Why Ice Floats
If you drop an ice cube into a glass of water, it bobs to the top and floats. That may seem ordinary, but it is actually unusual. For almost every other substance, the solid form is heavier than the liquid form and sinks in it. Water is one of the few exceptions.
The reason lies in how water freezes. As water cools, its tiny particles, called molecules, slow down and move closer together. Near the freezing point, however, they begin to lock into a rigid pattern with open spaces between them. The pattern holds the molecules slightly farther apart than they were as a liquid, so frozen water takes up about nine percent more space. The same amount of matter spread over more space is less dense, and less dense things float.
This odd behavior matters for life on Earth. When winter arrives, a pond cools from the top, and ice forms at the surface instead of sinking. The floating layer works like a blanket, slowing the loss of heat from the water below. Fish and other pond animals can survive in the liquid underneath all winter long.
Icebergs float for the same reason. Because ice is only a little lighter than liquid water, about nine tenths of an iceberg stays hidden below the surface.