04/11/2026
Two chondrites, two records of an impact.
Look closely at the material surrounding the larger fragments. That’s where the difference between these two meteorites becomes visible.
In the impact breccia on the left, finer fragments of rock and minerals form the matrix around the larger clasts. In the impact melt breccia on the right, some clasts survived the collision and became embedded in molten rock. As the melt cooled and solidified, it formed the matrix we see today.
A dark matrix can catch the eye, but colour alone is insufficient evidence of melting. The distinction lies in how the matrix formed.
Do you have a sample that might be a meteorite? At the Adara Institute Astromaterials Laboratory, we test suspected meteorites and provide laboratory characterisation and submission support for official meteorite classification.
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https://adarainstitute.com