Midnight Meteorites
This 15.44 gram meteorite (chondrite) was discovered near Mills, New Mexico in 1970. It is classified as a chondrite, specifically H6. “H” stands for high iron (around 25–30 wt% metal and iron-rich silicates) and "6” refers to its petrologic type, meaning it has been strongly thermally metamorphosed on its parent asteroid, so most original chondrules are subtle or diffuse compared to lower types.
This individual stone has a window cut into the side, which has been polished to reveal the stark contrast between the meteorite's interior and exterior.
This meteorite is from an older collection and maintains its original label. The label is consistent with Glenn Huss / American Meteorite Laboratory (AML) provenance.
This meteorite is not just a collectible; it’s an educational tool and conversation starter that brings the mystery and science of space directly into your hands.
The blue scale cube displayed in some of the photos is 1 cm x 1 cm x 1 cm and is used only to represent scale. It is not included in your purchase.
Your purchase includes the exact stone pictured, a Certificate of Authenticity, a custom 3D printed display stand, and a lunar surprise 🌙
--Ordinary Chondrite--
Ordinary chondrites make up about 85% of all known falls. They are stony meteorites composed primarily of silicate minerals like olivine and pyroxene, with small amounts of nickel-iron metal and chondrules—tiny, spherical grains that formed in the early solar system. Their composition provides valuable insights into the building blocks of planets and the history of our solar system.
--Chondrules--
Small, spherical particles found in some meteorites, particularly in chondrites. These are believed to be some of the oldest solid materials in our solar system.
Mills, New Mexico Windowed Chondrite with Huss AML Provenance - 15.44 grams
CSM-169
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