Articles tagged with Volcanoes
A new scenario proposes that Mars' oceans formed several hundred million years earlier than previously thought, linking their existence to the rise of the solar system's largest volcanic system, Tharsis. The model suggests that global warming and volcanic eruptions played a key role in allowing liquid water to exist on Mars.
Research shows that water-bearing minerals release water underneath geologic hot spots, lubricating earthquakes and fueling volcanoes. A new spectroscopy technique applied to garnet containing fragments of quartz reveals the source of water, contradicting conventional thermodynamic equations.
Recent studies suggest that the Hawaiian hotspot moved southward at a rate of several tens of kilometers per million years. This new evidence contradicts the long-held assumption that hotspots are stationary and supports a dynamic Earth model.
Researchers from Kobe University confirm a giant lava dome created 7300 years ago in Japan's Kikai Caldera, with a volume of over 32 cubic kilometers. The composition of the dome matches that of nearby Satsuma Iwo-jima Island, suggesting a possible current magma buildup.
Researchers have discovered tiny crystals forming deep in volcanoes can signal impending eruptions, offering hope for more effective evacuations and early warning systems. The study, led by Dr. Teresa Ubide, uses a new laser technique to examine the composition of these crystals, which may hold the key to predicting volcanic activity.
Researchers have found that small crystals in volcanic rocks contain growth layers similar to tree rings, which can record the processes leading up to an eruption. This discovery may lead to more effective volcanic hazard monitoring, including for dormant volcanoes.
Researchers find a sudden discontinuity in the flow behaviour of rhyolitic magmas, guiding whether a volcano erupts effusively or explosively. Variabilities at the nanoscale can dramatically increase the explosive potential of volcanoes.
Scientists studying submarine volcanoes have discovered distinct sound patterns emanating from two underwater eruptions, Ahyi and Bogoslof. These sounds can be detected by seismometers and hydrophone arrays, providing valuable insights into the monitoring of these volcanic events.
A team from the University of Bristol analyzed geological records to find that volcanic super-eruptions occur much more frequently than previously estimated, with a new average time between events of around 17 thousand years. This re-evaluation raises concerns about the potential impact on global weather patterns and human civilization.
Researchers at UNH used scientific sleuthing to better understand magma movement in Mount Etna, finding that ancient and present-day magma sources are similar. The study also revealed that crystals formed beneath the volcano were virtually chemically identical to erupted lavas, suggesting short crystal storage times.
Researchers discovered a possible reason for Ptolemy III's sudden return home: massive volcanic eruptions. These events cooled the planet's atmosphere, disrupting the Nile River's flow and leading to food shortages and heightened tensions. The study links eruptions to violent uprisings and other upheavals in ancient Egypt.
Researchers detect localized carbon dioxide sources from Mount Yasur and Los Angeles basin, providing insights into volcanic and anthropogenic emissions. The study supports the potential for space-based monitoring to prevent humanitarian disasters and reduce greenhouse gas-induced warming.
A recent study in the Journal of Applied Volcanology analyzed volcanic fatalities in unprecedented detail, identifying common causes and victims. The research found that nearly half of all fatal incidents occurred within 10 km of volcanoes, with tourists, media, and emergency response personnel being among the most at-risk groups.
Researchers have discovered a 'reverse energy cascade' that traps rising magma in the crust, forming massive granite bodies like Yosemite's El Capitan. This process helps build better understanding of volcanoes, their impacts on global climate, and where large volcanoes are likely to occur.
A network of microscopic crystals in magma can act like guard rails to channel gas out, lessening internal pressure and reducing explosiveness. The discovery challenges the prevailing assumption that silica content is the major driver of gas escape.
Researchers developed a new technique combining seismic noise interferometry with geophysical measurements to predict volcanic eruptions. By analyzing the speed of energy traveling through a volcano and correlating it with rock deformation, they found a strong correlation between bulging, shrinking, and impending eruptions.
Scientists studied zircon crystals to understand magma reservoirs, finding a more solid and crystalline environment than previously thought. The research sheds light on the pre-eruption phase and how mobile magma contributes to volcanic activity.
Scientists have found that magma reservoirs are less liquid and more crystalline than previously thought, with most crystals retaining their structure for tens of thousands of years before being exposed to molten magma. This discovery could help predict when volcanoes pose the greatest risk by identifying those with mobile magma.
Researchers analyzed zircon crystals in Taupo Volcanic Zone magma to determine its temperature history, finding a 'cool' period followed by rapid heating. The study's findings may help scientists recognize volcanoes on the verge of an eruption.
Researchers have developed a new method to investigate underwater volcanoes that produce Earth's tectonic plates. The study found that molten rock is present deeper than expected, indicating faster cooling of the plate, which affects friction at collision zones and megaquake sizes.
Researchers at UCL and the Vesuvius Observatory used a new model to investigate Campi Flegrei's unrest, finding a build-up of energy that makes the volcano more susceptible to eruption. The study suggests an increased possibility of eruption in the near future.
Astronomers have obtained an exceptionally detailed map of the largest lava lake on Io, showing two waves of lava sweeping from west to east at about 3,300 feet per day. The temperature variation across the surface of the lake reveals a smooth gradient, with the western end at 270 Kelvin and the southeastern end at 330 Kelvin.
A study by Australian National University reveals the world's biggest volcanoes in Hawaii formed along twin tracks due to a shift in the Pacific Plate's direction three million years ago. The discovery helps reconstruct Earth's history and understand volcanic activity away from tectonic plate boundaries.
Researchers have found that volcanoes collectively emit significant amounts of sulfur dioxide into the atmosphere, which is easier to detect from space. Human activities also emit large quantities of sulfur dioxide, but are declining in many countries due to pollution controls.
A team of researchers has created the first global inventory for volcanic sulfur dioxide emissions, using data from a NASA satellite. The data set provides annual estimates for 91 volcanoes worldwide and will help refine climate models and provide insight into human health risks.
Scientists propose that viscous relaxation on Ceres caused older cryovolcanoes to flatten over millions of years, making them indistinguishable from the planet's surface. This process may explain why Ahuna Mons stands alone as the only prominent ice volcano on the dwarf planet.
A Martian meteorite provides clues to the evolution of Mars, with evidence suggesting that some of the longest-lived volcanoes in the solar system are located on the Red Planet. The research offers new insights into the history of volcanic activity on Mars and confirms at least 2 billion years of volcanic activity.
Two new studies provide a step-by-step account of an underwater volcano eruption, revealing that deformation patterns and tidal activity can be used to estimate future eruptions. Monitoring magma pools underneath the Axial Seamount has been shown to help predict undersea eruptions.
A University of Washington study has captured the eruption of an underwater volcano in unprecedented detail, providing new clues about the behavior of volcanoes where two ocean plates are moving apart. The research used data from the Cabled Array seafloor observatory to analyze seismic vibrations and movement before and during the event.
Researchers discovered temperature and water content cycles within magma reservoirs affect eruptive styles, with varying points controlling explosive eruptions. The study provides insights into volcanic behavior, potentially helping forecast eruption explosivity.
Researchers found three areas of hot rock within the mantle beneath three separate volcanic provinces, indicating that Madagascar's volcanoes are not related to nearby tectonic activity. The study suggests that the island's unique geology, with a delaminated lithosphere and a mantle plume, led to the formation of these hot regions.
New faults in Mt. Aso's magma chamber and volcanic cones alter spatial and mechanical properties of the volcano, potentially changing its eruption dynamics. The study suggests that the 2016 Kumamoto earthquake accelerated the timing of a future eruption by creating new channels for magma venting.
Researchers developed a method to measure lithosphere strength using magnetotelluric imaging, revealing accurate descriptions of surface structures and correlating with volcanic and seismic activity. This technique may aid understanding of earthquake and volcanic processes.
A new study mapping Japan's Sakurajima volcano's 'plumbing system' reveals a substantial growing magma reserve, threatening the safety of nearby residents. The team believes their pioneering techniques could help improve eruption forecasting and hazard assessment globally.
Mount Etna's unusual crater formation is attributed to eastern flank instability, causing new stresses and pressures on the volcano's structure. This makes it a prime subject for study, with recent research monitoring its behavior over ten years to predict future eruptions.
Magma-limestone interaction may help explain why volcanoes like Vesuvius are particularly explosive, as it releases CO2 that contributes to Earth's carbon cycle. The process also triggers extreme behavior in volatile elements, potentially driving eruptions and affecting the planet.
Researchers found significant magma movement under Mount St Helens before 1980 eruption, indicating destabilization of magma system and possible future eruptions. Similar measurements may indicate risk at other well-studied volcanoes like Uturuncu in Bolivia.
Two new Geosphere articles reveal the geological history of a major ignimbrite flare-up in the Central Andes, providing insights into the formation of geothermal energy resources. Researchers also study a distinct style of arc volcanism linked to slab-rollback and its impact on continental margins.
Researchers have discovered a massive helium gas field in the Tanzanian Rift Valley, ensuring a stable supply of this finite resource. The find, associated with volcanoes, has calculated a probable resource of 54 Billion Cubic Feet, enough to fill over 1.2 million medical MRI scanners.
A new exploration technique has discovered significant helium reserves in Tanzania, providing a much-needed supply to address the growing demand. The discovery could fill over 1.2 million medical MRI scanners, alleviating a critical shortage of this vital element.
A team of scientists has discovered that dormant volcanoes exhibit predictable quiet periods immediately before eruptions. Longer quiet periods indicate a bigger eruption. This discovery allows for the forecasting of impending eruptions and could revolutionize volcanic monitoring.
A computer model simulates the formation of Io's mountains through the compression of rocks due to volcanic activity. The study suggests that this mechanism could have operated on early Earth, explaining why mountains like those on Io might have emerged first as land.
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 use refined techniques to detect and locate airwaves generated by volcanic explosions on seismic networks, providing an automated way to monitor volcanic eruptions. Ground-coupled airwaves can provide unambiguous evidence of eruptive activity and location of vents.
Scientists have found that rapid bubble formation in magma chambers may trigger sudden volcanic eruptions. This discovery could change the way volcanoes are monitored, focusing on changes in gas composition at the surface rather than seismic activity or ground deformation.
A recent study of Laguna del Maule volcanic field reveals dramatic uplift over the past 8 years, mirroring similar events in the past 10,000 years. The research suggests that sustained input of new magma underground is the most likely cause of this rapid deformation.
Major volcanic eruptions can trigger reduced river flow in tropical and northern Asia regions, including Amazon, Congo, and Nile, researchers found. The study also reveals increased flow in sub-tropical regions like the south-west US and parts of South America.
Researchers have identified a 2,000-kilometer-long chain of volcanoes running from the Whitsundays to near Melbourne. The volcanic chain was created over the past 33 million years as Australia moved northwards over a hotspot in the Earth's mantle.
New NASA research implies that oceans beneath the crusts of tidally stressed moons may be more common and last longer than expected. Fluid tides in a subterranean magma ocean on Io could produce surface heat patterns observed on the moon.
A new CT scan of Earth's interior connects deep mantle plumes to surface volcanoes like Hawaii, showing plumes are five times wider than previously thought. The scan reveals the connections between lower-mantle plumes and volcanic hotspots, including anchors at the core-mantle boundary.
Researchers simulated volcanic eruptions to understand how current forecasting models succeed in predicting magma properties. Heterogeneous magma leads to more accurate predictions, while homogeneous magma results in less precise forecasts.
Researchers from GEOMAR Helmholtz Centre for Ocean Research Kiel found that the Tristan-Gough hotspot changed composition about 70 million years ago, forming parallel but geochemically distinct volcanoes. The team suggests a huge lens of material in the lower mantle, called LLSVP, as a possible explanation.
Researchers at Trinity College Dublin have discovered a way to extract information from magma crystals, allowing them to reconstruct the history of global geography and predict future eruptions. This new method has the potential to improve our understanding of volcanic activity and provide more accurate predictions for eruptions.
A team of scientists has tracked the development of Galapagos volcanoes over 8-16 million years ago, discovering highly explosive eruptions that deposited ash layers 1200km away. The study sheds new light on Earth's volcanic history and climate evolution.
Researchers identified a previously unknown drop in pressure when magma stalled to form a horizontal sill, which can drive the release of dissolved gases and cause eruptions.
Researchers analyzed eruptive plumes and ash from Volcán de Colima, finding marked differences in vesicularity, crystal characteristics, and glass composition. The study suggests that degassing leads to varying gas-rich and gas-poor pulses within the conduit, controlling Vulcanian explosion explosivity.
Researchers at the University of Oregon have found that water plays a key role in forming magma and producing explosive volcanoes in the Cascade Range. The discovery, driven by computer modeling and data from olivine-rich basalt samples, helps solve a puzzle about plate tectonics and the Earth's deep water cycle.
Researchers found samples of seamounts that did not erupt from hot spots but formed from cracks in the oceanic crust. This discovery confirms their origins and helps explain the unique bend in the Hawaiian-Emperor chain.
Intruding magma interacting with regional tectonics sparks micro-earthquakes in Chiles and Cerro Negro volcanoes. The largest quake recorded was magnitude 5.6 in October 2014, causing damage to local houses and prompting residents to seek shelter.
The 1815 Tambora eruption, one of the largest in the last 1,000 years, killed over 60,000 people in Indonesia and led to a 'year without a summer' globally. A systematic exploration of available eruption archives is needed to better understand potential future hazards.