Asuka 881902 Meteorite Quick Facts
- Name: Asuka 881902
- Year Discovered: 1988
- Approximate Recovery Location: Antarctica
- Precise Recovery Location: (-72.0, 26.0)
- Mass: 907.87 grams
- Classification: Acapulcoite
- Discovery Type: Found
- Condition: Valid
More Details About the Asuka 881902 Meteorite
The Asuka 881902 meteorite was discovered in 1988. It was recovered in Antarctica (-72.0, 26.0). It has a mass of 907.87 grams.
Asuka 881902 is considered a “Valid” meteorite. “Valid” meteorites are typical meteorites with average weathering, while “relict” meteorites are those that have been extremely altered, either due to weathering over time or human intervention.
Asuka 881902’s official classification is Acapulcoite. The “Acapulcoite” classification refers to a meteorite that is part of the primitive achondrite group, indicating it has undergone heating and partial melting, maintaining a composition close to its original chondritic state. These meteorites, linked to the acapulcoite-lodranite family, are equigranular with fine grains, and sometimes include rare, original chondrules, displaying a unique mineral composition that is somewhat different from ordinary chondrites.
The Asuka 881902 meteorite is a “Found” meteorite. Meteorites are classified as “falls” if they were observed falling and recovered, while “finds” are those discovered later, often weathered by longer exposure to Earth’s environment and without a record of being seen as they fell.
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Last Updated: 1/10/24