The oldest known impact crater at 2.2 billion years. It may have ended the Snowball Earth period by vaporizing enough ice to warm the planet.
Timmons M. Erickson, Christopher L. Kirkland, Nicholas E. Timms, Aaron J. Cavosie & Thomas M. Davison, CC BY 4.0, via Wikimedia Commons
A scar half the age of the Earth
In the remote outback of Western Australia, there is no obvious sign of a 70-kilometer-wide crater. Two billion years of erosion have worn away its rim and bowl, leaving only subtle outcrops and magnetic anomalies beneath the red soil. This is the Yarrabubba impact structure, and it is the oldest confirmed impact crater on Earth. First identified as a potential impact site in 2003, its true significance was not understood for years. The crater sits on the Yilgarn Craton, one of the most ancient and stable sections of the Earth's crust, which is why any trace of this event survived at all.
Scientists determined its staggering age by analyzing microscopic crystals of zircon and monazite recovered from the site. An asteroid strike of this magnitude generates incredible heat and pressure, melting rock and resetting the "isotopic clocks" within these minerals. By measuring the ratio of uranium to lead, researchers pinned the impact to a precise moment: 2.229 billion years ago, give or take 5 million years. This date makes Yarrabubba approximately 200 million years older than the next-oldest known crater, the Vredefort Dome in South Africa.
The snowball melts
The timing of the Yarrabubba impact is is why it is a subject of scientific study. The event occurred at the very end of a period known as the Huronian glaciation, a time when Earth was likely locked in a global ice age often called "Snowball Earth". For hundreds of millions of years, ice sheets possibly several kilometers thick covered much of the planet. Geological records show that soon after the 2.229-billion-year mark, these widespread glacial deposits vanish for the next 400 million years.
Computer modeling suggests the connection is not a coincidence. Researchers simulated a 7-kilometer-wide asteroid striking a continental ice sheet between two and five kilometers thick. The models show the impact would have instantly vaporized a colossal amount of ice, blasting hundreds of billions of tons of water vapor into the atmosphere. Water vapor is a potent greenhouse gas. Injecting such a massive quantity into the stratosphere could have been enough to warm the planet, trigger a global thaw, and bring the "Snowball Earth" period to an abrupt end. While this hypothesis is still being studied, the Yarrabubba crater links extraterrestrial impacts and deep shifts in Earth's climate history.
💡Fun Facts
The age was determined using uranium-lead dating on shock-recrystallized zircon and monazite minerals just a few hairs' widths across.
The impact released an estimated 200 to 400 trillion pounds of water vapor into the atmosphere.
Today, the crater is so eroded that it has no visible surface expression and is primarily identified through aeromagnetic imaging and shocked minerals on the ground.
After the impact, glacial deposits disappear from the global rock record for about 400 million years.
The site is on Yarrabubba Station, a private pastoral lease, and is not a formal tourist destination. Access is not generally possible without permission or being part of a sanctioned geological tour.
Admission
Not applicable. Organized tours, when available, have their own costs. For example, a 2025 geological field trip had associated registration fees.
Accessibility
The terrain is remote, semi-arid outback with low-relief, rocky ground. It is located about 70 kilometers south of the town of Meekatharra. A 4WD vehicle is necessary, and any visit would require significant preparation for remote travel.
