Categories: Science

A Giant Asteroid Struck Australia 11 Million Years Ago. So Where Is the Crater?

A Giant Asteroid Struck Australia 11 Million Years Ago. So Where Is the Crater?

Uncovering a Hidden Impact: Tektites as Time Capsules

A recent study reveals that Australia holds a dramatic record of an ancient asteroid strike, not as a crater, but as tiny pieces of natural glass called tektites scattered across South Australia. The glass fragments are remnants of an event believed to have melted surface rocks and blasted debris across thousands of kilometers when a colossal asteroid collided with Earth about 11 million years ago. This discovery, led by scientists from Curtin University and Aix-Marseille University, marks the identification of a new tektite field, offering a fresh window into Earth’s dynamic impact history.

Co-author Professor Fred Jourdan of Curtin’s School of Earth and Planetary Sciences describes tektites as time capsules that preserve a snapshot of a moment when a planetary-scale event reshaped a region. “These glasses are unique to Australia and have recorded an ancient impact event we did not even know about,” Jourdan notes. In essence, the tektites capture the mess of molten rock and mineral debris hurled into the atmosphere and then dispersed across the landscape, providing crucial clues about the scale and mechanics of the impact.

What Makes These Tektites Special?

The study identifies a previously unrecognized tektite variety with chemistry and an age that sets it apart from the better-known Australasian tektite field, which formed around 780,000 years ago. Lead author Anna Musolino, a PhD student at Aix-Marseille University, explains that these tektites log a distinct chemical signature and a much older age, pointing to a separate giant impact event. “These tektites are unique because of their unusual chemistry and their age, which is about 11 million years,” she says. The discovery thus expands our understanding of how frequently Earth experiences massive asteroid impacts and how such events leave behind evidence even when craters are absent or obscured today.

Dating, Chemistry, and the Implications

The researchers used a combination of geochemical analyses and stratigraphic context to date the tektites and characterize their composition. The results indicate a tektite field that formed from material ejected by a volcanic arc impact crater, a scenario supported by the team’s co-authored work, published in Earth and Planetary Science Letters. The collaboration includes Emeritus Professor Pierre Rochette from Aix-Marseille University, with additional contributions from other experts. The paper’s findings suggest that older, larger impacts may be more common in Earth’s history than previously recognized, but their fingerprints can be surprisingly elusive if the resulting crater has been eroded, buried, or destroyed by geological processes over millions of years.

Where Is the Crater? A Challenge for Planetary Scientists

One of the most intriguing aspects of the discovery is that scientists have yet to locate the crater associated with this 11-million-year event. The authors propose that the crater could lie beneath younger sediments, be buried by volcanic or tectonic activity, or be located in a region where geological processes have erased obvious crater features. The concept of a crater being hidden or obliterated underscores why tektites are such powerful proxies for studying ancient impacts. They serve as durable, observable remnants when the crater itself has vanished from the landscape.

Why This Matters: Planetary Defense and Earth’s History

Beyond satisfying scientific curiosity, identifying a new tektite field has practical implications for planetary defense. By documenting a major impact event in Earth’s recent deep past, researchers gain insights into the frequency, scale, and consequences of asteroid impacts. Understanding the distribution and chemistry of tektites helps refine models of impact events and improves our ability to recognize similar signatures in other regions or times. The work not only highlights Australia’s role in global geology but also reinforces the importance of international collaboration in unraveling planetary history.

Reference: Musolino, Rochette, Barrat, Jourdan, Reynard, Devouard, Andrieu, Gattacceca, and Vidal, “A new tektite strewn field in Australia ejected from a volcanic arc impact crater 11 Myr ago,” Earth and Planetary Science Letters, 2025. DOI: 10.1016/j.epsl.2025.119600.