Snow is a solid state of matter. It forms when water vapor in the atmosphere condenses and freezes, creating ice crystals. These crystals clump together to form snowflakes, which eventually fall to the ground.
In its solid form, snow has a unique structure that makes it different from other solids. When snow accumulates, it can trap air and create an insulating layer, which is why it feels soft and fluffy. This structure is also why snow can vary in density and texture, depending on factors such as temperature and humidity.
So, while we often think of water as a liquid, in the case of snow, it has transitioned into a solid form through a natural process of freezing. Thus, we classify snow as a solid state of matter.