Strange Glass in Australia Reveals a Massive Impact We Never Knew About

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Strange glassy blobs strewn crossed the Australian godforsaken are grounds of an past meteorite interaction that scientists hadn't noticed until now.

According to a caller investigation led by geoscientist Anna Musolino of Aix-Marseille University successful France, tiny spheres of solid recovered successful South Australia correspond an impact-melt creation not recovered anyplace other successful the world.

These recently named ananguites, the researchers say, formed successful a elephantine interaction that took spot immoderate 11 cardinal years ago.

The sting successful this peculiar process is that geologists person yet to find immoderate hint of a crater associated with this lawsuit – an lawsuit almighty capable to permission mineral traces that persist successful detectable quantities for millions of years.

Related: A Massive Geological Surprise Has Been Discovered Under Greenland's Ice Sheet

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"These glasses are unsocial to Australia and person recorded an past interaction lawsuit we did not adjacent cognize about," says geochronologist and geochemist Fred Jourdan of Curtin University successful Australia.

"They formed erstwhile an asteroid slammed into Earth, melting aboveground stone and scattering debris for thousands of kilometres. These tiny pieces of solid are similar small clip capsules from heavy successful our planet's history.

"What makes the find adjacent much intriguing is that, though the interaction indispensable person been immense, scientists are yet to find the crater."

The godforsaken crossed confederate Australia is positively strewn with tiny beads of interaction solid called tektites. It's portion of a portion known arsenic the Australasian strewnfield, the fallout created by a elephantine meteorite interaction thought to person deed determination successful Southeast Asia astir 788,000 years ago.

The tektites from this fallout recovered successful Australia are known arsenic australites, and they're peculiarly abundant partially due to the fact that the suspected interaction took spot a comparatively abbreviated clip ago.

Way backmost successful 1969, scientists Dean Chapman and Leroy Scheiber of NASA made a chemic investigation of 530 australites. Among that number, they recovered eight with a mineral creation that did not lucifer the remainder of the sample.

They noted the strangeness of this, suggesting the 8 beads whitethorn person formed successful a abstracted impact, but nary 1 ever truly followed up.

Win a $10,000 Space Coast Adventure HolidayMusolino and her colleagues decided to dive backmost into the oddballs to fig retired what their woody is. The archetypal 8 samples were unavailable for re-analysis, but luckily Chapman and Scheiber had provided a elaborate chemic statement of the oddballs.

The differences of peculiar enactment see little silicon dioxide content, but higher levels of the oxides of iron, magnesium, and calcium. They're besides denser, with higher magnetic susceptibility, antithetic bubble patterns, and antithetic ratios of hint elements.

The six recently discovered ananguites. (Musolino et al., Earth Planet. Sci. Lett., 2025)

With this illustration successful hand, the researchers scoured the australite postulation astatine the South Australian Museum, screening it for outliers accordant with the oddballs identified by Chapman and Scheiber. They recovered six caller tektites successful the postulation that matched the mineral fingerprint of the earlier anomalies.

The creation of these ananguites powerfully indicates that they formed successful an interaction that occurred connected a antithetic portion of the crust from the Australasian strewnfield impact.

To confirm, Musolino and her colleagues performed argon dating connected 2 of the six samples; Jourdan and different researchers had utilized the aforesaid method successful 2019 to day tektites scattered astir Southeast Asia and Australia to 788,000 years old.

The squad deduced that the recently identified ananguites are 11 cardinal years aged – importantly older than the tektites. This property clinches it; this fistful of tiny solid blobs formed successful a different, earlier impact.

Where that interaction took place, however, is inactive a large mystery. That's not astonishing fixed the root crater of the Australasian strewnfield tektites is inactive unknown, considered thing of a "holy grail" for interaction cratering science.

There are besides a fewer reasons wherefore the ananguite root crater mightiness person vanished, including aggravated weathering and the aridification of cardinal Australia that started around 33 cardinal years ago. It whitethorn besides person been mistaken for a volcanic diagnostic successful regions specified arsenic Papua New Guinea.

"Geochemical and petrographic systematic differences betwixt occidental and eastbound ananguites, which inactive request to beryllium confirmed with further samples, whitethorn assistance constrain the determination of the impact," the researchers constitute successful their paper.

"However, it is besides imaginable that the crater has been buried during the past 11 cardinal years."

The findings person been published successful Earth & Planetary Science Letters.

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