Crystals open window into volcanic depths
When red-hot magma spews from a volcano, it is clearly flowing like a liquid. But before erupting, that same magma may have spent hundreds of thousands of years in a chunky state resembling cold porridge, a new study finds. The discovery suggests that hot, liquid magma pools may be useful as an indicator of impending eruptions.
Volcanic magma, the molten mix of rock and gas below Earth’s surface, leads a sort of double life: It spends some time as a hot liquid and some as a colder, rocky “crystal mush.” Scientists have long known that magma is mostly liquid only above 750° Celsius, and that in its colder state, it is too viscous to flow. Whether magma spends much of its existence in the hot, largely liquid state or heats up briefly before erupting has been a mystery.
Seeking answers, Kari Cooper of the University of California, Davis and Adam Kent of Oregon State University in Corvallis analyzed crystallized minerals in cooled magma that