The freezing point of a substance is the temperature at which it changes from a liquid to a solid state. For water, the freezing point is 0 degrees Celsius (0 °C) or 32 degrees Fahrenheit (32 °F) at standard atmospheric pressure.
It's important to note that the presence of impurities, such as salt, can lower the freezing point of water, a phenomenon known as freezing%20point%20depression. This is why salt is used on roads in winter to prevent ice formation. The phase%20transition from liquid to solid involves the molecules of the liquid slowing down and forming a more ordered structure, characteristic of the solid state. The freezing point depends on atmospheric%20pressure, but the values are generally given at standard conditions.
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