description Cranbourne Overview
Cranbourne is an IAB iron meteorite discovered near Cranbourne in Victoria, Australia, in the nineteenth century. Multiple masses have been recovered, collectively weighing several tonnes, and examples are held by major natural history collections. Its substantial recovered masses and association with the IAB iron group make it relevant to researchers studying differentiated and mixed meteorite parent bodies.
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Where was the Cranbourne meteorite discovered?
The Cranbourne meteorite was discovered near the town of Cranbourne in Victoria, Australia, during the nineteenth century. Multiple masses were recovered from this area, collectively weighing several tonnes. The largest specimens are held by major natural history collections, including the Melbourne Museum.
What type of meteorite is the Cranbourne meteorite?
Cranbourne is classified as an IAB iron meteorite. This means it is composed primarily of iron-nickel alloys and belongs to a group of meteorites that often contain silicate inclusions. Its substantial recovered mass makes it one of the largest iron meteorites found in Australia.
When exactly did the Cranbourne meteorite fall to Earth?
The exact date of the fall is unknown, but the meteorites were discovered in the 19th century. The two most famous masses, known as the Bruce and Abel meteorites, were found in 1854 and 1860 respectively. They were discovered by farmers and surveyors clearing land in the area.
Can you see the Cranbourne meteorite in a museum today?
Yes, significant portions of the Cranbourne meteorite are displayed in major museums. The Museum Victoria holds the largest pieces, including the massive Abel mass. Other smaller fragments are distributed among international meteorite collections.
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