New model reveals mantle wind fueling Yellowstone supervolcano

Researchers have developed a three-dimensional model showing that a broad eastward-moving mantle wind supplies magma to Yellowstone rather than a deep plume from Earth's core.

A team from the Institute of Geology and Geophysics of the Chinese Academy of Sciences built the model of western North America. It links the wind to remnants of the subducted Farallon Plate and shows how the flow creates a southwest-dipping channel through the lithosphere.

The channel allows hot asthenospheric material to rise and form the extensive magma mush system beneath the caldera. Yellowstone has produced two supereruptions in the past 2.1 million years.

The study, published in Science, matches existing geophysical and geochemical data. It offers a single framework for how large magmatic systems develop and persist under supervolcanoes worldwide.

Makala yanayohusiana

Researchers have created the first global map showing how Earth's deepest mantle is deformed, primarily in regions where ancient subducted tectonic slabs reside. Using over 16 million seismograms, the team confirmed patterns predicted by geodynamic models. The findings, published in The Seismic Record, offer new insights into mantle flow near the core-mantle boundary.

Imeripotiwa na AI

Gases from hot springs in central Zambia show signs of mantle fluids rising to the surface, suggesting an early-stage continental rift. Researchers say this could mark the start of a new tectonic plate boundary. The findings come from samples collected in the Kafue Rift.

Researchers have identified natural barrier zones on an underwater fault that act as brakes to stop earthquakes from growing larger. The findings come from detailed studies of the Gofar transform fault off Ecuador.

Imeripotiwa na AI

Researchers have verified a rare deep earthquake that struck beneath Utah in 1979 at a depth once thought impossible for such events under continents. New analysis of old data and a 2025 quake support the existence of continental mantle earthquakes.

Researchers at the Princeton Plasma Physics Laboratory have identified plasma rotation as the key factor explaining why particles in fusion tokamaks strike one side of the exhaust system more than the other. Their simulations, which matched real experiments, combined rotation with sideways drifts. The discovery could improve designs for future fusion reactors.

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