Description
Trinitite is a naturally occurring glass formed on July 16, 1945, when the first atomic bomb test — codenamed Trinity — was detonated in the New Mexico desert.
The explosion’s extreme heat fused the surrounding desert sand, quartz, and feldspar into a thin layer of greenish glass.
This 3.20 gram piece is a preserved fragment of that event, collected from the Trinity test site region. Each specimen displays a unique mix of green hues, air bubbles, and subtle textures — a geological artifact shaped by human history and atomic energy.
Scientific Classification
| Property | Value |
|---|---|
| Material Type | Natural Fulgurite-like Glass (Impact Glass) |
| Composition | Silica (SiO₂) with Feldspar, Quartz, and Trace Iron |
| Formation Process | Surface fusion by nuclear detonation (approx. 1,500–2,000°C) |
| Color | Olive to pale green, sometimes grayish or bubbly |
| Locality | Trinity Site, White Sands Missile Range, New Mexico, USA |
Collector and Educational Notes
Trinitite is no longer legally collectible from the original site, making all legitimate specimens historical relics sourced before restrictions.
Each piece tells the story of the dawn of the atomic age — valuable for collectors, educators, and those interested in the scientific and ethical legacy of nuclear research.
This specimen’s texture and color clearly reveal rapid melting and cooling processes, often showing trapped quartz grains or vesicles where vapor escaped.
Uses and Handling
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Suitable for scientific display, historical collections, and educational exhibits.
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Can be housed in a small specimen box or acrylic case for preservation.
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Not for metaphysical or energetic use due to its synthetic and historical origin.
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Handle gently; glass surface is brittle and may chip.
Care and Preservation
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Store in a dry, stable environment.
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Avoid moisture and high heat.
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Clean gently with a soft, dry brush — do not use water or chemicals.










