Exploring an undersea terrain sculpted by glaciers and volcanoes

Exploring an undersea terrain sculpted by glaciers and volcanoes

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Possibly counterintuitively, sediment layers are most likely to stay undamaged on the seafloor than on land, so they can offer a much better record of the area’s history. The seafloor is a more steady, oxygen-poor environment, minimizing disintegration and decay (2 factors researchers discover much more fossils of marine animals than land occupants) and protecting finer information.

A close-up view of a core sample taken by a vibracorer. Researchers mark locations they prepare to check more carefully with little flags.


Credit: Alex Ingle/ Schmidt Ocean Institute

Samples from various locations differ drastically in time protection, returning just to 2008 for some and back possibly more than 15,000 years for others due to extremely various sedimentation rates. Researchers will utilize methods like radiocarbon dating to identify the ages of sediment layers in the core samples.

ROV SuBastian found a helmet jellyfish throughout the exploration. These photophobic (light avoidant) animals radiance through bioluminescence.


Credit: Schmidt Ocean Institute

Tiny analysis of the sediment cores will likewise assist the group evaluate the method the eruption impacted marine animals and the chemistry of the seafloor.

“There’s a variety of life and sediment types discovered at the various websites we surveyed,” stated Alastair Hodgetts, a physical volcanologist and geologist at the University of Edinburgh, who took part in the exploration. “The earliest location we checked out– a location scarred by ancient glacier motion– is a fossilized seascape that was totally unforeseen.”

In an area beyond the dunes, ocean currents have actually kept the seafloor clear of sediment. That protects seabed functions left by the retreat of ice sheets at the end of the last glaciation.


Credit: Rodrigo Fernández/ CODEX Project

This function, too, informs researchers about the method the water relocations. Currents streaming over a location that was deteriorated long earlier by a glacier sweep sediment away, keeping the ancient surface noticeable.

“I’m really thinking about evaluating seismic information and associating it with the layers of sediment in the core samples to produce a timeline of geological occasions in the location,” stated Giulia Matilde Ferrante, a geophysicist at Italy’s National Institute of Oceanography and Applied Geophysics, who co-led the exploration. “Reconstructing the past in this method will assist us much better comprehend the sediment history and landscape modifications in the area.”

In this post-apocalyptic scene, recorded June 20, 2008, a thick layer of ash covers the town of Chaitén as the volcano continues to emerge in the background. Around 5,000 individuals left, and resettlement efforts didn’t start up until the list below year.


Credit: Javier Rubilar

The group has actually currently collected measurements of the quantity of sediment the eruption provided to the sea. Now they’ll work to identify whether older layers of sediment record previously, unidentified occasions comparable to the 2008 eruption.

“Better understanding past volcanic occasions, exposing things like how far an eruption reached, and how typical, serious, and foreseeable eruptions are, will assist to prepare for future occasions and minimize the effects they have on regional neighborhoods,” Watt stated.

Ashley discusses area for a professional for NASA’s Goddard Space Flight Center by day and freelances as an ecological author. She holds master’s degrees in area research studies from The University of North Dakota and science writing from The Johns Hopkins University. She composes the majority of her short articles with an infant on her lap.

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