Articles tagged with Earthquakes
A study by Shinshu University researchers used input-output analysis to quantify economic damage from Japan's earthquakes. The study found that the largest earthquakes require significant economic assistance for initial production and recovery, with some requiring up to 50% of initial production until recovery.
Researchers found echoes from features deep inside Earth, revealing more widespread and heterogeneous structures at the core-mantle boundary. The study provided a new perspective on the geologic processes happening deep inside Earth, shedding light on plate tectonics and planet evolution.
Seismological studies revealed that weak rocks formed over 500 million years ago controlled the pathways of the 2016 magnitude 6.0 Petermann earthquake. The unusually long and smooth rupture was guided by these zones of weaker rocks, which can help forecast future earthquakes.
Researchers from Cardiff University have identified specific conditions along the ocean floor where tectonic plates creep past each other instead of generating catastrophic earthquakes. This discovery could help scientists better understand stress at fault lines and improve earthquake forecasting.
The Fast Loaded Dice Roller (FLDR) algorithm simulates the roll of loaded dice to produce random integers with the best combination of speed, accuracy, and low memory requirements. FLDR can use up to 10,000 times less memory storage space than existing methods.
Engineers at the University of Missouri have developed a flexible material that can help buildings withstand multiple waves of energy in earthquakes. The material, which can stretch and form to a particular surface, protects against both longitudinal and shear energy waves.
A Florida State University researcher has identified 85 previously unknown submarine landslides in the Gulf of Mexico between 2008 and 2015. These landslides pose significant risks to coastal communities and seabed infrastructure, including oil platforms and pipelines.
Researchers confirm three historic earthquakes on the San Andreas Fault in the Monterey Bay Area, occurring in 1838, 1890, and 1906, using a new model that accounts for charcoal inbuilt ages. The study uses a technique called wiggle matching to determine precise dates and recurrence intervals.
Researchers used 'Lettere Patenti' documents to calculate intensities for a 1703 earthquake sequence in central Italy, revealing that the main earthquakes were likely intensity V or VI. The study provides a more realistic view of the earthquakes' impact than historical reports, shedding new light on seismic intensity assessment.
Researchers confirm that the Earth's inner core is rotating, contradicting previous studies suggesting it was stationary. The new evidence comes from analyzing seismic data from repeating earthquakes and precise arrival time analysis.
Researchers from Germany, Chile and the US use satellite data to identify Earth's surface deformation months before massive earthquakes. This detection enables scientists to better understand precursor activity that may trigger earthquakes.
Researchers found large-scale wobbling in the Earth's surface near plate boundaries before massive Chile and Japan quakes. The study suggests that periods of enhanced tugging may accelerate the inevitable failure at shallower segments of the subduction zone, leading to great earthquakes.
Researchers found a 'wobble' in Japan's landmasses before the 2011 magnitude-9 earthquake that killed over 15,500 people. The movement, detected by GPS data, may indicate future large subduction-zone earthquakes. However, the study's findings cannot be applied to other subduction zones without comparable data.
Researchers mapped and measured fault roughness using high-resolution seismic data, finding that rougher surfaces are stronger and more resistant to earthquake slip. The study's findings may help explain why certain earthquakes are stronger than others.
Researchers developed a holistic model combining property damage estimates with community-wide economic impacts and social costs. The study found that poorer individuals experience greater losses in well-being, with a 60% loss of average annual income for those at the bottom.
Researchers found that large earthquake sequences are 'burstier' and more difficult to predict than expected, with irregular gaps between event bursts. This finding could impact seismic hazard assessment and the way we evaluate an event's likelihood of repeating soon after a large earthquake.
Researchers demonstrate the potential for using existing optical fibers as seismic sensors, providing high-resolution maps of shallow subsurface and validating a new technique. The approach has great potential for use in large earthquake-threatened cities with extensive networks of buried optical cables.
Researchers found that variations in subducting sediments can influence the magnitude and location of megathrust earthquakes. Sediment thinning caused by volcanic activity may play a key role in determining the size and distribution of these catastrophic events.
An international team of scientists has identified the conditions that lead to slow motion earthquakes by drilling down to 1km deep in water depths off New Zealand. The study revealed a unique mix of different rock types and topography that causes slow slip events, which can trigger larger earthquakes and tsunamis.
Research from a global team of scientists found that diverse rock types at New Zealand's largest fault contribute to varying earthquake types. Slow slip events and tsunami-generating tremors are linked to the unique properties of each rock type.
Researchers found a strong 'cross-correlation' between inter-earthquake distances and times, especially after large earthquakes. The study's results could help seismologists better understand earthquake patterns and inform policymakers about disaster preparedness.
A major international study has shed light on the mechanisms triggering deep earthquakes up to 40km below the Earth's surface. The research suggests that interaction between creeping shear zones loads stiff rocks, causing them to snap and generate earthquakes.
A new study analyzed temporal evolution of seismicity and growth of maximum observed moment magnitudes in various stimulation projects. The results show a clear linear relation between injected fluid volume and cumulative seismic moments for most projects, indicating that seismicity can be managed by changes in injection strategy.
A new study found that underwater mountains pulled into subduction zones can set the stage for powerful quakes and create conditions that end up dampening them. Researchers used a computer model to simulate the effects of seamounts on surrounding rock and sediment, finding that the brittle rock ahead of the seamount creates powerful ea...
A new algorithm can detect changes in gravity caused by earthquakes, potentially leading to earlier warnings and more accurate predictions. The signal is generated by the sudden shift in the earth's internal mass during an earthquake, and its detection could help identify strong earthquakes that may trigger tsunamis.
A Montana State University researcher will investigate the extent and processes of microbial life in Yellowstone's subsurface using a specialized instrument triggered by earthquakes. The research aims to bridge biology and geology to understand how Earth's natural processes influence microbial evolution.
A new technique uses seismic waves from distant earthquakes to image the subterranean structure of Cleveland volcano. The study, published in Scientific Reports, resolved the architecture of the lower and middle crust for the first time, providing crucial information for emergency planning and saving human lives.
Researchers found that upper-plate earthquakes, not subduction earthquakes, caused coastal uplift along New Zealand's Northern Hikurangi Margin. Marine terraces at two sites showed different uplift patterns, leading to the mapping of new offshore faults that may contribute to these earthquakes.
Researchers found multiple faults with evidence of over 10 meters of slip during past large earthquakes in the Japan Trench fault zone, revealing a complex history of seismic activity. The technique used to analyze organic molecules in sedimentary rocks provides new insights into the likelihood of future tsunamis and earthquake hazards.
Researchers at the University of Ottawa have found evidence that slow earthquakes are related to dynamic fluid processes at the boundary between tectonic plates. The team used a technique similar to ultrasound imagery and analyzed rock properties to confirm that fluid pressures fluctuate during an earthquake cycle.
Researchers have discovered slow-slip events along the Nankai Trough subduction zone, which can last for hours or months and are difficult to detect using conventional seismological techniques. The study used a Global Navigation Satellite System-Acoustic ranging technique to monitor changes in the seafloor's position.
Researchers have observed processes in the upper mantle before a new submarine volcano formed off the Comoros island. The team reconstructed the partial emptying of a large magma reservoir and identified a dramatic movement of molten rocks before the eruption.
Researchers have transformed submarine cables into a seismic network, tracking earthquakes and ocean waves. The new technology has the potential to fill blind spots in the global seismic network.
Researchers at Penn State used fiber-optic cables to detect tiny seismic events caused by thunder during a storm, marking the first time scientists have recorded thunder-induced seismic events.
Researchers at City, University of London are developing new vibration-control devices based on Formula 1 technology that can reduce the required weight of current TMDs by up to 70%.
Researchers at University of Technology Sydney developed a novel ground anchor technology to protect bridges against catastrophic earthquakes. The system uses high-tensile capacity steel cables, embedded into the ground behind the bridge, to deliver incredible strength and energy dissipation.
A new algorithm developed by University of California, Riverside researchers can spot patterns in massive datasets quickly, improving earthquake detection and monitoring insect vectors. The SCAMP algorithm has been used to detect 16 times more earthquakes than previously known and can also analyze the behavior of chickens.
A team from University of Tokyo utilized Summit's AI architecture to develop a faster solver for earthquake simulations, enabling more accurate models. The new approach accelerated simulation times by a factor of 1000, improving the efficiency and reliability of earthquake modeling.
A team of researchers created a model to predict induced earthquake activity from wastewater injection, accounting for various variables such as subsurface hydrology parameters and regional stress on faults. The model can help oil operators restrict injection control and prevent large earthquakes in Oklahoma.
A University of Iowa-led study found that Southern California earthquakes increased stress on the Garlock Fault, a major earthquake fault line. The research showed 'aseismic creep' along a 12- to 16-mile section of the fault, indicating it is sensitive to stress changes.
Researchers have characterized slow-slip events more precisely than previously possible, finding they obey the same scaling laws as regular earthquakes. This discovery opens the door for geoscientists to study these frequent and nondestructive events to better understand earthquake mechanics.
Researchers have developed a new method to study rocks along fault lines, revealing clearer views of the Earth's crust. This technique combines acoustic mapping with full waveform inversion, enabling scientists to better understand why earthquakes and tsunamis occur.
Researchers analyzed past major earthquakes in Mexico and Chile to understand earthquake cycles and calculate future seismic hazards. The data also helped develop new ideas about the physical processes involved in seismic rupture, geometry of subduction, and tsunami generation in the region.
A new study published in Seismological Research Letters has found that a series of small earthquakes in Surrey, UK, were not triggered by nearby oil extraction. The quakes, which occurred between April 2018 and May 2019, were found to have moved ancient faults horizontally, indicating natural causes.
Researchers measured the tower's vibrations using seismometers and found two primary resonance modes at frequencies of 0.8 and 1.0 hertz. The results help scientists understand how human-made vibrations affect seemingly unmovable rocks, offering a geological checkup for natural rock forms.
Researchers have discovered a connection between earthquakes and volcanic eruptions at Mount Aso in Japan. By analyzing very long period seismic waves, they found that earthquakes can trigger changes in pressure variations associated with magmatic activity, leading to eruptions.
Researchers discovered that slow slip events can arise with rate-strengthening friction, which produces stable sliding. The team found that changes in poroelastic pressure reduce friction, leading to a slow slip event.
Researchers at UTSA are developing indestructible cells that can dissipate energy during earthquakes without deforming or requiring repairs. The new architectural materials could reduce structural steel costs, be lightweight, and absorb high levels of energy.
Researchers have discovered that natural disasters like earthquakes and hurricanes follow a power law distribution, where smaller events occur more frequently. However, some events like forest fires deviate from this pattern and follow a lognormal distribution, contradicting previous studies.
The University of Texas at Arlington is developing an algorithm that models the effects of earthquakes on water pipeline infrastructure. This model determines how best to use limited infrastructure funding to make pipelines less prone to earthquake damage.
A comprehensive map of over 250 faults has identified the Fort Worth Basin as highly susceptible to seismic activity, with many small faults potentially capable of triggering earthquakes. The study recommends increased regulation and monitoring of wastewater injection to minimize the risk of induced seismicity.
Scientists from SMU, UT Austin and Stanford University found that the majority of faults underlying the Fort Worth Basin are sensitive to forces that could cause them to slip. The new study provides fundamental information regarding earthquake hazard to the Dallas-Fort Worth region.
Researchers at Virginia Tech have discovered a link between oilfield wastewater disposal and increased high-magnitude earthquakes. The study found that the percentage of high-magnitude earthquakes increases with depth, suggesting that stronger earthquakes may occur years after injection rates decline or stop.
A $2.7 million NSF grant will study an active flat slab in Colombia, investigating its effects on the continental crust and volcanism. The research will compare two parts of the flat slab, allowing scientists to understand the initial migration and cessation of volcanism, as well as the formation of ore deposits.
A study published in Nature Communications suggests that historical earthquake stresses can predict future seismic activity. Researchers analyzed centuries-old written records of damage to reveal 97% of earthquakes occurred on positively stressed faults.
Researchers have found that faults in the Imperial Valley are mechanically linked, forming a continuous fault structure. This could increase the likelihood of larger earthquakes in Los Angeles and surrounding counties.
A comprehensive catalog of earthquake sequences in the Fort Worth Basin reveals a decrease in seismicity rates since 2014, corresponding to reduced wastewater injection. New faults have become active, and seismicity continues at greater distances from injection wells over time.
Researchers discovered that tidal fluctuations cause the magma chamber to expand, forcing the lower block of earth to slide up the fault, resulting in earthquakes. Even small stresses can trigger tremors, making it difficult to predict when an earthquake will occur.
Researchers from Georgia Institute of Technology found that perfecting an ideal 'invisibility' cloak for stress waves is impossible. However, limited cloaking technology could still provide a degree of protection against certain stress waves, particularly in earthquakes.
Researchers have found a consistent pattern in GPS data that can detect signs of acceleration 10-15 seconds into an earthquake, potentially enhancing early warning systems. This discovery could strengthen the accuracy of seismic alerts, especially for magnitude 9 Cascadia subduction zone ruptures.