Articles tagged with Earthquakes
Researchers discovered that slow-moving silent earthquakes can trigger swarms of tiny conventional tremors, potentially providing early warnings for mega-earthquakes. This discovery has raised hopes for seismic hazard forecasting in subduction zones worldwide.
Research suggests that seismic shaking can temporarily increase groundwater permeability, which could be exploited to enhance oil extraction. This phenomenon is caused by the gravitational effects of the moon on the solid Earth, forcing water in and out of wells.
Scientists studied earthquakes and tsunamis in the Bering Sea coastline, including magnitude 7.7 quakes, to understand the tectonic history of Kamchatka. The research suggests that Kamchatka sits atop a smaller plate called the Okhotsk block, which is being deformed by convergence zones of tectonic plates.
Researchers have recorded non-volcanic tremors in a deep borehole near Parkfield, California, providing insight into the San Andreas Fault's behavior. The findings help geologists understand whether the fault's deeply buried rocks behave similarly to those in the Cascadia Subduction Zone.
Scientists detect a seasonal pattern in glacial earthquakes in Greenland, with over one-third occurring during July and August. The increased frequency of these events may be a response to global warming, with significant implications for climate change.
Scientists have found that glacier melting in polar regions is causing a rise in seismic activity, with glacial earthquakes occurring most commonly in summer months. This phenomenon is linked to the movement of massive glaciers and their response to climate change.
Geophysicist Mark Zoback explains that the New Madrid seismic zone is prone to earthquakes due to the legacy effect of a massive glacier pressing into the Earth's surface. He predicts that earthquakes could continue to occur in the region for thousands of years, emphasizing the need for continued research and preparedness.
Researchers found that sediment-filled basins in subduction zones can strengthen the edge of the plate above, increasing the likelihood of large earthquakes. The Cascadia subduction zone is particularly prone to severe shaking due to its forearc basins, which can be up to 3 miles deep.
Researchers at Yale University discovered a key to identifying areas within subduction zones prone to severe damage during earthquakes. Sediment layers deposited on top of the overriding plate cause it to 'stick,' increasing the likelihood of earthquake events in these regions.
Researchers have found that a large swath of territory in the Northeast is slowly moving southward in relation to the rest of the continent. This region is recovering from the weight of ancient glaciers and has long been known to be rising slowly due to their retreat.
Recent Himalayan earthquakes may be followed by larger events in the same region, while medieval earthquakes were much larger and less frequent. The study aims to understand what governs the recurrence interval and size of these rare events.
The SAFOD project reveals a correlation between nonvolcanic tremors and microearthquakes, suggesting a possible causal relationship. The researchers also obtained seismic data during a magnitude 6.0 earthquake in 2004, indicating that damaged rock began forming mineral seals soon after the event.
Climate scientists highlight human impact on temperature extremes, while researchers develop a new method to predict catastrophic earthquakes. Meanwhile, hurricane intensification may be linked to eyewall precipitation patterns.
A geologist is proposing a new approach, called GeoTraverse, to select study sites for the NSF-funded EarthScope project. This approach aims to facilitate greater scientific collaboration and public engagement by selecting areas that can be connected into one or a few east-west transects.
Researchers analyzed seismic wave data from 30 earthquakes and found waves passing through the inner core arrived earlier when separated in time, indicating material had moved into the path taken by waves traveling through the inner core. The study's findings suggest a dynamic planet with significant changes over millions of years.
A new study reveals that earthquake recurrence times exhibit self-similarity, with smaller clusters of earthquakes grouped together within larger clusters. This critical phenomenon may improve risk estimation by showing a clear statistical dependence between earthquakes.
The Antares programme uses permanent deep-sea seismic sensors to monitor local and global earthquakes, improving risk assessment systems and studying submarine activity. The project overcomes challenges of instrument resistance and coherence between equipment and electronic systems.
A new study published in Geology estimates the maximum possible earthquake magnitude in the San Fernando and Northridge areas of Los Angeles County. The researchers used paleomagnetism to analyze sediments and found that the crust is broken into blocks, limiting the maximum earthquake magnitude to around 6.8.
Researchers at the Hebrew University of Jerusalem and Geological Survey of Israel developed a new method to date ancient earthquakes using cave evidence. They found evidence of earthquakes with magnitudes of 7.5 or greater occurring in the region over the last 200,000 years, but not in recent times.
Scientists have discovered that deep-sea tremors can be used to predict large earthquakes with high accuracy. By analyzing data from sensors deployed on the ocean floor, researchers were able to set up an early warning system that successfully predicted six major earthquakes in a 15-kilometer radius.
Researchers developed a system that predicted six major earthquakes along East Pacific Rise transform faults using sensor data and foreshock detection. The study suggests short-term earthquake prediction may be feasible under certain circumstances.
Researchers have developed a new method to measure surface waves from normal seismic noise, providing better resolution of the Earth's interior. This technique promises significant improvements in crust and upper mantle image quality down to 60 miles within the Earth.
Scientists have developed a new method to create detailed images of the Earth's interior, improving resolution and accuracy. This technique uses ambient seismic noise, rather than earthquakes, allowing for better understanding of the planet's structure.
Researchers have found evidence of coastal subsidence preceding major subduction zone quakes, potentially providing a warning system for tsunami alerts. The study suggests that areas along subduction zones should monitor subsidence to predict potential earthquakes and tsunamis.
Researchers measured ancient moraine crests to determine past movement on the Karakorum fault, revealing a significant right-lateral motion. The study's findings provide crucial insights into the Asian continent's movement and the collision of India and Asia.
Researchers detected continuous tremors near Cholame, 15 miles southeast of Parkfield, which are similar to those discovered in Japan and the Pacific Northwest. The tremors, which last more than four minutes each, may be precursory to earthquakes, potentially leading to earthquake forecasting and prediction.
A study by the University of Pennsylvania's Wharton School found that preparing for extreme events depends on a complex interplay between risk assessment, perception, and management. Understanding cumulative effects can increase people's willingness to take actions to mitigate risks.
Researchers found that El Nino climate changes contribute to Antarctic cooling through atmospheric circulation shifts. Deep-sea islands stir and fertilize the upper ocean by mixing cold waters with the surface layer, while Siberian forest fires produced hazardous air pollution in western North America.
A team of geologists reports that the Moho boundary is absent beneath California's San Joaquin Valley, due to a mantle drip. The study provides insight into mountain-building processes and explains how the Sierra Nevada formed.
Researchers at the University of Nevada, Reno recorded a cluster of nearly 1,600 small earthquakes beneath Lake Tahoe, causing the nearby Slide Mountain to rise by 8 millimeters. The earthquakes coincided with an unprecedented uplift of the mountain, which scientists believe was caused by magma movement about 20 miles deep.
A recent NASA study has found a significant correlation between the retreat of glaciers and an increase in earthquake activity in southern Alaska. As glaciers melt, they lighten the load on the Earth's crust, allowing tectonic plates to move more freely, which can lead to earthquakes.
A team of scientists has documented a new phenomenon where the seafloor creates a void that sucks in surrounding seawater. This discovery challenges scientific understanding of seafloor spreading and its impact on ocean crust. The researchers believe that the dilation of the ocean crust may lead to changes in water temperatures, chemic...
A new study suggests the Seattle fault played a role in causing damage to unreinforced brick chimneys in West Seattle and Bremerton after the 2001 earthquake. The research found that areas with heavy chimney damage experienced stronger shaking, indicating the fault may have acted as a megaphone to amplify seismic waves.
Researchers at Penn State found lags between the changes in forces and strength in laboratory simulations, with delays ranging from seconds to weeks after initial earthquakes. The study suggests a competition between compaction and dilation of granules in gouge zones contributes to delayed fault movements.
Small earthquakes with magnitudes zero to three are recorded in South African gold mines, providing a unique dataset for scientists. The researchers are using this data to investigate the properties of small earthquakes and bridge the gap between laboratory experiments and real-world seismic activity.
Researchers have discovered that the breakdown of mineral serpentine can trigger earthquakes in Earth's deeply buried crust. At pressures above a few tens of kilometers, scientists expected faulting instability only if volume change during serpentine breakdown was positive. However, experiments have shown that even with a strongly nega...
Researchers discovered that a mineral gel formed during rock abrasion can reduce friction between rocks to near-zero levels at high shearing speeds. This finding has implications for understanding and predicting earthquake damage, as it could lead to more accurate simulations of seismic slip speeds and fault weakening processes.
Researchers found a periodic increase in slip rate every three years along the northern half of the central San Andreas Fault, indicating a higher probability of moderate to large quakes. This cycle is characterized by an upswing of microquakes, followed by moderate to large earthquakes six to seven times more likely to occur.
The Plate Boundary Observatory (PBO) will map seismic processes across North America, enabling improved earthquake prediction and understanding. By deploying hundreds of sensors, researchers will measure subtle deformation and help geologists understand the shifting strains in the ground.
Researchers use seismographic data to produce a sharp image of the planet's interior, revealing giant spouts of heat known as mantle plumes. The findings confirm the existence of these column-like structures, which are believed to cause island chains like Hawaii and Iceland.
Researchers detected physical changes in faults using seismic data from the Parkfield experiment. The study provided evidence for structural changes in fault zones that can be viewed with active seismic monitoring systems.
New analysis suggests earthquakes in the Wadati-Benioff zone are confined to the uppermost part of the Juan de Fuca plate's crust, limiting their magnitude to around 7. However, a quake occurring in both layers could reach a magnitude of 8, posing a risk to the heavily populated Interstate 5 corridor.
The Penn State Earth 101 course uses B-movie clips to engage students in learning about natural disasters, promoting critical thinking and science-based decision-making. Students work on projects such as public affairs manuals for cities with earthquake histories, debating topics like government response to natural disasters.
A recent study by Tibi et al. provides new insights into the mechanism of deep earthquakes, with implications for earthquake prediction. The researchers demonstrated remote triggering of one deep earthquake by another, shedding light on how these powerful events begin.
A new study by Northwestern University suggests Memphis should consider California-style earthquake building codes, but experts argue the costs would be too high. The proposed code could cut earthquake damage in half, but would increase construction costs by 10-33% and have significant economic impacts.
A growing number of supercities, with over 200 globally, are located near major fault lines and could face devastating earthquakes. The number of fatalities from building collapses during earthquakes has increased four-fold since the 17th century due to urbanization.
Scientists are studying the impact of human activities on water quality in the Brush Creek watershed. Geophysicists have discovered small earthquakes in northeastern Kansas related to movements of the Earth's crust. Additionally, researchers are analyzing how irrigation affects summertime climate in the High Plains.
Scientists used NASA's Terra satellite to study the effects of a 7.7 magnitude earthquake in India, detecting dewatering and surface water far from the epicenter. The Multi-angle Imaging SpectroRadiometer (MISR) instrument provided compelling evidence of surface water in remote locations inaccessible to teams on the ground.
The church was founded on a cliff top due to its patron saint's martyrdom, but was soon hit by two earthquakes, a flood, and a landslide. Analysis suggests it may be the unluckiest church in the world.
Researchers at UCL create first laboratory-generated deep and intermediate focus earthquakes, recreating extreme pressure and temperature conditions. The study reveals dehydration reactions as the cause of these enigmatic earthquakes, which can occur hundreds of kilometers below the Earth's surface.
Preliminary study finds that modified structural steel connections may fail under small bomb blasts, compromising building stability. Researchers aim to address issues and consider progressive collapse of multi-story buildings.
Seismologists have made significant progress in identifying violations of the nuclear test ban treaty by analyzing technical characteristics of seismic signals. Nearly all questionable events since 1995 have been identified as nuclear explosions, chemical explosions, earthquakes, or mine collapses.
Scientists use microgravity to study soil behavior and simulate earthquake effects, aiming to improve foundation design and mitigate soil liquefaction. The experiment will analyze the strength and stiffness of sand under different conditions, shedding light on the physics behind soil movement.
Experts say preparing for natural disasters can also help mitigate the impact of terrorist attacks, emphasizing the importance of comprehensive approaches to risk management. Communities must consider all potential risks and develop disaster plans that address various types of hazards.
Researchers analyzed seismic activity from six stations in West Antarctica, discovering a significant number of small earthquakes. The study confirms that West Antarctica is prone to earthquakes due to its rift-like nature.
Researchers at Columbia University have discovered a correlation between earthquakes and ocean tides, with seismic activity increasing during tidal lows. This study suggests that the seafloor crust is breathing with the ocean tides, allowing for regular tidal scheduling of seismic energy release.
New research suggests earthquakes destroyed fortified buildings, changed river courses and made elite rulers vulnerable to attack in ancient civilizations. Scientists at Stanford University are painting a picture of an ancient world where earthquakes played a crucial role in shaping history.
Researchers found that vibrations recorded on September 11 were of a low magnitude, too small to cause structural damage. The collapse of the towers was attributed to the interaction between the ground and building foundations, transmitting energy from the impacts and collapses.
Seismologist Douglas A. Wiens finds deep earthquakes recur at the same spot repeatedly, supporting ductile shear zone model. The research uses seismic wave evidence to locate earthquakes with accuracy, enabling future study of deep fault zones.
By analyzing seismic waves, scientists have mapped the physical properties of the earth below, identifying regions with seismically fast mantle that produce gem-quality diamonds. This discovery could aid in locating new diamond mines by targeting areas with similar characteristics.