Ice crystals are formed when water vapor in the air freezes directly into solid ice without passing through the liquid phase, a process known as deposition. The shape of ice crystals is influenced by various factors such as temperature, humidity, and air currents. Warmer temperatures typically lead to the formation of simpler, hexagonal ice crystals, while colder temperatures can result in more intricate and delicate crystal structures. Humidity levels can affect crystal size and shape, with higher humidity generally producing larger and more irregular crystals. Lastly, air currents play a role in shaping ice crystals by affecting their growth patterns as they fall through the atmosphere.