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The Kima'Kho tuya forms a high relief structure covering 11 square miles (28 square kilometers), rising more than 6,300 feet (1,900 meters) above sea level on the Kawdy Plateau in British Columbia, Canada.
An ancient volcano that erupted 1.8 million years ago in western Canada burst through an ice sheet that was twice as thick as scientists had previously estimated, according to the results of a new study.
Researchers collected volcanic (or pyroclastic) samples from Kima'Kho, a partially eroded subglacial volcano located in the province of British Columbia, and made detailed observations of the surrounding terrain. These measurements enabled the scientists to make more accurate models of the regional ice sheet.
When a volcano erupts underneath a glacier, a subglacial volcano can form. These formations, called tuyas, can help researchers piece together details on how the Earth's climate has changed over the course of its history.
The shape of tuyas varies, depending on a number of environmental conditions at the time of the eruption, including the thickness of the ice sheet.
Scientists can also study the deposits made from these subglacial eruptions to determine whether they were generated above or below the waterline of the vast lakes within glaciers — similar to how water rings are left on the inside of a bathtub, the study researchers explained. Analyzing these different "rings," or passage zones, helps the researchers tease out information about how the glacier has evolved.
By calculating the depth and volume of water in these so-called englacial lakes, James Russell, a volcanologist at the University of British Columbia and lead author of the study, and his colleagues were able to make accurate measurements of the thickness of the ancient ice sheet when Kima'Kho erupted 1.8 million years ago.
"At Kima'Kho, we were able to map a passage zone in pyroclastic deposits left by the earliest explosive phase of eruption, allowing for more accurate forensic recovery of paleo-lake levels through time and better estimates of paleo-ice thicknesses," Russell said in a statement.
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Geologists from the University of British Columbia examine pyroclastic deposits on the south side of the Kima'Kho volcano.
(Image credit: UBC Science)
And the technique can be used to make the same estimates for other tuyas.
"Applying the same technique to other subglacial volcanoes will provide new constraints on paleoclimate models that consider the extents and timing of planetary glaciations," Russell said.
Tuyas are commonly found in Iceland, British Columbia, Oregon and beneath the Antarctic ice sheets, but are otherwise relatively scarce throughout the rest of the world.
The results of the study were published online Tuesday (April 30) in the journal Nature Communications.
Denise Chow was the assistant managing editor at Live Science before moving to NBC News as a science reporter, where she focuses on general science and climate change. Before joining the Live Science team in 2013, she spent two years as a staff writer for Space.com, writing about rocket launches and covering NASA's final three space shuttle missions. A Canadian transplant, Denise has a bachelor's degree from the University of Toronto, and a master's degree in journalism from New York University.
