Ice melts at a temperature of 0 degrees Celsius, which is equivalent to 32 degrees Fahrenheit. At this point, the solid structure of ice transitions into liquid water.
The melting process occurs because the molecular structure of ice (which is made up of water molecules) has a specific arrangement that holds the molecules in a solid state. When heat is applied, the energy causes the molecules to vibrate more vigorously, breaking the bonds that hold them in place, leading to a change from solid to liquid.
It’s important to note that while 0°C is the standard melting point for pure ice at sea level, factors like pressure can influence this temperature. In other conditions, such as at higher altitudes or under varying atmospheric pressure, the melting point may shift slightly.