Magma sitting 4-5km beneath the surface of Oregon's Mount Hood has been stored in near-solid conditions for thousands of years, but that the time it takes to liquefy and potentially erupt is surprisingly short - perhaps as little as a couple of months, researchers said.
The key, scientists said, is to elevate the temperature of the rock to more than 750 degrees Celsius, which can happen when hot magma from deep within the Earth's crust rises to the surface.
"If the temperature of the rock is too cold, the magma is like peanut butter in a refrigerator," Kent said.
"It just isn't very mobile. For Mount Hood, the threshold seems to be about 750 degrees C - if it warms up just 50 to 75 degrees above that, it greatly increases the viscosity of the magma and makes it easier to mobilise," said Kent.
The hotter magma from down deep warms the cooler magma stored at 4-5 kilometres, making it possible for both magmas to mix and to be transported to the surface to eventually produce an eruption.
A previous study by Kent and OSU postdoctoral researcher Alison Koleszar found that the mixing of the two magma sources - which have different compositions - is both a trigger to an eruption and a constraining factor on how violent it can be.
Little was known about the physical conditions of magma storage and what it takes to mobilise the magma, researchers said.
Researchers set out to find if they could determine how long Mount Hood's magma chamber has been there, and in what condition.
"What we found was that the magma has been stored beneath Mount Hood for at least 20,000 years - and probably more like 100,000 years," Kent said.
The study was published in the journal Nature.
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