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Glass Lava Flow Still Oozes a Year Later

Puyehue Cordón Caulle obsidian lava flow
Puyehue-Cordón Caulle volcano and its obsidian lava flow, still going nearly a year after the volcano stopped erupting.
(Image credit: NASA Earth Observatory)

A slow-moving lava flow made of glass is still inching its way down a volcano in Chile, nearly a year after it first erupted, geologists recently discovered.

The lava is made of obsidian, or volcanic glass. Researchers visiting Chile's Puyehue-Cordón Caulle volcano in January 2013 found the obsidian flow was moving, even though the volcano stopped erupting in April 2012, NASA's Earth Observatory reported.

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Becky Oskin
Contributing Writer
Becky Oskin covers Earth science, climate change and space, as well as general science topics. Becky was a science reporter at Live Science and The Pasadena Star-News; she has freelanced for New Scientist and the American Institute of Physics. She earned a master's degree in geology from Caltech, a bachelor's degree from Washington State University, and a graduate certificate in science writing from the University of California, Santa Cruz.