description Axtell Overview
Axtell is a CV3 carbonaceous chondrite meteorite found near Axtell, Texas, in 1943. Like other CV chondrites, it contains conspicuous chondrules and calcium-aluminum-rich inclusions, among the earliest solids formed in the Solar System. Its petrologic type 3 designation indicates that its original mineral textures and chemical variations experienced relatively little alteration on its parent body.
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What kind of meteorite is the Axtell meteorite?
The Axtell meteorite is a CV3 carbonaceous chondrite. This classification means it contains abundant calcium-aluminum-rich inclusions (CAIs) and conspicuous chondrules. It was found near Axtell, Texas, in 1943.
Why is the Axtell meteorite scientifically important?
Like other CV chondrites, Axtell contains calcium-aluminum-rich inclusions, which are among the earliest solids formed in the Solar System. Its petrologic type 3 designation indicates that it is relatively unequilibrated. This preserves early solar system textures that offer insights into planetary formation.
Where was the Axtell meteorite found?
The meteorite was found near the town of Axtell in McLennan County, Texas. The discovery was made in 1943 by a farmer plowing a field. It was initially mistaken for a piece of iron ore due to its heavy mass.
Where are the specimens of the Axtell meteorite kept today?
The main mass of the Axtell meteorite is held by the Center for Meteorite Studies at Arizona State University. Other pieces are distributed among various scientific collections worldwide. Researchers have access to these specimens to study their carbonaceous composition.
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