The researchers' analysis has revealed that all the recent eruptions have been fed from a shared magma reservoir lying about 6.5 miles beneath the volcano Fagradalsfjall. This magma reservoir is constantly being topped up by material rising from deeper within the Earth's mantle. Given this, the researchers expect more moderately sized eruptions of the kind that have forced the repeated (and sometimes permanent) evacuation of the town of Grindavík and surrounding areas in recent months.
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The researchers analysed earthquake data and lava samples to gain insights into the geological processes driving these recent eruptions. They found evidence of a shared magma reservoir beneath the peninsula, fed by molten rock rising from the mantle hot spot. This suggests the potential for a prolonged period of volcanic activity in the region, possibly lasting for years or even decades.
While the researchers are certain that more eruptions are on the way, the exact pattern and frequency of future events remains uncertain. “Nature is never simple," said volcanologist Ilya Bindeman of the University of Oregon. "We don't know how long and how frequently it will continue for the next ten or even hundred years. A pattern will emerge, but nature always has exceptions and irregularities," he further added.
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The researchers plan to further investigate the volcanic activity by drilling into the sites to acquire more detailed information on the eruption processes. Iceland's relatively runny, non-explosive magma makes it an ideal ‘natural laboratory’ for scientists to study active volcanoes up close. As study author Valentin Troll noted, "When you witness a volcanic eruption, you can feel that these are the massive forces of nature, and you yourself are very small." While these events may be ordinary on a geological timescale, they can be devastating for the human populations in their path.