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In page Hail:

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Unlike ice pellets, hailstones are layered and can be irregular and clumped together.[citation needed] Hail is composed of transparent ice or alternating layers of transparent and translucent ice at least 1 mm (0.039 in) thick, which are deposited upon the hailstone as it travels through the cloud, suspended aloft by air with strong upward motion until its weight overcomes the updraft and falls to the ground. Although the diameter of hail is varied, in the United States, the average observation of damaging hail is between 2.5 cm (0.98 in) and golf-ball-sized 4.4 cm (1.75 in).[4]