• At the moment, I am focused on four main broad research projects: the origin of arc magmas, the explosive behavior of silicic lava domes, the formation of subglacial volcanoes, and the unique terroir of volcanic soils. (uwm.edu)
  • At the moment, Dr. Cameron is focused on four main research projects: the origin of arc magmas, the explosive behavior of silicic lava domes, the nature of glaciovolcanism, and the rare explosive eruptions of Mt. Etna, Sicily. (uwm.edu)
  • During an eruption, some volcanoes vacillate unpredictably between effusive and explosive behavior. (earthmagazine.org)
  • This means that even seemingly gentler volcanoes present a potential for explosive behavior too. (newstarget.com)
  • Magma is produced by melting of the mantle or the crust in various tectonic settings, which on Earth include subduction zones, continental rift zones, mid-ocean ridges and hotspots. (wikipedia.org)
  • Mantle and crustal melts migrate upwards through the crust where they are thought to be stored in magma chambers or trans-crustal crystal-rich mush zones. (wikipedia.org)
  • During magma's storage in the crust, its composition may be modified by fractional crystallization, contamination with crustal melts, magma mixing, and degassing. (wikipedia.org)
  • Following its ascent through the crust, magma may feed a volcano and be extruded as lava, or it may solidify underground to form an intrusion, such as a dike, a sill, a laccolith, a pluton, or a batholith. (wikipedia.org)
  • Silicate magmas are molten mixtures dominated by oxygen and silicon, the most abundant chemical elements in the Earth's crust, with smaller quantities of aluminium, calcium, magnesium, iron, sodium, and potassium, and minor amounts of many other elements. (wikipedia.org)
  • It's not unusual for long-dead volcanos to still hold pockets of gooey magma, the researchers wrote, and when these fluids move, they can deform the crust and cause faults to slip and slide against one another. (livescience.com)
  • The newly discovered hotspot, an area where Earth's crust is thinner, allowing hot magma from Earth's mantle to come closer to the surface , is just below the ice sheet and could have caused it to form, von Frese and his team suggest. (nbcnews.com)
  • It's incredible how magma convection, a natural process within the Earth's crust, plays a vital role in its production. (managenergy.tv)
  • This convection mechanism allows for the transportation of heat from the deeper parts of the Earth's mantle to the crust, influencing the behavior of magma chambers and volcanic activity. (managenergy.tv)
  • Studies of the most recent activity before 2006, in 1976 and 1986, revealed that the volcano lately produces explosive eruptions that are preceded by months of unrest and injection of new magma into a storage region in the upper several kilometers of the crust. (usgs.gov)
  • Hafnium isotopes measured within the zircon were used to identify periods of time when there were influxes of juvenile magmas associated with crust production. (geosociety.org)
  • Around 27 percent of the magma there is properly molten, which is shy of the 50 percent needed to trigger an eruption. (iflscience.com)
  • Augustine's frequent eruptions and relatively easy access have long drawn volcanologists to study the accumulation, ascent, and eruption of andesitic to dacitic magma. (usgs.gov)
  • Petrologic and geophysical observations suggest that these three eruptions were triggered by similar magma mixing events and that the subsequent ascent and eruption of magma was governed by processes that were roughly constant from one eruption to the next. (usgs.gov)
  • Such changes could affect the vigor of an eruption by fluidizing a previously locked magma chamber or, conversely, by increasing the explosive potential of a magma by chemically stiffening it. (earthmagazine.org)
  • The modeling also showed how iron-bearing nanocrystals can suddenly precipitate in magma and potentially trigger a more explosive eruption by providing nucleation points for gas bubbles. (earthmagazine.org)
  • The results show that, despite their monotonous basaltic flows, the magma lying deep beneath each volcano extremely diverse and included compositions similar to those that caused the cataclysmic 1980 eruption of Mt. St. Helens in Washington state . (newstarget.com)
  • This behavior is attributable to either an increase in the gas content of the eruption jet or a decrease in vent radius with time. (usgs.gov)
  • An increase in the gas content may have occurred as the vent was cleared (by expulsion of a plug of pyroclasts) or as the eruption began to tap deeper, gas-rich magma after first expelling the upper, gas-depleted part of the magma body. (usgs.gov)
  • This mechanism requires that the conduit above the magma body be filled with a bed of pyroclasts, and that the vesiculation rate in the magma body be inadequate to sustain continuous eruption. (usgs.gov)
  • The eruption/repose sequence would be repeated until gas-production rates were inadequate to reopen the valve, either because the depth of the pyroclast bed had become too great, the volatile content of the magma had become too low, or the magma had been expended. (usgs.gov)
  • The Holuhraun eruption, which took place between August 31, 2014, and February 27, 2015, was part of a series of events which started in the volcano in 1974 and might provide evidence about the behavior of the volcano in the future. (icelandreview.com)
  • The magma came from Bárðarbunga and the caldera sank by 60 meters (197 feet) in the course of the eruption. (icelandreview.com)
  • This speeds up the rising melt, and a chain reaction starts that can lead to an eruption, if the gases don't run out and the magma doesn't encounter a barrier of some sort that it can't pass. (listverse.com)
  • Researchers tracked the volcano's behavior before and after the eruption: they monitored gases fuming from its crater, steam explosions burst through the ice on top of the volcano, and tremors from magma moving beneath the surface. (un-spider.org)
  • The most recent Kilauea status update offers three potential scenarios: no eruption (still the likeliest scenario), eruption on the upper parts of the SWRZ near the summit and eruption further down the SWRZ if magma underground migrates through Kilauea's magmatic system. (discovermagazine.com)
  • Dr. Mathez's second main field of research concerns the geochemistry of carbon, which includes everything from its behavior in the deep earth and during volcanic eruption to how it is distributed in crustal rocks. (amnh.org)
  • Augustine Volcano, a frequently active intermediate stratovolcano in the Alaska-Aleutian arc (USA), is an ideal setting to investigate magma reservoir processes due to its frequent modern and Holocene eruption history. (wwu.edu)
  • The difference in eruption style of the Post-contact eruptions (2006/1986 CE) and Pre-contact eruptions (Tephra M) can be explained by different plumbing system configurations, magma compositions, and temperatures. (wwu.edu)
  • The 2006 eruption was the result of four or more compositionally variable components (low- to high-silica andesites) that were generally hotter in temperature than the two compositionally and thermally contrasting BA and HSAD magmas of Tephra M. Tephrostratigraphy suggests that smaller Post-contact style eruptions may have occurred in between the main Pre-contact eruptions. (wwu.edu)
  • Besides molten rock, magma may also contain suspended crystals and gas bubbles. (wikipedia.org)
  • The quakes are triggered as molten rock moves into St. Helens' magma chamber about five to six miles below the surface, said Seth Moran , scientist-in-charge of the U.S. Geological Survey's Cascades Volcano Observatory. (seattletimes.com)
  • As molten rock moves into the underground chamber, it exerts pressure on the surrounding rocks, which can lead to fractures and earthquakes, said Wendy Bohrson, a geologist at Central Washington University who studies magma chemistry . (seattletimes.com)
  • Magma convection refers to the movement of molten rock beneath the Earth's surface. (managenergy.tv)
  • Joe's doctoral research focused on modeling the behavior of molten rock in the interior of Mars and Jupiter's moon Io, and linking results to observations of surface volcanism in order to constrain the structure and history of both bodies' interiors. (nasa.gov)
  • They are formed through the crystallization of magma or lava, which is molten rock material composed mainly of silicate minerals. (ez-life-001.net)
  • Basaltic magma is hot, crystal-poor, gas-poor and silica-poor (relative to rhyolite), so you expect that a basalt should have a lower viscosity than a rhyolite. (bigthink.com)
  • That's because heterogeneous melts are fewer , so they are easily overpowered by the greater basaltic magma. (newstarget.com)
  • The first concerns the solidification behavior of large basaltic magma chambers. (amnh.org)
  • Liquid magma may be moving through an extinct volcano beneath Japan, causing an ongoing earthquake swarm. (livescience.com)
  • An ongoing swarm of earthquakes under Mount St. Helens doesn't mean the volcano is likely to erupt soon, but scientists are studying the tiny temblors to see what they reveal about magma movement deep underground. (seattletimes.com)
  • Sulfur dioxide is released from a volcano when magma is relatively close to the surface. (scitechdaily.com)
  • Geologists are now investigating data, indicating that magma might be accumulating again under Bárðarbunga volcano in Vatnajökull glacier. (icelandreview.com)
  • Understanding volcanic behavior can help to track unrest-warning signs, to forecast volcano eruptions and possible related landslides and tsunamis, and consequently to activate emergency plans in a timely manner. (un-spider.org)
  • At a single volcano, eruptive behavior can change through time as the plumbing system evolves. (wwu.edu)
  • With such a high silica content, these magmas are extremely viscous, ranging from 108 cP (105 Pa⋅s) for hot rhyolite magma at 1,200 °C (2,190 °F) to 1011 cP (108 Pa⋅s) for cool rhyolite magma at 800 °C (1,470 °F). For comparison, water has a viscosity of about 1 cP (0.001 Pa⋅s). (wikipedia.org)
  • But when you consider how viscous rhyolitic magma can be, it makes sense, he says. (earthmagazine.org)
  • 1σ) °C) and a volumetrically larger, cooler, viscous HSAD magma (846 to 870 °C), promoting explosivity. (wwu.edu)
  • Because many of the properties of a magma (such as its viscosity and temperature) are observed to correlate with silica content, silicate magmas are divided into four chemical types based on silica content: felsic, intermediate, mafic, and ultramafic. (wikipedia.org)
  • There are a lot of factors that control viscosity in magma - the silica content, the crystal content, the gas content and temperature. (bigthink.com)
  • That is a remarkable range of viscosities and helps explain the widely different behaviors of volcanoes, as the viscosity of the magma will control how well gases can escape. (bigthink.com)
  • In low viscosity magmas, like basalt, gases can escape easier so there is less of a chance of explosive eruptions. (bigthink.com)
  • The viscosity of magmas as a function of temperature. (bigthink.com)
  • Usually these volcanoes erupt explosively due to the high viscosity of the magma, but sometimes they can erupt effusively," says Danilo Di Genova , an experimental volcanologist at the University of Bristol in England and lead author of the new study , published in Nature. (earthmagazine.org)
  • They found that seemingly small chemical differences in the magma - such as the ratio of sodium to potassium or the presence of iron-bearing nanocrystals - can dramatically affect a magma's viscosity, and therefore its explosivity. (earthmagazine.org)
  • Most magma is rich in silica. (wikipedia.org)
  • The volcanoes most likely to fluctuate are those fueled by rhyolitic magma, which is rich in silica. (earthmagazine.org)
  • Strives to link volatile contents in magma to eruptive style. (uwm.edu)
  • New research has identified a chemical tipping point in some magmas that may trigger the transition between such mild and violent eruptive cycles. (earthmagazine.org)
  • We can clearly separate the eruptive styles, so, thus far, these criteria seem to be universal" for rhyolite magmas, Di Genova says. (earthmagazine.org)
  • The recent behavior of Etna is characterized by nearly continuous eruptive activity from the summit craters and eruptions from new vents on the flanks at intervals of a few years to decades. (scienceblogs.com)
  • This could mean Augustine and its eruptive behavior bay be controlled by variable plumbing configurations of discrete batches of intermediate magmas. (wwu.edu)
  • Intermediate or andesitic magmas contain 52% to 63% silica, and are lower in aluminium and usually somewhat richer in magnesium and iron than felsic magmas. (wikipedia.org)
  • Felsic magma is very thin and fast moving. (weegy.com)
  • They include rhyolite and dacite magmas. (wikipedia.org)
  • Rhyolite is the opposite, where the high viscosities mean bubbles get trapped and explosions follow as the magma becomes overpressured with bubbles. (bigthink.com)
  • Seismologists are using swarms of small quakes under Mount St. Helens as a natural laboratory to study the way magma moves through chambers deep under the mountain. (seattletimes.com)
  • As magma approaches the surface and the overburden pressure drops, dissolved gases bubble out of the liquid, so that magma near the surface consists of materials in solid, liquid, and gas phases. (wikipedia.org)
  • Gases bubble out of the magma as it gets higher, since the pressure is decreasing because there is less rock. (listverse.com)
  • But our magma conduit is still capped, so the gases have nowhere to go but out into the conduit. (listverse.com)
  • This matters because rising magma is driven by gases. (listverse.com)
  • A recent study published in the journal Nature Communications found that benign volcanoes that produce basaltic lava flows hide highly explosive magma components . (newstarget.com)
  • However, the findings of the study suggest that the seemingly predictable behavior of the volcanoes belie potentially explosive activity. (newstarget.com)
  • By deciphering the composition of these rocks, the team could reconstruct the chemical and physical characteristics of magmas lying beneath the volcanoes. (newstarget.com)
  • The team posited that volcanoes consistently erupt homogeneous basaltic lava because the high volumes of magma flushing through the ground "overprint" chemical diversity. (newstarget.com)
  • These volcanoes are typically located close to a hot spot - a plume of hot magma rising towards the surface from deep within the Earth. (newstarget.com)
  • Taken together, this evidence help experts better monitor the behavior of the volcanoes and improve hazard assessments. (newstarget.com)
  • Learn more about how the behavior of volcanoes and volcanic eruptions at Disaster.news . (newstarget.com)
  • Overall, magma convection plays a significant role in harnessing the Earth's natural heat for energy production. (managenergy.tv)
  • These rocks are formed through the cooling and solidification of magma or lava, which can occur deep beneath Earth's surface or during volcanic eruptions. (ez-life-001.net)
  • Intermediate magmas show a greater tendency to form phenocrysts, Higher iron and magnesium tends to manifest as a darker groundmass, including amphibole or pyroxene phenocrysts. (wikipedia.org)
  • Subglacial intermediate volcanism at Kerlingarfjöll, Iceland: magma-water interactions beneath thick ice. (uwm.edu)
  • However, a major perturbation that upsets conditions within the magmatic system could occur, owing perhaps to the rise of a much larger or different parental magma or to a large edifice failure similar to the 1883 sector collapse. (usgs.gov)
  • The aim of this study was to investigate the mechanism of magma differentiation processes, parental magma compositions, changes and processes involved in the formation of the complex and related ore deposits. (scirp.org)
  • U-series disequilibria in Guatemalan lavas, crustal contamination, and implications for magma genesis along the Central American subduction zone. (uwm.edu)
  • Understanding the intricacies of convection in magma is vital for comprehending the processes that lead to the production and release of geothermal energy. (managenergy.tv)
  • This, in turn, can impact the overall productivity of the geothermal well, as the fluid composition is directly influenced by the convective processes occurring within the magma chamber. (managenergy.tv)
  • Lesher says isotope effects could shed light on the processes by which magma turns into rock. (aps.org)
  • Plate-tectonic processes have helped make our planet hospitable to life-shaping the composition and behavior of the hydrosphere, atmosphere, and biosphere. (geosociety.org)
  • Magma oceans and enhanced volcanism on TRAPPIST-1 planets due to induction heating, Nature Astronomy (2017). (phys.org)
  • Such a finding would suggest the lava flows developed as a consequence of late stage volcanism related to the OTVC and subsequent westward migration of magma along the fissure network. (confex.com)
  • Each of these eruptions then followed a similar progression from explosive to effusive behavior over several months. (usgs.gov)
  • The chemically diverse magmas could become mobile and ascend toward the surface, leading to more disruptive and possibly dangerous eruptions. (newstarget.com)
  • If the rate at which the magma produced gas exceeded the rate at which gas escaped to the atmosphere, the vertical pressure difference across the bed of pyroclastic debris would increase, as would the gas-flow rate. (usgs.gov)
  • These derived ages suggest the lavas erupted in a westward progression, which would imply a westward-moving magma source. (confex.com)
  • While the study of magma has relied on observing magma after its transition into a lava flow, magma has been encountered in situ three times during geothermal drilling projects, twice in Iceland (see Use in energy production) and once in Hawaii. (wikipedia.org)
  • In 2014, the USGS reported that several subtle signs, including small quakes and slight motion of GPS stations on the volcano's flanks, indicated that the magma chamber was inflating slowly, or recharging. (seattletimes.com)
  • Development of a magma ocean through induction heating in the mantle of exoplanet Trappist-1c. (phys.org)
  • Magma (from Ancient Greek μάγμα (mágma) 'thick unguent') is the molten or semi-molten natural material from which all igneous rocks are formed. (wikipedia.org)
  • By analyzing isotopes and trace elements within igneous rocks, researchers can reconstruct ancient volcanic activity, identify magma sources, and understand how continents have evolved over time. (ez-life-001.net)
  • The model was based on the latest physical understanding of the behavior of magma, its probable path of least resistance, and statistical data compiled from earlier eruptions. (acm.org)
  • These partition coefficients were combined with MELTS modeling (MELTS is a software package that is used for performing thermodynamically constrained phase equilibria calculations) to evaluate the behavior of scandium during fractional crystallization of a mafic melt and formation of a cumulate, the subsequent partial melting of that cumulate, then the isothermal decompression and final cooling of that melt. (umd.edu)
  • To get at the root of this problem, Di Genova and colleagues looked at the nanoscale structure of samples of rhyolitic magmas that mimic the compositional range of the Yellowstone volcanic system. (earthmagazine.org)
  • Cold-seal pressure vessel experiments have been performed on systems with basaltic to rhyolitic compositions in order to evaluate the behavior of scandium in upper crustal magmas. (umd.edu)
  • Around 760,000 years ago, LVC's cauldron-shaped 16 x 32 kilometer (10 x 20 mile) pit (its "caldera") formed when thick, gas-rich magma explosively depressurized. (iflscience.com)
  • Different isotopes of an element behave almost identically, but surprisingly, within matter that is at uneven temperature, such as magma that is slowly solidifying, heavier isotopes diffuse faster than lighter ones. (aps.org)
  • It's not even clear if the melt is arranged in a way that makes it more or less able to erupt en masse. (iflscience.com)
  • Some kinds of rock melt under these conditions, forming magma. (listverse.com)
  • As explained here , seismic waves change depending on what type of material they pass through, which means geophysicists can use them to approximate what down there is molten, and what is solid - and, as is normal for magma reservoirs, what's between the two. (iflscience.com)
  • In this article, we'll explore the intricate mechanisms of magma convection and its impact on geothermal reservoirs. (managenergy.tv)
  • Magma convection affects the flow and distribution of fluids in geothermal reservoirs. (managenergy.tv)
  • I observe that the impacts of magma convection on geothermal reservoirs are significant for understanding the behavior and potential of these underground energy sources. (managenergy.tv)
  • By studying the interaction between magma convection and geothermal reservoirs, we can gain valuable insights into harnessing this natural process for power generation. (managenergy.tv)
  • Imagine a scorching hot flow of molten magma erupting from the depths of the Earth, slowly cooling and solidifying to form unique rock formations. (ez-life-001.net)
  • As the Pacific plate moves slowly over the hot spot, magma rises to the surface, creating volcanic activity. (hawaiistar.com)
  • Although the microscopic behavior of a complex fluid such as magma is rather intricate, the physics behind isotope separation is ultimately simple, Lacks says. (aps.org)
  • However, a new study published June 8 in the journal JGR Solid Earth found that the quakes are occurring in a pattern that suggests liquid magma is still moving around deep below the surface in an ancient, collapsed caldera. (livescience.com)
  • Petrologists routinely express the composition of a silicate magma in terms of the weight or molar mass fraction of the oxides of the major elements (other than oxygen) present in the magma. (wikipedia.org)
  • By studying the effect of magma convection on geothermal fluid composition and well productivity, we can gain valuable insights into optimizing the utilization of geothermal energy resources. (managenergy.tv)
  • Magma consists of liquid rock that usually contains suspended solid crystals. (wikipedia.org)
  • Magma (sometimes colloquially but incorrectly referred to as lava by laypeople) is found beneath the surface of the Earth, and evidence of magmatism has also been discovered on other terrestrial planets and some natural satellites. (wikipedia.org)
  • In a study published by Nature Astronomy an international team led by the Space Research Institute of the Austrian Academy of Sciences with participation of the University of Vienna explains how magma oceans can form under the surface of exoplanets as a result of induction heating. (phys.org)
  • We have shown that for some of the planets, the heating is strong enough to drive enormous volcanic activity or even lead to the formation of a magma ocean beneath the planetary surface. (phys.org)
  • Geothermal fluids, consisting of water and steam, are heated by the surrounding hot rocks and magma, resulting in their upward movement towards the surface. (managenergy.tv)
  • You would have to wait until the magma reaches the surface to collect samples and make measurements, and at that point, you're better off standing back and collecting data remotely," he says. (earthmagazine.org)
  • This is in contrast to normal switch behavior where multicast traffic is typically forwarded on all interfaces. (rfc-editor.org)
  • Eventually a gas-flow rate would be achieved that would suddenly diminish the ability of the bed to maintain a pressure difference between the magma body and the atmosphere. (usgs.gov)
  • 24, 2019 A magma ocean existing during the core formation is thought to have been highly depleted in carbon due to its high-siderophile (iron loving) behavior. (sciencedaily.com)
  • Join me on this journey to uncover the possibilities and innovations in utilizing magma convection for geothermal power generation. (managenergy.tv)
  • Magma convection is crucial for energy production in geothermal systems. (managenergy.tv)
  • In geothermal systems, magma convection plays a crucial role in the production of energy. (managenergy.tv)
  • The interaction between magma and the geothermal reservoir plays a crucial role in determining the productivity of geothermal wells. (managenergy.tv)
  • These findings serve as a foundation for harnessing magma convection for geothermal power generation. (managenergy.tv)
  • The harnessing of magma heat has the potential to revolutionize the geothermal energy industry. (managenergy.tv)
  • However, by tapping into the immense heat generated by magma convection, we can significantly increase the efficiency and sustainability of geothermal power generation. (managenergy.tv)
  • Convection is driven by the density differences between hot and cold magma, resulting in the upward movement of heated material and the downward movement of cooler material. (managenergy.tv)
  • During a repose interval, vesiculation of the magma body would cause gas to flow upward through the bed of pyroclasts. (usgs.gov)
  • This movement is driven by the convection currents caused by the heat from the magma. (managenergy.tv)
  • The rock that sits around the magma chamber might crack a little bit. (seattletimes.com)
  • Surely the weight of the overlying rock helps squeeze the magma along? (listverse.com)
  • According to Páll Einarsson, professor of geophysics at the University of Iceland, the next few months will determine whether magma is in fact accumulating. (icelandreview.com)
  • A Californian Supervolcano Contains 1,000 Cubic Kilometers Of Magma. (iflscience.com)
  • Specifically, there are around 1,000 cubic kilometers (about 240 cubic miles) of magma within its plumbing system. (iflscience.com)