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Trinitite

Trinitite, also known as atomsite or Alamogordo glass, is the glassy residue left on the desert floor after the plutonium-based Trinity nuclear bomb test on July 16, 1945, near Alamogordo, New Mexico. The glass is primarily composed of arkosic sand composed of quartz grains and feldspar that was melted by the atomic blast. Trinitite is mildly radioactive but is safe to handle for short periods of time.

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trinitite-frst-atomicbomb_0140.jpg
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Ted Kinsman / Science Source Inc.
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5760x3840 / 10.7MB
Trinitite atomsite Alamogordo glass glassy plutonium atomic atomic bomb bomb first bomb Trinity nuclear bomb New Mexico. Glass arkosic sand atomic blast blast radioactive nuclear green artifact
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Trinitite, also known as atomsite or Alamogordo glass, is the glassy residue left on the desert floor after the plutonium-based Trinity nuclear bomb test on July 16, 1945, near Alamogordo, New Mexico. The glass is primarily composed of arkosic sand composed of quartz grains and feldspar that was melted by the atomic blast. Trinitite is mildly radioactive but is safe to handle for short periods of time.
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