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The far side of the Moon provides clues to a previous magnetic field

The far side of the Moon provides clues to a previous magnetic field

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The result: in the Dewar region, beneath the lunar surface, lies a rock body approximately 60 kilometres wide, extending to a depth of around 9 kilometres. It is much denser than the surrounding crust, while strongly magnetised at the same time. Combined with the surface geochemistry and an arched topography, the researchers conclude that this is solidified magma that has risen from the subsurface – a buried volcanic complex.

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ETH Zurich
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Original publisherETH Zurich
Canonical URLhttps://ethz.ch/en/news-and-events/eth-news/news/2026/09/the-far-side-of-the-moon-provides-clues-to-a-previous-magnetic-field.html
Publication timeSat, 26 Sep 2026 07:49:50 +0000
Retrieval time2026-09-26T10:36:00.198Z
Last seen2026-09-26T10:36:00.198Z
Headline sourcePublisher (no WeSearch rewrite)
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Excerpt methodFirst ~120 words (~800 chars) of extracted publisher body, fair-use limited.
SummaryWeSearch · cerebras-chat (WeSearch summarizer)
Summary source textcontentText
Citation coverageSummary is a WeSearch-generated derivative; primary citation is the original publisher URL.
ClusterQZC6Nq_m-a29 · 1 stories
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Ranking reasonStory pages are not engagement-ranked. Hub feeds use recency, with optional source-diversified chronological ordering (cap consecutive stories per source). No personalized ranking.
Publisher visitYes — open original
Substitutes article?No — link-out required for full text

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Basis: Derived from the published RSS/Atom feed. Contact: [email protected]. Reviewed: 2026-07-24.

Opening excerpt (first ~120 words) tap to expand

The result: in the Dewar region, beneath the lunar surface, lies a rock body approximately 60 kilometres wide, extending to a depth of around 9 kilometres. It is much denser than the surrounding crust, while strongly magnetised at the same time. Combined with the surface geochemistry and an arched topography, the researchers conclude that this is solidified magma that has risen from the subsurface – a buried volcanic complex. The age of the structure – 4.2 billion years – can be determined from the various deposits of impact material on the lunar surface. A surprisingly strong magnetic field “Because we know how much iron is present in such a rock body, we can estimate the minimum strength the magnetic field must have had as the magma cooled slowly.

…

Excerpt limited to ~120 words for fair-use compliance. The full article is at ETH Zurich.

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