Hail, in and of itself, is not an unusual weather phenomenon. The frozen precipitation occurs inside storm clouds when water droplets are cooled below freezing, yet remain in a liquid state. When the supercooled water encounters something solid, such as a speck of dust or an ice crystal, it sticks to the particle and freezes. Updrafts in the storm keep the hailstone aloft as it aggregates ice, growing until its weight is too heavy for the updraft, at which time it plunges to the Earth.
Some scientists believe that there is a larger, more sinister type of ice-chunk precipitation which can form outside of storms, making even the largest hailstones look puny in comparison. There is a great deal of disagreement in the scientific community regarding the origin of these falling slabs of ice, but it is certain that something is causing massive frozen chunks to occasionally drop from seemingly empty skies. The objects are called megacryometeors
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