![]() |
| Professor Chris Kirkland studying tiny zircon crystals in the lab. Photo Credit: Courtesy of Curtin University |
Scientific Frontline: Extended "At a Glance" Summary: North Pole Dome Asteroid Impact
The Core Concept: Researchers have successfully established the precise age of the oldest known asteroid impact crater on Earth, dating the event at the North Pole Dome in Western Australia to approximately 3 billion years ago.
Key Distinction/Mechanism: To bypass billions of years of geological alteration, geochronologists utilized a dual-mineral dating method. They analyzed resilient zircon crystals—specifically looking for impact-modified branching and skeletal shapes caused by intense heating and partial recrystallization—and corroborated the timeline using apatite formed by post-impact hydrothermal fluids.
Origin/History: The North Pole Dome, located in the Pilbara region of Western Australia, has long been debated as an ancient impact structure. A study conducted by Curtin University and the Geological Survey of Western Australia (GSWA) finally confirmed its 3-billion-year age, placing it in the Archean eon.
Major Frameworks/Components:
- Mineral Clocks: The utilization of highly resilient minerals that act as geological timekeepers by recording moments of extreme thermal and physical disruption.
- Zircon Recrystallization: The identification of unusual, skeletal zircon formations that indicate the mineral was disrupted and regrown during an impact event.
- Hydrothermal Apatite Formation: The independent dating of a secondary mineral, formed as hot fluids moved through shock-damaged rock, to verify the primary zircon data.














