Articles tagged with Earthquakes
The collaboration aims to refine national seismic hazard models by sharing expertise and research topics. The focus section discusses different modeling approaches and primary audiences, providing insights into the consequences of similar megathrust earthquakes in each region.
The UW RAPID facility will provide next-generation tools for collecting post-disaster data, including laser scanning equipment and mobile devices for social surveys. The center aims to reduce physical damage and socio-economic losses from future events by analyzing complex data sets and improving mathematical models.
A new fault has been identified in the Salton Sea area of Southern California, which could impact current seismic hazard models and earthquake risk assessment. The discovery provides much-needed information on the intricate structure of earthquake faults beneath the sea and may offer new insights into the region's earthquake cycle.
Scientists studying Indiana cave stalagmites may uncover evidence of past earthquakes in the region, according to a new study. The research team found that two stalagmite pairs stopped growing around 100,000 years ago and resumed growth at around 6,000 years ago, overlapping with known magnitude 7.1-7.3 earthquakes.
A new study by Scripps Institution of Oceanography has discovered that large earthquakes on one fault can trigger large aftershocks on separate faults within minutes. This finding has significant implications for earthquake-prone regions like California, where complex fault systems may lead to mega-earthquakes.
Researchers propose large-scale metamaterials as seismic shields to protect areas from earthquake damage. The shields work by inhibiting the propagation of incoming seismic waves through interference effects.
A new analysis reveals that massive earthquakes on the Cascadia Subduction Zone, affecting population centers like Portland and Seattle, may occur more frequently than thought. The study used detailed data from core samples and found slightly higher chances of an earthquake within the next 50 years.
Researchers studied 7th-century A.D. temples in northwest India to reconstruct historic earthquakes, finding evidence of damage from magnitude 7.8 and 7.6 quakes. The study extended rupture zones for two major earthquakes, suggesting the region is prone to powerful earthquakes.
A Kyoto University study shows tsunami-borne EM fields can extract key information about earthquake hypocenters, including fault dip direction, which helps with early warning systems. This discovery could lead to improved tsunami forecasting and timely evacuations.
Researchers discovered that coconut walls can dissipate energy via crack deflection, thanks to a distinct, ladder-like design of the vascular system. This structure could be applied to functionally graded concrete to enhance its energy dissipation capacity and protect buildings against earthquakes and other hazards.
The July 2016 issue of Geology features studies on pre-Mississippian tectonic affinity across the Canada Basin-Arctic margins, as well as hydrothermal alteration of seafloor peridotites. Researchers also investigate recent volcanic resurfacing of Venusian craters and cyanobacterial fossilization in Ediacaran siliciclastic environments.
A University of Montana researcher has contributed to a groundbreaking study on the complexity of earthquakes and their forecastability. The research found that smaller and larger quakes contribute to the movement of the Himalayas, increasing the frequency but reducing the impact of earthquakes in the region.
Earthquakes triggered by human activity have been widespread throughout Texas since the 1920s, according to a new review of evidence. Oil and gas operations are the primary cause, but specific techniques have varied over time.
A new study found that earthquakes can cause magma to slosh and create conditions for volcanic eruptions. The research used a precision shake table to model the movement of magma and found that sloshing can lead to the formation of bubbles, which release gas into the atmosphere, decreasing pressure and triggering an eruption.
A slow slip event in New Zealand's Hikurangi margin showed that subduction plates may be accumulating much more stress and strain than previously thought. This finding helps assess earthquake occurrence risk in coastal areas near subduction zones, especially at locations of shallow depth.
Researchers have discovered a slow-slip event that lasted two weeks, resulting in 15-20 centimeters of movement along the fault. The finding increases understanding of the relationship between slow slip and normal earthquakes, highlighting the potential for using offshore monitoring systems to predict damaging earthquakes.
Scientists have found that pieces of the underside of the North American Plate are peeling off, sinking into the mantle, and causing earthquakes in the southeastern US. This process is likely to produce more earthquakes in the future due to unbalanced stresses in the plate.
Researchers discovered that rainwater can channel up the Alpine Fault and overwhelm contributions from mantle-derived fluids, focusing it onto the fault. This finding sheds light on the trigger mechanisms for major seismic events and has implications for understanding catastrophic earthquakes.
Researchers examine factors influencing induced earthquake locations and strengths in central US and western Canada. The USGS report estimates 7 million people live in areas affected by induced seismicity.
A seismic network in Nevada is being used to monitor wildfires and provide early intelligence on more than 25 fires during the last fire season. The technology has the potential to remake firefighting by allowing for tactical suppression and scaling resources appropriately, saving time and money.
Researchers use new tools to detect patterns of seismic activity before volcanic eruptions, comparing them to past eruptions to determine when a particular volcano might erupt. The study also examines swarms of small earthquakes that appear to precede many eruptions, aiming to learn more about magma movement.
Researchers successfully replicated a range of fault slip modes found during earthquakes, quiet periods and slow earthquakes. They used ground quartz and a machine to apply pressure and alter stresses, revealing the forces behind slow earthquake mechanisms.
A new report published in Seismological Research Letters suggests a link between hydraulic fracturing and induced earthquakes in Western Canada. Researchers found that thousands of hydraulic fracturing wells are being drilled every year, increasing the likelihood of earthquake activity.
A new study suggests that real-time GPS data can be used to estimate how an earthquake deforms the sea floor, cutting tsunami warning times by nearly 20 minutes. This allows for more accurate warnings to be issued within two to three minutes, potentially saving lives.
The MyShake Android app uses smartphone accelerometers to detect earthquakes, analyzing data from millions of phones to create a dense seismic network. The goal is to provide early warning systems for areas without traditional networks.
A Northwestern University class estimated the costs and benefits of securing water heaters against earthquake damage. The study concluded that investing in water heater protection would yield a low return on investment compared to buying lottery tickets with high jackpots.
A research team found that a geologic event known as diking can cause strong earthquakes, with the potential to pose hazards to nearby communities. The team investigated ties between two natural disasters in the Democratic Republic of Congo and discovered that a dike intrusion could have induced a magnitude 6.2 earthquake.
Geologists from Brown University have discovered that water escaping from mineral lawsonite at high temperatures and pressures makes it prone to brittle failure, triggering earthquakes. This explains why certain quakes occur in cold subduction zones where lawsonite forms, but not in hot zones.
Seismologists have identified a zone deep in the crust where temperatures hover around 350 degrees Celsius, varying along the San Andreas strike. The zone separates shallow earthquakes from deeper low-frequency earthquakes (LFEs), with a puzzling five-kilometer wide gap between them.
A new study shows that Aboriginal burning practices in Australia had a minimal effect on the erosion of their inhabited landscapes. The researchers used beryllium-10 to model the impact of fire on landscape erosion and found that it was not intense enough to change the natural rate of erosion over thousands of years.
A kink in the regional fault line creates a ramp that raises the height of the mountains. The rupture on the fault stopped 11km below Kathmandu, indicating another major earthquake could occur within a shorter timeframe.
Scientists used a Baghdad seismometer to capture data on car bombs and mortar fire during the Iraq war. They identified distinct seismic signatures for different types of military operations in urban terrain, such as vehicle-borne improvised explosive devices and mortar fire.
Seismologists used a network of instruments deployed in Iraq to analyze the seismic patterns of explosions, including mortars, rockets, IEDs, helicopters, and drones. The analysis allowed them to reconstruct the sequence of events leading up to the 'cook-off' explosion.
A new study by Stanford researchers suggests that earthquakes triggered by human activity follow several indicative patterns that could help scientists distinguish them from naturally occurring temblors. The likelihood of large-magnitude manmade, or "induced," earthquakes increases over time, independent of the previous seismicity rate.
A team of scientists has discovered that strong medieval earthquakes in Nepal triggered massive debris flows that reshaped the landscape over a distance of more than 60 kilometers. The study used 14C radiocarbon dating to determine the timing of sediment deposits and found that they coincide with documented large earthquakes in the reg...
A new algorithm called Fingerprint And Similarity Thresholding (FAST) can identify previously overlooked microquakes in large databases of ground motion measurements, potentially helping predict larger quakes. By comparing seismic wave patterns, FAST finds weakly recorded earthquakes faster than conventional methods.
Lin has published 26 papers on using ambient seismic noise to reconstruct internal structures of the Earth and map out structures in the crust and upper mantle with unprecedented accuracy. His method has been used to create detailed images of the Earth's inner core and a vast magma plumbing system below Yellowstone National Park.
Scholz has made significant contributions to seismology, bridging laboratory studies of rock mechanics with fundamental research on crustal-scale deformation. He has developed influential models for earthquake prediction and helped create regional seismic hazard maps.
Bishal Upreti's research has practical implications in earthquake landslide hazard assessment, mineral exploration, and water resource development. His work maps active faults to evaluate seismic hazard in the Nepal Himalayan region.
Researchers found that areas with previous strong earthquakes were more likely to produce landslides after a second earthquake hit. The study's findings could lead to improved predictive models considering historical occurrences of past earthquakes.
Researchers found stratigraphic evidence of subsidence during large earthquakes beneath salt marshes in California's Humboldt Bay. Microfossil data analysis enabled more accurate estimates of subsidence, refining earthquake models that match observed measurements. New plant macrofossils provide tighter constraints on past earthquake ti...
Researchers found that triggered earthquakes change the elastic properties of the Earth's crust in regions up to 6,000 kilometers away. This dynamic and interconnected system can create a cascading sequence of events thousands of kilometers away.
A UT Arlington researcher is developing a comprehensive framework to analyze North Texas dams and detect damage from seismic activity. The framework will use geo-statistics and three key indicators of damage caused by earthquakes, including liquefaction, dynamic slope stability, and lateral spreading.
A University of Washington simulation demonstrates the individual crystals' movement in a magma chamber, providing insights into the motion of magma and buildup of pressure. The study helps volcanologists improve their understanding of volcanic systems and predict eruptions more accurately.
A team of geologists from GEOMAR and Spanish institutions presented an explanation for the smaller-than-expected 2014 Iquique earthquake. Seamounts in the region, which subduct under the South American plate, actively deformed the interface and reduced stress buildup, resulting in a smaller earthquake.
Researchers used a gel-like substance called Carbopol to study the resistance of rock formations in the middle crust to fracturing. The study provides insight into how large earthquakes and slower moving events interact, with potential implications for predicting seismic activity.
Lehigh University has received a $5 million grant from the National Science Foundation to improve infrastructure resilience and sustainability. The award supports research using Lehigh's ATLSS facilities, which will conduct real-time structural experiments to evaluate engineering designs and materials during natural disasters.
Researchers developed a model to simulate Mediterranean tsunami impact, showing how waves would hit and flood coastal areas in southern Italy and Greece. The study highlights the need for local authorities to identify vulnerable areas and plan defense strategies.
Researchers have identified a key factor driving intraplate seismicity: convective currents of semi-liquid rock beneath the Earth's crust. This process interacts with surface motion, influencing earthquake locations and frequency. The study's findings offer new insights into seismic hazard mapping in plate interiors.
Large earthquakes cause catastrophic landslides that can persist up to 20-fold after the earthquake, then gradually decrease over time. The magnitude of this response is linked to the size of the earthquake, with shaking-induced damage near Earth's surface and active healing processes playing a key role.
After strong earthquakes, landslides decrease due to an internal healing process of the landscape, returning to pre-earthquake levels in months to years. The destabilization caused by the quake gradually recovers as cracks close and are filled with sand and earth.
The Cascadia Initiative has deployed seismometers onshore and offshore to monitor the Cascadia subduction zone. The project provides a clearer picture of the region's seismic risk, including undetected small earthquakes and new offshore structures. The initiative also offers insights into tsunami detection and seismic wave readings.
Researchers found a unique insight into megathrust earthquakes through GPS data and radar measurements. The study revealed a pulse-like rupture that occurred over six seconds, with an extremely fast rupture velocity of approximately 3.2km/s.
Researchers found that precariously balanced rocks near the San Andreas Fault have survived due to interactions between the faults, which weakened ground shaking. This discovery could change how engineers plan for future earthquakes in the region, considering a broader impact of ruptures along both faults.
Researchers found that interaction between the San Jacinto and San Andreas faults weakened earthquake ground shaking near them, preserving precariously balanced boulders. This discovery has practical implications for earthquake planning scenarios in the region.
Researchers investigate granitic rocks in El Capitan using field mapping, rock climbing, and geochemical analyses. They found no systematic patterns in rock composition, challenging models of granite formation that rely on magma chambers.
Researchers found evidence of six large earthquakes in western Solomon Islands over the past 3,000 years, including five that were as large or larger than a devastating 2007 earthquake. The study used corals to analyze seismic events and provide insight into the relationship between earthquakes and long-term geological processes.
Researchers have discovered a new insight into glacier behavior, revealing the rapid movement of glaciers backward and downward during calving events. This phenomenon helps scientists measure glacier calving remotely and improve sea-level rise predictions.
Researchers monitored Helheim Glacier for 55 days and detected 10 large-scale calving events, revealing unique quakes registering magnitude five on the Richter Scale. These glacial earthquakes can serve as proxies for glacier edge breaking, offering insights into ice loss from glaciers.
Researchers studied earthquake history in the eastern Indian Ocean, tracing modes of coastal sedimentation over time. They discovered seven subduction zone earthquakes recorded 3,800 to 7,500 years ago, indicating past tsunamis occurred approximately four to six times.