Allende meteorite

The Allende meteorite is the largest carbonaceous chondrite ever found on Earth. The fireball was witnessed at 01:05 on February 8, 1969, falling over the Mexican state of Chihuahua. After it broke up in the atmosphere, an extensive search for pieces was conducted and over 2 tonnes (2.2 tons) were recovered. The availability of large quantities of samples of the scientifically important chondrite class has enabled numerous investigations by many scientists; it is often described as "the best-studied meteorite in history." The Allende meteorite has abundant, large calcium–aluminum-rich inclusions (CAI), which are among the oldest objects formed in the Solar System.

Allende
Allende fragment
TypeChondrite
ClassCarbonaceous chondrite
GroupCV3
Composition23.85% total iron
Shock stageS1
CountryMexico
RegionPueblito de Allende, Allende, Chihuahua
Coordinates26°58′N 105°19′W
Observed fallYes
Fall date01:05 local time (07:05 GMT) on 1969 February 8
TKW2 tonnes
Strewn fieldYes
Chondrules of Allende
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Carbonaceous chondrites compose about 4 percent of all meteorites observed to fall from space. Prior to 1969, the carbonaceous chondrite class was known from a small number of uncommon meteorites such as Orgueil, which fell in France in 1864. Meteorites similar to Allende were known, but many were small and poorly studied.

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