Pierceville (iron) Meteorite Quick Facts
- Name: Pierceville (iron)
- Year Discovered: 1917
- Approximate Recovery Location: V88M+M8 Pierceville, KS, USA
- Precise Recovery Location: (37.86667, -100.66667)
- Mass: 100000 grams
- Classification: Iron, IIIAB
- Discovery Type: Found
- Condition: Valid
More Details About the Pierceville (iron) Meteorite
The Pierceville (iron) meteorite was discovered in 1917. It was recovered in V88M+M8 Pierceville, KS, USA (37.86667, -100.66667). It has a mass of 100000 grams.
Pierceville (iron) 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.
Pierceville (iron)’s official classification is Iron, IIIAB. The classification “Iron, IIIAB” refers to an iron meteorite that belongs to the chemical group IIIAB. These meteorites are primarily composed of iron and nickel and formed from a molten state.
The Pierceville (iron) 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: 1/15/24