Ice is lighter than water because of a unique property of water known as density. Density is the measure of mass per unit volume of a substance. When water freezes and turns into ice, the water molecules rearrange themselves into a crystal lattice structure, forming a regular pattern. This structure creates empty spaces or gaps between the molecules, which increases the overall volume of the ice compared to the same amount of water.
Although the mass of the water molecules remains the same, the increased volume means that the density of ice is lower than that of water. In other words, a given volume of ice contains fewer water molecules compared to the same volume of liquid water.
This difference in density is responsible for the buoyancy of ice in water. Because ice is less dense than water, it floats on the surface. If ice were denser than water, it would sink instead. This unique property is crucial for aquatic ecosystems, as it allows bodies of water to freeze from the top down, providing insulation for the underlying water and enabling the survival of many organisms during cold winters.
It's worth noting that the anomaly of water's density is not commonly observed in other substances. Most substances tend to become denser and sink when they solidify.