Scientists uncover details of a catastrophic volcanic eruption and flood over 1,000 years ago

by

Editors' notes

This article has been reviewed according to Science X's editorial process and policies. Editors have highlighted the following attributes while ensuring the content's credibility:

fact-checked

peer-reviewed publication

trusted source

proofread

The location map of Changbaishan-Tianchi Volcano and distribution of lava flows and pyroclastic deposits around the crater lake (H. Q. Wei et al., 2013). NW-SE and NE-SW trending faults across Tianchi, and the lake depth contours are shown (M. J. Liu et al., 2004). Credit: Water Resources Research (2024). DOI: 10.1029/2024WR037085

In the year 946 CE, the Changbaishan-Tianchi volcano, on the border between China and North Korea, erupted ferociously. The eruption released dozens of cubic kilometers of magma and triggered a massive flood from the lake atop the volcano's summit, known today as Heaven Lake. Evidence of the flood can still be seen in the form of boulders and smaller rocks that washed down from the upper reaches of the volcano.

Changbaishan-Tianchi, known as Baekdu in Korean, could erupt again, so volcanologists want to understand the risks it poses. To investigate the catastrophic flood that followed the 946 eruption, Qin and team dug into the layered deposits from the volcano. Their work suggests that at least 1 cubic kilometer of water spilled from the volcano's caldera, causing sediment to erode at rates as high as 34 meters per hour over about 3 hours. The paper is published in the journal Water Resources Research.

The researchers also concluded that the eruption consisted of two phases, with the flood occurring between the two. Other scientists have hypothesized that the flood gushed out in one instantaneous outburst after the eruption cracked the volcano's rim, but this study's authors found that scenario unrealistic because the sediment is not as widely spread as would be expected from one sudden burst.

The researchers suggest three alternative scenarios. In the first, the water simply overflowed the edge of the caldera in response to magma rising from below it. In the second, the volcano triggered an earthquake that collapsed the inner wall of the caldera into the lake, causing it to overflow. And in the third, precipitation prior to the event filled the caldera to capacity and weakened the crater rim, allowing the water to flow out.

Understanding ancient floods like the 946 CE event may help vulnerable populations prepare for future natural disasters, not just at Changbaishan-Tianchi but also at volcanoes around the world, the researchers wrote.

More information: Shengwu Qin et al, Reconstruction of the Dynamics of a Catastrophic Crater Lake Outburst Flood, Changbaishan‐Tianchi Volcano, Water Resources Research (2024). DOI: 10.1029/2024WR037085

Journal information: Water Resources Research

Provided by American Geophysical Union

This story is republished courtesy of Eos, hosted by the American Geophysical Union. Read the original storyhere.