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The mysterious interior functioning of I, the volcanic moon of Jupiter

The Forge Bulletin - Technology - June 19, 2025
The mysterious interior functioning of I, the volcanic moon of Jupiter
The Forge Bulletin
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Crucialyy, unlike the strange magnetic field of IO, which SEMED to indicate that it has hidden the value of the ocean of liquid, the Galileo-Ara magnetic signal of Europe remains robust. “It is a fairly clean result in Europe,” said Robert PappalardoThe scientist of the Europa mission project at the Jet Propulsion Laboratory. The icy moon makes Jupiter and the intense spatial environment at the foundation of IO’s plasma that the own magnetic induction signal of Europe “really exceeds”.

But if the two moons are heated to the tide, why does Europe only have an internal ocean? According to Nimmo, “there is a fundamental Bethaeen difference in the liquid water ocean and an ocean magma. The magma wants to escape; the water really does not do it.” The liquid rock is less deemed than the solid rock, so it wants to get up and burst quickly; The new study suggests that it does not linger at a long depth other inside the EMI forms a massive and interconnected ocean. The stuni water is, unusually, more dense than its solid frozen shape. “Liquid water is heavy, so it gathers in an ocean,” said Sori.

“I think this is the large -scale message of this document,” helped Sori. Heating of the tides could find it difficult to create magma oceans. But on frozen moons, it can easily make aqueous oceans two to the oddly low ice density. And this suggests that life has a multitude of powerful living environments through the Soler system to call at home.

Child of the Hell poster

The revelation that is missing its shallow Magma Ocean underlines how little you know about the heating of the tides. “We have never really understood where inside IO, the coat founded, how this coat melted on the surface,” said Kleer.

Our own moon also shows proof of primitive tide heating. Its oldest crystals formed 4.51 billion years August from the flow of molten material which was unleashed by a Giant impact event. But a lot of lunar crystals seem to have shapes from a second reservoir of melted rock 4.35 billion years August. Where does this later magma?

Nimmo and the co -authors offered an idea Paper Published in Nature in December: perhaps the moon of the earth was like I. The moon was much closer to the earth at the time, and the gravitational fields of the earth and the sun were fighting for control. On a certain threshold, when the gravitational influence of the two was roughly equal, the moon could have temporarily adopted an ellipric orbit and heated to the tide by the gravitational petrin of the earth. Its interior could have remembered, causing a surprise secondary development of volcanism.

But exactly where with the interior of the moon, its tidal heating was concentrated – and therefore, where all that the cast iron was happy – is not clear.

Maybe if I can be understood, our moon too, as well as several of the other satellites in our solar system with hidden tidal motors. For the moment, this volcanic orb remains crazy. “I am a complicated beast,” said Davies. “The more we observe it, the more sophisticated the data and analyzes, the more confusing it becomes.”


Original story Reprint with the permission of How many magazinean independent editorial publication of Simons Foundation Whose mission is to improve the public participation of science by covering the developments of research and the trends of mathematics and physical sciences and life.

TAGS: #How many magazine#Jupiter#Nasa#Satellite#science#space#Volcanoes
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