BBC: Earth’s core lies about 1900 miles below sea level, beyond the reach of direct observation. To re-create conditions there, an experiment at the European Synchrotron Radiation Facility (ESRF) will subject iron and other materials to intense pressure using diamond anvil cells, which compress tiny material samples between the points of two diamonds. The compressed samples will then be heated to more than 10 000 °C with lasers fired through the diamonds, and x rays will probe the samples to give high-resolution snapshots of the reactions that occur as the samples are heated and squeezed. How the materials absorb the x rays should give clues to how Earth’s magnetic field is formed, why it changes, and how shock waves propagate through it.
The finding that the Saturnian moon may host layers of icy slush instead of a global ocean could change how planetary scientists think about other icy moons as well.
Modeling the shapes of tree branches, neurons, and blood vessels is a thorny problem, but researchers have just discovered that much of the math has already been done.
January 29, 2026 12:52 PM
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