The
largest volcanoes on our planet may take as little as a few hundred years to
form and erupt. These "supervolcanoes" were thought to exist for as
much as 200,000 years before releasing their vast underground pools of molten
rock. Researchers reporting in Plos One have sampled the rock at the supervolcano
site of Long Valley in California. Their findings suggest that the magma pool
beneath it erupted within as little as hundreds of years of forming. That
eruption is estimated to have happened about 760,000 years ago, and would have
covered half of North America in its ash. Such super-eruptions can release
thousands of cubic kilometres of debris - hundreds of times larger than any
eruption seen in the history of humanity. Eruptions on this scale could release
enough ash to influence the global weather for years, and one theory holds that
the Lake Toba eruption in Indonesia about 70,000 years ago had long-term
effects that nearly wiped out humans altogether. What little is known about the
formation of these supervolcanoes is largely based on the study of crystals of
a material called zircon, which contains small amounts of radioactive elements
whose age can be estimated using the same techniques used to date
archaeological artefacts and dinosaur bones.
Zircon studies to date have
suggested that the time between the formation of the enormous magma pools and
the eventual super-eruptions can be measured in the hundreds of thousands of
years. Now, Guilherme Gualda of Vanderbilt University and his colleagues
present several lines of evidence from the Bishop Tuff deposit at Long Valley,
suggesting that the pools are "ephemeral" - lasting as little as 500
years before eruption. Initially, the magma pools are nearly purely liquid
rock, with few bubbles or re-crystallised minerals. Over time, crystals
develop, but the process stops at the point of the eruption. As a result, the
characteristic development time of these crystals can also give an estimate of
how long a magma pool existed before erupting. Rather than zircon, the team's target
was crystals of the common mineral quartz. Because the processes and timescales
of quartz formation in the extraordinary underground conditions of a magma pool
are well-known, the team was able to determine how long the crystals were
forming within Long Valley's supervolcano before being spewed out in the
eruption. Their estimates suggest the quartz formed over a range of time
between 500 and 3,000 years. "Our study suggests that when these
exceptionally large magma pools form they are ephemeral and cannot exist very
long without erupting," said Dr Gualda. "The fact that the process of
magma body formation occurs in historical time, instead of geological time,
completely changes the nature of the problem." At present, geologists do
not believe that any of Earth's known giant magma pools are in imminent danger
of eruption, but the results suggest future work to better understand how the
pools develop, and aim ultimately to predict devastating super-eruptions.
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