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Hail is possible within most thunderstorms as it is produced by cumulonimbi, and within 2 nautical miles (3.7 km) of the parent storm. Hail formation requires environments of strong, upward motion of air with the parent thunderstorm (similar to tornadoes) and lowered heights of the freezing level.ny thunderstorm which produces hail that reaches the ground is known as a hailstorm. Hail has a diameter of 5 millimetres (0.20 in) or more. Hailstones can grow to 15 centimetres (6 in) and weigh more than 0.5 kilograms (1.1 lb). Unlike ice pellets, hailstones are layered and can be irregular and clumped together.
The layer of air replaced at the surface causes the air above it to be lifted and cooled. If there is enough moisture in the air, the cooling will cause it to condense and form clouds. If further condensation occurs then orographic precipitation can be produced. Mount Shasta is known for its beautiful clouds. The lenticular clouds, often called flying saucers, are probably the most well-known type of cloud in the region. However, there are many types of clouds that can be seen around Mount Shasta.