Kidairat Meteorite Quick Facts
- Name: Kidairat
- Year Discovered: 1983
- Approximate Recovery Location: , En Nuhud, West Kurdufan State, Sudan
- Precise Recovery Location: (14.0, 28.0)
- Mass: 100000 grams
- Classification: H6
- Discovery Type: fall
- Condition: Valid
More Details About the Kidairat Meteorite
The Kidairat meteorite was discovered in 1983. It was recovered in , En Nuhud, West Kurdufan State, Sudan (14.0, 28.0). It has a mass of 100000 grams.
Kidairat 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.
Kidairat’s official classification is H6. The “H6” classification refers to a high-iron, ordinary chondrite meteorite with distinct features like smaller chondrules and specific oxygen isotope ratios close to those found on Earth. This type 6 meteorite has undergone extensive metamorphism, leading to uniform mineral composition, larger secondary mineral sizes, and the fading of many chondrule outlines, yet without any melting.
The Kidairat meteorite is a “fall” 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: 12/29/23