Winter snowflakes are unique ice crystals that form in the atmosphere when water vapor freezes. Each snowflake begins as a tiny droplet of water that crystallizes around a dust particle. As it falls through the cold air, it collects more water vapor, which freezes and creates intricate patterns. No two snowflakes are exactly alike due to the varying conditions they encounter during their descent. The structure of a snowflake is influenced by temperature and humidity, leading to a wide variety of shapes, such as hexagons, needles, and plates. Snowflakes typically have six symmetrical arms, a result of the molecular structure of ice. These beautiful formations contribute to the winter landscape, creating a soft, white blanket that covers the ground.