Science News: Gold, platinum, and other similar heavy elements are siderophile—when molten they tend to form alloys with iron. About 98% of Earth’s siderophile elements are in the iron-dominated core, and the traditional view is that they sank to the core early in Earth’s history. David Rubie of the University of Bayreuth in Germany and his colleagues are challenging that view. They argue that the bombardment of asteroids and comets that occurred during the first 100 million years of Earth’s formation kept the planet’s internal pressure and temperature high enough that siderophile elements were less likely to bond with iron. If that’s true, then the heavy elements would have remained in Earth’s mantle until they reacted with sulfur, crystallized, and fell toward the core. Rubie’s group attributes the presence of precious metals in Earth’s crust to the subsequent bombardment of asteroids, which deposited the elements on the surface.
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
Get PT in your inbox
PT The Week in Physics
A collection of PT's content from the previous week delivered every Monday.
One email per week
PT New Issue Alert
Be notified about the new issue with links to highlights and the full TOC.
One email per month
PT Webinars & White Papers
The latest webinars, white papers and other informational resources.