Freezing temperature is the point at which a liquid turns into a solid. For water, this occurs at 32°F (0°C) under standard atmospheric pressure. This temperature is commonly referred to as “freezing point.”
Freezing is measured using thermometers calibrated in either Fahrenheit or Celsius, depending on the region. In science and precise applications, freezing is defined as the temperature where the molecules in a liquid slow down enough to form a structured, solid state.
While 32°F/0°C is standard for water, the freezing point of other substances may vary based on their chemical composition. Factors like impurities or pressure changes can also alter the freezing temperature, making it a fascinating process in both everyday life and scientific study.