Mundrabilla

Mundrabilla is an iron meteorite in the Nullarbor Plain consisting of two main fragments separated by about 180 meters and embedded in clayey soil. The larger pieces weigh 12.4 and 5.44 tonnes and contain a mixture of iron-nickel, troilite, graphite, and various other minerals.

Initial fragments were discovered in 1911 by Harry Kent during a geological survey, while larger accumulations were found by geologists in 1966. This later discovery helped scientists better understand and study the meteorite material.

The Western Australian Museum maintains the largest fragment, making it accessible for scientific research and public education.

The terrain in this flat region can be challenging to access, especially after rainfall when paths should be dry. Visitors should prepare for remote conditions and bring proper equipment for exploring this isolated area.

Researchers detected traces of superconductivity in the main mass, suggesting that naturally occurring superconductors might exist. This unexpected property makes the material interesting for material science and potential technical applications.

Location: Western Australia

GPS coordinates: -30.78333,127.55000

Latest update: December 10, 2025 20:10