An Impact Driven Dynamo for the Early Moon

An Impact Driven Dynamo for the Early Moon


The Royal Observatory of Belgium participates in an interdisciplinary study on the origin of the early magnetic field of the early Moon. Researchers from the field of fluid mechanics and lunar geophysics joined forces. They showed in their article in Nature that the early magnetic field was caused by movements of material after instantaneous changes of the rotation rate of the Moon due to large meteorite impacts.

More about this on the website of Nature (p.215)