Sea of ash Exploring an undersea terrain sculpted by glaciers and volcanoes Researchers found a fossilized seascape while studying the impact of a volcanic eruption. Ashley Balzer Vigil Dec 21, 2024 6:09 am | 0 This May 26, 2008 photo shows the Chaitn lava dome with lava spilling out the left side and agiant plume of ash blasting into the sky. The eruption lasted several months and blanketedsurrounding farmland in ash. Credit: United States Geological Survey This May 26, 2008 photo shows the Chaitn lava dome with lava spilling out the left side and agiant plume of ash blasting into the sky. The eruption lasted several months and blanketedsurrounding farmland in ash. Credit: United States Geological Survey Story textSizeSmallStandardLargeWidth *StandardWideLinksStandardOrange* Subscribers only Learn moreOn May 2, 2008, the Chaitn volcano in Chile awoke with unexpected fury after more than 9,000 years of dormancy. The eruption blasted rocks and ash a dozen miles into the air, and then heavy rainfall swept the fallen debris up in immense mudflows. A river of rubble carved a destructive path through the nearby town of Chaitn before surging into the sea. The town, practically split in two by the torrent that cut through its middle, was evacuated as ash blanketed over 200,000 square kilometers of surrounding land.While the terrestrial aftermath was plain to see, captured by both the local media and satellites, the impact on the sea was unknown. Mists shroud the hillsides at the entrance to Chaitn Bay, as seen from aboard the Schmidt Ocean Institutes Falkor (too) research vessel. Credit: Alex Ingle / Schmidt Ocean Institute The eruption released over 750 billion liters of lavaenough to fill more than 300,000 Olympic-sized swimming poolsmainly in the form of rock fragments. The debris flowed through rivers into the Northern Patagonian Sea, just six miles away.An international team of scientists set sail on the Schmidt Ocean Institutes Falkor (too) research vessel in September to trace the volcanic ashs flow and assess its effects. Along the way, they found an underwater valley carved out by ancient glaciers. Its hardly been altered in the 17,000 years or so since those glaciers retreated. Heavy rain following the eruption swept fallen ash into the sea, as seen in this satellite image. Credit: NASA Earth Observatory They wanted to explore how volcanoes impact the sea, its inhabitants, and underwater infrastructure.Our observations will allow us to explore how active volcanoes affect marine environments and infrastructure, ranging from fisheries to communication cables, the expeditions chief scientist, Sebastian Watt, an associate professor in Earth sciences at the University of Birmingham, said in a press release. The town of Chaitn is very rural, and the area itself lacks submarine cables, but the teams work could help assess whether volcanic activity might damage those cables at other locations across the globe.Because of how they form, volcanoes are nearly always found in or near the ocean, yet scientists have hardly studied how eruptions affect marine ecosystems. A range of hazards can impact communities in the aftermath of volcanic eruptions, Watt said, and the information we gather from studying the 2008 Chaitn eruption is relevant for coastal and island volcanoes globally. The remotely operated vehicle SuBastian is recovered onto the research vessel after an exploratory dive. Credit: Alex Ingle / Schmidt Ocean Institute A remotely operated vehicle (ROV) called SuBastian served as the teams underwater eyes. Fitted with a suite of lights, cameras, and sensors, the ROV explored the areas where volcanic debris had washed into the ocean.We used the ROV SuBastian to gather samples that would otherwise be impossible to obtain, said Rodrigo Fernndez, an assistant professor at the Universidad de Chile, who co-led the expedition. And the ability to see the sampling sites with our own eyes and select the very best targets is a game changer. We usually sample the seafloor blind, selecting targets based on geophysics data acquired from the vessel and then deploying equipment hundreds or thousands of meters down.The team collected samples that contain both sediment and shells, which theyll analyze to help determine the samples ages and to study microbial and geochemical changes. Comparing lower layers (from before the eruption) with higher ones will let them see how the eruption affected the marine ecosystem. Silhouetted against screens, remotely operated vehicle pilots take sediment samples using ROV SuBastian. Credit: Alex Ingle / Schmidt Ocean Institute The ROVs lights in the ocean shine like a candle in the night, casting an eerie glow on its immediate surroundings but unable to provide a big-picture view. For that, the team used sonar instruments on the ship to make a high-resolution 3D map of the seafloor. Underwater dunes offshore the Rayas River delta, mapped in 3D by the Schmidt Ocean Institute-funded CODEX project, extend for well over 10 kilometers. They indicate the presence of strong currents through the area, which transported the volcanic material carried into the ocean by rivers following the eruption. Credit: Rodrigo Fernndez / CODEX Project That map revealed underwater giantstowering mega-dunes made of volcanic ash. The dunes are an imprint that hints at the forces that sculpt the seafloor, allowing scientists to trace the transport of volcanic material after it was swept into the sea. The team mapped over 1,000 square miles, collected data on what lies more than six stories beneath the seafloor, and found ash more than 15 miles from the volcano. Macarena Prez (a PhD student at the University of Playa Ancha) and Sion Moraga (a student at the University of Chile) inspect a core sample. Credit: Alex Ingle / Schmidt Ocean Institute The ROV was equipped with a vibrating coring device, a straw-like instrument that gathered sediment samples by plunging into the seafloor. The layers of sediment collected in the core samples preserve evidence of the areas past geological and biological activity.Perhaps counterintuitively, sediment layers are more likely to remain intact on the seafloor than on land, so they can provide a better record of the regions history. The seafloor is a more stable, oxygen-poor environment, reducing erosion and decomposition (two reasons scientists find far more fossils of marine creatures than land dwellers) and preserving finer details. A close-up view of a core sample taken by a vibracorer. Scientists mark places they plan to inspect more closely with little flags. Credit: Alex Ingle / Schmidt Ocean Institute Samples from different areas vary dramatically in time coverage, going back only to 2008 for some and back potentially more than 15,000 years for others due to wildly different sedimentation rates. Scientists will use techniques like radiocarbon dating to determine the ages of sediment layers in the core samples. ROV SuBastian spotted a helmet jellyfish during the expedition. These photophobic (light avoidant) creatures glow via bioluminescence. Credit: Schmidt Ocean Institute Microscopic analysis of the sediment cores will also help the team analyze the way the eruption affected marine creatures and the chemistry of the seafloor.Theres a wide variety of life and sediment types found at the different sites we surveyed, said Alastair Hodgetts, a physical volcanologist and geologist at the University of Edinburgh, who participated in the expedition. The oldest place we visitedan area scarred by ancient glacier movementis a fossilized seascape that was completely unexpected. In a region beyond the dunes, ocean currents have kept the seafloor clear of sediment. That preserves seabed features left by the retreat of ice sheets at the end of the last glaciation. Credit: Rodrigo Fernndez / CODEX Project This feature, too, tells scientists about the way the water moves. Currents flowing over an area that was eroded long ago by a glacier sweep sediment away, keeping the ancient terrain visible.Im very interested in analyzing seismic data and correlating it with the layers of sediment in the core samples to create a timeline of geological events in the area, said Giulia Matilde Ferrante, a geophysicist at Italys National Institute of Oceanography and Applied Geophysics, who co-led the expedition. Reconstructing the past in this way will help us better understand the sediment history and landscape changes in the region. In this post-apocalyptic scene, captured June 20, 2008, a thick layer of ash covers the town of Chaitn as the volcano continues to erupt in the background. Around 5,000 people evacuated, and resettlement efforts didnt begin until the following year. Credit: Javier Rubilar The team has already gathered measurements of the amount of sediment the eruption delivered to the sea. Now theyll work to determine whether older layers of sediment record earlier, unknown events similar to the 2008 eruption.Better understanding past volcanic events, revealing things like how far away an eruption reached, and how common, severe, and predictable eruptions are, will help to plan for future events and reduce the impacts they have on local communities, Watt said.Ashley writes about space for a contractor for NASA's Goddard Space Flight Center by day and freelances as an environmental writer. She holds master's degrees in space studies from The University of North Dakota and science writing from The Johns Hopkins University. She writes most of her articles with a baby on her lap. 0 Comments