1. FROM WIKIPEDIA drdivyaclinic@gmail.com
TRINITITE
FROM WIKIPEDIA

2. 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 (both microcline and smaller amount of plagioclase with small amount of calcite, hornblende and augite in a matrix of sandy clay)[2] that was melted by the atomic blast. It is usually a light green, although color can vary. It is mildly radioactive but safe to handle.[3][4

3. In 2005 it was theorized by Los Alamos National Laboratory scientist Robert Hermes and independent investigator William Strickfaden that much of the mineral was formed by sand which was drawn up inside the fireball itself and then rained down in a liquid form.[7]