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The Origins of Meteorites 4

 


 

A few meteorites proved to be of a more prominent origin: the so-called planetary meteorites, genuine pieces of the Earth's own Moon, and the planet Mars. Massive chunks of matter have been blasted off of their respective parent body's surface by violent impacts, and catapulted into space. Some of these pieces finally went into a Earth-crossing orbit, and landed on Earth in form of meteorites. Planetary meteorites are ultra-rare, and just about one out of thousand meteorite finds or falls has its origin on the Moon, or on planet Mars.  

The Origins of Meteorites

> The Asteroid Belt Connection
> Asteroidal Meteorites Galore
> Dwarf Planet Vesta & the HEDs
> Genuine Mars & Moon Rocks

Genuine Mars & Moon Rocks: Planetary Meteorites

In the early 1980s, Japanese and American researchers discovered the first lunar meteorites in the ice fields of Antarctica - genuine pieces of the Earth's Moon! Subsequently, several other "lunars" have been recovered from the hot deserts of Australia, Africa, and Oman, bringing the total number of all known lunar meteorites to about 40, excluding all probable pairings. All of these meteorites were found to exhibit mineral compositions similar to the samples returned by the Apollo and Luna missions, proving their lunar origin beyond any doubt.

Lunar meteorites are of major scientific importance because most of them originate from areas of the Moon that were not sampled before. Most lunar meteorites in our collections have been blasted off of the lunar highlands that cover the far side of the Moon. Only a few lunars have their origin in the smooth lowlands, the lunar maria of the near side of the Moon which served as the preferred landing sites for the Apollo missions. Please visit the lunar section of this site for much more detailed information.

The meteorites of the SNC group, named for the 3 witnessed falls of Shergotty, Nakhla, and Chassigny, are even more fascinating since they represent genuine pieces of the planet Mars. With crystallization ages between 1.35 and 0.15 billion years, most SNC group members are exceptionally young compared to other achondrites. Obviously, they formed on a parent body that has retained its igneous activity until very recent times, suggesting that the source of these strange rocks is a planet.

In the 1980s, the discovery of trapped gas inclusions inside several SNC members provided a final answer. Based on the data obtained by the Viking probes, which landed on Mars in 1976, the composition of this trapped gas is more or less identical to the composition of the martian atmosphere, convincing most scientists that the SNC members are genuine samples of our red neighbor. The latest proof of martian origin for the SNC group has been delivered by the Mars Exploration Rover “Opportunity” in the year 2005: the rover studied a rock dubbed “Bounce” at Meridiani Planum with mineral compositions similar to EETA 79001, providing another strong link between Mars, and the meteorites of the SNC group. Consequently, the SNC members are also known as martian meteorites. Please visit our martian section to learn more about these unusual and enigmatic rocks from space.

   
The Moon, 3-Filter Color Image, Galileo Space Probe 1990

The Home of Lunar Meteorites

© NASA/JPL


Mars Near Opposition, Hubble Space Telescope 2001

The Home of Martian Meteorites

© NASA, ESA & HST (STScI)


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