Hail is formed in thunder clouds when ice pellets formed near the freezing level in the atmosphere are caught in air currents. They are tossed up and down by air currents within the thundercloud where these pellets collide and fuse with one another. Further deposition of water or ice, causes them to grow into hailstones. Certain conditions such as vertical upward air currents help prevent hail falling too quickly and results in the increase in the size of hailstones.