Researchers at the University of Bristol have developed a method to measure the movement of the Earth's deep interior, which controls continents and ocean locations. This technique uses seismic waves to study the properties of a mysterious layer called D″, where the mantle meets the core.
Research reveals a causal relationship between rainfall and earthquakes, with variations in rainfall affecting pore-fluid pressure at depth and triggering earthquakes. Ground motion patterns in the Santa Clara Valley are also studied, revealing complex geological structures that influence seismic wave propagation and amplification.
The University of Nevada, Reno's earthquake engineering lab is expanding with a $12.2 million grant from the US Department of Commerce's National Institute of Standards and Technology. The new facility will house the largest shake table in the US and enable researchers to simulate complex seismic tests.
Scientists have mapped the unexplored offshore Northern San Andreas Fault, revealing deep rifts and high walls with areas supporting animal life. The study aims to understand past earthquakes and their impact on biological diversity.
Researchers successfully recreated the conditions deep in the Earth's mantle to study the behavior of post-perovskite, a mineral that helps explain faster seismic waves. The discovery provides new insights into the earth's internal heating and cooling processes.
Scientists have used a new seismic method to investigate the collision process between India and Tibet, revealing a more pronounced boundary between rigid lithosphere and softer asthenosphere. The study provides insights into the processes involved in the collision and aims to reduce earthquake risk in the region.
Researchers identified two apparent faults cutting young deposits near Olympia, Washington, suggesting recent fault activity and potential earthquake hazards. The study utilizes marine seismic reflection data to explore shallow structures associated with inferred faults in the Tacoma and Olympia areas.
An international team of scientists studied two Sumatra earthquakes, finding differences in sediment composition between the rupture areas. This difference may have contributed to a larger tsunami in the 2004 event, highlighting the potential for high tsunami hazards in this region.
Researchers have identified zones in the Iberian Peninsula with potential for moderate earthquakes, including parts of the Cordillera Cantábrica and Pyrenees regions. The study uses morphostructural zoning method to analyze topographic, geological, and geophysical data.
A team of scientists discovered that seismic slip on the Central Peru Megathrust is caused by a combination of earthquakes and non-seismic creep. This finding indicates that movement along this subduction zone is more complex than previously thought.
Scientists discovered that aseismic slip in the Nazca tectonic plate can prevent earthquakes from propagating through certain areas. By analyzing GPS data and aftershock patterns, researchers found a 'patchwork' pattern of aseismicity, with some areas always slipping slowly and others rarely experiencing seismic activity.
The USGS is providing $7 million in funding for earthquake monitoring to support the development of the Advanced National Seismic System (ANSS). This initiative will enhance the country's ability to detect and respond to earthquakes, ultimately saving lives and reducing economic losses.
Researchers investigate seismic activity in the Midwest US, shedding light on causes of intraplate earthquakes. The study reveals insights into stress within fault zones and the impact of glacial rebound on earthquake frequency. Key findings also highlight correlations between mantle density structures and topographic uplift.
The Seismological Society of America presents on earthquake forecasting, quantifying seismic event likelihood to provide communities with information about seismic hazards. The session also explores near-surface deformation associated with active faults and debates in earthquake science.
David Boore developed a well-known method for computing estimates of ground motion from simulated earthquakes, known as SMSIM. His work has advanced understanding of strong-motion seismology and influenced seismic building standards worldwide.
Researchers are working together to understand intraplate earthquakes in an effort to minimize the loss of life and property. By deploying seismic recorders and analyzing data from two large experiments, the team aims to advance knowledge of earthquake causes and hazards.
Art Frankel led a team to update national seismic hazard maps, vastly improving public policy and building codes across the US. The new maps were used directly in building codes, enhancing earthquake safety nationwide.
This BSSA tip sheet documents the long history of earthquake monitoring by the Southern California Seismic Network (SCSN), detailing its evolving sensitivity over time. Researchers also examine the predictive capability of models to estimate ground shaking during large earthquakes in the San Francisco Bay Area.
Researchers found that toad populations in Italy shifted their behavior from breeding to evacuation mode five days before a significant earthquake. The ionosphere disruptions detected pre-seismic cues like radon gas releases and charged particles, allowing the toads to detect earthquakes earlier.
A Rensselaer Polytechnic Institute professor and his team are monitoring aftershocks in Chile following a massive 8.8-magnitude earthquake on Feb. 27. The 10-member team installed over 50 broadband seismometers to record seismic activity along a 500-kilometer zone, providing valuable data for understanding the earthquake's impact.
Researchers found a plausible cause for small earthquakes in North Texas linked to the operation of a saltwater injection disposal well. The study suggests that fluid injection may have affected tectonic stress, reactivating faults and generating quakes.
Researchers aim to improve understanding of earthquake mechanisms and volcanic eruptions using highly complex calculations on supercomputers. The QUEST project will provide a more detailed picture of the Earth's internal structure, enabling better modeling of earthquake scenarios.
Researchers detected ocean internal tides using seismic imaging, revealing a new tool for studying ocean mixing. Meanwhile, Arctic ice was found to be 'rotten' due to uniform temperature, threatening marine ecosystems and climate science.
Asteroids that come within a quarter of the distance between Earth and the moon experience seismic shakes strong enough to create fresh surface material. The finding helps answer decades-long questions about meteorite origins and opens a new field of asteroid seismology.
Researchers used high-resolution seismic data to analyze fault evolution across the Gulf of Corinth rift, revealing patterns of basin subsidence and fault activity. The study provides new insights into early rift history and the development of faults associated with the rift, shedding light on seafloor spreading mechanisms.
Researchers at UC San Diego's Englekirk Structural Engineering Center conducted comprehensive shake tests on semi-gravity reinforced concrete cantilever walls. The project aims to improve the seismic design of California's thousands of miles of retaining walls, ensuring safer transportation systems.
Researchers have imaged Yellowstone's plumbing using seismic waves, revealing a plume of hot rock rising from the northwest at a depth of at least 410 miles. The new findings suggest a larger magma chamber than previously thought, potentially leading to an even more catastrophic eruption.
A new study by an international team has used seafloor seismometers to image the Hawaiian mantle, revealing a high-temperature plume from the lower mantle. The findings suggest that the Hawaiian hot spot is the result of this upwelling plume, which tilts southeastward as it extends downward.
A recent study published in BSSA found that certain types of subduction zones exhibit lower earthquake production rates, contradicting previous assumptions. The research suggests that the efficiency of earthquake production is influenced by fault slip rate and relative plate velocity.
Seismic images of a mantle plume extending to depths of at least 1,500 kilometers reveal the roots of Hawaii's volcanic hotspot. The PLUME project provides high-resolution seismic images of the structure beneath the island of Hawaii.
Scientists discover that smaller tectonic structures near larger faults in southeast Spain partially offset the risk of earthquakes, reducing seismic activity. By studying fossils and geological data, researchers found that these small faults help relax energy associated with plate convergence.
Researchers aim to correlate seismic activity with glacier slip using pump tests and measurements of natural seismicity. The projects focus on stability of ice stream grounding zones and role of active subglacial lakes in ice sheet loss.
Scientists are using seismic noise to reconstruct the history of hurricanes in the North Atlantic, analyzing patterns produced during hurricanes and regular storms. Preliminary results suggest that hurricanes produce recognizable patterns, allowing researchers to potentially establish a link between global warming and hurricane frequen...
Scientists at Carnegie Institution found a way to monitor fault strength deep in the Earth using highly sensitive seismometers. This method detects subtle changes in earthquake waves indicating weakening of the fault and corresponding periods of increased small earthquakes.
A 2004 Sumatran earthquake may have weakened a portion of California's San Andreas Fault, changing its fault strength and potentially triggering increased global seismic activity. The study, published in Nature, examined seismic records from Parkfield, Calif., and found repeated microearthquakes occurred near the fault
New study locates source of L'Aquila earthquake, finding it increases seismic hazard in region. Researchers also find waning sea ice bodes stormier, rainier Arctic with increased precipitation. Additionally, scientists develop new method to measure snow depth using GPS technology.
Researchers found that elephants use two pathways to 'hear' ground-borne vocalizations: somatosensory pathway through feet and trunks, and bone conduction pathway through toenails. This allows them to understand seismic communication over long distances.
Scientists have developed a new method to monitor underground movements using earthquake data, allowing for comprehensive mapping of the Earth's seismic activity. This breakthrough increases the number of locations that can detect seismic activity and enables monitoring from far deeper within the Earth.
Using ambient noise correlation, University of Illinois researchers Xiaodong Song and Zhen J. Xu observed significant changes in the behavior of parts of Earth's crust affected by three major earthquakes. The technique allowed them to detect tiny changes in seismic velocity over large areas.
A team of scientists has deployed a seismic network around Isla Isabela in the Galapagos to study Sierra Negra volcano. The new data will provide the first 3-D pictures of the volcanic plumbing system, helping to clarify its depth and extent.
A new study found no daily or weekly pattern to earthquakes in Western U.S. due to human activity. Seismic stations struggle to detect M>1 earthquakes, making it appear like more occur on Sundays and late at night. Researchers explored speleothem records in caves for accurate quake documentation.
The University of Nevada, Reno's Seismological Lab is conducting a seismic survey through downtown Reno to create an earthquake hazard map. The team, led by Professor John Louie, is using industry techniques to map suspected faults and confirm previous findings.
A new study evaluates expected ground motion in Seattle, Victoria, and Vancouver from earthquakes of magnitude 7.5 - 9.0, providing a tool to build or retrofit structures to withstand seismic waves. Ground motions are estimated for firm ground at the three sites, with a model that engineers can adjust for local soil conditions.
A UT Knoxville-led research project is exploring the East Tennessee Seismic Zone (ETSZ) to better understand seismic activity and its impact on future earthquakes. The study aims to provide new information on past quakes and inform the planning of new large engineered structures.
Recent research includes the documentation of Holocene rupture on major faults in Lake Tahoe Basin and evidence for a large paleolake in Western Desert, Egypt. A study on groundwater system in southern Colorado Plateau-Arizona Transition Zone also sheds light on seismic hazards in western Washington State.
Chevron-shaped dunes are not indicative of mega-tsunamis, contrary to popular speculation. Microbial life extends fossil record by 1.5 billion years, while nanoscale cristobalite fibers in volcanic ash hint at adverse health effects. The largest trilobites ever found provide insight into Earth's first animals and fossil evidence.
Researchers found a layer on top of subducted plates where S-waves are 30-50% slower than typical oceanic crust, indicating high water saturation levels. This ultra-slow-velocity layer is linked to slow earthquakes and non-volcanic tremors, providing clues about their causes.
Researchers tested a one-story masonry structure with clay masonry veneer to evaluate its seismic safety. The test, which simulated earthquakes of up to 8.0 magnitude, showed the building performed well despite minor damage during initial shaking.
Recent observations from the USArray transportable array and EarthScope instruments have shed new light on seismic wave propagation and the evolution of the Yellowstone hotspot. The analysis suggests a common mantle source for the region's unique topographic features, providing valuable insights into geological processes.
Researchers linked pre-historic seismic events on the San Andreas Fault to assess likelihood of future great ruptures. Analysis suggests several events similar to a historical earthquake occurred since A.D. 900 on the southern San Andreas fault.
The newly-laid MARS cable enables the use of MOBB's broadband seismometer data in real-time with other land-based stations to determine earthquake locations and mechanisms. This improvement aims to enhance understanding of the San Andreas fault system and provide early warnings for ground shaking.
David Wald's work has advanced seismic data analysis, enabling efficient dissemination of earthquake information to first responders and the public. His programs, such as ShakeMap and 'Did You Feel It?', have become invaluable tools in humanitarian disasters.
AfricaArray trains masters and doctoral students in geophysics, supports research on the African superplume. The program combines student education with research and field schools, aiming to improve understanding of the continent's geological phenomena.
Research reveals that elephants rely on bone conduction to detect seismic signals in estrus calls, allowing them to triangulate the source with greater accuracy. This method is more effective than somatosensory reception, which involves vibration-sensitive cells in the foot.
A team of Danish researchers has discovered the origin of the Baikal Rift Zone, a 2000km long crack in the Earth's crust that created the world's deepest lake. The study shows that the bottom of the crust is flat across Lake Baikal, contrary to previous models, and is instead thinning due to magma intrusion.
Scientists investigated early warning system accuracy, finding it unlikely to estimate large earthquakes with high precision. Rapid magnitude estimation works better when using multiple seismic stations in close proximity to the fault.
Researchers have discovered two giant plumes of hot rock deep within the earth linked to plate motions that shape the continents. The superplumes, one beneath Hawaii and the other beneath Africa, are surrounded by a wall of plates from Earth's crust that have sunk into the mantle.
Researchers found that a magnitude 9.2 Indian Ocean earthquake triggered non-volcanic tremor at the Parkfield region of the San Andreas fault, approximately 125 miles away. This low-stress event sheds new light on seismic phenomenon and its potential role in releasing stress within an earthquake-producing fault.
Researchers use simulated earthquake tests to improve seismic assessment tools and critical retrofit designs for non-ductile reinforced concrete frames with masonry-infilled walls. The project aims to assess the resistance of these structures under realistic seismic load conditions, developing reliable analytical models to evaluate the...
A Caltech-led team found that the subduction zone in Sumatra has not released enough strain from recent earthquakes, increasing the likelihood of another large event. The researchers analyzed seismological records and data gathered by GPS stations to determine that only a quarter of the accumulated stress was released.