchers created an image showing a Vancouver elementary school after a major earthquake and found that people who saw it were more likely to sign a petition for seismic upgrades, wit...
Researchers used fiber-optic cables to create a seismic network that can detect earthquakes and map fault zones. The technique, known as Distributed Acoustic Sensing, uses laser light to measure strain in the cable, providing detailed images of the ocean floor.
A team of researchers from UC Riverside has determined a new geometric model for the Main Himalayan Thrust fault, allowing officials to better prepare for future earthquakes. The study found that the fault is still accumulating stress and may have increased the likelihood of another big earthquake nearby.
Researchers found that a shallow frozen ground layer likely caused more ground failure in the 1911 Kemin earthquake due to its ability to inhibit drainage of pore-pressure excess. The study suggests seismologists should consider seasonality in soil characteristics when making probabilistic liquefaction or ground failure assessments.
Researchers used 3D models of Cascadia megathrust events and geological evidence to recreate the 1700 earthquake's impact on the Pacific Northwest coast. The study suggests that a rupture extending just offshore could cause coastal subsidence, with an estimated magnitude between 8.7 and 9.2.
A new study published in Seismological Research Letters found that deep landslides triggered by the 1964 magnitude 9.2 Great Alaska earthquake were not reactivated by the 2018 magnitude 7.1 Anchorage earthquake. Researchers attributed this to the shorter duration and higher frequency of shaking during the 2018 quake, which likely kept ...
A comprehensive analysis of the Ridgecrest Earthquake Sequence reveals a web-like network of interconnected faults, challenging standard models of large seismic events. The complexity of the rupture is only clear due to the combined data from orbiting radar satellites and ground-based seismometers.
Researchers have discovered a new phenomenon where strong storms can produce vibrations in the ocean floor as strong as a magnitude 3.5 earthquake. The study found over 10,000 stormquakes occurring from 2006 to 2019 offshore of various locations, including New England and Florida.
Researchers found a connection between strong storms and intense seismic activity near the edge of continental shelves. Over 10,000 stormquakes were detected off the US and Canadian coasts from 2006 to 2019, lasting hours to days.
Regional seismic networks in North America contribute to nuclear test monitoring, particularly for low-yield explosions. These networks can detect and locate small seismic events that are difficult for global systems to identify.
Researchers at GFZ Potsdam identified clear warning signs before the Anak Krakatau volcano's flank collapse, which triggered a deadly tsunami. The study analyzed data from various sources, including satellites and seismic data, to better understand the event and improve early warning systems for other volcanoes.
Researchers found low-velocity pockets along the rifting axis indicating areas filled with gas, raising concerns about environmental implications. The trapped gas could be a potential untapped natural resource or contribute to greenhouse gases if released.
The PermaSense project has recorded a unique 10-year record of high-resolution data on the Hörnli ridge of the Matterhorn, offering a better understanding of processes that can lead to rock destabilization. The data set includes measurements of temperature, seismic activity, and deformation of the mountain ridge.
A new study found that seismic air gun signals can damage the sensory organs and righting reflexes of rock lobsters. The research, published in the Proceedings of the Royal Society B, reveals that exposure to these signals can cause lasting harm to lobsters' statocysts and ability to function in the wild.
A team of seismologists from Caltech is tracking thousands of tiny aftershocks in the Ridgecrest region using a novel fiber optic network. This technique involves shooting light down unused fiber optic cables, which act as individual seismometers, allowing for unprecedented detail on the evolution of earthquake sequences.
Researchers at KAUST have developed a computational method to model large accumulations of subsurface salt, a challenging material to derive accurately from seismic imaging data. This technique allows for the efficient extraction of oil and gas by pinpointing fossil fuel reservoirs with greater accuracy.
A new volcano monitoring platform, MOUNTS, analyzes satellite images using artificial intelligence to detect precursory signals and provide early warnings for volcanic eruptions. The platform, which integrates multiple sets of diverse data types, has been successfully tested on recent events and currently monitors 17 volcanoes worldwide.
The 2015 Gorkha earthquake filled a significant knowledge gap in understanding Himalayan seismicity, revealing that the Main Himalayan Thrust fault changes geometry along-strike. This finding improves understanding of earthquake hazards in India and Nepal by identifying potential locations for future earthquakes.
The 2015 Gorkha earthquake's rupture length was likely controlled by spatial variations in the Main Himalayan Thrust, according to a new study led by Prof. BAI Ling from the Institute of Tibetan Plateau Research. The researchers used seismic waveforms and waveform modeling to determine source parameters and velocity structures.
New research from University of Alberta scientists suggests the Canadian Rockies were formed through a westward collision event more than 100 million years ago. This finding challenges the traditional accretion model and instead proposes a sudden collision event between two continents.
Researchers used supercomputers to simulate complex earthquake ruptures, documenting interactions between faults and analyzing results with advanced visualization software. The model helps understand how faults interact during earthquake rupture, enabling scientists to study past earthquakes and possible future scenarios.