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Trinitite, also known as atomsite or Alamogordo glass, [1] [2] 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 desert sand, largely made of silica, melted and became a mildly radioactive light green glass, which was named trinitite. [106] The explosion created a crater approximately 4.7 feet (1.4 m) deep and 88 yards (80 m) wide. The radius of the trinitite layer was approximately 330 yards (300 m). [107] The 100-foot shot tower was completely ...
Sand will fuse into glass if it is close enough to the nuclear fireball to be drawn into it, and is thus heated to the necessary temperatures to do so; this is known as trinitite. [39] At the explosion of nuclear bombs lightning discharges sometimes occur. [40] Smoke trails are often seen in photographs of nuclear explosions.
Tell el-Hammam (also Tall al-Hammam) is an archaeological site in the Amman Governorate of Jordan, in the eastern part of the lower Jordan Valley 11.7 kilometers east of the Jordan River and not far from its mouth.
The trinitite was formed from feldspar and quartz which were melted by the heat. Two samples of trinitite were used, the first (left-hand-side bars in the graph) was taken from between 40 and 65 meters of ground zero while the other sample was taken from further away from the ground zero point.
Trinitite is part of WikiProject Central Asia, a project to improve all Central Asia-related articles. This includes but is not limited to Afghanistan , Kazakhstan , Kyrgyzstan , Mongolia , Tajikistan , Tibet , Turkmenistan , Uzbekistan , Xinjiang and Central Asian portions of Iran , Pakistan and Russia , region-specific topics, and anything ...
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