EF2C. Stay Current—Why Do Volcanoes Erupt?

2022-07-27. Massive undersea eruption filled atmosphere with water. [https://www.science.org/content/article/massive-undersea-eruption-filled-atmosphere-water] By Nathaniel Scharping, Science Magazine. Excerpt: On 15 January, Tonga’s Hunga Tonga-Hunga Ha’apai volcano erupted under the sea, rocking the South Pacific nation and sending tsunamis racing around the world. The eruption was the most powerful ever recorded, causing an atmospheric shock wave that circled the globe four times, and sending a plume of debris more than 50 kilometers into the atmosphere. …The ash and gasses punching into the sky also shot billions of kilograms of water into the atmosphere, a new study concludes. That water will likely remain there for years, where it could eat away at the ozone layer and perhaps even warm Earth. …In all, the plume shot approximately 146 billion kilograms of water into Earth’s stratosphere, an arid layer of the atmosphere that begins several miles above sea level, the authors report this month in Geophysical Research Letters. …Other volcanoes have added measurable amounts of water vapor to Earth’s atmosphere, he says, but the scale this time was unprecedented. That’s likely because of the eruption’s magnitude and underwater location, he says. The water will probably remain in the stratosphere for half a decade or more, [study co-author and JPL atmospheric scientist Luis Millán] says. Big volcanic eruptions often cool the climate, because the sulfur dioxide they release forms compounds that reflect incoming sunlight. But with so much water vapor flung aloft, the Tonga eruption could have a different impact. Water absorbs incoming energy from the Sun, making it a potent greenhouse gas. And the sulfur dioxide will dissipate in just a few years whereas the water will likely stick around for at least 5 years—and potentially longer Millán thinks.…

2022-06-01. ‘Singing’ lava lakes could help predict when volcanoes will blow. By Zach Savitsky, Science Magazine. Excerpt: In 2007, lava began to pool inside one of the craters atop Hawaii’s Kilauea volcano, a gentle eruption that would culminate more than a decade later in a spectacular display of spewed ash and massive lava flows. Until that final outburst, the lava lake was a tourist spectacle, a calm surface that hid the churn of magma deeper within the volcano. Now, researchers have found a new way to identify key signs of Kilauea’s eruptive potential—by listening to vibrations from these lava lakes. Eventually, they hope to use these lava “songs” to forecast when a volcano will start and stop erupting…. [https://www.science.org/content/article/singing-lava-lakes-could-help-predict-when-volcanoes-will-blow

2022-04-22. Studying Volcanoes through Myths, Legends, & Other Unconventional Data. By Nancy Averett, Eos/AGU. Excerpt: Studying historic eruptions through a storytelling lens often improves our understanding of and ability to prepare for such events.… [https://eos.org/features/studying-volcanoes-through-myths-legends-other-unconventional-data]

2022-03-10. New insight into magma chambers could improve volcano models. By Colin Barras, Science Magazine. Excerpt: Researchers have discovered a simple and surprising control over the depth of a volcano’s magma chamber: how much water it contains. The finding is significant because water fuels the most devastating eruptions—from Vesuvius in 79 C.E. to Mount Pinatubo in 1991. The work could also help improve models that predict eruptions, which for years have been based on a volcano’s seismic rumblings and records of its past behavior. …Daniel Rasmussen …and his colleagues wanted to understand why magma chambers—slushy mixes of molten rock, solid crystals, and gases—lie anywhere between about 1 kilometer and 12 kilometers below the surface of “arc” volcanoes, a common kind of volcano that forms near the boundaries of tectonic plates. When plates of ocean crust slide into the mantle, the layer that makes up most of Earth’s interior, they drag water with them that gets locked away in minerals. This water then fuels the formation of magmas. As this magma rises through cracks and fissures, it is depressurized …much like the bubbles in a popped can of carbonated soda. But magma also gets stickier as it loses water, and …gradually becomes so thick it can rise no farther—at least until a physical disturbance such as an injection of extra magma drives an eruption. …A magma body with 1% water by weight would begin to lose water just 1 kilometer below the surface, …but for magma with 7% water by weight, loss would begin much deeper, at about 12 kilometers. This means, counterintuitively, that “wetter” magmas—even though they’re initially more fluid—thicken up and stall out at greater depths than “drier” ones. The researchers thought this could explain why magmas occur at different depths.… [https://www.science.org/content/article/new-insight-magma-chambers-could-improve-volcano-models]

2022-01-21. Radiometric Dating Sheds Light on Tectonic Debate. By Aaron Sidder, Eos/AGU. Excerpt: At the far edges of continents, where the continental shelf transitions into the deep ocean, continental and oceanic plates come face to face. At many of these margins, the denser oceanic plate is pushed below the continental plate in a process called subduction. However, in some cases, known as obduction, the oceanic plate ends up atop the more buoyant continental plate instead of diving below it. …The resulting ophiolites—slices of oceanic crust and mantle atop a continental plate—offer uncommon opportunities to view seafloor geology from the comfort of land. The Samail Ophiolite (Oman–United Arab Emirates), in the northeastern corner of the Arabian Peninsula, is frequently studied as a model of obduction because of its well-exposed and well-studied geology. …In a new study, Garber et al. sought to clarify the timing of the obduction episode in Oman. …Samarium-neodymium (Sm-Nd) and uranium-lead (U-Pbradiometric dating on the garnet, zircon, and rutile crystals in the rocks helped determine the age of the subduction event. …The results indicate that the episode occurred approximately 81–77 million years ago when the Arabian continental plate subducted to the northeast below the Samail Ophiolite.… [https://eos.org/research-spotlights/radiometric-dating-sheds-light-on-tectonic-debate]

2022-01-19. Here’s What Scientists Know About the Tonga Volcano Eruption. By Henry Fountain, The New York Times. Excerpt: The explosion probably won’t cool the planet as some previous eruptions have done, but it could affect weather in the short term.… [https://www.nytimes.com/2022/01/19/climate/scientists-tonga-volcano-eruption-effects.html]

2022-01-04. Sensing Iceland’s Most Active Volcano with a “Buried Hair”. By Sara Klaasen,  Sölvi Thrastarson,  Andreas Fichtner,  Yeşim Çubuk-Sabuncu and  Kristín Jónsdóttir, Eos/AGU. Excerpt: Distributed acoustic sensing offered researchers a means to measure ground deformation from atop ice-clad Grímsvötn volcano with unprecedented spatial and temporal resolutions.… [https://eos.org/science-updates/sensing-icelands-most-active-volcano-with-a-buried-hair]

2021-09-15. Forget oil or water. In Iceland, well diggers seek to tap a volcano’s magma. Source: By Paul Voosen, Science Magazine. Excerpt: KRAFLA VOLCANO IN ICELAND—After years of effort, volcanologists are ready to open a gateway to hell. From the rim of the Víti (“hell” in Icelandic) crater—a smaller crater within Krafla’s 10-kilometer caldera—Ottó Elíasson looks down on at a tranquil grassy field disturbed only by a spindly weather station. …The main attraction lies 2 kilometers below this spot on this volcanically hyperactive island, which is being split in two by the spreading Mid-Atlantic Ridge. In 2009, drillers trying to tap hot water for geothermal energy here accidentally pierced a hidden magma chamber. After an outpouring of steam and glass shards from quenched magma, the borehole created the hottest geothermal well ever measured—until the casing failed. Now, researchers are returning to penetrate the molten rock on purpose, using hardier equipment, to create the world’s only long-term magma observatory. …They could also shed light on how the continents formed and grew.… [https://www.science.org/content/article/forget-oil-or-water-iceland-well-diggers-seek-tap-volcano-s-magma] For GSS Energy Flow chapter 2.

2021-08-31. Anticipating Climate Impacts of Major Volcanic Eruptions. Source: By Simon A. Carn, Paul A. Newman, Valentina Aquila, Helge Gonnermann, and Josef Dufek, Eos/AGU. Excerpt: NASA’s rapid response plan for gathering atmospheric data amid major volcanic eruptions, paired with efforts to improve eruption simulations, will offer better views of these events’ global effects.… [https://eos.org/science-updates/anticipating-climate-impacts-of-major-volcanic-eruptions]. See also Making the Most of Volcanic Eruption Responses.

2021-08-06. Don’t Call It a Supervolcano. Source: By Mary Caperton Morton, Eos/AGU Excerpt: Yellowstone National Park, the world’s first and arguably most famous national park, is home to one of the planet’s largest and potentially most destructive volcanoes. The 50- by 70-kilometer Yellowstone caldera complex is so massive that it can really be appreciated only from the air. But although the caldera isn’t always visible on the ground, it’s certainly no secret: Copious thermal features like hot springs and geyser basins dot the landscape and have attracted people to the uniquely beautiful and ecologically rich area for at least 11,000 years. …Every season, recurring bouts of earthquake swarms trigger sensational stories that Yellowstone could be gearing up for another “big one.” But there’s no need to cancel your family vacation to see the park’s free-roaming bison and grizzly bears: The geologists who keep a very close eye on the Yellowstone caldera system say it’s not going to erupt again in our lifetimes. …The story of Yellowstone begins around 16.5 million years ago, when a plume of magma began fueling intense bouts of volcanism along the border of what is now Idaho, Nevada, and Oregon. This magma plume, like the one that formed the Hawaiian Islands, is stationary, but as the North American plate moves to the southwest over the hot spot, its surface expression migrates, creating a 750-kilometer-long trail of volcanism, including dozens of calderas, across southern Idaho and into northwest Wyoming…. [https://eos.org/features/dont-call-it-a-supervolcano]

2021-06-14. [https://eos.org/research-spotlights/magma-pockets-lie-stacked-beneath-juan-de-fuca-ridge] – Magma Pockets Lie Stacked Beneath Juan de Fuca Ridge. Source: By Sarah Stanley, Eos/AGU. Excerpt: Off the coast of the U.S. Pacific Northwest, at the Juan de Fuca Ridge, two tectonic plates are spreading apart at a speed of 56 kilometers per 1 million years. As they spread, periodic eruptions of molten rock give rise to new oceanic crust. Seismic images captured by Carbotte et al. now provide new insights into the dynamics of magma chambers that feed these eruptions. …Sites of fast and intermediate spreading are typically fed by a thin, narrow reservoir of molten magma—the axial melt lens—that extends along the ridge at an intermediate depth in the oceanic crust, but still well above the mantle. …some seafloor spreading sites around the world contain additional magma chambers beneath the axial melt lens. These additional chambers are stacked one above another in the “crystal mush zone,” an area of the actively forming oceanic crust that contains a low ratio of melted rock to crystallized rock. Beneath the Axial Seamount portion of the Juan de Fuca Ridge …a 2020 investigation showed evidence of stacked magma chambers in the crystal mush zone beneath the large magma reservoir that underlies this on-axis hot spot. …These findings…suggest that these stacked chambers are short-lived and may arise during periods when the crystal mush zone undergoes compaction and magma is replenished from the mantle below. The chambers do not cool and crystallize in place, but instead are tapped and contribute magma to eruptions and other crust-building processes…. 

2021-05-14. [https://eos.org/articles/high-school-junior-builds-cheap-earthquake-warning-device] – High School Junior Builds Cheap Earthquake Warning Device. Source: By Jack Lee, Eos/AGU. Excerpt: A Southern California high school junior has developed a low-cost seismometer using parts that total less than $100—a fraction of the cost of a scientific-grade system. …“It’s small and cheap and accessible,” said Vivien He, a student at Palos Verdes Peninsula High School in Rolling Hills Estates, Calif. In April, she presented her work at the 2021 Annual Meeting of the Seismological Society of America. …When an earthquake occurs, it generates compressional (P) waves and shear (S) waves, which emanate from the epicenter through Earth. Sensors that detect P waves can provide a warning before slower—but more destructive—S waves arrive. “Even with just a few seconds of warning, we can provide a useful alert to people: that they can do something…to protect themselves,” said Angie Chung, a seismologist at the Berkeley Seismological Laboratory in Berkeley, Calif. For instance, someone could duck under a table for protection from falling objects…. 

2021-02-25. Fleets of radar satellites are measuring movements on Earth like never before. By Julia Rosen, Science Magazine. Excerpt: East Africa …the geologically active region has also given birth to dozens of volcanoes. Few have been monitored for warnings of a potential eruption, and until recently, most were believed to be dormant. Then, Juliet Biggs decided to take a closer look—or rather, a farther look. Biggs, a geophysicist at the University of Bristol, uses a technique called interferometric synthetic aperture radar (InSAR) to detect tiny movements of Earth’s surface from space. In a series of studies, she and her co-authors analyzed satellite data on the East African volcanoes. According to their latest results, which were published last month, 14 have been imperceptibly growing or shrinking in the past 5 years—a clue that magma or water is moving underground and that the volcanoes are not completely asleep. …After data showed that the Corbetti volcano, which abuts the fast-growing city of Hawassa, Ethiopia, is inflating steadily at a rate of 6.6 centimeters per year, Biggs’s Ethiopian colleagues included it in the country’s geological hazard monitoring network. …Individual GPS stations can track surface movements of less than 1 millimeter, but InSAR can measure changes almost as subtle across a swath hundreds of kilometers wide. …With InSAR, scientists are tracking how ice streams flow, how faults slip in earthquakes, and how the ground moves as fluids are pumped in or out…. [https://www.sciencemag.org/news/2021/02/fleets-radar-satellites-are-measuring-movements-earth-never] See also A technique to track Earth’s subtle movements with orbiting radars is heating up, by Meagan Cantwell, Science Magazine, Mar 5, 2021.

GSS book cover for Energy Flow

Non-chronological resources

Earthquake Resources

Volcano Resources

Internal Earth Processes – 36 multimedia resources from Teachers’ Domain Earth and Space Science multimedia resources (movies and interactives).

Website discussing the origin of hot spot vulcanism.

Plate tectonic, continental drift animations from UC Berkeley Museum of Paleontology

Subduction in a Nutshell

USGS Hazards Gateway – about earthquakes, floods, hurricanes, landslides, tsunamis, and volcanoes.

USGS Volcano site 

Volcano Observatories