The Seismological Society of America honors MIT's M. Nafi Toksoz for his 40-year investment in the field, defining seismology and its practice. He has mentored over 100 postdoctoral students, promoting a research environment at MIT.
Researchers adapt oil industry technology to image the core-mantle boundary at 2,900 kilometers beneath Central and North America, providing detailed views of the lower mantle. The technique helps understand Earth's internal heat engine and giant cycle of heat production and transfer.
Dr. Elizabeth Cochran receives the 2006 Subaru Outstanding Woman in Science Award for her groundbreaking work on earthquake triggering, microcracks, and post-seismic displacements. Her research explores intriguing facets of earthquakes using InSAR technology.
Researchers have developed a new method using GPS technology that can determine the true size of an earthquake within minutes, allowing for faster tsunami warnings. This is much faster than current methods and has the potential to improve future tsunami danger assessments.
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.
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.
John Castagna's developed an algorithm to predict seismic-wave velocities for direct hydrocarbon indicator analysis, detecting oil and gas reservoirs more effectively. This advancement enables explorers to locate hydrocarbon discoveries with higher accuracy, reducing the need for costly drilling operations.
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.
Researchers used various models to recreate the rupture history and variation along the fault, revealing the earthquake's length, epicenter, and speed. The study provided valuable insights into one of the largest earthquakes recorded on modern equipment.
The study provides a comprehensive analysis of the earthquakes, including the longest fault rupture and duration of faulting, as well as the seismic waves that traveled around the globe. The researchers also found that the earthquake caused the planet to vibrate with 'free oscillations,' like the ringing of a bell.
The University of Ulster team found significantly increased levels of stress on two fault zones in Indonesia, including the Sunda trench and Sumatra fault. The analysis suggests a high risk of another earthquake, potentially triggering another tsunami.
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.
The Global Seismographic Network can track seismic signals in real-time, allowing researchers to compile and interpret information about potential hazards sooner. The network's unparalleled detail enables scientists to quickly determine the magnitude and location of an event in near real-time.
Researchers have developed a system to detect landmines using sound waves, while also studying the water-absorbing properties of aged soot and its potential impact on climate models. Additionally, scientists have made new discoveries about natural lightning, including X-ray emissions during thunderstorms.
Physicists at UC Berkeley have successfully produced a quantum whistle in superfluid helium-4 using an array of tiny holes. The whistle is achieved at a temperature of 2 Kelvin, making the sensors user-friendly for scientists unfamiliar with cryogenic technology.
The Indonesian earthquake's unique combination of a subduction zone and shallow depth made it particularly deadly, resulting in over 150,000 deaths. Scientists have developed technology to warn people of pending tsunamis, but an early warning system is lacking in the Indian Ocean.
Researchers at the University of Nevada, Reno developed a model that estimates the impact of a large earthquake in Los Angeles by studying an earthquake in Kern County. The study found that the hanging-wall side of thrust-fault earthquakes experiences more extreme motion and damage than the footwall side.
Researchers used seismic signals and computer analysis to derive outlines of possible secondary faults in the San Andreas Fault zone. The study's findings suggest that continued drilling will encounter significant structures before reaching the fault zone.
A University of Michigan professor is developing new computer animations to help students better understand the Earth's structure and internal processes. His approach complements existing techniques, allowing students to progress from simpler models to more complex representations.
The newly launched San Andreas Fault Observatory at Depth (SAFOD) will provide researchers with tools for continuous monitoring from inside an active earthquake zone. This project is part of the larger EarthScope initiative, which aims to investigate geological forces shaping the North American continent.
Researchers chart seismic effects on water levels to better understand the impact of earthquakes on hydrology. The study found that wells and aquifers respond differently to earthquakes than surface water, with effects recorded at greater distances.
Researchers DePaolo and Manga argue that mantle plumes are the primary cause of volcanic activity on Earth. They cite strong evidence from Hawaii and other hotspots, including rapid magma movement and unique chemical signatures. The debate highlights the importance of understanding plume origins for connecting seismology and geochemistry.
Princeton students have created a comprehensive map of the US's natural hazard risks, revealing that large events like hurricanes and earthquakes drive costs. The data also suggests a 30-year east-to-west oscillation in hurricane tracks, potentially shifting their trajectory northward.
Researchers used experiments and mathematical modeling to understand seismic wave behavior in the lower mantle, finding that mineral grain alignment causes unusual wave behavior. The study provides a window into Earth's inner workings and is an important step toward integrating seismology and geodynamics in the lower mantle.
Richard Monastersky and Diane Tennant have won the American Geophysical Union's 2002 David Perlman and Walter Sullivan Awards for Excellence in Science Journalism. Monastersky won for his news article on the Near Earth Asteroid Rendezvous mission, while Tennant won for her seven-part series on a local meteor impact story that spans 35 ...
Scientists study seismic waves to understand tectonic plate dynamics, aiming to resolve the long-standing 'great plate debate'. They use data from seismometers worldwide to characterize wave origins and time delays, creating a X-ray image of the planet's internal structure.
Despite technological advancements, earthquake prediction remains elusive due to the Heat-Flow Paradox and debates on fault strength. Research efforts have shed light on variations along the San Andreas fault, with some areas experiencing locked stresses while others creep slowly.
Researchers have observed an 'earthquake' in a slow-spinning, highly magnetic collapsed star, confirming it as a neutron star. The finding supports the magnetar hypothesis and provides strong evidence for the existence of these rare objects.
The American Geophysical Union's 2000 Spring Meeting will feature a wide range of scientific sessions and press conferences on cutting-edge research. The conference will be held May 30 to June 3 at the Washington Convention Center, with special focus on interdisciplinary collaboration.
A team of researchers is using seismic equipment to map the Earth's structure beneath the Rocky Mountains, aiming to understand how ancient land masses collided to form the continent. By analyzing density and material properties of rocks, they hope to visualize the structure of what lies far under the Earth's surface.
The MIT researchers' new model explains minute differences in magma composition by shifting densities due to iron and silicon, offset by soaring temperatures. This resolves the long-standing debate on convection in the Earth's mantle, providing a new framework for further investigations.
Scientists at Lawrence Berkeley National Laboratory used seismic data from 40,000 earthquakes to characterize the Earth's structure from crust to inner core. They found evidence of heterogeneity in the outer core, suggesting a liquid iron-nickel-sulfur compound that could help explain the Earth's magnetic field.
Scientists from the National Science Foundation and IRIS have ruled out cult activities and nuclear detonations as causes of a 1993 Australian seismic event. They now believe that an iron meteorite of about two meters in diameter could have created the tremors, but no crater has been found.
Researchers analyzed seismic data to determine cause of 1993 event in Australian outback. An iron meteorite over 3 meters in diameter is suggested as possible cause.
The NSF is installing 250 ground-based monuments to track satellites and study earth movements in Southern California, enabling scientists to follow Earth's crust movements with unprecedented detail. The network will provide valuable insights into earthquake potential and strain buildup, helping to identify areas of high seismic activity.
A $1.5 million seismic network around Kilauea Volcano will help scientists make more accurate predictions about when volcanoes will erupt and determine potential hazards in nearby areas. The network, which contains 116 stations, is designed to understand the physical characteristics of earthquakes associated with eruptions.
The US has signed the Comprehensive Test Ban Treaty, which will be verified through a global seismic monitoring system. The treaty bans nuclear testing in all environments except underground, and the global network is being installed by IRIS and the National Science Foundation to detect seismic events of magnitude 4.25 or larger.