Trinitite
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Trinitite, also known as Atomsite or Alamogordo Glass, is the name given to 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 (both microcline and smaller amount of plagioclase with small amount of calcite, hornblende and augite in a matrix of sandy clay) that was melted by the atomic blast. It is usually a light green, although color can vary. It is mildly radioactive, but is safe to handle.
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Trinitite info and photos Trinitite info and photos www.orau.org/ptp/collection/hiroshimatrinity/trinitite.htm - Web |
Radiographic spectrum of Trinitite Radiographic spectrum of Trinitite www.randomuseless.info/spectra/results/trinitite/index.html - Web |
Ralph Pray's account of removing Trinitite from th... Ralph Pray's account of removing Trinitite from the site www.mine-engineer.com/mining/trinity.htm - Web |
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Another version of Ralph Pray's account Another version of Ralph Pray's account libertyunbound.com/archive/2003_07/pray-groundzero.html - Web |
Trinitite in The Corning Museum of Glass collectio... Trinitite in The Corning Museum of Glass collection www.cmog.org/article/glass-nature - Web |