Overview
- Shatter cones discovered in the rust-coloured basalts at North Pole Dome verified that the Miralga site was formed by a meteorite impact.
- Orientation mapping of hundreds of shatter cones recalibrated the crater’s diameter to about 16 km, down from earlier estimates of over 100 km.
- Field observations found shatter cones only in rocks dating to 3.47 Ga and 2.77 Ga, constraining the impact to between 2.7 billion and 400 million years ago.
- Researchers are pursuing isotopic analyses to pinpoint the crater’s precise age within the broad stratigraphic window.
- Designated the Miralga impact structure to honor the Nyamal people, the site offers a rare example of a basalt-hosted crater relevant to Earth and Mars studies.