100°C is the boiling point of water
The boiling point of water is the temperature at which water changes completely from the liquid state to the gaseous state. Under normal atmospheric pressure at sea level, pure water boils at 100°C. This value is considered the standard boiling point and is commonly used in schools, laboratories, and scientific measurements.
When water reaches this temperature, it forms bubbles throughout the liquid. These bubbles rise to the surface and release steam, showing that the water is turning into vapor.
This is why boiling is faster and more active than simple evaporation.
At high altitudes or hill stations, air pressure is lower. Because of this, water boils at a lower temperature (around 90–95°C). This is why cooking takes longer in mountainous regions.
In a pressure cooker, pressure increases as steam gets trapped. The boiling point rises above 100°C, making food cook faster. This is a common example of how pressure affects boiling.
When substances like salt, sugar, or minerals dissolve in water, the boiling point increases slightly. This effect is called boiling point elevation. For example, salty water takes longer to boil than pure water.