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A younger surface on an older moon

The moon looks like a fixed relic, but the article presents it as an archive whose first pages may have been partly rewritten. Scientists have long had two competing clocks for the moon’s birth. Lunar rock samples suggest that the moon-forming impact happened about 4.35 billion years ago. Planet-formation models and zircon fragments from the lunar surface, however, point to an older origin, at least 4.51 billion years ago. That gap of roughly 150 million years is not a small bookkeeping error. It changes the story of how Earth, the moon and the early solar system settled into their present forms.

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The sun did not travel alone

The article frames the sun as a migrant. Its current position, in a relatively quiet part of the Milky Way, is probably not where it began. Astronomers have long inferred from the sun’s age and chemistry that it formed closer to the galaxy’s crowded center, where earlier generations of stars enriched the gas with heavier elements more quickly than in the outer disk. Over 4.6 billion years, the sun appears to have moved roughly 10,000 light-years outward.

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A planet that does not fit the old boxes

The article uses the exoplanet L 98-59 d as a reminder that astronomy’s neat categories are often temporary. The planet orbits a red dwarf star trillions of miles from Earth, and the observations gathered so far make it look stranger than the usual menu of small-world types. It is not simply a rocky planet with a thick hydrogen atmosphere. It is not an ocean world. The best current interpretation is more exotic: a hot, low-density planet with a sulfur-rich atmosphere and a surface that may be a global or near-global magma ocean.

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Quantum hardware is still an open contest

The article turns a familiar abstraction into a hardware problem. Quantum computing is often described through the power of qubits, but a qubit is not a single kind of object. It is a way of encoding quantum information in a physical system, and researchers are still testing several very different systems to see which ones can become reliable, scalable machines.

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Robin George Andrews begins with a proposal that sounds reckless at first: put a nuclear reactor on the moon. Yet the basic logic is hard to escape. Any permanent lunar base will need steady electricity and heat through a night that lasts roughly 14 Earth days. Solar panels and batteries alone are unlikely to support habitats, scientific instruments and machinery for extracting water from lunar soil. If NASA wants the moon to become an outpost for research, mining and eventual travel to Mars, nuclear fission may be the only practical long-term power source.

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When satellites stop inspiring wonder

Phil Plait begins with a change in perspective. As a teenager, he felt awe when he first spotted a satellite sliding across the night sky. Today the same sight fills him with dread. The difference is scale. Satellites are no longer occasional visitors overhead. Companies and governments are building constellations of thousands of spacecraft, and proposals for much larger swarms could turn low-Earth orbit into industrial infrastructure.

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Quantum mechanics is one of science’s most successful theories, but success has not made it intuitive. Its predictions have survived experiment after experiment and underpin modern electronics. Yet its usual mathematical description allows particles to exist in several possible places at once until a measurement returns one definite result. Entangled particles add another puzzle: measuring one appears to determine the state of another, even across a great distance. Physicists agree that the calculations work. They still disagree about what kind of reality those calculations describe.

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Robin George Andrews treats the new push back to the moon as more than a spaceflight milestone. If NASA’s Artemis program and related robotic missions create a lasting presence there, the moon could become a scientific instrument in its own right: a quiet, ancient body covered with clues that Earth has largely erased. Plate tectonics, weather, oceans and life have constantly recycled Earth’s oldest rocks. The moon, by contrast, has preserved much of its early history in place.

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Joseph Howlett’s article argues that the return to the moon is not only a human-spaceflight story. It could also reshape astronomy. NASA’s Artemis program, along with related commercial lunar landers, is opening a way to place scientific instruments on the lunar surface. For astronomers facing shrinking support for conventional observatories, the moon offers something rare: a physically stable, radio-quiet and human-serviceable platform close enough for repeated missions but different enough from Earth to make new measurements possible.

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Artemis II was designed as a test flight, but Nadia Drake frames it as something larger: the moment human spaceflight returned to the moon after more than half a century. The mission did not land. Instead, commander Reid Wiseman, pilot Victor Glover, mission specialist Christina Koch and Canadian mission specialist Jeremy Hansen rode NASA’s Orion spacecraft on a looping 10-day path around the moon, proving out the systems that are supposed to support later lunar landings and, eventually, a sustained human presence near the lunar south pole.