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Tag: Volcanic eruptions

  • How Prehistoric Humans Survived a Supervolcano So Big We Probably Should Have Gone Extinct

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    If you were lucky 74,000 years ago, you would have survived the Toba supereruption, one of the largest catastrophic events that Earth has seen in the past 2.5 million years.

    While the volcano is located in what’s now Indonesia, living organisms across the entire globe were potentially affected. As an archaeologist who specializes in studying volcanic eruptions of the past, I often think about how incredible it is that humans survived this extinction-level event that was over 10,000 times larger than the 1980 Mount St. Helens eruption.

    Volume of material ejected during key explosive eruptions. For reference, 1 cubic kilometer (km3) is roughly equivalent to 0.24 cubic miles. The largest circle depicts the Toba supereruption, with the 1980 Mount St. Helens eruption denoted by the smaller green circle.
    USGS Volcanic Hazards Program, CC BY

    The Toba supereruption ejected 672 cubic miles (2,800 km³) of volcanic ash into the stratosphere, producing an enormous crater roughly 1,000 football fields in length (62 x 18 miles, or 100 x 30 kilometers). An eruption this size would have produced black skies blocking most of the sunlight, potentially causing years of global cooling. Closer to the volcano, acid rain would have contaminated water supplies, and thick layers of ash would have buried animals and vegetation.

    With all those odds stacked against Homo sapiens as a species, how did we survive to piece together the story today?

    Survival amid the ashes

    Human populations living in close proximity to the Toba volcano were probably completely wiped out. Whether people on other parts of the globe were affected is a question that scientists are still investigating.

    The Toba catastrophe hypothesis was one prominent school of thought for many years. It proposes that the Toba supereruption caused a global cooling event that lasted up to six years. Its effects, according to the hypothesis, caused human population sizes to plummet to fewer than 10,000 individual people living on Earth.

    This scenario is supported by genetic evidence found in the genomes of people alive today. Our DNA suggests that modern humans spread into separate regions around 100,000 years ago and then shortly after that experienced what scientists call a genetic bottleneck: an event, such as a natural disaster or disease outbreak, that leads to a large decline in population sizes. These calamities drastically reduce the genetic diversity in a group.

    Whether this apparent reduction in human population size resulted from the Toba supereruption or some other factor is heavily debated. As scientists collect more data from climate, environmental and archaeological records, we can begin to understand what conditions were most important for human survival.

    How to study a supereruption’s impact

    To piece together what happened 74,000 years ago, scientists have one direct line of evidence they can use: the rock and ash ejected from the volcanic eruption itself. This material is referred to as tephra. Scientists can trace the layers of tephra across the landscape both visually and chemically.

    black and white image of a lighter grey blob with a few dark spots on it against a darker grey background
    A backscatter image of a volcanic glass shard, taken with a microscope that uses electrons instead of light. The glass here is very small – 50-60 microns, about the diameter of a human hair – and looks light in color. It also appears to contain holes that formed from air bubbles during the time of eruption.
    Jayde N. Hirniak

    Microscopic volcanic glass called cryptotephra travels the farthest, making it important for understanding the true extent of an eruption. Because cryptotephra is not visible to the naked eye, it can be really challenging to identify. Researchers like me carefully separate out the tiny glass shards by sifting through the dirt and using a micromanipulator, a tool that can pick up and move microscopic grains. This process can feel like looking for a needle in a haystack and can take months to complete for one site.

    Every volcanic eruption has a unique chemistry, which scientists can use to determine which eruption a particular sample of volcanic material originated from. For instance, tephra from one eruption might have more iron in it compared to tephra from another eruption. With this knowledge, we can begin to understand how large past eruptions were and who they directly affected.

    When I work in the field, I look for cryptotephra that settled on archaeological sites – places with traces of past human activity such as tools, art or even buried remains. I collect samples from areas of the site that have been excavated and bring them back to the lab to extract the microscopic volcanic glass out of the dirt. Then I chemically analyze the glass to figure out the volcanic fingerprint.

    first panel shows a woman standing on a ladder working on the dirt face of the wall in front, second panel is a close up of hands carefully picking at the dirt face
    Author sampling for cryptotephra at an archaeological site. Samples are collected in a continuous column along an exposed stratigraphic section.
    Jayde N. Hirniak

    But even if I determine that a certain sample from an archaeological site is from the Toba supereruption, what does that reveal about whether people survived the blast?

    Once we identify a tephra or cryptotephra layer, the next step is to look closely at what’s preserved in the archaeological record before and after that eruption. In some cases, people change their behavior after an eruption, such as using a new stone tool technology or eating something different. Sometimes, people even abandon a site, leaving no trace of human activity after a catastrophic event.

    Studying volcanic deposits on archaeological sites fills in only one piece of the puzzle, though. Environmental and climate records preserve information on how the local vegetation or global temperatures changed at the time of the eruption. This information helps scientists understand why people made the changes they did.

    What does the archaeological evidence reveal?

    Given the size and intensity of the Toba supereruption, it almost seems inevitable that humans across the globe would have suffered immensely. However, most archaeological sites tell a story of resilience.

    In places such as South Africa, humans not only survived this catastrophic event but thrived. At archaeological site Pinnacle Point 5-6, evidence of cryptotephra from Toba shows that humans occupied the site before, during and after the eruption. In fact, human activity increased and new technological innovations appeared shortly after, demonstrating humans’ adaptability.

    This miraculous result was not restricted to South Africa. Similar evidence is also preserved at archaeological site Shinfa-Metema 1 in the lowlands of Ethiopia, where cryptotephra from Toba was present in layers that also preserve human activity.

    Here, past humans adapted to changes in the local environment by following seasonal rivers and fishing in small, shallow waterholes present during long dry seasons. Around the time of the Toba supereruption, humans in this region also adopted bow-and-arrow technology. This behavioral flexibility allowed people to survive the intense arid conditions and other potential effects of the Toba supereruption.

    Through the years, archaeologists have found similar results at many other sites in Indonesia, India and China. As the evidence accumulates, it appears that people were able to survive and continue to be productive after Toba blew its stack. This suggests that this eruption might not have been the main cause of the population bottleneck originally suggested in the Toba catastrophe hypothesis.

    While Toba might not help scientists understand what caused ancient human populations to plummet to 10,000 individuals, it does help us understand how humans have adapted to catastrophic events in the past and what that means for our future.

    What could a future disaster mean?

    The good news is that we are a lot more prepared now than people were 74,000 years ago, and even then, they were able to adapt and find new solutions in the wake of devastating events. Today, programs such as the USGS Volcanic Hazards Program and the Global Volcanism Program focus on preparation by monitoring active volcanoes through a variety of techniques. In fact, you can check out what volcanoes are currently erupting at any time.

    Cartoon showing various ways to monitor for volcanic activity including gas, remote sensing, ground vibrations and deformation
    Different methods of volcanic monitoring conducted by the USGS Volcanic Hazards Program.
    Lisa Faust, USGS, CC BY

    Aside from our increased preparedness, humans are defined by our adaptability to almost any condition, even cataclysmic events. By studying the impact of volcanic eruptions in the archaeological record, we can better understand what conditions were key for human survival in the past and apply these lessons to the future.

    Jayde N. Hirniak, Ph.D. Candidate in Anthropology, Institute of Human Origins, Arizona State University. This article is republished from The Conversation under a Creative Commons license. Read the original article.
    The Conversation

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    Jayde N. Hirniak, The Conversation

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  • Startling video of Iceland volcano eruption quickly goes viral

    Startling video of Iceland volcano eruption quickly goes viral

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    A jaw-dropping aerial video shared on social media shows a volcano erupting in Iceland on Monday.

    Monday’s eruption, which began shortly after 10 p.m. local time, was not unexpected as scientists warned an one was looming, but the event was much larger than expected, according to media reports. The location of the more than 2.5-mile volcanic fissure, which is oozing lava through the cracks, poses a risk to a nearby power plant and town, the New York Times reports.

    Scientists have been monitoring the situation for months after magma, which is molten rock beneath the ground, has been showing signs of erupting as lava in a volcanic explosion. Last week, researchers shared their latest findings, following tests around the Icelandic southwest region of Svartsengi.

    Iceland had been bracing for a significant eruption after huge cracks had opened up in the ground, splitting roads in two, as a series of earthquakes rocked the region. The town of Grindavík, where 4,000 people call home, has been evacuated prior to Monday’s eruption.

    Roads in the town of Keflavik, Iceland, are pictured as smoke billows with lava coloring the night sky orange from a volcanic eruption on the Reykjanes peninsula in western Iceland on December 18, 2023. A volcanic eruption began on Monday night following an earthquake swarm, Iceland’s Meteorological Office reported.
    Maria Steinunn Johannesdottir / AFP

    Nahel Belgherze shared an incredible aerial video on X, formerly Twitter. The clip, which quickly amassed more than 800,000 views in less than 2 hours on the social media platform, also garnered nearly 10,000 likes and 4,000 shares.

    “JUST IN: First aerial footage captured just minutes ago of the newly opened volcanic fissure near Grindavík, Iceland,” Nahel Belgherze posted on X. “It is estimated to be about 3 km long!”

    Newsweek reached out via email on Monday night to the Icelandic Meteorological Office for an update.

    The Icelandic Meteorological Office said in an update on the volcanic eruption early Tuesday morning that the latest aerial observations and seismicity, show the fissure is “expanding to the south.”

    “At the time of publication, the southern end of the fissure was close to Sundhnúkur,” the weather agency said in an online statement shortly after 2 a.m. local time on Tuesday.

    During the first two hours of the eruption, the rate of lava discharge “was thought to be on a scale of hundreds of cubic meters per second, with the largest lava fountains on the northern end of the fissures,” according to the Icelandic Meteorological Office.

    The agency said that real-time GPS measurements showed areas of “significant” ground deformation.

    Around midnight local time, the level of seismicity at the eruption site began to decrease, the meteorological office said.

    AccuWeather shared a video on X showing thick smoke that prompted road closures.

    “Volcano erupts near Grindavik after weeks of intense earthquake activity,” AccuWeather posted on X. “Footage shows thick smoke wafting skyward and lava spewing from the volcano’s mouth. The Icelandic Road Administration announced the closure of all roads in the area.”

    The Icelandic National Broadcasting Service is live-streaming the volcanic eruption on YouTube.