What Ice crystals too large to be suspended in the cloud?

Ice crystals that are too large to be suspended in a cloud are typically referred to as snowflakes. These crystals form when water vapor freezes directly into ice in the upper atmosphere and can grow larger as they collide with other ice particles. Once they reach a sufficient size and weight, they fall to the ground as precipitation, contributing to snowfall. Their size and structure can vary significantly depending on temperature and humidity conditions during their formation.