There have been proposed hypotheses as to how the Moon could have developed a core dynamo. For instance, a 2022 analysis ...

An unexpected find in tiny crystals hints that the Earth’s mantle may not quite behave as has been believed for nearly a century.

Despite numerous studies investigated convection in the mantle and the lithosphere ... After the implementation of a supercontinent, the σ θθ stresses in the mantle areas where there are no strong ...

and it drives plate tectonics through slow-moving convection currents. Scientists have long known that different materials in the mantle affect the speed of seismic waves. Faster wave speeds ...

On Earth, convection currents churn through the mantle (the layer that lies beneath the crust), causing tectonic plates to move around the planet's surface and triggering geological activity like ...

The crust of volcanically active Venus could be churning with convection currents just like the Earth's mantle. This is the conclusion of researchers from the Washington University in St. Louis ...

The movement we see on the Earth’s surface is largely guided by convection currents in the mantle. This is what pushes tectonic plates apart in some areas and pushes them against each other in ...

Heat from the Earth’s core causes convection currents in the mantle, where hot material rises, cools near the crust, and then sinks back down, creating a continuous cycle. This process plays a key ...

In the near future, studies of slow strain waves may lead to a fundamental revision of the current concepts about the physics of the seismic process.